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A Review Of Model Applications For Structured Soils: A) Water Flow And Tracer Transport

机译:结构性土壤模型应用的综述:A)水流和示踪剂运输

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Although it has many positive effects, soil structure may adversely affect the filtering function of the vadose zone that protects natural water resources from various sources of pollution. Physically based models have been developed to analyze the impacts of preferential water flow (PF) and physical non-equilibrium (PNE) solute transport on soil and water resources. This review compiles results published over the past decade on the application of such models for simulating PF and PNE non-reactive tracer transport for scales ranging from the soil column to the catchment area. Recent progress has been made in characterizing the hydraulically relevant soil structures, dynamic flow conditions, inverse parameter and uncertainty estimations, independent model parameterizations, stochastic descriptions of soil heterogeneity, and 2D or 3D extensions of PNE models. Two-region models are most widely used across all scales; as a stand-alone approach to be used up to the field scale, or as a component of distributed, larger scale models. Studies at all scales suggest that inverse identification of parameters related to PF is generally not possible based on a hydrograph alone. Information on flux-averaged and spatially distributed local resident concentrations is jointly required for quantifying PNE transport. At the column and soil profile scale, model predictions of PF are becoming increasingly realistic through the implementation of the 3D soil structure as derived from hydrogeophysical and tracer techniques. At the field scale, integrating effects of the soil structure and its spatial variability has been attempted by combining ID PNE approaches with stochastic parameter sampling. At the catchment area scale, the scarcity of data makes validation of PF related model components a task yet to be accomplished. The quest for easily measurable proxy variables, as 'the missing link' between soil structure and model parameters, continues in order to improve the practical predictive capability of PF-PNE models. A follow-up paper complementing this manuscript reviews model applications involving non-equilibrium transport of pesticides, as representatives of reactive solutes.
机译:尽管它具有许多积极作用,但土壤结构可能会对渗流带的过滤功能产生不利影响,渗流带保护天然水资源免受各种污染源的侵害。已经开发了基于物理的模型来分析优先水流(PF)和物理非平衡(PNE)溶质运移对土壤和水资源的影响。这篇综述汇编了过去十年发表的关于使用这种模型模拟PF和PNE非反应性示踪剂传输的结果的结果,其范围从土壤柱到集水区。在表征与水相关的土壤结构,动态流动条件,反参数和不确定性估计,独立模型参数化,土壤异质性的随机描述以及PNE模型的2D或3D扩展方面已取得了最新进展。两区域模型在所有规模上使用最广泛。作为可用于现场规模的独立方法,或作为分布式较大规模模型的组成部分。各种规模的研究表明,仅基于水位图通常不可能对与PF有关的参数进行逆识别。共同需要有关通量平均和空间分布的本地居民浓度的信息,以量化PNE运移。在柱和土壤剖面尺度上,通过实施从水文地球物理和示踪技术获得的3D土壤结构,PF的模型预测变得越来越现实。在田间尺度上,已经尝试通过将ID PNE方法与随机参数采样相结合来综合考虑土壤结构及其空间变异性的影响。在集水区范围内,数据的稀缺性使得与PF相关的模型组件的验证成为一项尚未完成的任务。为了提高PF-PNE模型的实际预测能力,人们一直在寻求易于测量的代理变量,作为土壤结构与模型参数之间的“缺失环节”。补充该手稿的后续论文回顾了涉及农药非平衡转运(作为反应性溶质的代表)的模型应用。

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