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中国西南喀斯特石漠化时空演变特征、发生机制与调控对策 被引量:126

Occurrence,spatial-temporal dynamics and regulation strategies of karst rocky desertification in southwest China
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摘要 中国西南喀斯特石漠化及发展态势的遏制与综合治理是长江、珠江流域的生态安全需要。通过总结前人的研究成果、采集中国科学院环江喀斯特生态试验站部分收集整理和试验数据,尝试性地提出了新的石漠化概念和分类标准,探讨了西南喀斯特石漠化的空间分布及动态变化规律,阐明了不同石漠化程度生态系统的植被和土壤物理、化学、微生物等属性的表现特征,从自然和人为两个方面揭示了西南喀斯特石漠化的发生机制,提出了不同石漠化程度的治理对策,以促进喀斯特区域生态、经济、社会的全面协调与可持续发展。 The karst landscape in China are mainly located in the southwest of China around Guizhou province and cover an area of 550 000 km2. Southwest China is most famous in the world for the continuous distribution of karst landscape, for holding the largest area of bare carbonate rocks and for experiencing the strongest karst development in the world. The karst area in southwest China is characterized by unique geological background, high landscape heterogeneity, low ecological capacity. In the meanwhile, this region is populous and in turn the exploitation of natural resources has been very high. For example, most natural vegetation has been converted to croplands. As a consequence, the region has experienced serious soil erosion or rocky desertification over the past decades due to the fragile nature of the ecosystems here, which posed great threat on the sustainable development of this region. In addition, since southwest China is located in the headwaters region of the Pearl River and Yangtze River, the ecological degradation in this region directly impacts the ecological safety the in the middle or lower reaches of the two rivers' watersheds. Therefore, a comprehensive control of the karst rocky desertification and an effective restoration of the degraded areas are necessary for ensuring the ecological security of the Yangtze and Pearl rivers' watersheds. In this paper, we systematically synthesized the information regarding rock desertification in the karst area in southwest China obtained largely from but not limited to Huanjiang Observation andResearch Station of Karst Ecosystem, Chinese Academy of Sciences. We proposed a new definition of rocky desertification and its classification criteria. Based on remote sensing data, we discussed the spatial distribution and dynamics of rock desertification in the karst area in southwest China. At different stages of rocky desertification, the ecosystems were related to different characteristics embodied by a combination of vegetation, soil physics, chemistry, and microorganism. The occurrence of karst rocky desertification was explained from natural factors (e.g., geological factors) and human activities, especially agricultural activities. We proposed several regulation strategies according to the degree of rocky desertification to boost the harmonious and sustainable development of ecology, economy and society in the karst areas of southwest China.
出处 《生态学报》 CAS CSCD 北大核心 2014年第18期5328-5341,共14页 Acta Ecologica Sinica
基金 中国科学院西部行动计划项目(KZCX2-XB3-10) 国家自然科学基金项目(U1033004 31370485)
关键词 西南喀斯特 石漠化 时空变化 发生机制 综合治理 karst area rocky desertification spatial-temporal dynamics occurrence regulation strategies
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