**Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces**

Seth I. Manuwa

[40] Weerts, A. H.; Kandhai, D.; Bouten, W. and Sloot, P. M. A. (2001): Tortuousity of an unsaturated sandy soil estimated using gas diffusion and bulk soil electrical conduc‐ tivity: comparing analogy-based models and Lattice-Boltzmann simulations. Soil Sci‐

[41] White, E.M. and F.E.A. Wilson (2006): Responses of grain yield, biomass and harvest index and their rates of genetic progresses to nitrogen availability in ten winter

[42] Wösten, J.H.M.; Pacheps, Ya.A.and Rawls, W.J. (2001): Pedotransfer functions: bridg‐ ing the gap between available basic soil data and missing soil hydraulic characteris‐

[43] WCCS/World Climate Classification System (2009): http://www.physicalgeogra‐

[44] Zdruli, Pandi; Robert J.A. Jones and Luca Montanarella (2004): Organic Matter in Soils of Southern Europe. European Soil Bureau Research Report No. 15, Office for Official Publications of the European Communities. Luxembourg. EUR 21083 EN, 16

ence Society of America Journal. 65: 1577-1584.

wheat varieties. Iris Jo. Agric. Food Res. 45: 8-101.

tics. Journal of Hydrology 251 (2001): 123-150.

phy.net/fundamentals/7v.html

pp.

150 Advances in Agrophysical Research

Additional information is available at the end of the chapter

http://dx.doi.org/10.5772/52774

## **1. Introduction**

Soil strength has been regarded as important characteristics that affect many aspects of agricultural soils, such as the performance of cultivation implements, root growth, leastlimiting water range and trafficabilty [1]. They further reported that characterization of soil strength is usually made by measuring the response of a soil to a range of applied forces.

Soil compaction may be defined as the densification of unsaturated soil due to reduction in air volume without change in mass wetness [2].Soil compaction occurs in unsaturated soils when subjected to mechanical forces [3]. While soil compaction is essential in many engineering works (especially civil engineering) it is undesirable in agricultural production to a large extent. Compaction reduces the soil permeability to water, so that run off and erosion may occur and adequate recharge of ground water is prevented. Compaction reduces regeneration of the soil, so that metabolic activities of roots are impaired. Compaction increases the mechanical strength of the soil, so root growth is impeded. It is known that in agricultural system, the risk of soil compaction increases with the growth of farm size, increased mecha‐ nization and equipment weight, and the drive for greater productivity. Soil compaction also has negative effects on the environment by increasing runoff and erosion thereby accelerating potential pollution of surface water by organic wastes and applied agrochemicals [4]. All of these effects may reduce the quality and quantity of food and fibre grown on the soil. Therefore, the knowledge of soil compaction is increasingly important and desirable within agriculture and environmental protection.

The state of soil compactness is expressed in several ways: bulk density (expressed on a wet or dry basis), porosity and apparent specific gravity [5]. Accurate compaction behaviour equations will provide a means to predict compaction. The ability to predict compaction is the first requirement for attaining control of compaction. Considerable research has been per‐

© 2013 Manuwa; licensee InTech. This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. © 2013 Manuwa; licensee InTech. This is a paper distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

formed in attempts to develop soil compaction behaviour equations [6, 7, 8, 9, 10, 11, and 12]. Others have also reported on effects of organic matter and tractor passes on compaction and yield of crops [13, 14].

**3. Materials and method**

compression tests.

25 to 280

dept of 40 cm.

**ii.** Unconfined Compression Test

also determined using standard methods.

textural and soil analysis.

**3.2. Analytical methods**

**i.** Confined compression test: soil samples were taken from three sites for the confined

three horizons from top to bottom was 8, 15 and 15 cm, respectively.

**b.** Igbokoda loamy sand soil: the soil used in this study was the major soil pre‐ dominant in Igbokoda (headquarters of Ilaje Local Government area), Ondo State, South Western Nigeria. The soils were collected from the main agricultural production areas. This region is predominantly rainforest zone. Rainfall is in the order of 150 cm to 300 cm per annum, and mean annual temperature ranges from

**c.** Ilorin silt loam soil: the soil sample was taken from the arable soils of National Centre for Agricultural Mechanization (NCAM) Ilorin, Kwara State, Nigeria (8.30 N 4.32 E). The soil was Regosols (FAO). The soil samples were collected from the first 35 cm of soil profile; each sample was dug to a radius of 15 cm and then mixed thoroughly to get a homogeneous mixture, and then taken to the

The study was carried out in August 2010 in an experimental plot located at The Federal University of Technology, Akure (FUTA) Step-B (Science and Technology Education Post –

is a two-hectare arable land and was manually cleared to avoid compaction due to machinery impacts on the land. The experimental plot of length and width 48.00 m by 12.00 m, respec‐ tively, was divided into three transects each of 16 m by 4 m. There was also a control plot of the same dimensions as transect. Soil samples were carefully collected from the test plots for

Particle size analyses of all the experimental soils for both confined and unconfined samples were performed using hydrometer method [16]. Organic matter content of the soils was determined using the [16] method. Other physical and chemical properties of the soils were

laboratory for further processing and analysis.

Basic) project site Akure, with geographical coordinate of 7o

C. Soil samples were taken from freshly cut faces in open shallow pit to

10 North and 5o

05 East. The site

**a.** Akure sandy clay loam soil: the site was a portion of agricultural land under fallow at the Federal University of Technology, Akure, Nigeria (70 151

and elevation 210 m. The soil is Oxic paleustalf (Alfisol) or ferric Luvisol (FAO). A mini soil pit was dug to expose the profile. The site was designated Experi‐ mental Bin Soil (EBS). Three horizons EBS1, EBS2, and EBS3, from top to bottom respectively, were identified and samples taken from each. The thickness of the

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

N, 50 151

http://dx.doi.org/10.5772/52774

E),

153

**3.1. Sites of samples**

The aim of this chapter therefore was to observe the behaviour of textured soils under uniaxial compression in confined spaces and also in unconfined spaces under the influence of agricultural machines as it is affected by applied pressure and water content and also to model the behaviour using regression analysis for the purpose of prediction.

## **2. Soil under pressure**

When forces are applied to soil it changes its stateof compactness to have greater density. The pressure can be applied pressure or natural forces. Applies pressure can be due to animals like horses and cattle (160 kPa), man (95 kPa), sheep (60 kPa). The pneumatic wheels of vehicles can be inflated to 100 kPa for tractors and 200 kPa for for trailers and may produce local stresses twice these values [3]. The problem therefore is that over the years arable soils have suffered degradation as a result of excessive compaction of surface and sub surface soil horizon through overuse of agricultural machinery. This trend has global phenomenon as man labours to meet the ever increasing demand for food, feed and fibre for the increasing population of the world.

### **2.1. Application area**

Soil compaction has many areas of application in human endeavour apart from agriculture and forestry. When a seed is sowed the soil has to be sufficiently firmed around it (compacted) to to enable it germinate. Arable terrains require appropriate level of compaction for it to be effectively trafficked by running gears like wheels and tracks. In sports the field must have the required strength or bearing capacity (a measure of some level of compaction) for it to be good for sporting activities.

#### **2.2. Research course**

In this chapter soil compaction is considered in two regimes: in confined and unconfined spaces. The former is typical of studies under laboratory conditions while the latter signifies field conditions. The three experimental soils studied under uni-axial compression have textures of sandy clay loam, loamy sand and silt loam according to the USDA Soil Textural Classification, while the soil studied under field condition was sandy clay. In Nigeria, published data on compressibility and compaction of agricultural and forestry soils are scarce. The development and implementation of practical guidelines in order to manage soil com‐ paction for a wide range of machinery types and forestry soils depend upon an understanding of the relative importance of applied pressure and water content during the compaction process.

## **3. Materials and method**

#### **3.1. Sites of samples**

formed in attempts to develop soil compaction behaviour equations [6, 7, 8, 9, 10, 11, and 12]. Others have also reported on effects of organic matter and tractor passes on compaction and

The aim of this chapter therefore was to observe the behaviour of textured soils under uniaxial compression in confined spaces and also in unconfined spaces under the influence of agricultural machines as it is affected by applied pressure and water content and also to model

When forces are applied to soil it changes its stateof compactness to have greater density. The pressure can be applied pressure or natural forces. Applies pressure can be due to animals like horses and cattle (160 kPa), man (95 kPa), sheep (60 kPa). The pneumatic wheels of vehicles can be inflated to 100 kPa for tractors and 200 kPa for for trailers and may produce local stresses twice these values [3]. The problem therefore is that over the years arable soils have suffered degradation as a result of excessive compaction of surface and sub surface soil horizon through overuse of agricultural machinery. This trend has global phenomenon as man labours to meet the ever increasing demand for food, feed and fibre for the increasing population of the world.

