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Results 1 to 25 of 83

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MODELS OF GROUNDWATER FLOW IN STATISTICALLY HOMOGENEOUS POROUS FORMATIONSDAGAN G.1979; WAT. RESOURCES RES.; USA; DA. 1979; VOL. 15; NO 1; PP. 47-63; BIBL. 13 REF.; 7 ILL.Article

THE GENERALIZATION OF DARCY'S LAW FOR NONUNIFORM FLOWSDAGAN G.1979; WAT. RESOURCES RES.; USA; DA. 1979; VOL. 15; NO 1; PP. 1-7; BIBL. 12 REF.Article

A NOTE ON PACKER, SLUG, AND RECOVERY TESTS IN UNCONFINED AQUIFERSDAGAN G.1978; WAT. RESOURCES RES.; USA; DA. 1978; VOL. 14; NO 5; PP. 929-934; BIBL. 4 REF.; 3 ILL.Article

ANALYSIS OF FLOW THROUGH HETEROGENEOUS RANDOM AQUIFERS; 2, UNSTEADY FLOW IN CONFINED FORMATIONS = ANALYSE DE L'ECOULEMENT A TRAVERS DES NAPPES IRREGULIERES HETEROGENES; 2, REGIME TRANSITOIRE DANS DES FORMATIONS CAPTIVESDAGAN G.1982; WATER. RESOUR. RES.; ISSN 0043-1397; USA; DA. 1982-10; VOL. 18; NO 5; PP. 1571-1585; BIBL. 17 REF.; ILL.Article

A DERIVATION OF DUPUIT SOLUTION OF STEADY FLOW TOWARD WELLS BY MATCHED ASYMPTOTIC EXPANSIONS.DAGAN G.1968; WAT. RESOURCES RES.; USA; 1968(4), VOL. 4, NUM. 0002, P. 403 A 412Miscellaneous

TAYLOR INSTABILITY OF A NON-UNIFORM FREE-SURFACE FLOW.DAGAN G.1975; J. FLUID MECH.; G.B.; DA. 1975; VOL. 67; NO 1; PP. 113-123; BIBL. 13 REF.Article

WAVES AND WAVE RESITANCE OF THIN BODIES MOVING AT LOW SPEED.: THE FREE-SURFACE NON LINEAR EFFECT.DAGAN G.1975; J. FLUID MECH.; G.B.; DA. 1975; VOL. 69; NO 2; PP. 405-416; BIBL. 13 REF.Article

A METHOD OF COMPUTING NONLINEAR WAVE RESISTANCE OF THIN SHIPS BY COORDINATE STRAINING.DAGAN G.1975; J. SHIP RES.; U.S.A.; DA. 1975; VOL. 19; NO 3; PP. 149-154; BIBL. 14 REF.Article

Natural sciences versus engineering sciences: The case of hydrology and the role of the stochastic approachDAGAN, G.Stockholm water symposium. 1998, pp 25-33, isbn 91-971929-9-6Conference Paper

Stochastic modelling of solute transport by groundwater flow: state of the art = Elaboration de modèle stochastique pour l'étude du transport de soluté par l'écoulement de l'eau souterraineDAGAN, G.IAHS-AISH publication. 1985, Num 146, pp 91-101, issn 0144-7815Conference Paper

STABILITY OF DISPLACEMENT OF A COLD FLUID BY A HOT FLUID IN A POROUS MEDIUMBACHU S; DAGAN G.1979; PHYS. OF FLUIDS; USA; DA. 1979; VOL. 22; NO 1; PP. 54-59; BIBL. 6 REF.Article

Theory of solute transport by groundwater = Théorie du transport de soluté par l'eau souterraineDAGAN, G.Annual review of fluid mechanics. 1987, Vol 19, pp 183-215, issn 0066-4189Article

WELL PUMPING IN UNCONFINED AQUIFERS: THE INFLUENCE OF THE UNSATURATED ZONE.KROSZYNSKI UI; DAGAN G.1975; WAT. RESOURCES RES.; U.S.A.; 1975, VOL. 11, NUM. 0003, P. 479 A 490Serial Issue

