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The effects of soil organic matter on soil water retention and plant water use in a meadow of the Sierra Nevada, CA

机译:内华达山脉草甸的土壤有机质对土壤水分保持和植物水分利用的影响

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摘要

Tuolumne Meadows is a groundwater dependent ecosystem in the Sierra Nevada of California, USA, that is threatened by hydrologic impacts that may lead to a substantial loss of organic matter in the soil. In order to provide a scientific basis for management of this type of ecosystem, this paper quantifies the effect of soil organic content on soil water retention and water use by plants. First, we show a substantial dependence of soil water retention on soil organic content by correlating Van Genuchten soil water retention parameters with soil organic content, independent of soil texture. Then, we demonstrate the impact of organic content on plants by simulating the degree to which root water uptake is affected by soil water retention with the use of a physically based numerical model of variably saturated groundwater flow. Our results indicate that the increased water retention by soil organic matter contributes as much as 8.8 cm to transpiration, or 35 additional water-stress free days, during the dry summer when plants experience increased water stress.
机译:Tuolumne Meadows是美国加利福尼亚内华达山脉的一个依赖地下水的生态系统,受到水文影响的威胁,这可能导致土壤中有机物的大量流失。为了为管理这种类型的生态系统提供科学依据,本文量化了土壤有机含量对土壤保水量和植物用水的影响。首先,我们通过将Van Genuchten土壤保水参数与土壤有机物含量相关联来显示土壤保水量对土壤有机物的依赖性,而与土壤质地无关。然后,我们使用可变饱和地下水流量的基于物理的数值模型,通过模拟根系水分吸收对土壤水分保持的影响程度,来证明有机含量对植物的影响。我们的结果表明,在干旱的夏季,植物遇到水分胁迫时,土壤有机质增加的保水量对蒸腾作用的贡献最大为8.8 cm,或者另外35天无水分胁迫。

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