作　　者： ; ;

机构地区： 暨南大学文学院

出　　处： 《河北学刊》 2009年第5期86-89,共4页

摘　　要： 元代卫运河的修通,使冀鲁交界运河区域的盐碱地分布不断向东扩展,由唐宋御河以西扩展到卫运河以东。这一地区盐碱地的形成原因比较复杂,是气候、水文、地形、土壤、人为等多种因素综合作用的结果。而当地盐碱地的不断扩张,使棉花、豆类的种植进一步扩大,形成以芦苇为主的草编业,也使以苜蓿为原料的牧业兴盛起来。 Yuan Dynasty Wei Canal＇s laying, makes the Hebei and Shandong border canal region the saline and alkali land distribution to expand unceasingly to the east, expands from the Tang Song Yu River west to the Wei Canal＇s east. This local saline and alkali land＇s formation reason is quite complex, is the climate, the water environment, the terrain, the soil, artificial and so on many kinds of factor combined action result. But the local saline and alkali land＇s unceasing expansion, makes the cotton, legumes＇planter to further expand, forms by the reed straw braid industry primarily, also causes take the alfalfa to be prosperous as raw material animal husbandry.

关 键 词： 元明清时期 卫运河南段 盐碱地 农牧业

领　　域： [历史地理] [历史地理]