摘要
明代在内蒙古西部地区的开发,历时短暂,极为有限。明与蒙古的势力分布状况表明,明朝在内蒙古西部的建置并不长久。正统十四年土木之变,诸卫或废或徙,明势力撤至大同、偏关,即今明长城一线,土默川、蛮汗山地区尽弃边外,鄂尔多斯地区,明朝始终未设治。生态脆弱的鄂尔多斯地区,明初至正统70年间基本上是无人区,极少耕牧。正统初至成化八年不过40年,在榆林等23个营堡越境种田。此后,明朝军民已停止了在河套、毛乌素沙地南缘略具规模的农垦活动。史籍描绘的万历年间延绥中路边墙沙壅问题及毛乌素沙地东南缘流沙猖獗,是自然因素所致。
In Ming Dynasty, about the exploration of the Inner Mongolian Western area, the proeess was temporary and the influences which were coursed by the humanbeing was limited. The distributive power about the Ming and the Mongolia showed that the Ming central government hadn＇t governed this area for long time. The Ming Royal set up some governments called Wei to control this area. After the Zheng Tong 14＇s Tumu Coup.some of the Wei were abolished, others moved. The Ming＇s orbit withdrew to Datong, Pianguan. which is the trace of today＇s Ming Great wall. Tumo Plain and Manhan Mountain were abandoned. For the Erduos, the Ming Royal had never established government to control this place. The Erduos＇ ecology was delicate, and from the beginning of the Ming Dynasty to Zheng Tong, nearly 70 years, no people explored this plaee. From Zheng Tong to Cheng Hua 8, during this period, only planting at Yulin and other 92 barracks. After that, the Ming＇s soldiers and people had stopped the mass and centralized exploration on the Hetao and the southern area of the Maowusu Desert. Consequently, the history materials mentioned the problems in the Wan Li period, such as the sand stuffed up the side wall of the Yansui Middle Road and the fierce quicksand of the southeast area of the Maowusu Desert factors.
出处
《内蒙古大学学报（哲学社会科学版）》
CSSCI
北大核心
2006年第1期23-26,共4页
Journal of Inner Mongolia University(Philosophy and Social Sciences)
关键词
明代
有限垦殖
毛乌素
流沙
原因
Ming Dynasty
limited exploration
Maowusu
quicksand
reason