A few aspects of stochastic modeling of groundwater contamination due to a nuclear power plant accidentDAGAN, G.Hydrological considerations in relation to nuclear power plants. 1993, pp 122-130Conference Paper

PARTIAL REFLEXION OF WATER WAVES BY NON-UNIFORM ADVERSE CURRENTSSTIASSNIE M; DAGAN G.1979; J. FLUID MECH.; GBR; DA. 1979; VOL. 92; NO 1; PP. 119-129; BIBL. 7 REF.Article

COMMENT ON "A STOCHASTIC-CONCEPTUAL ANALYSIS OF ONE-DIMENSIONAL GROUNDWATER FLOW IN NONUNIFORM HOMOGENEOUS MEDIA".DAGAN G; FREEZE RA.1976; WAT. RESOURCES RES.; U.S.A.; DA. 1976; VOL. 12; NO 3; PP. 567-568; BIBL. 2 REF.Article

NONLINEAR SHIP-WAVE THEORIES BY CONTINUOUS MAPPING. = THEORIES NON LINEAIRES DE L'ONDE DE BATEAU BASEES SUR LA TRANSFORMATION CONFORME CONTINUENOBLESSE F; DAGAN G.1976; J. FLUID MECH.; G.B.; DA. 1976; VOL. 75; NO 2; PP. 347-371; BIBL. 22 REF.Article

CONVECTIVE CURRENTS IN A POROUS LAYER HEATED FROM BELOW: THE INFLUENCE OF HYDRODYNAMIC DISPERSION. = COURANTS DE CONVECTION DANS UNE COUCHE POREUSE CHAUFFEE PAR-DESSOUS: INFLUENCE DE LA DISPERSION HYDRODYNAMIQUENEISCHLOSS H; DAGAN G.1975; PHYS. OF FLUIDS; U.S.A.; DA. 1975; VOL. 18; NO 7; PP. 757-761; BIBL. 13 REF.Article

A DEPENDENT DOMAIN MODEL OF CAPILLARY HYSTERESIS.MUALEM Y; DAGAN G.1975; WAT. RESOURCES RES.; U.S.A.; 1975, VOL. 11, NUM. 0003, P. 452 A 460Serial Issue

Higher-order correction of effective permeability of heterogeneous isotropic formations of lognormal conductivity distributionDAGAN, G.Transport in porous media. 1993, Vol 12, Num 3, pp 279-290, issn 0169-3913Article

Stochastic modeling of groundwater flow by unconditional and conditional probabilities. 2. The solute transportDAGAN, G.Water resources research Washington. 1982, Vol 18, Num 4, pp 835-848Article

SOLUTE DISPERSION IN UNSATURATED HETEROGENEOUS SOIL AT FIELD SCALE. I: THEORY SOLUTE DISPERSION IN UNSATURATED HETEROGENEOUS SOIL AT FIELD SCALE. II: APPLICATIONSDAGAN G; BRESLER E.1979; SOIL. SCI. SOC. AMER. J.; USA; DA. 1979; VOL. 43; NO 3; PP. 461-472; BIBL. 24 REF.; 8 ILL.Article

HYDRAULIC CONDUCTIVITY OF SOILS: UNIFIED APPROACH TO THE STATISTICAL MODELSMUALEM Y; DAGAN G.1978; SOIL SCI. SOC. AMER. J.; USA; DA. 1978; VOL. 42; NO 3; PP. 392-395; BIBL. 12 REF.Article

SOLUTIONS OF HYDRODYNAMIC DISPERSION IN POROUS MEDIAELDOR M; DAGAN G.1972; WAT. RESOURCES RES.; U.S.A. ; 1972, VOL. 8, NUM. 0005, P. 1316 A 1331Serial Issue

Upscaling of dispersion coefficients in transport through heterogeneous formationsDAGAN, G.International conference on computational methods in water resources. 1994, pp 431-439Conference Paper

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