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Soil moisture prediction of bare soil profiles using diffuse spectral reflectance information and vadose zone flow modeling

机译:利用漫反射光谱信息和渗流区流模拟预测裸土剖面的土壤水分

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Soil hydraulic property information of the vadose zone is key to quantifying the temporal and spatial variability of soil moisture, and for modeling water flow and contaminant transport processes in the near surface. This study deals with exploring the feasibility of using diffuse soil spectral information in the visible, near-infrared and shortwave infrared range (350-2500 nm) to estimate coarse-scale soil hydraulic parameters and predict soil moisture profiles using a topography-based aggregation scheme in conjunction with a 1D mechanistic water flow model. Three different types of parametric transfer functions (so-called spectrotransfer functions, STFs; pedotransfer functions, PTFs; and spectral pedotransfer functions, SPTF5) were aggregated from the point scale to 1 km(2) pixel size. to provide coarse scale estimates of van Genuchten-Mualem (VGM) hydraulic parameters. The coarse scale hydraulic parameters were evaluated by simulating soil water dynamics of the 1 km(2) pixels across the Zanjanrood River sub-watershed (ZRS) in northwest Iran. Resultant soil water states were compared with ground-truth measurements and advanced synthetic aperture radar (ASAR) estimates of soil water content. The topography-based aggregation scheme was found to provide effective values of the VGM hydraulic parameters across the ZRS study site. The coarse scale STFs performed best in terms of simulating surface, near-surface and subsurface soil water dynamics, followed by the coarse scale SPTFs and PM, which performed similarly. The average simulated soil water contents of the surface layer closely correlated with ASAR estimates during relatively wet periods. Simulated subsurface soil water dynamics matched well with the ground-truth measurements. These findings indicate the feasibility of using spectral data to predict VGM hydraulic parameters and, ultimately, to predict soil water dynamics at the larger scales. (C) 2016 Elsevier Inc. All rights reserved.
机译:渗流带的土壤水力特性信息对于量化土壤水分的时空变化以及为近地表水流和污染物输送过程建模提供了关键。这项研究探讨了使用可见,近红外和短波红外范围(350-2500 nm)中的弥散性土壤光谱信息来估计粗尺度土壤水力参数和使用基于地形的聚集方案来预测土壤水分剖面的可行性。结合一维机械水流模型。从点规模到1 km(2)像素大小,聚合了三种不同类型的参数传递函数(所谓的光谱传递函数,STF; pedotransfer函数,PTF;和光谱pedotransfer函数,SPTF5)。提供van Genuchten-Mualem(VGM)水力参数的粗略估计。通过模拟伊朗西北部Zanjanrood河子流域(ZRS)上1 km(2)像素的土壤水动力学来评估粗尺度水力参数。将所得的土壤水分状态与地面测量值和先进的合成孔径雷达(ASAR)估算的土壤水分含量进行了比较。发现基于地形的聚集方案可在整个ZRS研究现场提供VGM水力参数的有效值。在模拟地表水,近地表水和地下土壤水动力学方面,粗尺度STF表现最佳,其次是表现相似的粗尺度SPTF和PM。在相对潮湿的时期,表层平均模拟土壤含水量与ASAR估计值密切相关。模拟的地下土壤水动力学与地面实测值非常吻合。这些发现表明使用光谱数据预测VGM水力参数,并最终预测较大规模土壤水动力学的可行性。 (C)2016 Elsevier Inc.保留所有权利。

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