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干旱区地理 ›› 2012, Vol. 35 ›› Issue (6): 996-1003.

• 区域发展 • 上一篇    下一篇

从《清实录》看清代1644-1795 年中国北方农牧交错带东段的农业开发

樊星1,叶瑜1,2,罗玉洪1   

  1. 1 北京师范大学地理学与遥感科学学院, 北京 100875;2 北京师范大学环境演变与自然灾害教育部重点实验室, 北京 100875
  • 收稿日期:2011-10-10 修回日期:2012-02-25 出版日期:2012-11-25
  • 通讯作者: 叶瑜,(1979- ),副教授,主要研究领域:历史土地覆盖变化,历史气候变化影响与适应.Email:yeyuleaffish@bnu.edu.cn
  • 作者简介:樊星(1986-),,河北省张家口市人,在读硕士,研究方向:环境演变.Email:fanxing58@163.com
  • 基金资助:

    国家自然科学基金(40901099);全球变化研究国家重大科学研究计划(2010CB950103);“十一五”国家科技支撑计划项目(2008BAK50B07)资助

Agriculture exploitation in the east part of North Agro-pasture Transitional Zone during 1644-1795 by Actual Annals of Qing Dynasty

FAN Xing1,YE Yu1,2,LUO Yu-hong1   

  1. 1 School of Geography, Beijing Normal University, Beijing 100875,China;2 Key Laboratory of Environment Change and Natural Disaster; Ministry of Education; BNU; Beijing 100875,China
  • Received:2011-10-10 Revised:2012-02-25 Online:2012-11-25

摘要: 我国北方农牧交错带东段当前很多生态问题与历史农业开发过程是有联系的。从清代顺治朝(1644-1661年)到乾隆朝(1736-1795 年)末,该区经历了一次较大的农业垦殖扩张,土地利用方式发生了很大变化。利用《清实录》中顺康雍乾四朝(1644-1795 年)清政府对该区进行土地管理与利用的信息,分析该地区农垦区扩张的历史,得出以下结论:(1)四朝以来该区的开垦强度在增大,开垦速度不断加快。乾隆朝新垦速率最快;(2)农耕区的发展呈现新垦区北扩和已垦区内填充式开垦两种形式。从顺治朝到乾隆朝,农耕区界线逐渐北扩,从长城一线以南扩展到太仆寺—多伦—赤峰—围场—敖汉一线境内。开垦界线在雍正朝达到最北,到达科尔沁、阿鲁科尔沁境内,但未达到现代农牧交错带东段北界,这与清初清政府对东蒙地区土地开垦的封禁政策相关;(3)各朝垦殖政策有发展变化,总体来说为厉禁。但在人民生计困难的压力下,面对出关口逃生的流民,政府不得不放松关口的封禁,默许流民进入口外开垦。

关键词: 北方农牧交错带东段, 农业开发, 清代, 土地管理

Abstract: The east part of North Agro-pasture Transitional Zone in north China located between the south edge of Inner Mongolia plateau and the Great Wall. It is considered as one of the most sensitive regions of China, for it is in the transitional region among different climatic zones and controlled by the southeast monsoon. The one hand, the area provides human with broad space and huge material production potential,moreover, it plays an important role in the change of regional and global climate and the maintenance of ecological functions; the other hand, the ecological issues of the area are very prominent and ecological environment here is manifold, complex and vulnerable, because of the superposition of topography, climate, vegetation and economic activities in the transitional zone of superposition. Arid climate, water deficit are the main features in the area. The relationship between local people and the environment is very special and important to the locally fragile ecological environment. Some current ecological problems being existed in this area are highly correlated with the historical agricultural development. A climax of reclamation began from Shunzhi (顺治) to Qianlong(乾隆) Period (1644-1795), meanwhile land use patterns in the area also changed. This study area includes 34 cities/counties in the eastern Inner Mongolia, 20 cities/counties in Hebei, 3 counties in northern Beijing, 3 cities/counties in Heilongjiang, 8 cities/counties in Jilin, and 11 cities/counties in the south of Liaoning. In the area, the precipitation is 300-450 mm, and dryness is 1-2; From the southeast to northwest, the terrain gradually transforms from the northeast plains to Inner Mongolia plateau. The land administration information, such as reclamation policy, bumper & poor harvest, reclamation area and so on, are collected from Actual Annals of  the Qing Dynasty(《清实录》)in the periods and are analyzed by the methods of historical literature law and information extraction and classification. Based on the records, the paper analyzes the history of cropland expansion and uses ArcGIS to demonstrate it with spatial distribution maps. The main conclusions are as follows: (1) The cropland continuously increased and accelerated during the 152 years, which was cultivated most in the Qianlong Dynasty. (2) Cropland expansion was mainly brought by northward extension of new croplands and refilling in the existed cropland area. The northern boundary of stable cropland area extended northward from the regions to the south of the Great Wall to the line of Taipusi(太仆寺)-Duolun(多伦)-Chifeng(赤峰)-Weichang(围场)-Aohan(敖汉).  The northern boundary of unstable cropland area went on to the furthest north, reaching the line of Horqin(科尔沁)-Aluhorqin(阿鲁科尔沁) in Yongzheng Period, however, it was more southerly than that of the northern boundary of modern cultivation. (3) People’s spontaneous reclamation was the main reason of the cropland expansion. (4) The northern pastoral area boundary changes express the change of land administration policy under population pressure.  Reclamation policy in the area changed under the four emperors’ reign and generally it tended to acquiesce in refugees’ immigrating.

Key words: east part of North Agro-pasture Transitional Zone, agricultural development process, Qing Dynasty, land administration

中图分类号: 

  • F329