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首页> 外文期刊>日本砂丘学会誌 >Practical Estimation Method for Soil Hydraulic Properties Based on Observed Data in Short-term Experiments Conducted in a Foreign Field
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Practical Estimation Method for Soil Hydraulic Properties Based on Observed Data in Short-term Experiments Conducted in a Foreign Field

机译:野外短期试验中基于观测数据的土壤水力特性实用估算方法

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This study investigated a practical method to estimate soil hydraulic properties based on observed data in existent experiments conducted in a foreign field for short-term stays. This method involved a series of procedures composed of laboratory and in-situ experiments and the inverse estimation of soil hydraulic parameters as results. The laboratory experiments included a falling-head method for the saturated hydraulic conductivity and a one-step outflow experiment. The in-situ experiment was an irrigation-drainage experiment. The inverse estimation technique combined a one-dimensional numerical solution of the Richards equation with Marquartdt-Levenberg optimization. In this paper, this method was applied to a loess field in a semi-arid region inChina to evaluate its effectiveness. These experiments were conducted using portable apparatuses without external power supplies. The inverse approach to the one-step experiment was performed to determine soil hydraulic parameters. The estimations of cumulative outflow using the identified parameters corresponded to the observations. Based on the results, simulations for the in-situ experiment were conducted under three scenarios that changed the number of parameters determined by the inverse approach.The scenario identifying the twelve parameters successfully determined appropriate soil hydraulic parameters under field conditions. The bulk density observed in the field gave good outlines for selecting the parameters for the inverse approach. A minimum of seven to ten days is needed to obtain the essential information for this method, which is one practical technique to comparatively easily estimate appropriate soil hydraulic properties for foreign fields.
机译:这项研究研究了一种实用的方法,该方法可以根据在国外进行的短期停留的现有实验中的观测数据估算土壤水力特性。该方法涉及一系列程序,包括实验室和原位实验,以及土壤水力参数的反估计。实验室实验包括用于饱和水力传导率的落头法和一步流出实验。原位实验是灌溉排水实验。逆估计技术将Richards方程的一维数值解与Marquartdt-Levenberg最优化结合在一起。本文将该方法应用于中国半干旱地区的黄土田,以评价其有效性。这些实验是使用不带外部电源的便携式设备进行的。进行了单步实验的逆方法以确定土壤水力参数。使用识别出的参数对累计流出量的估计与观测值相对应。根据这些结果,在三种情况下进行了原位实验的模拟,这三种情况改变了通过反演方法确定的参数数量。确定十二种参数的情况成功地确定了田间条件下合适的土壤水力参数。在现场观察到的堆积密度为选择反演方法的参数提供了很好的轮廓。至少需要7到10天才能获得此方法的基本信息,这是一种实用技术,可以比较容易地估算出适合于外地的土壤水力特性。

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