Is the environment in Kuitun, Xinjiang good? Specific point

(1) Kuitun City is located in the front of the piedmont alluvial-diluvial inclined plain and some lakes and marshes plains. It is about 50 kilometers away from Tianshan Mountain in the south and 8 kilometers away from Kuitun River in the west. The terrain is high in the southwest and low in the northeast. The height difference between north and south is reduced from 610m to 320m, and the height difference between east and west is reduced from 610m to 460m. The slope of the ground decreases from south to north to 10-30‰ and from west to east to 3-5‰. The whole landform is relatively simple, and the surface is mostly Gobi or clay silt, with a thickness of tens of centimeters to 30m. There are about 200,000 mu of cultivated land in this area, which has been reclaimed170,000 mu. The cultivated land is surrounded by Gobi wasteland, with perennial shrubs and grass growing, and the city is an oasis landscape. There is diving or spring water exposed in front of the alluvial fan of Kuitun River, and vegetation such as reed, lake grass and willow grows along the water surface. The east and west reed lakes in the northeast of Kuitun city are formed by diving or spring water exposure. Due to the upstream water intake and groundwater exploitation, the East and West Reed Lakes are shrinking year by year.

Because it is located in the piedmont depression of Tianshan Mountain, its landforms can be divided into four categories according to the formation reasons: accumulation landforms (such as alluvial, lacustrine plain and swamp plain), denudation accumulation landforms, erosion accumulation landforms and erosion structural landforms.