高原内陆湖萎缩区盐碱地生态修复研究: 以内蒙古达里诺尔湖为例

    Study on the Ecological Restoration of Saline-alkali Soils Lands in the Shrinkage Area of Plateau Inland Lakes: A Case Study of Dalinor Lake in Inner Mongolia

    • 摘要: 气候变化和人类活动易导致干旱区湖泊萎缩进而影响区域生态安全, 近年来湖泊萎缩区生态修复和生物多样性恢复受到高度关注。为探究气候变化背景下高原湖泊萎缩区生态修复的影响因素, 以内蒙古达里诺尔湖为例, 对湖泊萎缩区"近湖裸地-碱蓬修复区-湿地修复区"和浑善达克沙地修复样地的土壤pH、养分和植被变化开展研究, 探讨"气候变化-湖泊萎缩-生态修复"的适应气候变化对策。结果表明: (1)湖泊萎缩区样地土壤pH值与土壤肥力高于沙地修复样地, 随着与湖泊岸线距离的增加和海拔高度的增大, 部分土壤养分指标有所改善。与近湖裸地相比, 碱蓬修复区和湿地修复区全碳、全氮、全钾含量等显著增加。(2)达里诺尔湖泊萎缩区植被恢复成效较好, 垂直于湖岸线方向上的"近湖裸地-碱蓬修复区-湿地修复区"植被盖度、植株数量逐步提高。(3)干旱区湖泊萎缩后产生的土壤盐碱地为植物困难立地, 植被恢复指标与土壤全碳、全氮、有机质含量的相关性显著, 湖泊萎缩区盐碱地植被恢复应根据主要生态功能进行生态修复分区分类。研究结果对于加强干旱区湖泊萎缩后气候变化风险的适应性管理和生态功能修复具有参考价值。

       

      Abstract: Climate change and human activities tend to cause the shrinkage of lakes in arid areas, thus affecting regional ecological security. In recent years, biodiversity conservation and ecological restoration in lake shrinking areas have attracted significant attention. To explore the factors of ecological restoration in the shrinkage areas of plateau lakes under global climate change, a case study was carried out in Dalinor Lake in Inner Mongolia. Soil pH, nutrients, and revegetation effectiveness of different ecological restoration sites, including bare land near the lake, Suaeda heteropteran planted area, wetland restored area, and revegetated sandy land, were compared. The adaptation strategy of "climate change-lake shrinking-ecological restoration" was also discussed. The results show that: (1) soil pH values and fertility in the lake shrinking areas were higher than those in revegetated sandy lands. Some soil nutrient indicators improved with the increase in elevation and distance from the lake shoreline. Compared with bare land near the lake, the total carbon, total nitrogen, and total potassium contents in the Suaeda heteropteran planted area and wetland restored area increased significantly. (2) The revegetation effectiveness in the shrinking area of Dalinor Lake has achieved remarkable results, with a gradual increase in vegetation coverage and plant number along the direction of "bare land near the lake-Suaeda heteropteran planted area-wetland restored area" perpendicular to the shoreline of the lake. (3) The saline-alkaline soil produced after the shrinkage of lakes in arid regions is difficult for plants. Revegetation indicators were significantly correlated with soil total carbon (TC), total nitrogen (TN), and organic matter (SOC) contents. The revegetation countermeasures of saline-alkali lands in lake shrinking areas should be classified according to the main functions of ecological restoration zones. The research findings could provide references for strengthening the adaptive management of climate change risks and ecological function restoration for shrinking lakes in dry areas.

       

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