Soil compaction has many areas of application in human endeavour apart from agriculture and forestry. When a seed is sowed the soil has to be sufficiently firmed around it (compacted) to to enable it germinate. Arable terrains require appropriate level of compaction for it to be effectively trafficked by running gears like wheels and tracks. In sports the field must have the required strength or bearing capacity (a measure of some level of compaction) for it to be good

In this chapter soil compaction is considered in two regimes: in confined and unconfined spaces. The former is typical of studies under laboratory conditions while the latter signifies field conditions. The three experimental soils studied under uni-axial compression have textures of sandy clay loam, loamy sand and silt loam according to the USDA Soil Textural Classification, while the soil studied under field condition was sandy clay. In Nigeria, published data on compressibility and compaction of agricultural and forestry soils are scarce. The development and implementation of practical guidelines in order to manage soil com‐ paction for a wide range of machinery types and forestry soils depend upon an understanding of the relative importance of applied pressure and water content during the compaction

the behaviour using regression analysis for the purpose of prediction.

yield of crops [13, 14].

152 Advances in Agrophysical Research

**2. Soil under pressure**

**2.1. Application area**

for sporting activities.

**2.2. Research course**

process.

	- **a.** Akure sandy clay loam soil: the site was a portion of agricultural land under fallow at the Federal University of Technology, Akure, Nigeria (70 151 N, 50 151 E), and elevation 210 m. The soil is Oxic paleustalf (Alfisol) or ferric Luvisol (FAO). A mini soil pit was dug to expose the profile. The site was designated Experi‐ mental Bin Soil (EBS). Three horizons EBS1, EBS2, and EBS3, from top to bottom respectively, were identified and samples taken from each. The thickness of the three horizons from top to bottom was 8, 15 and 15 cm, respectively.
	- **b.** Igbokoda loamy sand soil: the soil used in this study was the major soil pre‐ dominant in Igbokoda (headquarters of Ilaje Local Government area), Ondo State, South Western Nigeria. The soils were collected from the main agricultural production areas. This region is predominantly rainforest zone. Rainfall is in the order of 150 cm to 300 cm per annum, and mean annual temperature ranges from 25 to 280 C. Soil samples were taken from freshly cut faces in open shallow pit to dept of 40 cm.
	- **c.** Ilorin silt loam soil: the soil sample was taken from the arable soils of National Centre for Agricultural Mechanization (NCAM) Ilorin, Kwara State, Nigeria (8.30 N 4.32 E). The soil was Regosols (FAO). The soil samples were collected from the first 35 cm of soil profile; each sample was dug to a radius of 15 cm and then mixed thoroughly to get a homogeneous mixture, and then taken to the laboratory for further processing and analysis.

#### **ii.** Unconfined Compression Test

The study was carried out in August 2010 in an experimental plot located at The Federal University of Technology, Akure (FUTA) Step-B (Science and Technology Education Post – Basic) project site Akure, with geographical coordinate of 7o 10 North and 5o 05 East. The site is a two-hectare arable land and was manually cleared to avoid compaction due to machinery impacts on the land. The experimental plot of length and width 48.00 m by 12.00 m, respec‐ tively, was divided into three transects each of 16 m by 4 m. There was also a control plot of the same dimensions as transect. Soil samples were carefully collected from the test plots for textural and soil analysis.

#### **3.2. Analytical methods**

Particle size analyses of all the experimental soils for both confined and unconfined samples were performed using hydrometer method [16]. Organic matter content of the soils was determined using the [16] method. Other physical and chemical properties of the soils were also determined using standard methods.

#### **3.3. Confined compression tests**

**i.** Akure sandy clay loam soil: sample were collected, air-dried and ground to pass through a 2- mm sieve. The moisture content level for compaction for each soil sample was chosen according to the consistency limits of the soils determined by the procedure described [15]. Soil sample was placed in aluminium sleeve 75 mm in diameter and 50 mm long similar to that described 11].The cylinder was then placed on a 5 mm perforated metal base before the soil was added and tapped gently tapped to allow settling of the soil particles. Such prepared soil samples in the cylinders were then subjected to applied pressures 17.5, 100, 200, 300, 400, 500 and 618 kPa in turn applied by an Hydraulic Universal Testing machine (SM100, model No CPI-60) of 0.1 kN sensitivity, manufactured by TEC QUIPMENT Ltd, Nottingham, England). A hand pump of the machine was used to generate the required pressure on the soil. The soil samples were allowed to rebound before final heights were measured. The depression in the soil surface from the rim of the cylinder was measured at three points around the core by using a vernier caliper. These measurements were used to calculate bulk density in each test.

in turn to 75, 100, 150, 200, 300, 400, 500, 600 kPa. The soil displacement and mass were recorded for each compaction treatment. The mass was used to calculate bulk density of the compacted soil sample. The proctor mould was 16.8 cm height and 10 cm diameter. A circular thick metal plate was placed on the compression end of the UTM to effect uniform compaction in the proctor mould. After each compaction test, the change in depth of compressed soil was measured with the aid of a digimatic

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

http://dx.doi.org/10.5772/52774

155

Penetration resistance or Cone index (CI) was determined using a Rimick CP20 recording penetrometer (model CP 20 ultrasonic, Agridry Rimik Pty Ltd, Toowoomba), with a standard

were taken at two depths 5 and 10 cm of the proctor mould and the average of the readings

Shear strength values of experimental soils were observed using a shear vane tester of 19 mm vane. Measurements were taken at two depths of 5 and 10 cm in the Proctor's mould and the

**i. Experimental treatments and layout:** the machinery used for this specific study was

on the data and means were analyzed by Duncan's multiple range test.

cone of 322-mm2

**ii. Soil response variables:** experimental variables related to soil compaction include

dry bulk density measured by the cylinder core soil sampler method, soil moisture content measured with moisture meter model PMS- 714, Taiwan with 0.1% resolution over the depth ranges of 0-10, 10-20, 20-30, 30-40 mm. Bulk density was the average of five measurements. Moisture content was verified by gravimetric method. Soil penetration resistance PR, or cone index CI was determined using a Rimick CP20 recording penetrometer (model CP 20 ultrasonic, Agridry Rimik Pty Ltd, Toowoom‐

10 mm/s. Data were recorded at depth increments of 50 mm. Cone index was the average of 15 measurements per plot. The resistance of the soil was measured in the centre line of the foot print of the excavator tract. Rut depth of the excavator foot print was measured using a profile meter similar to that reported [18]. The bar was placed across the wheel tracks, perpendicular to the direction of travel and rods position to

base area. The penetration rate was less than

a medium Bobcat 430 Excavator of 31.9 kW power used to induce the necessary compaction on the experimental plots. The characteristics of the excavator are presented in Table 1. Seven treatments were imposed on plots 48 m long x 4 m wide, while the experimental variable was traffic frequency of 0, 1, 3, 5, 7, 9 and 11 excavator passes on the same tracks, with 3 m wide buffer zones between plots to avoid interactions. Plots were completely randomized having three replications. Statistical analysis was performed utilizing Excel 2007. An analysis of variance was carried out

average recorded to represent the shear strength of the specific sample treatment.

base area and a penetration rate was less than 10 mm/s. Measurements

vernier caliper.

**3.5. Shear strength measurement**

**3.6. Unconfined compression test**

ba), with a standard 300

cone of 322-mm2

300

**3.4. Penetration resistance measurement**

was taken as the representative value of cone index at that test.


in turn to 75, 100, 150, 200, 300, 400, 500, 600 kPa. The soil displacement and mass were recorded for each compaction treatment. The mass was used to calculate bulk density of the compacted soil sample. The proctor mould was 16.8 cm height and 10 cm diameter. A circular thick metal plate was placed on the compression end of the UTM to effect uniform compaction in the proctor mould. After each compaction test, the change in depth of compressed soil was measured with the aid of a digimatic vernier caliper.

#### **3.4. Penetration resistance measurement**

**3.3. Confined compression tests**

154 Advances in Agrophysical Research

density.

calculate bulk density in each test.

**i.** Akure sandy clay loam soil: sample were collected, air-dried and ground to pass

**ii.** Igbokoda Loamy Sand Soil: similarly, samples were air-dried and pulverized to pass

**iii.** Ilorin Silt Loam Soil: samples were collected were each air-dried and ground to pass

through a 2-mm sieve. The moisture levels for compaction tests were chosen accord‐ ing to the consistency limits of the soils determined by the procedure described by [15]. Compaction test was performed by filling the proctor mould with a known mass of soil and placed under a uni-axial compression apparatus (Universal Testing Machine (UTM), manufactured by the Testometric Co. Ltd., U. K.). Compression was carried out at a steady speed of 30 mm/min. Soil samples in the mould were subjected

through a 2 mm sieve. Each soil was wetted to a range of water contents between saturation and wilting point. For each sample, approximately 2 kg or air-dry soil was poured into a plastic tray. The soil was wetted with an atomizer and thoroughly mixed to bring the soil to the desired water content. The tray was then placed in a plastic bag and the sample was allowed to equilibrate for 48 hr. After equilibration, a soil sample at particular water content was placed in steel sleeve, 90 mm in diameter and 100 mm long. The cylinders were then placed on a 5 mm perforated metal base with cheesecloth before the soil was added. The cylinders were gently tapped to allow settling of the soil particles. Soil samples in the cylinders were then subjected to applied pressures of 0, 17.5, 100, 175, 289.5, 404, 511 and 618 kPa respectively, applied by a Universal Testing machine (SM100, model No CPI-60) of 0.1 kN sensitivity, manufactured by TEC QUIPMENT Ltd, Nottingham, England), consisting of an hydraulic ram connected to a piston. The compression force was read through a digital load meter. A hand pump was used to generate the required pressure on the soil. The pressure was maintained for a few second and then released. The samples were allowed to 'rebound' before final heights were measured. Water and air could escape around the piston and through fine perforations in the base plate. The depression in the soil surface from the rim of the cylinder was measured at three points around the core by using a vernier scale. This procedure was similar to that reported by research [10]. These measurements were used later to calculate bulk

