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首页> 外文期刊>Journal of Hydrology >Estimating hydraulic properties of rainfall-induced soil surface seats from infiltration experiments and X-ray bulk density measurements
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Estimating hydraulic properties of rainfall-induced soil surface seats from infiltration experiments and X-ray bulk density measurements

机译:通过入渗实验和X射线堆积密度测量估算降雨引起的土壤表层的水力特性

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Soil and surface seat hydraulic properties were determined from simulated rainfall experiments by the inverse method applied to the Richards equation. Measurements used for the estimation include the soil water pressure head versus time at two distances from the soil surface, the transient infiltration rate at the soil surface and the drainage rates at the bottom of the soil profile. Seat properties were evaluated using a model that simulates changes in the seat bulk density with respect to time and space. Uncertainties, correlations and sensitivities of the soil and seat parameters were quantified to evaluate the accuracy of the model estimation and to compare the information content of each measurement type to parameter estimations. It appears that the uncertainties related to three seat parameter estimations, namely the parameter related to the dynamics of seat formation, the modelled seat thickness and the initial bulk density, were larger than 50% of the parameter values, because of the tow sensitivity of the model to them and their multiple correlations. In addition to seat hydraulic parameter estimation, bulk density profiles of the soil surface were measured after the rainfall simulations using the X-ray method. The exponential-decay shape assumed in the soil surface seat model was found to correctly reproduce the measured distribution of bulk density with depth. However, the measurements showed a less developed seat than that suggested by the bulk density profile estimated from rainfall experiments. Finally, bulk density measurements were used as given input parameters of the model. Setting the initial bulk density and its maximal. change over time at the measured values greatly decreased the seat parameter uncertainties. The method proposed could be used to improve the experimental design used to quantify the seat's hydraulic properties using inverse techniques. (c) 2007 Elsevier B.V. All rights reserved.
机译:通过应用Richardson方程的反演方法,通过模拟降雨实验确定了土壤和表层的水力特性。用于估算的度量包括距土壤表面两个距离处的土壤水压头与时间的关系,土壤表面的瞬态渗透率和土壤剖面底部的排水率。使用模拟座椅体积密度随时间和空间变化的模型评估座椅性能。对土壤和座位参数的不确定性,相关性和敏感性进行了量化,以评估模型估计的准确性,并将每种测量类型的信息内容与参数估计进行比较。似乎与三个座椅参数估计有关的不确定性,即与座椅形成动力学有关的参数,建模的座椅厚度和初始堆积密度,由于该座椅的拖曳敏感性大于参数值的50%。对它们及其多个相关性进行建模。除座位水力参数估算外,在降雨模拟后使用X射线方法还测量了土壤表面的堆积密度分布。发现在土壤表层模型中假设的指数衰减形状可以正确地再现所测得的堆积密度随深度的分布。然而,这些测量结果显示出的座位比降雨实验估计的堆积密度分布图所暗示的座位少。最后,堆积密度测量值用作模型的给定输入参数。设置初始堆积密度及其最大值。随时间变化的测量值大大降低了座椅参数的不确定性。所提出的方法可用于改进使用逆向技术量化座椅液压性能的实验设计。 (c)2007 Elsevier B.V.保留所有权利。

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