印度卡纳塔克邦Netravati流域土壤物理和水力特性的空间变异评价

B. P. Ganasri, G. Dwarakish
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引用次数: 3

摘要

特定地点管理和精准农业旨在识别和分析土壤特性的可变性。利用分布式水文模型进行径流预测和产沙量估算需要空间分布的土壤数据,特别是饱和水力传导性、含水量和粒度分布。因此,土壤数据成为任何流域管理研究的主要投入之一。本研究旨在分析印度卡纳塔克邦内特拉瓦蒂河流域土壤物理和水力特性的空间变异。采用普通克里格法(OK)、距离逆加权法(IDW)和径向基函数法(RBF)对土壤性质进行空间插值。结果表明,%砂、%粉、%粘土等土壤性质具有较高的变异性,其标准差分别为16.08、13.27和8.82。OK方法对砂、粉、粘土及饱和水力渗流预测是有效的。IDW和RBF方法预测有机质含量和容重的可接受误差分别为1.084%、1.09%和0.05gm/cc、0.04gm/cc。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of spatial variability of soil physical and hydraulic properties in Netravati catchment, Karnataka State, India
Site specific management and precision agriculture seeks to identify and analyze variability in soil properties. Runoff prediction and sediment yield estimation using distributed hydrologic modeling requires spatially distributed soil data especially saturated hydraulic conductivity, water content and particle size distribution. Therefore, soil data becomes one of the major inputs in any watershed management studies. The present study was conducted to analyse spatial variability in soil physical and hydraulic properties in Netravati river basin, Karnataka State, India. The spatial interpolation of soil properties was carried out by using three methods such as Ordinary Kriging (OK), Inverse Distance Weighting (IDW) and Radial Basis Function (RBF). Results indicate that soil properties such as %sand, %silt and %clay are highly variable in nature with standard deviation value of 16.08, 13.27 and 8.82. The OK method is efficient in predicting sand, silt, clay and saturated hydraulic conducted. IDW and RBF methods predicted organic matter content and bulk density with acceptable error of 1.084%, 1.09% and 0.05gm/cc, 0.04gm/cc respectively.
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