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江汉平原涝渍地域退田还湖的地质环境适宜性分析
引用本文:刘章勇. 江汉平原涝渍地域退田还湖的地质环境适宜性分析[J]. 湖北农学院学报, 2004, 24(2): 134-137
作者姓名:刘章勇
作者单位:长江大学涝渍灾害与湿地农业实验室,湖北,荆州,434025
基金项目:湖北省教育厅重点实验室开放基金资助项目(HNKFJ2002A01)
摘    要:江汉平原涝渍环境的形成是地质、气候等自然因素和人类干预交互叠加作用的结果,各个历史时期的围湖垦殖活动加速了涝渍生境的劣化进程。目前荆江河段的构造沉降仍在继续,适度退田还湖是恢复和重建江汉平原涝渍地域生态环境的有效手段。

关 键 词:江汉平原 涝渍环境 退田还湖 地质适宜性分析 气候变化 围湖垦殖
文章编号:1004-3888(2004)02-0134-04
修稿时间:2003-12-31

Geological Adaptability of Restoration from Paddy Field to Lake in Waterlogging Area in Jianghan Plain
LIU Zhang-yong. Geological Adaptability of Restoration from Paddy Field to Lake in Waterlogging Area in Jianghan Plain[J]. Journal of Hubei Agricultural College, 2004, 24(2): 134-137
Authors:LIU Zhang-yong
Abstract:The formation of the waterlogging evolvement in Jianghan Plain is the result of affecting in turn by the naturalness of the geological structure and climate and mortal intervention. The reclaiming land from lakes in various history periods accelerate the inferior course of waterlogging evolvement. The sedimentation of geological construct is continuing in Jingjiang part. The restoration from paddy field to lake moderately is an effective means of resuming and rebuilding the waterlogging ecological environment in Jianghan Plain.
Keywords:waterlogging enviroment  restoration from paddy field to lake  geological adaptability  Jianghan Plain
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