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一、基本情况1.地貌和地形 阿克苏地区位於喀什平原的北部,是一个与天山南麓相接的倾斜平原,其南部与塔里木盆地相联,由细颗粒的坡积——洪积物组成,在过渡地带及倾斜平原中有许多有盐结皮覆盖的风积沙丘.洗盐的试验地点设在胜利三场3127号(1956年)及4221号(1957年)条田中.农场的坡度为1/800-1/1,500.2.气候概述 本地区为大陆性气候,年平均气温10.5℃,最低在12月,为-28℃ ; 最高在6月,为37.6℃.雨量少,蒸发大,年降水量在100毫米以下,年蒸发量由2,240到3,350毫米,尤以6、7两月份蒸发最烈.
First, the basic situation 1. Landform and topography Akesu region is located in the northern Kashi Plain, is a tianping south slope of the plains, the southern associated with the Tarim Basin, composed of fine-grained slope plot - There are many salt-rich sand dunes covered by salt crusts in the transitional zone and the sloping plains, and the salt water test sites are located in fields numbered 3127 (1956) and 4221 (1957) of Victory, with a slope of 1 /800-1/1,500.2. Climatic Overview The climate in this area is continental with average annual temperature of 10.5 ℃ and lowest of -28 ℃ in December and highest of 37.6 ℃ in June. Rainfall, evaporation and annual precipitation Below 100 mm, annual evapora- tions ranged from 2,240 to 3,350 mm, most notably in February and February.