through a 2- mm sieve. The moisture content level for compaction for each soil sample was chosen according to the consistency limits of the soils determined by the procedure described [15]. Soil sample was placed in aluminium sleeve 75 mm in diameter and 50 mm long similar to that described 11].The cylinder was then placed on a 5 mm perforated metal base before the soil was added and tapped gently tapped to allow settling of the soil particles. Such prepared soil samples in the cylinders were then subjected to applied pressures 17.5, 100, 200, 300, 400, 500 and 618 kPa in turn applied by an Hydraulic Universal Testing machine (SM100, model No CPI-60) of 0.1 kN sensitivity, manufactured by TEC QUIPMENT Ltd, Nottingham, England). A hand pump of the machine was used to generate the required pressure on the soil. The soil samples were allowed to rebound before final heights were measured. The depression in the soil surface from the rim of the cylinder was measured at three points around the core by using a vernier caliper. These measurements were used to

Penetration resistance or Cone index (CI) was determined using a Rimick CP20 recording penetrometer (model CP 20 ultrasonic, Agridry Rimik Pty Ltd, Toowoomba), with a standard 300 cone of 322-mm2 base area and a penetration rate was less than 10 mm/s. Measurements were taken at two depths 5 and 10 cm of the proctor mould and the average of the readings was taken as the representative value of cone index at that test.

#### **3.5. Shear strength measurement**

Shear strength values of experimental soils were observed using a shear vane tester of 19 mm vane. Measurements were taken at two depths of 5 and 10 cm in the Proctor's mould and the average recorded to represent the shear strength of the specific sample treatment.

#### **3.6. Unconfined compression test**


conform to the shape of the depression. Rut depth was calculated as the average depth of 40 readings on the 1 metre bar. The estimated rut depth at any traffic frequency was calculated as the mean of the total number of sections' ruts at that frequency.

( ) 0.083 2 BD = 0.09763X R = 0.9805 (2)

http://dx.doi.org/10.5772/52774

157

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

( ) ( ) <sup>2</sup> BD = 0.079Ln X + 1.089 R = 0.9938 (3)

( ) <sup>2</sup> BD = 0.0005X + 1.189 R = 0.9312 (4)

( ) <sup>2</sup> BD = 1.342e0.0002X R = 0.9899 (5)

( ) ( ) <sup>2</sup> BD = 0.187Ln X + 0.907 R = 0.9562 (6)

( ) ( ) <sup>2</sup> BD = 0.163Ln X + 0.736 R = 0.9968 (7)

( ) 0.066 2 BD = 1.115X R = 0.9826 (8)

( ) ( ) <sup>2</sup> BD = 0.091Ln X + 1.065 R = 0.9842 (9)

( ) 0.042 2 BD = 1.267X R = 0.9455 (10)

( ) 0.0001X 2 BD = 1.403e R = 0.9539 (11)

where BD = bulk density, Mg/m3

10.2, 7.4, 5.1, 3.6, and 2.2%, respectively.

X = applied pressure, kPa

X = applied pressure, kPa

12.95, 7.7, 6.4, 5.5 and 2.3%, respectively.

and

Similarly, the relationships between applied pressure and bulk density for horizon 2 (EBS2) are represented by equations (6) to (11) below representing those for moisture contents of 17.0,

Furthermore, the relationships between applied pressure and bulk density for horizon 3 (EBS3) are represented by equations (12) to (16) below representing those for moisture contents of

## **4. Results and discussion**

#### **4.1. Confined compression**

#### *4.1.1. Sandy clay loam soil*

The physical and some other properties of the experimental sandy clay loam soil are shown in Table 2.Soil samples EBS1 and EBS2 have similar characteristics yet not the same as they are different physically especially in colour which may be due to presence of more dead organic material in the EBS1 than in the EBS2. Bulk density increased with increase in applied pressure, initially at a decreasing rate and further reaching an asymptotic value especially at applied pressure of about 600 kPa and beyond. Most relationships observed between soil bulk density and applied pressures were nonlinear. At moisture contents less than 12.9 %, it was observed that bulk density change little with applied pressure in the soil as reflected from the third horizon. There was little change in bulk density between 0 and 600 kPa pressure. This can be adduced to relatively high clay content of the third horizon (EBS3), and its least organic carbon content. A clay soil is naturally more compact than a sandier or silty soil; hence its bulk density changes little under applied pressure. Generally, a very strong correlation was observed for relationship between applied pressure and bulk density, R2 values ranged from 0.92 to 0.99. The relationships between applied pressures for horizon 1 are represented by equations (1) to (5) for moisture contents of 10.4, 8.4, 4.7, 3.5 and 1.6 %, respectively.


**Table 2.** Physical Properties of experimental sandy clay loam Soils

$$\mathbf{B}\mathbf{D} = 0.8654\mathbf{X}^{0.114} \left(\begin{array}{c} \mathbf{R}^2 = 0.9967 \end{array}\right) \tag{1}$$

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces http://dx.doi.org/10.5772/52774 157

$$\mathbf{B}\mathbf{D} = 0.09763\mathbf{X}^{0.083} \left(\mathbf{R}^2 = 0.9805\right) \tag{2}$$

$$\text{BD} = 0.079 \text{Ln} \left( \text{X} \right) + 1.089 \left( \text{R}^2 = 0.9938 \right) \tag{3}$$

$$\text{BD} = 0.0005\text{X} + 1.189\left(\text{R}^2 = 0.9312\right) \tag{4}$$

$$\text{BD} = 1.342 \text{e} 0.0002 \text{X} \left( \text{R}^2 = 0.9899 \right) \tag{5}$$

where BD = bulk density, Mg/m3 and

X = applied pressure, kPa

conform to the shape of the depression. Rut depth was calculated as the average depth of 40 readings on the 1 metre bar. The estimated rut depth at any traffic frequency was calculated as the mean of the total number of sections' ruts at that frequency.

The physical and some other properties of the experimental sandy clay loam soil are shown in Table 2.Soil samples EBS1 and EBS2 have similar characteristics yet not the same as they are different physically especially in colour which may be due to presence of more dead organic material in the EBS1 than in the EBS2. Bulk density increased with increase in applied pressure, initially at a decreasing rate and further reaching an asymptotic value especially at applied pressure of about 600 kPa and beyond. Most relationships observed between soil bulk density and applied pressures were nonlinear. At moisture contents less than 12.9 %, it was observed that bulk density change little with applied pressure in the soil as reflected from the third horizon. There was little change in bulk density between 0 and 600 kPa pressure. This can be adduced to relatively high clay content of the third horizon (EBS3), and its least organic carbon content. A clay soil is naturally more compact than a sandier or silty soil; hence its bulk density changes little under applied pressure. Generally, a very strong correlation was observed for

The relationships between applied pressures for horizon 1 are represented by equations (1) to

**Mg/m3**

**Sat hyd cond**

54 21 25 1.43 1.21 33.3 46 1.41

54 21 25 1.55 1.22 33.3 46 1.22

52 17 31 1.39 0.85 44.9 48 0.87

( ) 0.114 2 BD = 0.8654X R = 0.9967 (1)

values ranged from 0.92 to 0.99.

**O.C %**

**mm/min Clay ratio Clay + silt**

relationship between applied pressure and bulk density, R2

**Texture**

% % %

**Table 2.** Physical Properties of experimental sandy clay loam Soils

(5) for moisture contents of 10.4, 8.4, 4.7, 3.5 and 1.6 %, respectively.

