Soil hydraulic conductivity and diffesivity were measured with Hot AIR Method, Bruce and Klute Method and One-Step Method. The deviations of each curve were caused by hystericis phenomena. The seepage conditions were studied applying various types of irrigation intensity, irrigation amount and irrigation duration. With trial and error method, the soil hydraulic conductivity and diffusivity were modified. Those values showed good explanation on the various types of irrigation condisions.
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