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Predicting Soil Infiltration and Horizon Thickness for a Large-Scale Water Balance Model in an Arid Environment

机译:干旱环境下大型水量平衡模型的土壤入渗和地层厚度预测

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Prediction of soil characteristics over large areas is desirable for environmental modeling. In arid environments, soil characteristics often show strong ecological connectivity with natural vegetation, specifically biomass and/or canopy cover, suggesting that the soil characteristics may be predicted from vegetation data. The objective of this study was to predict soil infiltration characteristics and horizon (soil layer) thickness using vegetation data for a large-scale water balance model in an arid region. Double-ring infiltrometer tests (at 23 sites), horizon thickness measurements (58 sites) and vegetation surveys (35 sites) were conducted in a 30 km × 50 km area in Western Australia during 1999 to 2003. The relationships between soil parameters and vegetation data were evaluated quantitatively by simple linear regression. The parameters for initial-term infiltration had strong and positive correlations with biomass and canopy coverage ( R 2 = 0.64 ? 0.81). The horizon thickness also had strong positive correlations with vegetation properties ( R 2 = 0.53 ? 0.67). These results suggest that the soil infiltration parameters and horizon thickness can be spatially predicted by properties of vegetation using their linear regression based equations and vegetation maps. The background and reasons of the strong ecological connectivity between soil and vegetation in this region were also considered.
机译:对于环境建模,需要对大面积土壤特性进行预测。在干旱环境中,土壤特征通常表现出与天然植被(特别是生物量和/或冠层覆盖物)的强生态连通性,这表明可以从植被数据中预测土壤特征。这项研究的目的是使用干旱地区大型水平衡模型的植被数据预测土壤的入渗特性和地层(土壤层)厚度。 1999年至2003年,在澳大利亚西部的30 km×50 km地区进行了双环渗透仪测试(在23个地点),水平厚度测量(58个地点)和植被调查(35个地点)。土壤参数与植被之间的关系数据通过简单的线性回归进行定量评估。初期入渗参数与生物量和冠层覆盖度呈强正相关(R 2 = 0.64?0.81)。地层厚度也与植被性质有很强的正相关(R 2 = 0.53?0.67)。这些结果表明,土壤的入渗参数和地层厚度可以通过使用基于线性回归方程和植被图的植被特性在空间上进行预测。还考虑了该地区土壤与植被之间强大的生态联系的背景和原因。

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