**Sand silt clay Bulk density**

**4. Results and discussion**

**4.1. Confined compression**

*4.1.1. Sandy clay loam soil*

156 Advances in Agrophysical Research

**Soil Type**

Sandy clay loam (EBS1)

Sandy clay loam (EBS2)

Sandy clay loam (EBS3)

Similarly, the relationships between applied pressure and bulk density for horizon 2 (EBS2) are represented by equations (6) to (11) below representing those for moisture contents of 17.0, 10.2, 7.4, 5.1, 3.6, and 2.2%, respectively.

$$\text{BD} = 0.187 \text{Ln} \left( \text{X} \right) + 0.907 \left( \text{R}^2 = 0.9562 \right) \tag{6}$$

$$\text{BD} = 0.163 \text{Ln} \left( \text{X} \right) + 0.736 \left( \text{R}^2 = 0.9968 \right) \tag{7}$$

$$\mathbf{B}\mathbf{D} = 1.115\mathbf{X}^{0.066} \quad \left(\mathbf{R}^2 = 0.9826\right) \tag{8}$$

$$\text{BD} = 0.091 \text{Ln} \left( \text{X} \right) + 1.065 \left( \text{R}^2 = 0.9842 \right) \tag{9}$$

$$\mathbf{RBD} = \mathbf{1.267} \mathbf{X}^{0.042} \quad \left(\mathbf{R}^2 = 0.9455\right) \tag{10}$$

$$\text{BD} = \text{1.403e}^{0.0011\text{X}} \quad \left(\text{R}^2 = 0.9539\right) \tag{11}$$

#### X = applied pressure, kPa

Furthermore, the relationships between applied pressure and bulk density for horizon 3 (EBS3) are represented by equations (12) to (16) below representing those for moisture contents of 12.95, 7.7, 6.4, 5.5 and 2.3%, respectively.

$$\text{BD} = 0.225 \text{Ln} \left( \text{X} \right) + 0.604 \left( \text{R}^2 = 0.9787 \right) \tag{12}$$

soil bulk density is less than 10% and the applied pressure should not exceed 200kPa, as

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

http://dx.doi.org/10.5772/52774

159

**Figure 1.** Effect of applied pressure, moisture content on bulk density of sandy clay loam soil (EBS1), Layer1 (54, 21, 25)

**Figure 2.** Effect of applied pressure, moisture content on bulk density of sandy clay loam soil (EBS2), Layer2 (54, 21, 25)

indicated by this study.

$$\mathbf{RBD} = \mathbf{1.006} \mathbf{X}^{0.079} \text{ (R}^2 = 0.9859) \tag{13}$$

$$\mathbf{B}\mathbf{D} = 1.222\mathbf{X}^{0.051} \left(\mathbf{R}^2 = 0.9287\right) \tag{14}$$

$$\text{BD} = 1.416 \text{X}^{0.019} \text{ (R}^2 = 0.9028) \tag{15}$$

$$\text{BD} = 1.425 \text{\AA}^{0.015} \quad \left(\text{R}^2 = 0.9954\right) \tag{16}$$

where BD = bulk density, Mg/m3 and

#### X = applied pressure, kPa

The above models (equations 1 to 16) were best fitted equations to the experimental values of the bulk density-applied pressure relationships. They enable prediction of bulk density of the soil to be possible in the range of moisture content and applied pressure considered in this study. The study showed that four types of models (power, logarithmic, exponential and linear functions) could be used to describe the relationship of bulk density and applied pressure at a specific moisture level, judging from their high coefficients of determination that ranged from 0.9028 to 0.9968. However, the best model at each moisture content level was reported in this paper. Power function seemed to be the best and most popular model, followed by logarithmic, exponential and linear function in that order. Substituting extra values of applied pressure and moisture content, which were not used in establishing the models, validated the models. There was high correlation (r > 0.9936) between predicted and measured values of bulk density and the errors less than 5.6 %. Other researchers had reported similar result. Researchers [20] fitted exponential curves for loamy soils while [21] reported logarithmic curves. Researchers [3] fitted logarithmic and power functions for sandy loam and clay soils at different moisture content levels and applied pressure. Figures 1, 2 and 3 indicate that irrespective of soil horizon of the soil sample and applied pressure, soil compactability increased as the moisture content increased to a limit. Generally, bulk density increased with moisture content irrespective of the value of applied pressure. Compaction caused squeezing out of water from the pores, especially the macrospores. The implication is that tillage whether manual or mechanical should be done when the soil is moist rather than wet condition. From this work, moisture content of 10% and above is unfavourable since soil compaction at these levels of moisture content would enhance soil compaction as indicated by excessively high soil bulk density. Considering the bulk density value of 1.5 Mg/m3 which is indicated to be critical for crop production [22], the moisture contents of 10.0 (Figure 1), 17.0 (Figure 2) and 12.9% (Figure 3) are liable to produce high bulk density if pressure is applied at 200 kPa and above. The recommended moisture content for minimizing soil compaction (for sandy clay loam) or soil bulk density is less than 10% and the applied pressure should not exceed 200kPa, as indicated by this study.

( ) ( ) <sup>2</sup> BD = 0.225Ln X + 0.604 R = 0.9787 (12)

0.079 2 BD = 1.006X R = 0.( 9859) (13)

( ) 0.051 2 BD = 1.222X R = 0.9287 (14)

0.019 2 BD = 1.416X R = 0.( 9028) (15)

( ) 0.015 2 BD = 1.425X R = 0.9954 (16)

where BD = bulk density, Mg/m3

X = applied pressure, kPa

158 Advances in Agrophysical Research

and

The above models (equations 1 to 16) were best fitted equations to the experimental values of the bulk density-applied pressure relationships. They enable prediction of bulk density of the soil to be possible in the range of moisture content and applied pressure considered in this study. The study showed that four types of models (power, logarithmic, exponential and linear functions) could be used to describe the relationship of bulk density and applied pressure at a specific moisture level, judging from their high coefficients of determination that ranged from 0.9028 to 0.9968. However, the best model at each moisture content level was reported in this paper. Power function seemed to be the best and most popular model, followed by logarithmic, exponential and linear function in that order. Substituting extra values of applied pressure and moisture content, which were not used in establishing the models, validated the models. There was high correlation (r > 0.9936) between predicted and measured values of bulk density and the errors less than 5.6 %. Other researchers had reported similar result. Researchers [20] fitted exponential curves for loamy soils while [21] reported logarithmic curves. Researchers [3] fitted logarithmic and power functions for sandy loam and clay soils at different moisture content levels and applied pressure. Figures 1, 2 and 3 indicate that irrespective of soil horizon of the soil sample and applied pressure, soil compactability increased as the moisture content increased to a limit. Generally, bulk density increased with moisture content irrespective of the value of applied pressure. Compaction caused squeezing out of water from the pores, especially the macrospores. The implication is that tillage whether manual or mechanical should be done when the soil is moist rather than wet condition. From this work, moisture content of 10% and above is unfavourable since soil compaction at these levels of moisture content would enhance soil compaction as indicated by excessively high soil bulk density. Considering the bulk density value of 1.5 Mg/m3 which is indicated to be critical for crop production [22], the moisture contents of 10.0 (Figure 1), 17.0 (Figure 2) and 12.9% (Figure 3) are liable to produce high bulk density if pressure is applied at 200 kPa and above. The recommended moisture content for minimizing soil compaction (for sandy clay loam) or

**Figure 1.** Effect of applied pressure, moisture content on bulk density of sandy clay loam soil (EBS1), Layer1 (54, 21, 25)

**Figure 2.** Effect of applied pressure, moisture content on bulk density of sandy clay loam soil (EBS2), Layer2 (54, 21, 25)

The compatibility of the soils was also considered in terms of the minimum increase in compaction (when the soil was dry) and maximum increase in compaction (when the soil was wet). For the soil in the uppermost horizon (EBS1), the minimum and maximum increases in compaction were 5.5 and 61.5% respectively. For the soil in the middle horizon (EBS2), the values were 3.9 and 53.6% while for the bottom horizon; the values are 4.5 and 76.9% respec‐ tively. From the foregoing, it was obvious that sandy clay loam soils are sensitive to water content at the time of compaction. This is in agreement with the findings reported by [11]. The results also show that the percentage increase in soil compaction for the sandy clay loan is related more to changes in water content than to applied pressure. Scheduling tillage opera‐ tions on this type of soil in drier condition will have greatest benefit in lowering soil compaction not withstanding changes in ground pressure.

the data of bulk density variation with moisture content. By simply "eyeballing" the data in the scatter diagram, it was apparent that a parabolic (or quadratic model) was the best model. This was confirmed by comparing the coefficients of determination of possible models:

cients, R2 = coefficient of determination. The coefficients of the model are presented in Table

**MC (%) db Model type Correlation coeff. (r) Model Equation**

4.5 (PWRFIT) 0.9977 ρb = 1.127σ 0.0397 4.7 (PWRFIT) 0.9900 ρb = 1.216σ 0.0327

8.0 (LOGFIT) 0.9938 ρb = 1.0416 + 0.071n σ 10.4 (PWRFIT) 0.9828 ρb = 1.3086σ 0.0252

13.0 (LINFIT) 0.9919 ρb = 1.4728 +0.000213σ

**Table 4.** Bulk density and applied pressure relationships at different moisture content for Igbokoda loamy sand soil.

17.5 1.4827 -0.0717 0.00567 0.6312 1.499 -0.0415 0.00337 0.6421 1.4991 -0.034 0.00291 0.7344 289.5 1.5121 -0.0315 0.00291 0.214 1.5377 -0.0296 0.00265 0.6643 1.5377 -0.0281 0.00254 0.7516 1.5525 -0.0312 0.00281 0.6452

**Model Coefficients**

) of the effect of moisture content on bulk

A B C R2

LINFIT = Linear fit ; EXPFIT = Exponential fit LOGFIT = Logarithmic fit; PWRFIT = Power fit

**Table 5.** Regression coefficients of quadratic models (*y* = *A* + *Bx* + *Cx* <sup>2</sup>

0.01 (LINFIT) 0.9956 ρb = 1.5913+7.898E-5σ 0.1 (EXPFIT) 0.9908 ρb = 1.4405EXP (1.043E-4σ) 1.6 (LINFIT) 0.9830 ρb = 1.3697 +1.411E - 4σ 1.9 (LOGFIT) 0.9943 ρb = 1.09158+ 5.413E-21nσ

were high enough to make the models suitable for predictions.

