古地图与现代空间数据的河道变迁研究——以清代潇河为例  

River channel changes based on old maps and modern spatial data——taking Xiaohe River during Qing Dynasty as an example

作　　者：孟万忠[1,2] 

机构地区：[1]陕西师范大学,西安710062 [2]太原师范学院,太原030012

出　　处：《测绘科学》2011年第2期73-75,共3页Science of Surveying and Mapping

基　　金：山西省人文社科重点研究基地项目-历史时期汾河流域生态环境与城市布局变迁;山西省高校重点学科建设专项基金-历史流域学的理论与实践;山西省软科学项目-汾河上游地区生态与经济协调发展机制构建研究(2010041025-03)

摘　　要：潇河是汾河的第二大支流,清代河道变迁频繁。本文利用清代山西地方志中的舆地图和现代空间数据,结合历史文献记载与实地考察,研究了潇河河道变迁最为剧烈的时期——清代近300年间的变迁过程,复原了不同时段的面貌,并对变迁原因进行了分析。认为在气候变干的大背景下,河道变迁的原因主要有两个:一是潇河及其支流泥沙含量大,造成旧河道的淤积而改道,清代潇河河道的变迁具有往复性;二是疏浚河道、开挖灌溉渠道,过度利用水资源等人类活动的影响。XiaoHe River is the second largest tributai7 of the Fenhe River. Xiaohe River channel had frequent changes during Qing Dynasty. The use of tile Qing Dynasty Shanxi ancient maps and gazetteers in the modern spatial data, combined with historicai re- cords and field trips to study the Xiaohe River in the most dramatic changes in the period-nearly 300 years of the Qing dynasty changes in the process of recovery in the face of different periods, and their causes were analyzed in the paper. The author believed that climate change context of dry, channel changes is due to two main reasons ： first, Xiaohe River and its tributaries contain large content of silt, resulting in the old river sihation and diversion of the Qing Xiao River with the reciprocating nature of the changes ; second, dredging, digging irrigation process, the transitional use of water resources and other human activities caused the effect.

关 键 词：古地图 地理空间数据 潇河 河道变迁 

分 类 号：P208[天文地球—地图制图学与地理信息工程] P28[天文地球—测绘科学与技术]