明清以来晋南山麓平原地带的水利与社会——基于龙祠周边的考察  

Water Resources and Society in Piedmont Plain in Southern Shanxi Province since Ming and Qing Dynasty:A Study around Longci Village

作　　者：周亚[1] 

机构地区：[1]山西大学历史文化学院,山西太原030006

出　　处：《中国历史地理论丛》2011年第3期104-114,共11页Journal of Chinese Historical Geography

基　　金：国家社会科学基金项目(07CZS015);山西省高等学校哲学社会科学研究基地项目(1005728)

摘　　要：晋南山麓平原地带存在着两种类型的地表水资源:流量稳定的泉水和季节性的洪流。在龙祠周边,龙子祠泉是最重要的泉水资源,经过千余年的开发,于明代末年形成较为稳定的渠道系统和灌溉区域。在渠系建设和运行过程中,面对发源于山间的洪流,引泉灌区通过避、堵、疏三种技术手段加以防治,并用规范化的制度体系予以保障。被引泉灌区视为隐患的洪流,在边山地带却成了重要的资源,人们引用洪流淤灌土地,同样形成了一套技术和制度体系。地方社会围绕同一条洪流的防治与利用形成了两个不同的利益群体,双方在趋利避害的路径选择上逐渐找到平衡点,实现了互利共存。There are two types of surface water resources in the piedmont plain in southern Shanxi Province：spring and flood current.Around Longci village,Longzici spring is the most important spring resources,after thousands of years of development,the stable channel system and irrigation area were formed in late Ming dynasty.The community of irrigation have prevented and controlled flood current through dodging,plugging,dredging and the system of administration.Nearby the foot of hill,flood current was important resources,people have used it to do warping irrigation,and also formed a set of technology and system.Two groups of different interests have been formed all around the prevention,control and utilization of one flood current,and achieved routualism from seeking advantages and avoiding disadvantages.

关 键 词：山麓平原 引泉灌溉 引洪淤灌 人地互动 互利共存 

分 类 号：K29[历史地理—历史学] F426.91[历史地理—中国史]