where y = bulk density (Mg/m3

5. The values of the R2

**Pressure (kPa)**

density at different applied pressures

<sup>2</sup> y = A + Bx + Cx , (17)

http://dx.doi.org/10.5772/52774

161

), x = moisture content, % (db), A,B,C = regression coeffi‐

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

#### *4.1.2. Loamy sand soil*

Physical and some other properties of the loamy sand soil are shown in Table3. Values of bulk density (ordinate) were plotted against applied pressure (abscissa). The best-fit models at each moisture level were established using regression analysis with the regression models and their coefficients shown (Table 4). The models vary from linear to intrinsically linear models: Linear fit (LINFIT); Exponential fit (EXPFIT); Logarithmic fit (LOGFIT) and power fit (PWRFIT). It was observed that experimental soil showed similar behaviour under compression when it is very dry and when it is almost saturation. This report is similar to that reported elsewhere [10]. The linear model describing the compression at those moisture levels could explain this. At intermediate moisture contents, the models are only intrinsically linear. The high coefficients of correlation of the models showed that the models are adequate for the prediction of the soil behaviour. It was reported [11] that the values for applied pressure should be regarded as relative and that the pressure required in a uni-axial test to produce the same bulk density in the field was considerably higher [23].


**Table 3.** Physical properties of the experim ental loamy sand soil

**Effect of moisture content on bulk density**: The variation of bulk density with water content at the different levels of applied pressure is governed by a quadratic relationship of the type shown in Equation (17). It is observed that bulk density decreased with increase in water content at any particular applied pressure, to a minimum density and then increased again. The range of applied pressure considered (17.5 to 618 kPa) covered the range common in agricultural productions. For the purpose of predictions, best models were established to fit the data of bulk density variation with moisture content. By simply "eyeballing" the data in the scatter diagram, it was apparent that a parabolic (or quadratic model) was the best model. This was confirmed by comparing the coefficients of determination of possible models:

The compatibility of the soils was also considered in terms of the minimum increase in compaction (when the soil was dry) and maximum increase in compaction (when the soil was wet). For the soil in the uppermost horizon (EBS1), the minimum and maximum increases in compaction were 5.5 and 61.5% respectively. For the soil in the middle horizon (EBS2), the values were 3.9 and 53.6% while for the bottom horizon; the values are 4.5 and 76.9% respec‐ tively. From the foregoing, it was obvious that sandy clay loam soils are sensitive to water content at the time of compaction. This is in agreement with the findings reported by [11]. The results also show that the percentage increase in soil compaction for the sandy clay loan is related more to changes in water content than to applied pressure. Scheduling tillage opera‐ tions on this type of soil in drier condition will have greatest benefit in lowering soil compaction

Physical and some other properties of the loamy sand soil are shown in Table3. Values of bulk density (ordinate) were plotted against applied pressure (abscissa). The best-fit models at each moisture level were established using regression analysis with the regression models and their coefficients shown (Table 4). The models vary from linear to intrinsically linear models: Linear fit (LINFIT); Exponential fit (EXPFIT); Logarithmic fit (LOGFIT) and power fit (PWRFIT). It was observed that experimental soil showed similar behaviour under compression when it is very dry and when it is almost saturation. This report is similar to that reported elsewhere [10]. The linear model describing the compression at those moisture levels could explain this. At intermediate moisture contents, the models are only intrinsically linear. The high coefficients of correlation of the models showed that the models are adequate for the prediction of the soil behaviour. It was reported [11] that the values for applied pressure should be regarded as relative and that the pressure required in a uni-axial test to produce the same bulk density in

> Bulk density Mg/m3

Loamy Sand 85 3 12 1.56 5.3 13.6 15 1.12

**Effect of moisture content on bulk density**: The variation of bulk density with water content at the different levels of applied pressure is governed by a quadratic relationship of the type shown in Equation (17). It is observed that bulk density decreased with increase in water content at any particular applied pressure, to a minimum density and then increased again. The range of applied pressure considered (17.5 to 618 kPa) covered the range common in agricultural productions. For the purpose of predictions, best models were established to fit

Sat. hydraulic conductivity mm/min

Clay ratio %

Clay + silt %

LOI %

not withstanding changes in ground pressure.

the field was considerably higher [23].

Sand %

Texture

**Table 3.** Physical properties of the experim ental loamy sand soil

Clay %

Silt %

*4.1.2. Loamy sand soil*

160 Advances in Agrophysical Research

Soil type

$$\mathbf{y} = \mathbf{A} + \mathbf{B}\mathbf{x} + \mathbf{C}\mathbf{x}^2,\tag{17}$$

where y = bulk density (Mg/m3 ), x = moisture content, % (db), A,B,C = regression coeffi‐ cients, R2 = coefficient of determination. The coefficients of the model are presented in Table 5. The values of the R2 were high enough to make the models suitable for predictions.


LINFIT = Linear fit ; EXPFIT = Exponential fit LOGFIT = Logarithmic fit; PWRFIT = Power fit

**Table 4.** Bulk density and applied pressure relationships at different moisture content for Igbokoda loamy sand soil.


**Table 5.** Regression coefficients of quadratic models (*y* = *A* + *Bx* + *Cx* <sup>2</sup> ) of the effect of moisture content on bulk density at different applied pressures

Multiple regression of moisture content and applied pressure on bulk density: multiple regression analysis was carried out to assess the effects of water content, applied pressure on bulk density. The range of pressure was 17.5 to 511 kPa and 0 to 13% (db) water content. The multiple regression equation was:

$$\mathbf{y} = \mathbf{1}.4359 + 0.00017 \,\mathbf{X}\_1 - 0.0039 \,\mathbf{X}\_{2'} \,\, \mathbf{R}^2 = 0.6114 \,\tag{18}$$

**ii. Strength properties:** shear strength and cone index are indicators of soil strength.

between cone index and surface shear resistance of soil.

Shear strength is the resistance of soil to shearing or structural failure. The shear strength of an individual clod decreases with wetting, but more importantly, the strength of the bulk soil increases with increasing moisture up to the lower plastic limit at which each particle is surrounded by a film of water which acts as lubricant. Soil strength drops sharply from that point to the upper plastic limit, where the soil becomes viscous. The effects of moisture content and applied pressure on shear strength of the experimental soils are presented in Figure 4. Shear strength increased with increase in applied pressure and moisture content until a peak value was reached after which the value of the parameter declined with further increase in moisture content. This is a typical soil behaviour which has been reported by other researchers. The peak value occurred at higher moisture content as the applied pressure increased. The maximum shear strength of the soils at applied pressure of 600 kPa was 1025 kPa at moisture content of 9.1 % (db). Similarly, the effect of moisture content and applied pressure on cone index of the soil is presented in Figure 5. The relationship is similar to that exhibited by shear strength. The maximum cone index at applied pressure of 600 kPa was 1325 kPa at moisture content of 5.0 % (db). However, the effects of moisture content and applied pressure on bulk density showed different behaviour from those of shear strength and cone index (Figure 6). Bulk density increased with increase in moisture content for all the applied pressure in the range of moisture content considered, however the increase was with a peak at about the plastic limit. Bulk density increased with increase in moisture contents up to a maximum because addition of water increased cohesion. Bulk density decreased at higher moisture content after the peak value because further addition of water created greater water pressure which reduced soil compressibility. The maximum bulk density at applied pressure of 600 kPa was 2.1 Mg/m3 at moisture content of 10.0 % (db). This moisture content was significant because it was the moisture content at which the soil reached maximum bulk density. This is in agreement with other researchers' report that soils with high amount of fine particles (clay plus silt) are more susceptible to compactability [17]. The regression models that describe the behaviour of soil parameters shown in Figures 4 to 6 are presented in Table 7. The models are largely nonlinear and they agree well with those reported by other researchers [6, 7, 8, 9, 11, and 12]. Regression models (Table 8) were also established to show relationships between compaction indices such as shear strength, cone index and bulk density at applied pressures of 75, 300 and 600 kPa representing a range of low to medium and high pressures. The relationships varied from linear to exponential and to polynomial functions. The results also found a linear correlation between cone index and shear strength at a low applied pressure of 75 kPa. This agrees well with the findings of Vanags et al. [1] who reported linear relationship

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

http://dx.doi.org/10.5772/52774

163

where y = bulk density (Mg/m3 ), X1 = applied pressure (kPa), X2 = water contents (%) db, R2 = coefficient of determination. The multiple regression analysis (Equation 18) showed that the effect of moisture content was greater than that of applied pressure on the bulk density, judging from the higher coefficient of the independent variable, water content.

#### *4.1.3. Silt loam soil*

**i. Physical properties:** The soil studied was a silt loam soil according to the USDA textural classification of soils. Table 6 shows some physical and chemical properties of the soil. The consistency limits of the soils are presented in Table 6. Plasticity index is an index of workability of the soil and a large range of plasticity index implies a need for large amounts of energy to work the soil to a desired tilth.


