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Unsaturated zone modelling: the role of soil database classification

机译:非饱和带建模:土壤数据库分类的作用

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Physical and hydraulic soil properties are essential input parameters for models from different sciences (e.g. hydrology, agriculture, water management, nature preservation). Generally texture composition, porosity and other easily measurable physical properties of soils are known. However, saturated hydraulic conductivity and characteristic values of the water retention curve are usually missing information. Therefore, based on the physical similarity of soils (classes), they are substituted by data derived from soil databases. The aim of this study was to assess the currently unknown uncertainties of such classified databases. To do so, a large variety of tests were carried out: (ⅰ) static and dynamic, (ⅱ) 1D and 3D (ⅲ) hydraulic and hydrologic applied tests, (ⅳ) real and synthetic soils, parameterized accordingly, and (ⅴ) HUNSODA and/or HYPRES databases. The results were sorted with respect to FAO and USDA classification systems. Soil class overlapping was evaluated through the statistics of basic hydraulic parameters (retention curve, hydraulic conductivity). Indicators related to hydrologic extremities (excess water and drought) were used to quantify the uncertainties of soil texture based on parameter substitution. It was concluded that the two evaluated soil classification systems did not sort soils reliably from the hydrologic and hydraulic viewpoint: the test results of classes showed major overlaps. Moreover, in most cases class synthetic parameter combinations poorly represented real soils. As a general consequence the results based on classified soil databases should be accepted only with reservation.
机译:物理和水力土壤特性是来自不同科学(例如水文学,农业,水管理,自然保护)的模型的基本输入参数。通常,土壤的质地组成,孔隙率和其他易于测量的物理性质是已知的。但是,饱和的水力传导率和保水曲线的特征值通常缺少信息。因此,根据土壤(类)的物理相似性,它们被土壤数据库中的数据替代。这项研究的目的是评估此类机密数据库目前未知的不确定性。为此,进行了大量测试:(ⅰ)静态和动态,(ⅱ)一维和3D(ⅲ)水力和水文应用测试,(ⅳ)相应地参数化的真实和合成土壤,以及(ⅴ) HUNSODA和/或HYPRES数据库。根据粮农组织和美国农业部分类系统对结果进行了分类。通过基本水力参数(保持曲线,水力传导率)的统计数据评估土壤类别的重叠。与水文极端有关的指标(过量的水和干旱)被用来量化基于参数替换的土壤质地的不确定性。结论是,从水文和水力的角度来看,这两个评估的土壤分类系统不能可靠地对土壤进行分类:分类的测试结果显示出重大的重叠。而且,在大多数情况下,类综合参数组合很难代表真实的土壤。一般而言,基于分类的土壤数据库的结果应仅在保留的情况下接受。

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