Titlebook: Unsaturated Flow in Hydrologic Modeling; Theory and Practice H. J. Morel-Seytoux Book 1989 Kluwer Academic Publishers 1989 Drainage.Filtrat

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Prediction of Water Table Mound Development and Aquifer Recharge from an Infiltrating Areawith the underlying water-table aquifer. Due to the frequent presence of a clogged layer the water flow below the infiltration zone is often unsaturated. Recharge occurs only after the unsaturated wetting front reaches the water-table. On the other hand, long after infiltration has ceased at the soi

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Remote Sensing of Watershed Characteristics and Rainfall Inpute and time. Conventional point measurements are not very suitable for this purpose, while various remote sensing (RS) techniques are of great advantage in many cases. After a brief discussion of RS platforms and sensors relevant for hydrological applications, techniques are discussed which can estim

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Mortal

Comparative Evaluation of Unsaturated Flow Methods in Selected USDA Simulation ModelsAgricultural Research Service (ARS). Four of these models are compared to illustrate strengths and weaknesses of the numerical features of each. Three numerical solutions for Richards’ equation and two conceptual linked-storage models are compared using a corn growth season example from a small catc

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The Unsaturated Components of Swatch: A Multiprocess Watershed Model for Runoff Generation and Routi has the ability to generate flow as overland runoff, interflow and base flow. Two examples of application are provided for one watershed in Portugal and one in the state of Georgia. In both cases verification of the model is quite satisfactory. The ability to predict the recovery in infiltration ca

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Book 1989eling" held at "Les Villages du Soleil" near ArIes, France from June 13 to 17, 1988. Let me therefore acknowledge properly, at the very beginning, the gratitude of all the participants to the NATO Science Committee for its generous support and worthwhile goal of bringing together scientists of many

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Multiphase Flow in Porous Media: Description at the Pore and Macroscopic Scaleiquid by another is studied experimentally and numerically in a model porous medium composed of rod cylinders. The mathematical model of multiphase continua is derived at the macroscopic scale of a porous medium, by using averaging procedures. Present applications in subsurface hydrology and needed developments are discussed.

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