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Title: THE ENERGY CONCEPT OF SOIL MOISTURE AND MECHANICS OF UNSATURATED FLOW
Accession Number: 00234464
Record Type: Component
Availability: Transportation Research Board Business Office 500 Fifth Street, NW Abstract: THE MOISTURE RETAINING AND TRANSMITTING PROPERTIES OF UNSOLIDIFIED POROUS MATERIALS IS OF CONSIDERABLE IMPORTANCE IN DETERMINING THE PHYSICAL PROPERTIES AND SUITABILITY FOR CERTAIN ENGINEERING APPLICATIONS. SOIL MOISTURE CONDITIONS MAY BE DESCRIBED IN TERMS OF THE SECURITY WITH WHICH THE WATER IS HELD BY THE SOIL. THIS SECURITY CAN BE MEASURED IN TERMS OF THE THERMODYNAMIC FREE ENERGY OF THE WATER ITSELF. MEASUREMENTS OF THE PRESSURE, VAPOR PRESSURE, FREEZING POINT DEPRESSION, ETC., MAY BE USED TO EVALUATE THIS FREE ENERGY FUNCTION. PF CURVES RELATING THE MOISTURE CONTENT OF SOILS TO A LOGARITHMIC FUNCTION OF THE FREE ENERGY REVEAL THAT A CONTINUOUS FUNCTIONAL RELATIONSHIP EXISTS OVER A MOISTURE CONTENT RANGE EXTENDING FROM SATURATION TO OVEN DRYNESS. MOISTURE CONDITIONS IN SITU CAN BE FOLLOWED WITH A MINIMUM OF DISTURBANCE TO THE SURROUNDING SOIL BY THE USE OF A TENSIOMETER. TENSIOMETERS ARE OF USE IN FOLLOWING FLUCTUATIONS IN ELEVATION OF WATER TABLES AND IN TRACING THE ADVANCE OF A WETTING FRONT THROUGH A SOIL FOLLOWING THE ADDITIONS OF WATER BY RAINFALL OR BY IRRIGATION. THE ENERGY CONCEPT OF SOIL MOISTURE AIDS IN EXPLAINING MOISTURE FLOW PHENOMENA. FOR SATURATED FLOW DARCY'S LAW STATES THAT THE RATE OF FLOW IS PROPORTIONAL TO A POTENTIAL GRADIENT CALLED THE HYDRAULIC GRADIENT. THE PROPORTIONALITY CONSTANT IS KNOWN AS THE COEFFICIENT OF SATURATED PERMEABILITY. IN PROBLEMS INVOLVING THE FLOW OF MOISTURE THROUGH AN UNSATURATED POROUS MEDIA THE RATE OF FLOW IS PROPORTIONAL TO THE POTENTIAL GRADIENT. THE NUMERICAL VALUE OF THE PROPORTIONALITY CONSTANT HAS BEEN SHOWN TO VARY WIDELY AND TO BE A FUNCTION OF THE FREE ENERGY OF THE MOISTURE IN THE UNSATURATED SOIL. UNSATURATED MOISTURE FLOW OCCURS AS THE RESULT OF A PRESSURE GRADIENT WHICH, BECAUSE OF TEXTURAL DIFFERENCES, MAY BE QUITE INDEPENDENT OF THE MOISTURE PERCENTAGE GRADIENT. IT IS THEN EVIDENT THAT MOISTURE MOVEMENT THROUGH UNSATURATED MATERIALS IS LARGELY A FUNCTION OF THE FREE ENERGY OF THE WATER IN THE SOIL RATHER THAN OF THE ACTUAL AMOUNT OF MOISTURE PRESENT.
Supplemental Notes: Vol 21, pp 435-450, 8 FIG, 2 TAB, 23 REF. Distribution, posting, or copying of this PDF is strictly prohibited without written permission of the Transportation Research Board of the National Academy of Sciences. Unless otherwise indicated, all materials in this PDF are copyrighted by the National Academy of Sciences. Copyright © National Academy of Sciences. All rights reserved.
Monograph Accession #: 01490426
Authors: Russell, M BSpangler, M GKrynine, D PWinterkorn, HEditors: Crum, Roy WPublication Date: 1942 (approximate)
Serial:
Highway Research Board Proceedings
Volume: 21 Media Type: Digital/other
TRT Terms: Uncontrolled Terms: Old TRIS Terms: Subject Areas: Geotechnology; Highways
Files: TRIS, TRB
Created Date: Aug 19 1994 12:00AM
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