龙映豪, 李旭东, 程东亚. 贵州岩溶峡谷地表覆盖变化的地形分异特征[J]. 土壤通报, 2021, 52(4): 767 − 776. DOI: 10.19336/j.cnki.trtb.2019120301
引用本文: 龙映豪, 李旭东, 程东亚. 贵州岩溶峡谷地表覆盖变化的地形分异特征[J]. 土壤通报, 2021, 52(4): 767 − 776. DOI: 10.19336/j.cnki.trtb.2019120301
LONG Ying-hao, LI Xu-dong, CHENG Dong-ya. Topographic Differentiation of Land Cover in Karst Canyon of Guizhou[J]. Chinese Journal of Soil Science, 2021, 52(4): 767 − 776. DOI: 10.19336/j.cnki.trtb.2019120301
Citation: LONG Ying-hao, LI Xu-dong, CHENG Dong-ya. Topographic Differentiation of Land Cover in Karst Canyon of Guizhou[J]. Chinese Journal of Soil Science, 2021, 52(4): 767 − 776. DOI: 10.19336/j.cnki.trtb.2019120301

贵州岩溶峡谷地表覆盖变化的地形分异特征

Topographic Differentiation of Land Cover in Karst Canyon of Guizhou

  • 摘要: 岩溶峡谷是典型的喀斯特生态脆弱区,研究其地表覆盖变化对山区生态保护和国土资源空间优化具有重要意义。以贵州境内岩溶峡谷为研究区,选取2000—2020年地表覆盖数据,提取海拔、坡度、坡向三种地形因子,探究其地表覆盖变化及地形分异特征。得出以下结论:(1)2000—2020年研究区各类地表覆盖面积变化差异明显,林地、草地、水域、建设用地面积增加,耕地面积减少;(2)研究时段内随着海拔上升,研究区耕地面积呈现上升-下降-上升-下降的变化趋势;林地面积总体呈现先上升后下降趋势,峰值大致在1800 ~ 2200 m;草地和建设用地面积均存在两个相对高值区,分别出现在1200 ~ 1400 m和2200 ~ 2400 m、1200 ~ 1400 m和1800 ~ 2000 m;水域面积在小于800 m、2000 ~ 2200 m相对较高;(3)随着坡度上升,研究区耕地、林地和草地面积呈现先上升后下降趋势,分别在10° ~ 15°、15° ~ 20°、10° ~ 15°出现最高值;建设用地面积随坡度增加总体呈现下降趋势;(4)在随着坡向变化中,研究区耕地、林地、草地、建设用地面积在无坡向地区分布较少;2020年建设用地面积在西南坡分布相对较多。

     

    Abstract: The karst canyon is a typical karst ecological fragile area, in which the land cover changes’ research is of great significance to the ecological protection of mountainous areas and the optimization of land resources. Taking the karst canyon of Guizhou as the research area, the land cover data from 2000 to 2020 were selected to explore the changes in land cover and the law of topographic differentiation by extracting three topographic factors of altitude, slope, and aspect. The results showed that: (1) The land cover area of the study area was varied significantly from 2000 to 2020. The areas of woodland, grassland, water area, and construction land were increased, while the area of arable land was decreased; (2) As the altitude increased during the study period, the area of arable land from 2000 to 2020 presented an upward-decreasing-increasing-declining trend; The area of woodland generally showed an upward trend first and then downward, with a peak value of altitude approximately at 1800 ~ 2200 m; There were two relatively high-value areas in grassland and construction land, appearing at the altitudes of 1200 ~ 1400 m and 2200 ~ 2400 m, 1200 ~ 1400 m and 1800 ~ 2000 m, respectively; The water area was mainly distributed at the altitudes of lower than 800 m and 2000 ~ 2200 m; (3) As the slope rose, the areas of arable land, woodland and grassland would increase first and then decrease, showing the highest slope value observed at 10° ~ 15°, 15° ~ 20°, and 10° ~ 15°, respectively; The area of construction land showed a downward trend with an increase of slope; (4) With the change of slope, the areas of the flat lands were less distributed in the Non-slope area, the woodland, the grassland and the construction land; Meanwhile, the construction land in 2020 was relatively high in the southwest slope.

     

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