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Extra resources for Fundamentals of Transport Phenomena in Porous Media
J. DE RWET (1964), J. Catalysis, 3, 341. 6. HUGO,P AND A. PARATELLA (1966), Consiglio Nazionale Delle Ricerche, Vol. 5 , Roma. 7. PIRET,E. , R. A. EBEL,C. T. KIANGAND W. ARMSTRONG (1951). Chem. Engng. , 47, 405. 8. POLLARD,W. G. AND R. D. PRESENT (1948), Phys. , 73,762. 9. PRICE, M. S. T. A. Symposium on Nuclear Graphite, p. 71. 10. SCHNEIDER, P. AND J. M. SMITH (1968), Paper presented on the IV. Intern. Congr. on Catalysis, Novosibirsk. 11. WAKAO,N. AND J. M. SMITH (1962), Chem. Engng. , 17, 825.
WEISZ,P. B. (1957), Z . physikal. Chemie N . , 11, 1. 13. WEISZ,P. B. AND A. B. SCHWARTZ (1962), J. Catalysis, 1, 399. 14. WICKE,E. AND R. , 97, 135. , Dep. of Agriculture, Bureau of Soils, Bull. No. 25 (1904). 1. 2. 3. 4. ~IYSIKALISCHECHEMIE DER MUNSTER, WEST-GERMANY New Address: UNIVERSITAT MUNSTER, 2 HAMBURG 11, POSTFAC1929 P. HUGO,DEOGRANDEL. STATIONARY HEAT TRANSPORT BY PLANE GROUNDWATER MOVEMENT IN A THIN OR A THICK LAYER A. VERRUIJT 1. INTRODUCTION For the application of groundwater for cooling purposes use is often made of a system of sources and sinks operating in a confined aquifer.
AND F. LEHNER (1969), Appl. Sci. , 20, 309-31 1. 5. LAUWERIER, H. A. (1956), Appl. Sci. , A5, 145-150. 6. MUSKATM. , McGraw-Hill, New York. 7. SHAMIR, U. Y. AND D . R. F. , 3, 557-581. TECHNOLOGICAL UNIVERSITY, DEPARTMENT OF CIVIL ENGINEERING, DELFT,NETHERLANDS THE SIGNIFICANCE OF THE NET TRANSFER OF VISCOUS STRESS ENERGY AND THE LOCAL PRODUCTION OF KINETIC ENERGY IN STATIONARY SOIL WATER FLOW P. H. GROENEVELT ABSTRACT For stationary saturated flow of water through a homogeneous porous medium non-equilibrium thermodynamics provides a scheme in which measurable fluxes and forces are connected to each other by linear homogeneous relationships.
Fundamentals of Transport Phenomena in Porous Media by IAHR (Eds.)