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Delineation of hydrologically similar units in a watershed based on fuzzy classification of soil hydraulic properties

机译:基于土壤水力特性模糊分类的流域水文相似单元划分

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Evaluation of flow and transport processes in a watershed-scale requires that the watershed be divided into homogenousnspatial units referred to as hydrologically similar units (HSUs). Although a few discretization schemes are already in use,na universally acceptable method of obtaining HSUs is yet to emerge. In this study, we developed a fuzzy inference systemn(FIS) to classify the saturated hydraulic conductivity (Ks) and two water-retention parameters ˛ and n into fuzzy logic-basednsoil hydrologic classes (FSHCs). Analysis of these classes showed that soil properties within an FSHC have less variabilitynand those between two FSHCs have large variability. This result suggested that soils belonging to a specific FSHC may benmore similar than those across different FSHCs and may be grouped together to represent an HSU. Soils within a specificnhydrologic class were aggregated to delineate HSUs within the watershed. For the Dengei Pahad micro-watershed (DPW), thisnapproach showed five distinct regions representing a discretized zone having similar soil hydraulic properties. Application ofnthis approach on a larger international database of soil hydraulic properties revealed that the developed hydrologic classes arenquite comparable across different databases. The delineated HSUs based on these FSHCs were also better than the soil seriesnmap of the watershed in maintaining the soil heterogeneity of the watershed. Moreover, this new discretization scheme usingnthe SWAT modelling environment showed better performance than the soil series-based discretization approach. Copyright n2010 John Wiley & Sons, Ltd.
机译:在分水岭规模的流量和运输过程的评估中,要求将分水岭划分为同质的空间单位,称为水文相似单位(HSU)。尽管已经使用了一些离散化方案,但尚未出现一种普遍接受的获取HSU的方法。在这项研究中,我们开发了一种模糊推理系统n(FIS)将饱和导水率(Ks)和两个保水参数˛和n分为基于模糊逻辑的土壤水文分类(FSHCs)。对这些类别的分析表明,FSHC内的土壤性质变异性较小,而两个FSHC之间的土壤性质变异性较大。该结果表明,属于特定FSHC的土壤可能比不同FSHC的土壤更相似,并且可以组合在一起代表HSU。将特定水文学类别内的土壤聚集起来,以描绘流域内的HSU。对于Dengei Pahad微流域(DPW),该方法显示了五个不同的区域,代表了具有相似土壤水力特性的离散带。这种方法在更大的国际土壤水力学数据库中的应用表明,在不同的数据库中,已开发的水文分类是相当的。在保持流域土壤异质性的基础上,基于这些FSHCs划定的HSU也优于流域土壤序列图。而且,这种新的在SWAT建模环境下的离散化方案表现出比基于土壤系列的离散化方法更好的性能。版权所有©n2010 John Wiley&Sons,Ltd.

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