南太行地区(河南境内)石漠化分级评价及演进过程研究

Classification and evaluation of rocky desertification and evolution process in South Taihang Area

  • 摘要: 以南太行地区为例,采用遥感解译技术,选取植被、土被和基岩裸露率三个评价因子,构建适用于该区域的石漠化分级标准,开展该区域石漠化问题的研究。结果显示:(1)通过缨帽变换的第二分量(绿度指数)进行验证,证实由植被、土被和基岩裸露率三个因子构建的北方地区石漠化分级标准合理、可行;(2)1995—2020年研究区域的石漠化问题呈现出前8 a快速恶化,后25 a缓慢改善的态势;石漠化区域高度集中于研究区的东南部、南部及西北部,这些区域多临近农田、城镇与矿区且受人类生产建设活动的干扰强烈;而无石漠化区域多集中于研究区西北部及北部边界局部地带;(3)地质环境与人类活动相互作用、相互促进,导致区内土地生产力退化、植被生存环境恶化及水土涵养能力下降,反过来促进土壤侵蚀、碳酸盐岩溶蚀与侵蚀的恶性循环,推动石漠化问题的持续发展。

     

    Abstract: Taking the southern Taihang Mountains area as an example, remote sensing interpretation technology was adopted, three evaluation factors (vegetation, soil cover, and bedrock exposure rate) were selected, a rocky desertification classification standard suitable for this region was established, and research on the rocky desertification issue in the area was carried out. The results showed that:(1) Verification was conducted using the second component (greenness index) of the tasseled cap transformation, which confirmed that the rocky desertification classification standard for northern China constructed based on the three factors (vegetation, soil cover, and bedrock exposure rate) was reasonable and feasible; (2) From 1995 to 2020, the rocky desertification in the study area showed a trend where it deteriorated rapidly in the first 8 years and improved slowly in the subsequent 25 years; The rocky desertification areas were highly concentrated in the southeast, south, and northwest parts of the study area. Most of these areas were adjacent to farmland, towns, and mining areas, and were strongly disturbed by human production and construction activities; In contrast, areas without rocky desertification were mostly concentrated in the northwest part of the study area and some local areas along the northern border; (3) The geological environment and human activities interacted with and promoted each other, which led to the degradation of land productivity, the deterioration of the vegetation living environment, and the decline of water and soil conservation capacity in the area. In turn, this promoted a vicious cycle of soil erosion, carbonate rock dissolution, and erosion, driving the continuous development of the rocky desertification problem.

     

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