**Table 6.** Some physical and chemical properties of Ilorin silt loam soil

**ii. Strength properties:** shear strength and cone index are indicators of soil strength. Shear strength is the resistance of soil to shearing or structural failure. The shear strength of an individual clod decreases with wetting, but more importantly, the strength of the bulk soil increases with increasing moisture up to the lower plastic limit at which each particle is surrounded by a film of water which acts as lubricant. Soil strength drops sharply from that point to the upper plastic limit, where the soil becomes viscous. The effects of moisture content and applied pressure on shear strength of the experimental soils are presented in Figure 4. Shear strength increased with increase in applied pressure and moisture content until a peak value was reached after which the value of the parameter declined with further increase in moisture content. This is a typical soil behaviour which has been reported by other researchers. The peak value occurred at higher moisture content as the applied pressure increased. The maximum shear strength of the soils at applied pressure of 600 kPa was 1025 kPa at moisture content of 9.1 % (db). Similarly, the effect of moisture content and applied pressure on cone index of the soil is presented in Figure 5. The relationship is similar to that exhibited by shear strength. The maximum cone index at applied pressure of 600 kPa was 1325 kPa at moisture content of 5.0 % (db). However, the effects of moisture content and applied pressure on bulk density showed different behaviour from those of shear strength and cone index (Figure 6). Bulk density increased with increase in moisture content for all the applied pressure in the range of moisture content considered, however the increase was with a peak at about the plastic limit. Bulk density increased with increase in moisture contents up to a maximum because addition of water increased cohesion. Bulk density decreased at higher moisture content after the peak value because further addition of water created greater water pressure which reduced soil compressibility. The maximum bulk density at applied pressure of 600 kPa was 2.1 Mg/m3 at moisture content of 10.0 % (db). This moisture content was significant because it was the moisture content at which the soil reached maximum bulk density. This is in agreement with other researchers' report that soils with high amount of fine particles (clay plus silt) are more susceptible to compactability [17]. The regression models that describe the behaviour of soil parameters shown in Figures 4 to 6 are presented in Table 7. The models are largely nonlinear and they agree well with those reported by other researchers [6, 7, 8, 9, 11, and 12]. Regression models (Table 8) were also established to show relationships between compaction indices such as shear strength, cone index and bulk density at applied pressures of 75, 300 and 600 kPa representing a range of low to medium and high pressures. The relationships varied from linear to exponential and to polynomial functions. The results also found a linear correlation between cone index and shear strength at a low applied pressure of 75 kPa. This agrees well with the findings of Vanags et al. [1] who reported linear relationship between cone index and surface shear resistance of soil.

Multiple regression of moisture content and applied pressure on bulk density: multiple regression analysis was carried out to assess the effects of water content, applied pressure on bulk density. The range of pressure was 17.5 to 511 kPa and 0 to 13% (db) water content. The

coefficient of determination. The multiple regression analysis (Equation 18) showed that the effect of moisture content was greater than that of applied pressure on the bulk density, judging

**i. Physical properties:** The soil studied was a silt loam soil according to the USDA

need for large amounts of energy to work the soil to a desired tilth.

textural classification of soils. Table 6 shows some physical and chemical properties of the soil. The consistency limits of the soils are presented in Table 6. Plasticity index is an index of workability of the soil and a large range of plasticity index implies a

from the higher coefficient of the independent variable, water content.

**Property Values** Sand (%) 22.6 Silt (%) 62.8 Clay( %) 14.5 Silt + clay (%) 77.3 Texture (%) Silt loam Organic carbon (g/kg) 2.03 Organic matter (%) 3.51 Total nitrogen g/kg) 0.18 pH in H2O (1:2) 7.93 Ca 2+ (cmol/kg) 0.17 Mg 2+(cmol/kg) 1.70 Na +(cmol/kg) 0.17 K + (cmol/kg) 0.29 P (mg/kg) 4.00 Plastic limit (%) 9,2 Liquid limit (%) 40 Plasticity index 30.8

**Table 6.** Some physical and chemical properties of Ilorin silt loam soil

2 1 2 y = 1.4359 + 0.00017 X - 0.0039 X , R = 0.6114 (18)

), X1 = applied pressure (kPa), X2 = water contents (%) db, R2

=

multiple regression equation was:

162 Advances in Agrophysical Research

where y = bulk density (Mg/m3

*4.1.3. Silt loam soil*


**Figure 3.** Effect of applied pressure, moisture content on bulk density of sandy clay loam soil (EBS3), Layer3 (52, 17,

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

http://dx.doi.org/10.5772/52774

165

**Figure 4.** Effect of moisture content and applied pressure on shear strength

31)

CI = cone index; BD = bulk densityMC = moisture content; SS = shear strength

**Table 7.** Relationships between dependent and independent variables Ilorin silt loam soil


**Table 8.** Relationships between cone index, shear strength and bulk density of Ilorin silt loam soil

**Dependent variables**

164 Advances in Agrophysical Research

**Dependent variables**

**Independent variables**

**Independent variables**

**Predictive models R2 Applied**

SS MC y = -0.797x2 + 21.77x + 21.63 0.9733 75 polynomial SS MC y = -1.384x2 + 35.46x + 52.5 0.9394 150 polynomial SS MC y = -2.54x2 + 55.09x + 191.1 0.7899 300 polynomial SS MC *y* = −3.875*x* <sup>2</sup> + 97.17*x* + 39.08 0.468 600 polynomial

CI MC y = -1.056x2 + 25.1x + 83.75 0.8061 75 polynomial CI MC y = -1.53x2 + 34.2x + 177.3 0.8384 150 polynomial CI MC y = -2.63x2 + 52.79x + 342.1 0.7914 300 polynomial CI MC *y* = −4.543*x* <sup>2</sup> + 82.54*x* + 698.9 0.729 600 polynomial

BD MC *y* =1.133*e* 0.022*<sup>x</sup>* 0.9661 75 exponential

BD MC *y* = −0.001*x* <sup>2</sup> + 0.059*x* + 1.395 0.9442 600 Polynomial

**Predictive models R2 Applied**

CI SS *y* =1.184*x* + 24.52 0.6651 75 linear CI SS y = 0.0006x2 + 0.97x + 60.5 0.7914 150 polynomial CI SS y = 177.59e0.0025x 0.9687 300 exponential CI SS *y* =0.001*x* <sup>2</sup> −1.406*x* + 866.8 0.2600 600 polynomial

CI BD y = -627.3x2 + 1890x - 122 0.4711 75 polynomial CI BD y = -0.0014x2 + 4.42x - 3108.8 0.8094 150 polynomial CI BD y = -0.0017x2 + 5.30x - 3108.8 0.4531 300 polynomial CI BD y = -10128x2 + 36518x - 31362 0.7790 600 polynomial

BD MC y = 31.4x + 1228.7 0.9624 150 linear BD MC y = 32.02x + 1304.5 0.8976 300 linear

CI = cone index; BD = bulk densityMC = moisture content; SS = shear strength

CI = cone index; BD = bulk densityMC = moisture content; SS = shear strength

**Table 8.** Relationships between cone index, shear strength and bulk density of Ilorin silt loam soil

**Table 7.** Relationships between dependent and independent variables Ilorin silt loam soil

**pressure, kPa**

**pressure, kPa**

**Model type**

**Model type**

**Figure 3.** Effect of applied pressure, moisture content on bulk density of sandy clay loam soil (EBS3), Layer3 (52, 17, 31)

**Figure 4.** Effect of moisture content and applied pressure on shear strength

**4.2. Unconfined compression**

The most common causes of soil compaction are agricultural machines such as tractors; harvesting equipment and implement wheels travelling over moist, lose soils [24]. Soils tend to be more compacted deeper into the soil profile due to the weight of overlaying soil. Heavily compacted soils contain few large pores, less total pore volume and conse‐ quently a greater density [25]. The experimental excavator can be categorized as light ma‐ chinery in agreement with the report [26]. Also the characteristics of the experimental soil are shown in Table 9. This soil texture (sandy clay) is one of the dominant textures in the locality and even the state in general. Table 10 shows the rut that was produced as a re‐ sult of the traffic frequency. This was considered to be high for the moisture content range (11 to 15% (db)) at which the experiment was carried out. A typical excavator track footprint (rut) is shown in Figure 7. For each traffic treatment, cone index, bulk density and rut depth were measured at 2 m intervals along a 48 m transect within the excavator tracks (left and right). All measurements were made in the centrelines of the tracks be‐ cause that was where the compressive effects tend to concentrate [19]. Cone penetration resistance and bulk density were also measured in the control treatment where no tracks (excavator) had passed (Figure 8). Soil penetration resistance at the control site (zero exca‐ vator traffic) increased with depth due to shaft friction, and overburden pressure of the weight of soil above the specific depth (Figure 8). Also, lateral forces on the penetrometer cone increase with increasing depth so that more force was needed for the cone to dis‐ place soil [27]. Resistance can also increase with depth because of changes in soil texture, gravel content, structure and agricultural traffic if it had occurred. The variation of pene‐ tration resistance with depth along the excavator foot prints as a result of machinery traf‐ fic is presented in Figure 9. Generally, penetration resistance increased with depth up to a point and then decreased. This trend is consistent with the findings of many researchers. It was observed that the mean values of penetration resistance along the left and right foot prints of the excavator for each treatment were not significantly different from each other at 5% level of significance. It was reported that bulk density and penetration resist‐ ance increase with the number of passes but bulk density tended to be less responsive than penetration resistance [27]. Despite this, the measured changes in bulk density agreed with soil behaviour suggested by changes in penetration resistance. The result of this study agreed with this assertion. Examination of soil responses to traffic in deeper layers revealed that soil compaction increased as the traffic intensity increased. This also agreed with the findings of other researchers [28, 27]. Effect of traffic on bulk density is presented in Table 11 at two depths only due to the limitation imposed by the short (35 cm) shank of the penetrometer used in this study. At 9 and 11 passes, soil bulk density

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

http://dx.doi.org/10.5772/52774

167

became significantly different than at lower traffic frequency.

