Identify the soil texture (use the soil texture triangle) and provide its porosity, saturated hydraulic conductivity, and saturated matric head based on Tables 7.1 and 7.2. Based on those parameters calculate the field capacity and wilting point for the soil*.

Principles of Foundation Engineering (MindTap Course List)
9th Edition
ISBN:9781337705028
Author:Braja M. Das, Nagaratnam Sivakugan
Publisher:Braja M. Das, Nagaratnam Sivakugan
Chapter3: Natural Soil Deposits And Subsoil Exploration
Section: Chapter Questions
Problem 3.15P
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A soil sample is analyzed via a sieve analysis and determined to have the following size distribution: 10% sand and 45% silt.

  1. a)  Identify the soil texture (use the soil texture triangle) and provide its porosity, saturated hydraulic conductivity, and saturated matric head based on Tables 7.1 and 7.2. Based on those parameters calculate the field capacity and wilting point for the soil*.

  2. b)  Make a plot of the matric head vs. volumetric soil moisture and of the hydraulic conductivity vs. volumetric soil moisture for this soil.

TABLE 7.2. AVERAGE BROOKS-COREY PARAMETERS
AS A FUNCTION OF SOIL TYPE (CLAPP &
HORNBERGER,
1978). VALUE SHOWN IN
PARENTHESES IS THE STANDARD DEVIATION.
SOIL
TYPE
Sand
Loamy sand
Sandy Loam
Silt Loam
Loam
Sandy clay
loam
Silty clay
loam
Clay loam
Sandy clay
Silty clay
Clay
SAT.
HYDRAULIC
CONDUC-
TIVITY
[cm/hr]
63.36
56.16
12.49
2.59
2.50
2.27
0.61
0.88
0.78
0.37
0.46
SAT.
MATRIC
HEAD
[cm]
-12.1 (14.3)
-9.0 (12.4)
-21.8 (31.0)
-78.6 (51.2)
-47.8 (51.2)
-29.9 (37.8)
-35.6 (37.8)
-63.0 (51.0)
-15.3 (17.3)
-49.0 (62.1)
-40.5 (39.7)
BROOKS-
COREY
PARAMETER
4.05 (1.78)
4.38 (1.47)
4.90 (1.75)
5.30 (1.96)
5.39 (1.87)
7.12 (2.43)
7.75 (2.77)
8.52 (3.44)
10.4 (1.64)
10.4 (4.45)
11.4 (3.7)
Transcribed Image Text:TABLE 7.2. AVERAGE BROOKS-COREY PARAMETERS AS A FUNCTION OF SOIL TYPE (CLAPP & HORNBERGER, 1978). VALUE SHOWN IN PARENTHESES IS THE STANDARD DEVIATION. SOIL TYPE Sand Loamy sand Sandy Loam Silt Loam Loam Sandy clay loam Silty clay loam Clay loam Sandy clay Silty clay Clay SAT. HYDRAULIC CONDUC- TIVITY [cm/hr] 63.36 56.16 12.49 2.59 2.50 2.27 0.61 0.88 0.78 0.37 0.46 SAT. MATRIC HEAD [cm] -12.1 (14.3) -9.0 (12.4) -21.8 (31.0) -78.6 (51.2) -47.8 (51.2) -29.9 (37.8) -35.6 (37.8) -63.0 (51.0) -15.3 (17.3) -49.0 (62.1) -40.5 (39.7) BROOKS- COREY PARAMETER 4.05 (1.78) 4.38 (1.47) 4.90 (1.75) 5.30 (1.96) 5.39 (1.87) 7.12 (2.43) 7.75 (2.77) 8.52 (3.44) 10.4 (1.64) 10.4 (4.45) 11.4 (3.7)
TABLE 7.1. AVERAGE POROSITY AS A FUNCTION OF
SOIL TYPE (CLAPP & HORNBERGER, 1978). VALUE
SHOWN IN PARENTHESES IS THE STANDARD
DEVIATION.
SOIL TYPE
Sand
Loamy sand
Sandy Loam
Silt Loam
Loam
Sandy clay loam
Silty clay loam
Clay loam
Sandy clay
Silty clay
Clay
POROSITY
0.395 (0.056)
0.410 (0.068)
0.435 (0.086)
0.485 (0.059)
0.451 (0.078)
0.420 (0.059)
0.477 (0.057)
0.476 (0.053)
0.426 (0.057)
0.492 (0.064)
0.482 (0.050)
Transcribed Image Text:TABLE 7.1. AVERAGE POROSITY AS A FUNCTION OF SOIL TYPE (CLAPP & HORNBERGER, 1978). VALUE SHOWN IN PARENTHESES IS THE STANDARD DEVIATION. SOIL TYPE Sand Loamy sand Sandy Loam Silt Loam Loam Sandy clay loam Silty clay loam Clay loam Sandy clay Silty clay Clay POROSITY 0.395 (0.056) 0.410 (0.068) 0.435 (0.086) 0.485 (0.059) 0.451 (0.078) 0.420 (0.059) 0.477 (0.057) 0.476 (0.053) 0.426 (0.057) 0.492 (0.064) 0.482 (0.050)
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