川西高原荒漠化时空变化特征及驱动力分析
[Abstract]:As one of the most serious ecological problems, land desertification brings great harm to the ecological environment and resources, restricts the social and economic development and the improvement of the people's living standard, and even endangers the survival of the residents. It is an important factor that hinders the sustainable development of a region. It is of great significance to evaluate desertification accurately and to grasp the dynamic and driving factors of desertification change in time and effectively. The western Sichuan Plateau is located in the western part of Sichuan Province, and is one of the most serious desertification areas in Sichuan. According to the definition of desertification, this paper combines the actual situation of desertification in the western Sichuan Plateau on the basis of the principle of selecting desertification evaluation index by predecessors. The desertification in western Sichuan Plateau is evaluated, and the characteristics and driving forces of desert temporal and spatial variation in West Sichuan Plateau from 2001 to 2014 are analyzed. The main results and conclusions are as follows: (1) vegetation coverage is selected from four aspects: vegetation, topography, soil and climate. The evaluation index system of desertification was constructed by slope, soil texture and moisture index, and the spatial distribution of desertification in West Sichuan Plateau was obtained from 2001 to 2014. Most of the desertification areas are located in the west of and near the Shaluli Mountains and the northern part of the Bayankra Mountains, as well as in the regions of Daxue Mountain, Qionglai Mountain and Minshan Mountains. (2) the area of desertification reversal in 2001-2014 is about 8745.81 km2, accounting for 3.51% of the study area. Desertification develops to 4666.50 km2, accounting for 1.87% of the study area. Among them, the average annual change rate of severe desertification area is the largest, while the change rate of light and moderate desertification area is small, but the change area and transfer rate of light and moderate desertification land in 14 years are larger, but the change area of heavy desertification area is larger. The rate of transfer is low, and the trend of slight, moderate and severe desertification is decreasing, which indicates that the natural environment is gradually improving in the past 14 years. The response of light desertification land and moderate desertification land to the environmental change in this period is the largest. (3) the desertification distribution is different under different heights. High altitude areas, due to the accumulation of snow and glaciers at the top of the mountain and the erosion of the region by the melting of snow and glaciers, result in very little vegetation cover in the region, large amounts of desertification, and a better vegetation growth environment in areas with lower elevations, (4) the main driving forces of desertification in western Sichuan Plateau are natural and man-made, the contribution rate of natural driving factors to desertification change is low, and the contribution rate of human driving factors is larger. At different elevations, the contribution rate of natural and human factors is different. The higher the altitude is, the smaller the influence of human factors is, and the greater the influence of natural factors is. With the continuous improvement of population quality and the encouragement of national policy, the environment of western Sichuan plateau is improved continuously under the artificial action, and desertification is gradually reduced.
【学位授予单位】:成都理工大学
【学位级别】:硕士
【学位授予年份】:2017
【分类号】:X171
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