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

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

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

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

Transport by two-dimensional random velocity fields : Effective dispersion coefficients of a finite plumeDAGAN, G.International conference on stochastic and statistical methods in hydrology end environmental engineering. 1994, pp 113-126Conference Paper

Statistical theory of groundwater flow: pore- to laboratory, laboratory- to formation and formation- to regional-scale = La théorie statistique de l'écoulement souterrain de l'échelle du pore à celle du laboratoire, de celle-ci à celle de la formation et de cette dernière à l'échelle régionaleDAGAN, G.L'approche stochastique des écoulements souterrains. Symposium. 1985, pp 1-32Conference Paper

Solute transport in heterogeneous porous formationsDAGAN, G.Journal of Fluid Mechanics. 1984, Vol 145, pp 151-177, issn 0022-1120Article

FREE-SURFACE FLOW PAST OSCILLATING SINGULARITIES AT RESONANT FREQUENCYDAGAN G; MILOH T.1982; J. FLUID MECH.; ISSN 0022-1120; GBR; DA. 1982; VOL. 120; PP. 139-154; BIBL. 15 REF.Article

Stochastic modeling of groundwater flow by unconditional and conditional probabilities. 1. Conditional simulation and the direct problemDAGAN, G.Water resources research Washington. 1982, Vol 18, Num 4, pp 813-833Article

COMPARISON OF NONLINEAR WAVE-RESISTANCE THEORIES FOR A TWO-DIMENSIONAL PRESSURE DISTRIBUTIONDOCTORS LJ; DAGAN G.1980; J. FLUID MECH.; GBR; DA. 1980; VOL. 98; NO 3; PP. 647-672; BIBL. 19 REF.Article

Dispersion of a passive solute in non-ergodic transport by steady velocity fields in heterogeneous formationsDAGAN, G.Journal of Fluid Mechanics. 1991, Vol 233, pp 197-210, issn 0022-1120Article

THEORETICAL HEAD VARIOGRAMS FOR STEADY FLOW IN STATISTICALLY HOMOGENEOUS AQUIFERS = THEORIE DES VARIABLES REGIONALISEES APPLIQUEES A L'ETUDE STATISTIQUE DE L'ECOULEMENT PERMANENT D'AQUIFERES HOMOGENESCHIRLIN GR; DAGAN G.1980; WATER RESOUR. RES.; ISSN 0043-1397; USA; DA. 1980; VOL. 16; NO 6; PP. 1001-1015; BIBL. 22 REF.; 1 TAB. ; ILL./TABL.Article

SOLUTIONS OF HYDRODYNAMIC DISPERSION IN POROUS MEDIAELDOR M; DAGAN G.1972; WAT. RESOURCES RES.; U.S.A.; DA. 1972; VOL. 8; NO 5; PP. 1316-1331; BIBL. 13 REF.; 9 ILL.Serial Issue

STATISTICAL ANALYSIS OF CROP YIELD UNDER CONTROLLED LINE SOURCE IRRIGATIONBRESLER E; DAGAN G; HANKS RJ et al.1982; SOIL SCI. SOC. AM. J.; USA; DA. 1982; VOL. 46; NO 4; PP. 841-847; BIBL. 9 REF.Article

Upscaling of conductivity of heterogeneous formations: general approach and application to isotropic mediaINDELMAN, P; DAGAN, G.Transport in porous media. 1993, Vol 12, Num 2, pp 161-183, issn 0169-3913Article

A study of nonlinear wave resistance using integral equations in Fourier spaceMILOH, T; DAGAN, G.Journal of Fluid Mechanics. 1985, Vol 159, pp 433-458, issn 0022-1120Article