THE SIGNIFICANCE OF THE STORAGE PARAMETER IN SATURATED-UNSATURATED GROUNDWATER FLOWNARASIMHAN TN.1979; WAT. RESOURCES RES.; USA; DA. 1979; VOL. 15; NO 3; PP. 569-576; BIBL. 18 REF.; 14 ILL.Article

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RATIO METHOD FOR DETERMINING CHARACTERISTICS OF IDEAL,LEAKY AND BOUNDED AGUIFERS.NARASIMHAN TN.1968; ASS. INTERNATION. HYDROGEOLOGUES, BULL. INFORM.; FRA; 1968(2), VOL. 13, NUM. 0001, P. 70 A 83Miscellaneous

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NUMERICAL MODEL FOR SATURED-UNSATURED FLOW IN DEFORMABLE POROUS MEDIA. III: APPLICATIONSNARASIMHAN TN; WITHERSPOON PA.1978; WAT. RESOURCES RES.; USA; DA. 1978; VOL. 14; NO 6; PP. 1017-1034; BIBL. 26 REF.; 46 ILL.Article

NUMERICAL MODEL FOR LAND SUBSIDENCE IN SHALLOW GROUNDWATER SYSTEMS.NARASIMHAN TN; WITHERSPOON PA.1977; I.A.H.S.-A.I.H.S. PUBL.; U.S.A.; DA. 1977; NO 121; PP. 133-143; BIBL. 10 REF.; 12 ILL.; (SUBSIDENCE TERR. COLLOQ. INT. 2. ACTES; ANAHEIM, CALIF.; 1976)Conference Paper

AN INTEGRATED FINITE DIFFERENCE METHOD FOR ANALYZING FLUID FLOW IN POROUS MEDIA.NARASIMHAN TN; WITHERSPOON PA.1976; WAT. RESOURCES RES.; U.S.A.; DA. 1976; VOL. 12; NO 1; PP. 57-64; BIBL. 30 REF.; 10 ILL.Article

AN INTEGRATED FINITE DIFFERENCE METHOD FOR ANALYZING FLUID FLOW IN POROUS MEDIA.NARASIMHAN TN; WITHERSPOON PA.sdBERKELEY UNIV. CALIFORNIA,1975, P. 1 A 32Book

THE ROLE OF PORE PRESSURE IN DEFORMATION IN GEOLOGIC PROCESSES = RAPPORT SUR LA CONFERENCE PENROSE: LE ROLE DE LA PRESSION INTERSTITIELLE DANS LA DEFORMATION LORS DE PROCESSUS GEOLOGIQUESNARASIMHAN TN; HOUSTON WN; NUR AM et al.1980; GEOLOGY (BOULDER); ISSN 0091-7613; USA; DA. 1980; VOL. 8; NO 7; PP. 349-351Article

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NUMERICAL MODEL FOR SATURATED-UNSATURATED FLOW IN DEFORMABLE POROUS MEDIA-2. THE ALGORITHM.NARASIMHAN TN; WITHERSPOON PA; EDWARDS AL et al.1978; WAT. RESOURCES RES.; USA; DA. 1978; VOL. 14; NO 2; PP. 255-261; BIBL. 8 REF.; 3 ILL.Article

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