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首页> 外文期刊>Forests >Groundwater Depth and Soil Properties Are Associated with Variation in Vegetation of a Desert Riparian Ecosystem in an Arid Area of China
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Groundwater Depth and Soil Properties Are Associated with Variation in Vegetation of a Desert Riparian Ecosystem in an Arid Area of China

机译:干旱区荒漠河岸生态系统植被变化与地下水深度和土壤特性的关系

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Groundwater is a major driving force for plant community distribution in arid areas worldwide. Although it is well known that groundwater has a significant impact on soil and vegetation, there is little information on how groundwater depth affects soil and vegetation in an arid inland basin desert riparian ecosystem. Therefore, quantitative analysis of the relationships among groundwater depth, soil properties and plant community distribution is necessary. A desert riparian ecosystem in the lower reaches of the Heihe River in an arid area of Northwest China was used to determine quantitative relationships among groundwater depth, soil and vegetation. Groundwater depth significantly increased with increased distance from the river. Soil and vegetation characteristics showed a significant trend with increasing groundwater depth. With increasing groundwater depth, soil water content, soil total nitrogen, soil total carbon, soil available phosphorus and soil available potassium decreased, while the soil bulk density and soil carbon:nitrogen (C:N) ratio increased. Soil pH and soil electrical conductivity followed quadratic function relationships with groundwater depth. Species richness, aboveground biomass, community coverage, community height, foliage projective cover and leaf area index all significantly decreased with increased groundwater depth. Groundwater depth and soil were associated with vegetation variance, explaining 85.8% of the vegetation variance. Groundwater depth was more important in explaining vegetation variance than soil properties (soil bulk density) and soil pH. Our observations indicate that changes in groundwater depth would have a significant influence on desert riparian forest vegetation, and that maintaining appropriate groundwater depth is necessary to preserve the riparian ecosystem.
机译:地下水是分布在全球干旱地区植物群落的主要动力。尽管众所周知,地下水对土壤和植被有重大影响,但关于干旱内陆盆地沙漠河岸生态系统中地下水深度如何影响土壤和植被的信息很少。因此,有必要对地下水深度,土壤性质和植物群落分布之间的关系进行定量分析。利用西北干旱地区黑河下游的荒漠河岸生态系统确定了地下水深度,土壤和植被之间的定量关系。随着距河的距离增加,地下水深度显着增加。土壤和植被特征随着地下水深度的增加呈现出明显的趋势。随着地下水深度的增加,土壤含水量,土壤总氮,土壤总碳,土壤有效磷和土壤有效钾减少,而土壤容重和土壤碳氮比增加。土壤pH和电导率与地下水深度呈二次函数关系。物种丰富度,地上生物量,群落覆盖度,群落高度,枝叶射影覆盖和叶面积指数均随着地下水深度的增加而显着降低。地下水深度和土壤与植被变化有关,解释了植被变化的85.8%。在解释植被变化时,地下水深度比土壤性质(土壤容重)和土壤pH值更为重要。我们的观察表明,地下水深度的变化将对沙漠河岸森林植被产生重大影响,并且维持适当的地下水深度对于保护河岸生态系统是必要的。

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