Organic soils are typically characterized by high void ratio, low specific gravity, and high compressibility. Following are the results of a consolidation test on a sample of organic soil obtained from southwest Florida. Pressure, o' (kN/m²) Change in dial reading, AH (mm) 0.242 12 0.201 24 0.317 48 0.552 100 0782 200 2.193 400 4.429 Given that the initial height of the specimen = 20.6 mm, mass of dry specimen = 12 g, area of specimen = 31.67 cm², and G, = 2.49, a. Plot the e-log ơ' curve. b. Determine the preconsolidation pressure. c. Calculate the compression index, C. O Congage learning 2014

Structural Analysis
6th Edition
ISBN:9781337630931
Author:KASSIMALI, Aslam.
Publisher:KASSIMALI, Aslam.
Chapter2: Loads On Structures
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Organic soils are typically characterized by high void ratio, low specific gravity,
and high compressibility. Following are the results of a consolidation test on a
sample of organic soil obtained from southwest Florida.
Pressure, o' (kN/m) Change in dial reading, AH (mm)
0.242
12
0.201
24
0.317
48
0.552
100
0782
200
2.193
400
4.429
Given that the initial height of the specimen = 20.6 mm, mass of dry specimen
12 g, area of specimen = 31.67 cm², and G, = 2.49,
a. Plot the e-log o' curve.
b. Determine the preconsolidation pressure.
c. Calculate the compression index, C
Congage Learning 2014
Transcribed Image Text:Organic soils are typically characterized by high void ratio, low specific gravity, and high compressibility. Following are the results of a consolidation test on a sample of organic soil obtained from southwest Florida. Pressure, o' (kN/m) Change in dial reading, AH (mm) 0.242 12 0.201 24 0.317 48 0.552 100 0782 200 2.193 400 4.429 Given that the initial height of the specimen = 20.6 mm, mass of dry specimen 12 g, area of specimen = 31.67 cm², and G, = 2.49, a. Plot the e-log o' curve. b. Determine the preconsolidation pressure. c. Calculate the compression index, C Congage Learning 2014
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