英语翻译对科尔沁沙地西部地区流动沙丘和固定沙丘的迎风坡表层干沙层厚度进行观测,分析了沙丘坡面干沙层的空间分布特点.结果表

英语翻译
对科尔沁沙地西部地区流动沙丘和固定沙丘的迎风坡表层干沙层厚度进行观测,分析了沙丘坡面干沙层的空间分布特点.结果表明：研究区沙丘迎风坡表层干沙层厚度主要在5~15 cm,92.0%的流动沙丘区域和98.6%的固定沙丘区域的干沙层厚度分布在此范围内；固沙植物影响沙丘表层干沙层的厚度变化和空间分布,流动沙丘表层干沙层厚度表现出明显的空间差异性,迎风坡上部西侧区域干沙层厚度较大,下部东侧区域相对较薄,其平均厚度为9.58±3.95 cm,在0~40 cm范围内变化,变异系数为0.41,干沙层空间分布的变异函数表现为球形模型,具有中等的空间相关性；固定沙丘的干沙层厚度表现为明显的均一性,空间差异性不明显,平均厚度为10.91±1.7 cm,变化范围在0~20 cm,变异系数仅为0.16.
Based on the observation of the thickness of dry sand layer in mobile and fixed dunes’ windward slope in the west of Horqin sandy land,we investigated the spatial distribution of dry sand layer.The results showed that the thickness of dry sand layer in windward slope was mainly between 5 and 15 cm,92.0% and 98.6% of thickness of dry sand layer in mobile and fixed dunes belong to this extent,respectively.Sand fixing plants played an important role in the thickness and spatial distribution of dry sand layer in dunes.The thickness of dry sand layer in mobile dunes showed significant differences,while the thickness of dry sand layer in windward slope was much thicker in the upper west areas,it was much thinner in the lower east areas in mobile dunes,its average thickness was 9.58±3.95 cm changing from 0 to 40 cm and the coefficient of variation was 0.41.The spatial distribution of dry sand layer showed spherical model,and there was moderate spatial correlation through variogram.In contrast,the thickness of dry sand layer in fixed dunes was more evenly distributed and there were no significant differences in dry sand layer of fixed dunes,its average thickness was 10.91±1.7 cm ranging from 0 to 20 cm,and the coefficient of variation was only 0.16.

我仔细读了一遍,感觉翻译的挺好的.千万不要借助于翻译软件,不然那就毁了!
再问： 谢谢了，可是老师说我的还是有些地方不通顺，不知道再怎么对细节方面进行修改了
再答： while the thickness of dry sand layer in windward slope was much thicker (than that) in the upper west areas