李乡旺, 陆素娟. 云南石漠化区划研究[J]. 西南林业大学学报, 2019, 39(2): 1-10. DOI: 10.11929/j.swfu.201810220
引用本文: 李乡旺, 陆素娟. 云南石漠化区划研究[J]. 西南林业大学学报, 2019, 39(2): 1-10. DOI: 10.11929/j.swfu.201810220
Xiangwang Li, Sujuan Lu. Regionalization of Stony Desertification in Yunnan Province[J]. Journal of Southwest Forestry University, 2019, 39(2): 1-10. DOI: 10.11929/j.swfu.201810220
Citation: Xiangwang Li, Sujuan Lu. Regionalization of Stony Desertification in Yunnan Province[J]. Journal of Southwest Forestry University, 2019, 39(2): 1-10. DOI: 10.11929/j.swfu.201810220

云南石漠化区划研究

Regionalization of Stony Desertification in Yunnan Province

  • 摘要: 云南的石漠化区域涵盖了从北热带到青藏高原高寒气候带,分布于海拔76~5 000 m,海拔高度变化大;受地貌、土壤、植被及各种生态因子的影响,环境条件复杂多样,差异十分明显,其中生态因子对石漠化治理有直接影响,在治理区域划分中起决定性作用,温度、湿度影响最重要。通过对云南石漠化区域的地理因子、环境因子、云南的灾害性天气、洪涝灾害、土壤及植被等因子的综合分析,将云南65个石漠化综合治理县划分为7个区10个亚区19个小区,分别是北热带低山河谷盆地石漠化区、南亚热带中低山河谷盆地石漠化区、中亚热带高原山地石漠化区、北亚热带高中山石漠化区、暖温带高中山石漠化区、青藏高原东南缘高原温带石漠化区、金沙江燥热河谷石漠化区。研究石漠化区域划分有关影响因子,因地制宜地指导石漠化综合治理,以便对不同的石漠化区域采取不同的植物措施及工程措施。

     

    Abstract: The stony desertification area in Yunnan extends from the northern tropics to the alpine climate zone of the Qinghai-Tibet Plateau, which is located at 76-5 000 m above sea level and varies greatly in altitude. Influenced by landform, soil, vegetation and various ecological factors, the environmental conditions in this area are complex and varied, with obvious differences. Ecological factors, especially temperature and humidity, have a direct impact on the control of stony desertification and play a decisive role in the division of control region. Geographical factors, environmental factors, disastrous weather, floods, soil and vegetation in stony desertification area were comprehensively analyzed. Sixty-five comprehensive treatment counties of stony desertification in Yunnan were divided into 7 districts, 10 sub-districts and 19 villages.They are the stony desertification areas in the low-mountain valley basin in the north tropics, the middle-low valley basin in the south subtropics, the plateau mountain in the middle subtropics, the high-middle mountain in the north subtropics, the high-middle mountain in the warm temperate zone, the plateau temperate zone in the southeastern margin of the Qinghai-Tibet Plateau and the dry-hot valley of the Jinsha River. To study the factors affecting the division of stony desertification regions, guide the comprehensive treatment of stony desertification according to local conditions, so as to take different plant measures and engineering measures for different stony desertification regions.

     

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