Calculation of Temperature Effects on Wetting Coefficients of Porous Solids and Their Capillary Pressure Functions

We explored the notion that changes in wetting coefficients of porous solids contributed to the temperature sensitivities of capillary pressure functions (CPFs). A chemical-thermodynamic explanation for these contributions was developed. If the temperature sensitivities of CPFs were due to capillarity (i.e., due to temperature-induced changes in liquid-gas interfacial tensions or wetting coefficients), then for a given degree of saturation the ratios of capillary pressures to their temperature derivatives should have been linear functions of thermodynamic temperature with slopes equal to 1. This indeed was the case for samples of both synthetic and natural porous media. Further, the estimated intercepts of these linear functions indicated that changes with temperature of these porous materials' wetting coefficients had pronounced effects on temperature sensitivities of their CPFs. A simple model for temperature effects on CPFs, which was derived from the linear relationship between temperature and the ratio of capillary pressure to its temperature derivative, could be fitted precisely by nonlinear regression to CPFs of two soils determined at four temperatures.

[1]  D. R. Nielsen,et al.  Water movement in glass bead porous media: 1. Experiments of capillary rise and hysteresis , 1994 .

[2]  William G. Gray,et al.  Thermodynamic basis of capillary pressure in porous media , 1993 .

[3]  Michael A. Celia,et al.  MICROMODEL STUDIES OF THREE-FLUID POROUS MEDIA SYSTEMS : PORE-SCALE PROCESSES RELATING TO CAPILLARY PRESSURE-SATURATION RELATIONSHIPS , 1993 .

[4]  J. Constantz Comparison of Isothermal and Isobaric Water Retention Paths in Nonswelling Porous Materials , 1991 .

[5]  U. Demlehner The Contact Angle of Liquids in Porous Media , 1991 .

[6]  A. Salehzadeh The Temperature Dependence of Soil Moisture Characteristics of Agricultural Soils , 1990 .

[7]  E. E. Miller,et al.  The temperature dependence of isothermal moisture vs. potential characteristics of soils. , 1986 .

[8]  P. Tarazona,et al.  Fluids in narrow pores: adsorption, capillary condensation, and critical points , 1986 .

[9]  J. Witmer,et al.  Nonlinear Regression Modeling. , 1984 .

[10]  Van Genuchten,et al.  A closed-form equation for predicting the hydraulic conductivity of unsaturated soils , 1980 .

[11]  J. Rouquerol,et al.  Calorimetric determination of surface areas: Possibilities of a modified Harkins and Jura procedure , 1979 .

[12]  A. Khalil Thermal treatment of nonporous silica , 1978 .

[13]  W. Jury,et al.  Measurement of the Transport Coefficients for Coupled Flow of Heat and Moisture in a Medium Sand 1 , 1974 .

[14]  Y. Mualem,et al.  A conceptual model of hysteresis , 1974 .

[15]  Gaylon S. Campbell,et al.  A SIMPLE METHOD FOR DETERMINING UNSATURATED CONDUCTIVITY FROM MOISTURE RETENTION DATA , 1974 .

[16]  D. H. Everett,et al.  Manual of Symbols and Terminology for Physicochemical Quantities and Units, Appendix II: Definitions, Terminology and Symbols in Colloid and Surface Chemistry , 1972 .

[17]  Hiroshi Akima,et al.  A New Method of Interpolation and Smooth Curve Fitting Based on Local Procedures , 1970, JACM.

[18]  J. Bikerman Surface energy of solids , 1965 .

[19]  J. Whalen THERMODYNAMIC PROPERTIES OF WATER ADSORBED ON QUARTZ , 1961 .

[20]  N. Hackerman,et al.  Heats of Immersion. I. The System Silica–water , 1959 .

[21]  J. R. Philip,et al.  Moisture movement in porous materials under temperature gradients , 1957 .

[22]  R. Gardner RELATION OF TEMPERATURE TO MOISTURE TENSION OF SOIL , 1955 .

[23]  W. D. Harkins,et al.  Surfaces of Solids. XII. An Absolute Method for the Determination of the Area of a Finely Divided Crystalline Solid , 1944 .

[24]  R. H. Oppermann,et al.  Properties of ordinary water-substance: by N. Ernest Dorsey. 673 pages, illustrations, tables, 16 × 24 cms. New York, Reinhold Publishing Corporation, 1940.Price $15.00. , 1940 .