Measurement and Modeling of Infiltration Rate at Campus Area-University of Nusa Putra, Sukabumi

D. T, Iqbal Sadam Mustakim, Eka Nurachman, Lyisa Nurpaidah, Randi Ferdiansah, M. Ammar, Rida I. Sitepu
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Abstract

One important parameter to determine the carrying capacity of a land of a region is the rate of infiltration. The objective of this article is to measure and model the infiltration rate in the area of Nusa Putra University Campus. Measurements are carried out to obtain detailed data about the carrying capacity of land around the Nusa Putra Campus to absorb water into the soil. The method used is to use double ring infiltrometer. The area covered is ± 10 ha. The results show that the rate of vegetation infiltration is larger (11.57 cm/h) than in non-vegetation land (7.47 cm/h). The infiltration rate model on vegetation soil condition was f_(cm/h) = -0.023ln(t)+0.2536 and the infiltration rate model on non-vegetation vegetation condition was f_(cm/h) = -0.072ln(t)+0.4465
校园区域入渗速率的测量与模拟-努沙普特拉大学,苏卡umi
决定一个地区土地承载力的一个重要参数是入渗率。本文的目的是测量和模拟在努沙普特拉大学校园地区的渗透率。进行测量是为了获得努沙普特拉校区周围土地吸收水分到土壤中的承载能力的详细数据。使用的方法是使用双环渗透计。覆盖面积为±10公顷。结果表明:植被入渗速率(11.57 cm/h)大于无植被土地(7.47 cm/h);植被土壤条件下的入渗速率模型为f_(cm/h) = -0.023ln(t)+0.2536,非植被植被条件下的入渗速率模型为f_(cm/h) = -0.072ln(t)+0.4465
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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