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Pp. 363-380. in In-Situ Determination of Directional Conductivities of Soil 33 Darcy’s law mostly governs the flow of fluid in a porous medium. For an anisotropic medium, Darcy’s law at a point P in a porous continuum (Bear, 1972) may be expressed as  ∂φ  −  ∂x1  v1   K11 K12 K 13     ∂φ     (1) = v K K K 2 21 22 23  − ∂x     2  v3   K 31 K 32 K 33   ∂φ  −   ∂x3  where v1 , v2 and v3 are the components of Darcy velocity v and φ is the average hydraulic head over a representative elemental volume REV at the point P.

To define water erosion at the study area, monthly and annual rainfall rate values based on long term observations are analysed. 99). 99) (Figure 1). u (model, m/s) u(observation)-u(m odel) 15 10 5 0 0 5 10 15 u(observation, m/s) Figure 1. Linear relation between average wind speed values at Gökçeada (Tuzla, Ugurlu, Çinaralti, National Station) between 1992-1993 and 1997-1998. Modelling of Environmental and Climatic Problems 29 ACKNOWLEDGEMENTS This study has been supported by The Turkish Scientific and Research Council (TÜBİTAK, Project No: TOGTAG- 2846).

II. Precipitation Scenarios. Nuovo Cimento C. 22C. 5. pp. 649 - 661. 1065-9, Trieste, Italy. Skidmore, E. , (1986) Wind Erosion Climatic Erosivity, Climate Change, 9, pp. 195-208. , 873-19, Trieste, Italy. 30 Z. , (2000a) Air, Soil, and Water Quality as Influenced by Wind Erosion and Strategies for Mitigation, AGROENVIRON2000: 2nd. 216-221. , (2000b) Sustainable Agriculture: Actions and Strategies, AGROENVIRON2000: 2nd. International Symposium on New Technologies for Environmental Monitoring and Agro-Applications”, Proceedings (Workshops), Tekirdag, Turkey, pp.

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LNS18 College on Soil Physics

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