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Soil water balance dynamics on reclaimed mine land in the southwestern United States

机译:美国西南部开垦矿区的土壤水平衡动态

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Understanding the dynamics of soil water movement in arid and semi-arid environments is critical to successful reclamation of mined lands. Characteristics of applied topsoil impact soil water processes and long-term ecosystem health. The objective of this study was to better understand the soil water balance at a reclaimed mine in the southwestern United States through the investigation of soil hydraulic properties and subsequent one-dimensional water balance modeling. The study was conducted on a mine reclaimed using geomorphic principles. Complementary field and laboratory techniques were used to describe soil properties. Dry bulk density of topsoil at the mine sites increased with depth, while saturated hydraulic conductivity decreased with increasing bulk density. Two discrete one-dimensional models were created to investigate soil water dynamics and results indicate the importance of appropriately describing soil layering to create more accurate model predictions. In addition, results suggest that matric potentials during the study period were often too low for substantial plant growth. Models similar to those created in this study may be helpful in future assessment of seed germination on reclaimed lands as well as the implications that global climate change may have on reclamation strategies in the future. (C) 2016 Elsevier Ltd. All rights reserved.
机译:了解干旱和半干旱环境中土壤水分运动的动态对于成功开垦雷区至关重要。施用表土的特性会影响土壤水分过程和长期的生态系统健康。这项研究的目的是通过调查土壤水力特性和随后的一维水分平衡模型,更好地了解美国西南部一家再生矿山的土壤水分平衡。该研究是在使用地貌原理回收的矿山上进行的。互补的田间和实验室技术用于描述土壤特性。矿区表土的干堆积密度随深度增加,而饱和水力传导率随堆积密度的增加而减小。创建了两个离散的一维模型来调查土壤水分动力学,结果表明了适当描述土壤分层以创建更准确的模型预测的重要性。此外,结果表明,在研究期间基质潜能通常对于植物的大量生长而言过低。与该研究中创建的模型相似的模型可能有助于将来评估开垦土地上的种子发芽,以及未来全球气候变化可能对开垦策略产生的影响。 (C)2016 Elsevier Ltd.保留所有权利。

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