地下水位变化对干旱和半干旱采煤区土壤特性和植被反应的影响。

IF 3.2 3区 环境科学与生态学 Q3 ENGINEERING, ENVIRONMENTAL Environmental Geochemistry and Health Pub Date : 2024-09-24 DOI:10.1007/s10653-024-02222-w
Pingshun Wang, Shaogang Dong, Xuchao Zang, Xuedong Yang, Yaxin Ji, Lu Li, Xuemin Han, Fulai Hou
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引用次数: 0

摘要

在干旱和半干旱地区开采煤炭往往会导致许多生态和环境问题,如含水层枯竭、湖泊萎缩、植被退化和地表荒漠化。采煤活动产生的排水是地下水-土壤-植被系统演变的主要驱动力。为探讨地下水位波动对采煤区土壤性质的影响及地表植被的响应机制,本研究以博江海子盆地水文地质和生态植被调查为基础,在不同地下水位区域采集土壤和植被样品,借助数值统计、线性回归、相关分析等方法,利用Origin软件对土壤和植被指标进行分析。结果表明,地下水位(GWT)与土壤含水量(SWC)、土壤电导率、土壤有机质(SOM)、土壤可利用氮(SAN)和土壤可利用钾(SAK)之间存在明显的负相关。采矿活动破坏了土壤结构,大大降低了土壤的保水保肥能力。采矿区的 SWC、SOM 和 SAN 含量明显降低,比采矿区周围至少低 49.73%、47.56% 和 59.90%。在湖泊南北两侧,地下水位深度为 7 米的湖滨地带土壤盐碱化严重,地表植被只能依靠有限的大气降水提供水分。当地下水埋深大于 7 米时,地表植被只能依靠有限的大气降水提供水分,耐旱植物主要生长在这些区域。该研究不仅为世界同类矿区的可持续发展和环境保护提供了科学依据,而且对指导煤矿区的生态管理和水资源的合理利用具有重要意义。此外,本研究还为干旱和半干旱地区水资源的可持续管理提供了宝贵的见解,对减轻煤矿开采活动对生态环境的影响至关重要。
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Effects of groundwater level changes on soil characteristics and vegetation response in arid and semiarid coal mining areas.

Coal mining in arid and semiarid regions often leads to numerous ecological and environmental problems, such as aquifer depletion, lake shrinkage, vegetation degradation, and surface desertification. The drainage from coal mining activities is a major driving force in the evolution of the groundwater-soil-vegetation system. In order to explore the effect of groundwater level fluctuation on soil properties and the response mechanism of surface vegetation in coal mining areas, this study is based on hydrogeological and ecological vegetation investigations in the Bojianghaizi Basin, and soil and vegetation samples are collected in the areas with different groundwater levels, and soil and vegetation indexes are analyzed with the aid of methods such as numerical statistics, linear regression, and correlation analysis with the aid of the Origin software. The results show that there is a significant negative correlation between groundwater table (GWT) and soil water content (SWC), soil conductivity, soil organic matter (SOM), soil available nitrogen (SAN), and soil available potassium (SAK). Mining activities have led to the destruction of the soil structure, greatly reducing its ability to retain water and fertilizer. The contents of SWC, SOM, and SAN in the mining area are significantly reduced, which are at least 49.73%, 47.56% and 59.90% lower than those around the mining area. On the northern and southern sides of the lake, serious soil salinization exists in the lakeshore zone where the depth to the water table is <0.5 m, and the water required for the growth of vegetation here mainly comes from the groundwater, so there are only a few water-loving and saline-resistant plants; when the depth to the water table is 0.5-7 m, the growth of surface vegetation is influenced by the double impacts of the water table and atmospheric precipitation with a high degree of species richness; when the depth to the water table is >7 m, the surface vegetation is only dependent on the limited atmospheric precipitation for water. When the depth of groundwater is >7 m, the surface vegetation only relies on limited atmospheric precipitation for water, and drought-tolerant plants mainly grow in these areas. This study not only provides a scientific basis for the sustainable development and environmental protection of similar mines in the world, but also has important significance in guiding the ecological management and rational utilization of water resources in coal mine areas. What is more, This study provides valuable insights into sustainable water resource management in arid and semi-arid regions, crucial for mitigating the ecological impacts of coal mining activities.

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来源期刊
Environmental Geochemistry and Health
Environmental Geochemistry and Health 环境科学-工程:环境
CiteScore
8.00
自引率
4.80%
发文量
279
审稿时长
4.2 months
期刊介绍: Environmental Geochemistry and Health publishes original research papers and review papers across the broad field of environmental geochemistry. Environmental geochemistry and health establishes and explains links between the natural or disturbed chemical composition of the earth’s surface and the health of plants, animals and people. Beneficial elements regulate or promote enzymatic and hormonal activity whereas other elements may be toxic. Bedrock geochemistry controls the composition of soil and hence that of water and vegetation. Environmental issues, such as pollution, arising from the extraction and use of mineral resources, are discussed. The effects of contaminants introduced into the earth’s geochemical systems are examined. Geochemical surveys of soil, water and plants show how major and trace elements are distributed geographically. Associated epidemiological studies reveal the possibility of causal links between the natural or disturbed geochemical environment and disease. Experimental research illuminates the nature or consequences of natural or disturbed geochemical processes. The journal particularly welcomes novel research linking environmental geochemistry and health issues on such topics as: heavy metals (including mercury), persistent organic pollutants (POPs), and mixed chemicals emitted through human activities, such as uncontrolled recycling of electronic-waste; waste recycling; surface-atmospheric interaction processes (natural and anthropogenic emissions, vertical transport, deposition, and physical-chemical interaction) of gases and aerosols; phytoremediation/restoration of contaminated sites; food contamination and safety; environmental effects of medicines; effects and toxicity of mixed pollutants; speciation of heavy metals/metalloids; effects of mining; disturbed geochemistry from human behavior, natural or man-made hazards; particle and nanoparticle toxicology; risk and the vulnerability of populations, etc.
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