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THE RELATION BETWEEN LITHOLOGICAL PROPERTIES AND THE SHAPE OF THE DESCRIPTION CURVE.VISSER WC.1968; PUBL.ASSOC.INTERN.HYDROL.SCI.; 1968, VOL. 1, NUM. 0082, P. 305 A 310Miscellaneous

THE MODEL OF THE WATER BALANCE AND NUTRIENT UPTAKE AS A BASIS FOR HYDROLOGICAL, AGRO-HYDROGICAL AND OTHER PROJECTS.VISSER WC.sdASS. INTERNATION. SCI. HYDROL., PUBL.; U.S.A.; (MODELS MATH. HYDROL. SYMP. II; WARSAW; 1971),1974, NUM. 0101, P. 580 A 597Miscellaneous

THE AIM OF MODERN HYDROLOGY.VISSER WC.1970; INST. LAND WAT. MANAG. RES., TECH. BULL.; NLD; 1970, NUM. 0090, P. 15 A 43Serial Issue

UNSATURATED SOIL MOISTURE CONDITIONS STUDIED FROM FIELD OBSERVATIONS.VISSER WC.1969; INST.LAND.WATER.MANAG.RES.-MISCEL.REPRINTS-NEDERL; NLD; 1969, NUM. 0086, P. 952 A 966Miscellaneous

AN EMPIRICAL EXPRESSION FOR THE DESORPTION CURVE.VISSER WC.1969; INST.LAND.WATER.MANAG.RES.-MISCEL.REPRINTS-NEDERL; NLD; 1969, NUM. 0083, P. 329 A 335Miscellaneous

THE RELATION BETWEEN LITHOLOGICAL PROPERTIES AND THE SHAPE OF THE DESCRIPTION CURVE.VISSER WC.1968; PUBL.ASSOC.INTERN.HYDROL.SCI.; 1968, VOL. 1, NUM. 0082, P. 305 A 310Miscellaneous

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