地球科学进展 doi: 10.11867/j.issn.1001-8166.2025.091

   

科尔沁沙地恢复的生物地理学基础与成效
陈雪萍1,2,赵学勇1,2*,杨小菊1,2,王瑞雄1,2   
  1. (1. 中国科学院西北生态环境资源研究院,干旱区生态安全与可持续发展国家重点实验室,奈曼沙漠化研究站,甘肃 兰州730000;2. 中国科学院大学,北京 100049)
  • 基金资助:
    国家自然科学基金面上项目(42177456);内蒙古科技成果转化项目(2021CG0012)资助.

Biogeographical Basis of Desertified Land Restoration and Achievements in Horqin Sandy Land

CHEN Xueping1, 2, ZHAO Xueyong1, 2*, YANG Xiaoju1, 2, WANG Ruixiong1, 2   

  1. (1. Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Naiman Desertification Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; 2. University of Chinese Academy of Sciences, Beijing 100049, China)
  • About author:CHEN Xueping, research area includes desert ecology. E-mail: chenxp0305@163.com
  • Supported by:
    Project supported by the National Natural Science Foundation of China (Grant No.42177456); The Science and Technology Transformation Project in Inner Mongolia (Grant 2021CG0012).
科尔沁沙地位于半干旱与半湿润气候过渡区,生态系统类型复杂且脆弱,是中国北方沙漠化最为严重的地区之一。然而,有关该区域土地沙漠化的生物地理学基础及治理成效的综合研究较为薄弱。科尔沁沙地深厚的沙质沉积(80~200 m)地层结构是该区域地下水储量相对丰富的基础。1985—2000 年,科尔沁沙地土地沙漠化防治成效显著,此后,治理出现瓶颈(沙漠化土地面积减小幅度下降,生物量恢复趋势平缓)。尤其在气候变化条件下,科尔沁沙地土地沙漠化防治面临的主要挑战是水资源胁迫。通过综述与分析科尔沁沙地生态脆弱的地理学基础、土地沙漠化与恢复过程、生物生产力变化与地下水动态等研究成果,为科尔沁沙地水土资源的科学管理及退化土地持续恢复提供了理论依据和数据支撑。
Abstract:The Horqin Sandy Lands, located in the ecologically sensitive transitional belt between semi-arid and semi-humid climatic zones, support a complex mosaic of ecosystems characterized by inherent vulnerability and represent one of the most severely desertified regions in northern China. Despite its environmental significance, comprehensive studies that systematically integrate the biogeographical mechanisms underlying desertification with rigorous assessments of control efficacy in this region remain notably scarce. The region's comparatively substantial groundwater resources are fundamentally underpinned by an extensive and porous sandy sedimentary stratum, measuring 80 to 200 meters in thickness, which serves as a critical aquifer system. The period from 1985 to 2000 witnessed remarkable progress in desertification control, marked by a significant reversal in land degradation trends. Nevertheless, the subsequent phase post-2000 has been defined by a pronounced operational bottleneck, manifesting as a markedly decelerated rate of reduction in desertified land area and a stagnating trajectory in the recovery of biomass. In the context of ongoing climate change, the foremost challenge confronting sustainable desertification management in the Horqin Sandy Lands is escalating water resource stress, which threatens the longevity of past restoration gains and future initiatives. This review systematically synthesizes and critically evaluates a substantial body of research pertaining to the geographical foundations of ecological vulnerability, the dynamic processes and mechanisms of desertification and ecological recovery, and the intricate interrelationships between biological productivity fluxes and groundwater dynamics. By constructing a comprehensive synthesis from these diverse research strands, this review aims to elucidate the complete narrative of desertification control tracing its foundations, achievements, and contemporary challenges, thereby providing a robust theoretical framework and empirical evidence base to inform the scientific management of soil and water resources and to guide the sustainable restoration of degraded landscapes in the Horqin Sandy Lands.

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