*4.2.1. Sandy clay soil*

**Figure 5.** Effect of moisture content and applied pressure on cone index

**Figure 6.** Effect of moisture content and applied pressure on bulk density

#### **4.2. Unconfined compression**

#### *4.2.1. Sandy clay soil*

**Figure 5.** Effect of moisture content and applied pressure on cone index

166 Advances in Agrophysical Research

**Figure 6.** Effect of moisture content and applied pressure on bulk density

The most common causes of soil compaction are agricultural machines such as tractors; harvesting equipment and implement wheels travelling over moist, lose soils [24]. Soils tend to be more compacted deeper into the soil profile due to the weight of overlaying soil. Heavily compacted soils contain few large pores, less total pore volume and conse‐ quently a greater density [25]. The experimental excavator can be categorized as light ma‐ chinery in agreement with the report [26]. Also the characteristics of the experimental soil are shown in Table 9. This soil texture (sandy clay) is one of the dominant textures in the locality and even the state in general. Table 10 shows the rut that was produced as a re‐ sult of the traffic frequency. This was considered to be high for the moisture content range (11 to 15% (db)) at which the experiment was carried out. A typical excavator track footprint (rut) is shown in Figure 7. For each traffic treatment, cone index, bulk density and rut depth were measured at 2 m intervals along a 48 m transect within the excavator tracks (left and right). All measurements were made in the centrelines of the tracks be‐ cause that was where the compressive effects tend to concentrate [19]. Cone penetration resistance and bulk density were also measured in the control treatment where no tracks (excavator) had passed (Figure 8). Soil penetration resistance at the control site (zero exca‐ vator traffic) increased with depth due to shaft friction, and overburden pressure of the weight of soil above the specific depth (Figure 8). Also, lateral forces on the penetrometer cone increase with increasing depth so that more force was needed for the cone to dis‐ place soil [27]. Resistance can also increase with depth because of changes in soil texture, gravel content, structure and agricultural traffic if it had occurred. The variation of pene‐ tration resistance with depth along the excavator foot prints as a result of machinery traf‐ fic is presented in Figure 9. Generally, penetration resistance increased with depth up to a point and then decreased. This trend is consistent with the findings of many researchers. It was observed that the mean values of penetration resistance along the left and right foot prints of the excavator for each treatment were not significantly different from each other at 5% level of significance. It was reported that bulk density and penetration resist‐ ance increase with the number of passes but bulk density tended to be less responsive than penetration resistance [27]. Despite this, the measured changes in bulk density agreed with soil behaviour suggested by changes in penetration resistance. The result of this study agreed with this assertion. Examination of soil responses to traffic in deeper layers revealed that soil compaction increased as the traffic intensity increased. This also agreed with the findings of other researchers [28, 27]. Effect of traffic on bulk density is presented in Table 11 at two depths only due to the limitation imposed by the short (35 cm) shank of the penetrometer used in this study. At 9 and 11 passes, soil bulk density became significantly different than at lower traffic frequency.


**Figure 7.** Plan view of the rut produced by the excavator tracks during experimentation

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

http://dx.doi.org/10.5772/52774

169

**Figure 8.** Variation of cone penetration resistance with depth at control plot

**Table 9.** Soil properties of sandy clay soil


Different letters within each traffic treatments show significant difference at 1% level of significance, Duncan's multiple range test)

**Table 10.** Effect of Excavator traffic frequency on rut depth


Values with different letters (horizontally Bulk) are significantly different at each depth (P less than 0.001 Duncan's multiple range test).

**Table 11.** Bulk Density (Mg m -3) at two depths under different degrees of Excavator traffic (1, 3, 5, 7, 9, 11)

**Figure 7.** Plan view of the rut produced by the excavator tracks during experimentation

**Properties Values** Sand (%) 51 Silt (%) 10 Clay( %) 39

168 Advances in Agrophysical Research

Texture (%) Sandy clay Organic carbon (g/kg) 1.5 Organic matter (%) 2.58 C/N ratio 7.89 Total nitrogen g/kg) 0.19 pH in H2O (1:2) 6.75 Ca 2+ (cmol/kg) 3.30 Mg 2+(cmol/kg) 2.20 Na +(cmol/kg) 0.14 K + (cmol/kg) 0.26 P (mg/kg) 17.54

**Table 9.** Soil properties of sandy clay soil

**Table 10.** Effect of Excavator traffic frequency on rut depth

range test)

**Depth (mm) Control plot**

multiple range test).

**Traffic treatments (No of passes) Mean rut depth (mm)** 1 27 a 3 45 b 5 70 c 7 99 d 9 132 e 11 148 f

Different letters within each traffic treatments show significant difference at 1% level of significance, Duncan's multiple

0-150 1.242 1.251 a 1.259 a 1.301 a 1.319 a 1.435 b 1.442 b 150-300 1.407a 1.422a 1.427a 1.431a 1.439a 1.506b 1.534b

**Table 11.** Bulk Density (Mg m -3) at two depths under different degrees of Excavator traffic (1, 3, 5, 7, 9, 11)

Values with different letters (horizontally Bulk) are significantly different at each depth (P less than 0.001 Duncan's

**Excavator traffic frequency (No of passes)**

1 3 5 7 9 11

**Figure 8.** Variation of cone penetration resistance with depth at control plot

**5. Conclusion**

pressure in the compaction process.

applied pressure at the time of compaction.

depths, at 5% level of significance.

**Acknowledgements**

chapter.

1.2389 to 1.6393 Mg/m3

**2.** The study shows that compaction behaviour of Akure sandy clay loam soil in a confined compression could be modelled after certain non-linear equations. The model derived from the data can be used to evaluate the relative importance of water content and applied

**3.** Similarly, the behaviour of Igbokoda loamy sand soil has been studied.The soil showed similar behaviours in the dry and near saturation conditions. Bulk density varied from

**4.** The study also showed that compaction behaviour of Ilorin silt loam soil could be modelled after certain linear and non-linear regression equations. Cone index have good positive linear relationship with shear strength, but can also be fitted with polynomial (quadratic) function with higher coefficient of determination. The effect of moisture content and applied pressure on cone index, shear strength was best fitted with polyno‐ mial function of the second order. The effect of applied pressure and moisture content on bulk density of silt loam could be modelled after linear, exponential and polynomial

**5.** The study of the compaction behaviour of Akure sandy clay in unconfined space (field) showed that Cone penetration resistance values under left and right centre lines of excavator tracks was not significantly different from one another. There were significant differences in the mean rut of traffic frequencies at 5% level of significance. There were also significant differences in the mean bulk density due to traffic frequencies at two

I hereby acknowledge the following that have made the various studies reported in this chapter possible: the Federal university of Technology, Akure (FUTA), Nigeria for the Senate Research Grant No (URG/MINOR/98/105); the National Centre for Agricultural Mechanisation (NCAM) for the privilege to use the facility of their Research Laboratory; World Bank for the STEP-B research Grant to the Institution (FUTA); and to my numerous undergraduate and post graduate students who have assisted in collecting useful data for the work reported in this

regression functions. Cone index has good correlation with shear strength

linear and quadratic models can be used to describe the behaviour of the soil for the purpose of predictions. In a multiple regression analysis, it was observed that the principal factor influencing compaction of the loamy sand soil was water content rather than

in the range of applied pressure of 0 to 618 kPa. Linear, intrinsically

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

http://dx.doi.org/10.5772/52774

171

**Figure 9.** Cone penetration resistance in the centre lines of the excavator tracks- (a) 1 pass (b) 3 passes (c) 5 passes (d) 7 passes (e) 9 passes (f) 11 passes

## **5. Conclusion**

7 passes (e) 9 passes (f) 11 passes

**Penetration resistance (kPa)**

**Penetration resistance (kPa)**

**Penetration resistance (kPa)**

170 Advances in Agrophysical Research

0 10 20 30 40

Left track Right track

0 10 20 30 40

Left track Right track

Depth (cm)

0 10 20 30 40

Depth (cm)

Left track Right track

Depth (cm)

(c) (d)

 (e) (f)

**Figure 9.** Cone penetration resistance in the centre lines of the excavator tracks- (a) 1 pass (b) 3 passes (c) 5 passes (d)

(a) (b)

**Penetration resistance (pKa)**

**Penetration resistance (kPa)**

**Penenetration resistance (kPa)**

**0 10 20 30 40**

**Depth (cm)**

Left track Right track

0 10 20 30 40

Left track Right track

0 10 20 30 40 Depth (cm)

Depth (cm)

 **Left track Right track**


## **Acknowledgements**

I hereby acknowledge the following that have made the various studies reported in this chapter possible: the Federal university of Technology, Akure (FUTA), Nigeria for the Senate Research Grant No (URG/MINOR/98/105); the National Centre for Agricultural Mechanisation (NCAM) for the privilege to use the facility of their Research Laboratory; World Bank for the STEP-B research Grant to the Institution (FUTA); and to my numerous undergraduate and post graduate students who have assisted in collecting useful data for the work reported in this chapter.

