(一)自 然 情 况 寻邬县位于江西东南隅,气候较暖,年平均温度24℃左右,无霜期295日,年雨量1300毫米左右。4、5、6月降水比较集中,其它各月,分布亦较调匀。 全县境内多山,由蜿蜒的群山分割成若干个小型盆地和谷地。山地地层主要是花岗岩和云母片岩,在其上发育着红壤,堆积到山坡和山麓,或经水流挟带沉积于盆地中间。位于不同地形和母质上的土壤,经过长期种植水稻,形成了各种水稻土。 (I) Natural Situation Xunwu County is located in the southeast corner of Jiangxi Province. Its climate is warmer, its annual average temperature is around 24 ℃, its frost-free period is 295 days and the annual rainfall is about 1300 mm. April, May and June precipitation is more concentrated, the other months, the distribution is also more uniform. Mountainous throughout the county, divided by meandering mountains into a number of small basins and valleys. The mountain strata are mainly granite and mica schist, on which red soil is developed, deposited on hillsides and foothills, or entrained in water by sediments in the middle of the basin. Soil in different terrain and parent material, after long-term cultivation of rice, formed a variety of paddy soil.