When soil water potential in a sandy loam soil goes from -0.1 to -10 bars, the height of an equivalent column of capillary water increases 100 times. The rate of water movement (the hydraulic conductivity): O increases by a factor of about 100 times increases by a factor of about 10 times remains little affected O decreases by a factor of about 1000 times decreases by a factor of about 10 times

Fundamentals of Geotechnical Engineering (MindTap Course List)
5th Edition
ISBN:9781305635180
Author:Braja M. Das, Nagaratnam Sivakugan
Publisher:Braja M. Das, Nagaratnam Sivakugan
Chapter6: Hydraulic Conductivity
Section: Chapter Questions
Problem 6.1P
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When soil water potential in a sandy loam soil goes from -0.1 to -10 bars, the height
of an equivalent column of capillary water increases 100 times. The rate of water
movement (the hydraulic conductivity):
O increases by a factor of about 100 times
increases by a factor of about 10 times
remains little affected
O decreases by a factor of about 1000 times
decreases by a factor of about 10 times
Transcribed Image Text:When soil water potential in a sandy loam soil goes from -0.1 to -10 bars, the height of an equivalent column of capillary water increases 100 times. The rate of water movement (the hydraulic conductivity): O increases by a factor of about 100 times increases by a factor of about 10 times remains little affected O decreases by a factor of about 1000 times decreases by a factor of about 10 times
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