植被建设对黄土高原土壤水分的影响
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国家自然科学基金资助项目(41771558)


The effects of vegetation construction on soil moisture in the Loess Plateau of China
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    摘要:

    为明确自退耕还林以来,黄土高原地区不同植被建设对土壤水分的影响。以Web of Science核心合集中黄土高原土壤水分研究的相关文献为对象,通过CiteSpace生成文献中的关键词并绘制关键词聚类图谱,分析植被建设对黄土高原水分的研究热点及前沿;同时以植被建设对黄土高原土壤水分影响的文献为基础,通过Meta分析量化了不同条件下(海拔,降雨、坡度等)植被建设对黄土高原土壤水分的影响程度。分析Web of Science核心合集中黄土高原土壤水分相关文献共232篇,结果显示近20 a黄土高原土壤水分研究主要包括4个方面的内容:(1)植被建设引起的土壤水分下降问题,(2)土壤水分时空变异特征,(3)土壤水分时空变异的影响因素,(4)遥感和水文模型模拟土壤水分四个方面。同时使用Meta分析了已发表的黄土高原植被建设对土壤水分影响文章103篇,结果表明:黄土高原植被建设大量消耗该区域土壤水分,乔木、灌木及草本植物对土壤水分的结合效应值(ES)依次为-1.893、-1.661、-1.239。植被建设对土壤水分的影响程度随年均降雨量的增大而减小,不同降雨区间的ES值为-0.864(≥500 mm)、-1.423(400-500 mm)、-1.534(<400 mm);在不同海拔区间,植被建设对土壤水分的消耗程度随海拔高度的增加而增加;在3个坡度范围,植被建设对土壤水分消耗程度以<15°最大,>25°次之,15-25°最小。总体而言,植被建设对土壤水分的消耗随着生长年限的增长而加剧,而灌木植被中柠条出现差异,其不同生长年限的效应值为-1.983(>30 a),-1.642(<20 a),-1.107(20-30 a)。由于黄土高原处于干旱与半干旱地区,大面积植被恢复加剧土壤水分消耗,影响到植被生长及其功能的可持续性。因此,应选择适宜植被并给予适当管理(修枝、稀植等措施)以提高土壤水分利用效率,使该地区土壤水分状况得到改善。

    Abstract:

    This study aims to analyze the impacts of vegetation construction on the soil moisture on the Chinese Loess Plateau. Using the CiteSpace software to associate literature of soil moisture on the Loess Plateau, the research hotspots and frontiers of vegetation construction on soil moisture were evaluated. Keywords of the relevant literature were examined and the cluster maps were formed. Meanwhile, through Meta-analysis, the effect degree of vegetation construction on soil moisture was measured by using the literature of vegetation construction on soil moisture. A total of 232 publications of soil moisture on the Loess Plateau were analyzed from the Web of Science core collection for this study. The results showed that soil moisture research on the Loess Plateau was focused on four aspects in the last 20 years: 1) soil moisture reduction due to vegetation construction; 2) spatiotemporal variations of soil moisture on the Loess Plateau; 3) influence factors of spatiotemporal variations in soil moisture; and 4) soil moisture simulation using remote sensing and hydrology models. Additionally, this article collected and analyzed 103 published studies on the effect of vegetation construction on soil moisture on the Loess Plateau by Meta-analysis. Results showed that vegetation construction increased soil moisture consumption on the Loess Plateau. Forest, shrub, and grass cumulative effect size (ES) on soil moisture were -1.893, -1.661, and -1.239, respectively. With decreasing precipitation, the effect of vegetation construction on soil moisture increased; the ES for ≥500 mm, 400—500 mm, and < 400 mm were -0.864, -1.423, and -1.534, respectively. With the increasing elevation in different elevation parts, the consumption of vegetation construction on soil moisture increased. The consumption of vegetation construction on soil moisture was <15o, >25o, and 15—25o, respectively, in the order of high to low. In general, as the growing year progress, consumption enhances the vegetation"s reliance on soil moisture. While the caragana was different, the ES of growth years >30 a, <20 a, and 20—30 a were -1.983, -1.642, and -1.107, respectively. Because the Loess Plateau is located in arid and semi-arid regions, the wide area of vegetation construction increases soil moisture consumption, affecting vegetation development and function sustainability. As a result, appropriate vegetation should be adopted and properly managed (i.e., trimming, sparse planting) to increase soil moisture use efficiency and promote the sustainability of region"s soil moisture.

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丁文斌,王飞.植被建设对黄土高原土壤水分的影响.生态学报,2022,42(13):5531~5542

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