## **Author details**

Seth I. Manuwa\*

Address all correspondence to: sethimanuwa@yahoo.com

Department of Agricultural Engineering, School of Engineering and Engineering Technolo‐ gy, The Federal University of Technology, Akure, Nigeria

[12] Fritton, D. D. An Improved Empirical Equation for Uni-axial Soil Compression for a Wide Range of Applied Stresses, *Soil Science Society of America, Journal*, (2001). , 65,

Soil Behaviour Characteristics Under Applied Forces in Confined and Unconfined Spaces

http://dx.doi.org/10.5772/52774

173

[13] Ohu, J. O, Raghavan, G. S. V, Mckyes, E, & Mehuys, G. Shear Strength Prediction of Compacted Soils with Varying added Organic Matter Contents,'' *Transactions of the*

[14] Onwualu, A. P, & Anazodo, U. G. N. Soil Compaction Effect on Maize Production under Various Tillage Methods in a Derived Savanna Zone of Nigeria, '' *Soil & Tillage*

[16] Walkley, A, & Black, I. A. An Examination of the Different Methods for Determining Soil Organic Matter and a Proposed Modification of the Chromic Acid Titration

[17] Krzic, M, Bulmer, C. E, Teste, F, Dampier, L, & Rahman, S. Soil properties Influenc‐ ing Comppactability of Forest Soils in British Columbia, *Can. J. Sci.* (2004). , 84,

[18] Manuwa, S. I. (2009). Performance evaluation of tillage tines operating under differ‐ ent depths in a sandy clay loam soil. Soil and tillage research, , 103, 399-405.

[19] Sohne, W. (1958). Fundamentals of pressure distribution and soil compaction under

[20] Dexter, A. R, & Tanner, D. W. (1973). Response of unsaturated soils to isotropic

[21] Bertilsson, G. (1971). Topsoil reaction to mechanical pressure. Swede. Journal of Agri‐

[22] Fulton, J. P, Wells, L. G, Shearer, S. A, & Barnhisel, R. I. (1996). Spatial variation of soil physical properties: A precursor to precision tillage. ASAE Paper International

[23] Ssullivan, O, & , M. F. Uni-axial compaction effects on soil physical properties in rela‐

[24] [24]Alakuku, L, Weisskopf, P, Chamen, W. C. T, Tijink, F. G. J, Van Der Linden, J. P, Pires, S, Sommer, C, & Spoor, G. (2003). Prevention strategies for field traffic-induced subsoil compaction: A review. Part 1.Machine/soil interactions- *Soil and Tillage Res.*, ,

[25] Horn, R, & Van Den, J. H. Akker and J. and Arvidsson. (Eds.) ((2001). Subsoil Com‐ paction- Distribution, Processes and Consequences.- *Advances in Geology* 32, Catena-

tion to soil type and cultivation. Soil & Tillage Research, , 24, 257-269.

*American Society of Agricultural Engineers*, (1986). , 29(2), 251-255.

[15] Lambe, T. W. Soil Testing for Engineers,'' John Wiley, New York, (1951).

678-684.

219-226.

73, 145-160.

Verlag, Reiskirchen

*Research,* (1989). , 14, 99-114.

Method,'' *Soil Science*, (1934). , 37, 29-38.

tractor tyres. Agric. Eng. , 39, 276-281.

cultural Research, , 1, 179-189.

stress. Journal of Soil Science, , 24, 491-502.

Meeting, Phoenix, Arizona. July (961002), 14-18.

## **References**


**Author details**

172 Advances in Agrophysical Research

Seth I. Manuwa\*

**References**

(1971).

ton, D. C., (1968).

York, (1983). , 171-280.

*ica*, (1991). , 22(2), 27-31.

Address all correspondence to: sethimanuwa@yahoo.com

gy, The Federal University of Technology, Akure, Nigeria

asssi/supersoil2004/s14/poster/1565\_vanagsc.htm.

*Society of America Journal*, (2002). , 66, 1784-1787.

tion,'' *Advances in Soil Science*, (1987). , 6, 65-100.

*Engineering Research*, (1974). , 19, 271-278.

Department of Agricultural Engineering, School of Engineering and Engineering Technolo‐

[1] Vanags, C, Minasny, B, & Mcbratney, B. and A. B. The Dynamic Penetrometer for As‐ sessment of Soil Mechanical Resistance,'' (2004). http://www.regional.org.au/au/

[2] Hillel, H. Soil and Water: Physical and processes,''. Academic Press, New York,

[3] Gill, W. R. and G. E. Van den Berg, ''Soil Dynamics in Tillage and Traction,'' Hand‐ book 316, Agricultural Research Service, U. S. Department of Agriculture, Washing‐

[4] Assouline, S. Modeling Soil Compaction under Uniaxial Compression,'' *Soil Science*

[5] Koolen, A. J, & Kuipers, H. Agricultural Soil Mechanics,'' Springer- Verlag. New

[6] Koolen, A. J. A method of Soil Compatibility Determination,'' *Journal of Agricultural*

[7] Larson, W. E, Gupta, S. C, & Useche, R. A. Compression of Agricultural Soils from Eight Soil Orders,'' *Soil Science Society of America Journa*l, (1980). , 44, 450-457.

[8] Saini, G. R, Chow, T. L, & Ghanen, I. Compatibility Indexes of Some Agricultural

[9] Gupta, S. C, & Allmaras, R. R. Models to Assess the Susceptibility of Soil to Compac‐

[10] Oni, K. C. Traffic Compaction and Tillage Effects on the Performance of Maize in Sandy loam Soil of Nigeria,'' *Agricultural Mechanization in Asia, Africa and Latin Amer‐*

[11] Smith, C. W, Johnston, M, & Lorentz, A. Assessing the Compaction Susceptibility of South African Forestry Soils. 1. The Effect of Soil Type, Water Content and Applied

Pressure on Uni-axial Compaction,'' *Soil Tillage & Research*, (1977). , 41, 53-73.

Soils of New Brunswick, Canada,'' *Soil Science*, (1984). , 137, 33-38.


[26] Botta, G. F, Jorajuria, D, Rosatto, H, & Ferrero, C. (2006). Light tractor traffic frequen‐ cy on soil compaction in the rolling Pampa region of Argentina, Soil & Tillage Re‐ search, , 86, 9-14.

**Chapter 8**

**Microaggregate Stability of Tropical Soils and its Roles**

Soil aggregate stability influences a wide range of physical and biogeochemical processes in the agricultural and natural environments, including soil erosion [3]. The relative prepon‐ derance of aggregates of various sizes in the soil and their stability to external forces are, therefore, an issue of major concern to soil scientists. By definition, an aggregate is a compo‐ site body or granule of loosely bound mineral particles within a soil, the binding of which is characteristically mediated by a relatively minor amount of organic matter [Encyclopedia of Soil Science, ESS 2008]. The mineral and organic particles involved in such a natural con‐ glomeration, otherwise known as aggregation, cohere to each other more than to the neigh‐ bouring particles and/or aggregates [ESS 2008]. Soil aggregates are therefore soil structural units of which classical soil research recognizes two major size-based categories, macroag‐ gregates and microaggregates. Collapse of macroaggregates yields microaggregates. Thus, macroaggregates may be viewed as having microaggregates as their building blocks. Some‐ times, external forces acting on a soil can also foster formation of aggregates from dispersed materials. It is the interplay of aggregate formation and breakdown that results in soil struc‐ ture [54]. Although extremities in either of these structure-promoting processes are undesir‐ able, they are considered an agronomic and environmental problem only in the case of breakdown. This is because it is much easier to break down over-sized aggregates into fa‐ vourably sized ones than to achieve aggregation in structurally dilapidated soils. Conse‐ quently, studies on the responses of soil aggregates to natural and anthropogenic forces appear to tilt more towards stability or otherwise of soil aggregates than to their coalescence by these forces. Soil aggregation includes the processes of formation and stabilization, both of which occur continuously and concurrently [3]. Soil aggregate/structural stability may be defined as a measure of the ability of the soil structural units to resist change or the extent to

> © 2013 Igwe and Obalum; licensee InTech. This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Attribution License (http://creativecommons.org/licenses/by/3.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

© 2013 Igwe and Obalum; licensee InTech. This is a paper distributed under the terms of the Creative Commons

**on Soil Erosion Hazard Prediction**

Additional information is available at the end of the chapter

C.A. Igwe and S.E. Obalum

http://dx.doi.org/10.5772/52473

**1. Introduction**

