摘要
江西长江防洪干堤修筑在九江—黄梅平原第四系冲积层之上。作者通过对长江沿岸(江西段南岸)环境地质调查,依据大量的钻探工程资料,基本查明了防洪干堤基础工程地质条件,并对干堤形成水患灾害的类型、分布特征和致灾机制进行了综合分析,从而为今后防洪减灾提供了基础性地质依据。
Flood bank in Jiangxi is built on the Quaternary alluvium of Huangmei Plain. Based on the environment geologic investigation and many drilling data, comprehesive analyses have been made for the types of flood catastroples, flood distribution and causes of catastroples. The analyses provide some imformation for controlling flood and avoiding calamity.
出处
《资源调查与环境》
2002年第4期292-298,共7页
Resources Survey & Environment
基金
国家地质调查项目:项目名称"长江中游主要水患区环境地质调查评价"
项目编号 1 9991 2 3 0 0 0 3 0 44。
关键词
水患灾害
致灾机制
防洪干堤基础
江西江段
长江中游
防洪工程
flood catastrophe
causing catastrophe mechanism
flood bank basement
Jiangxi River
Middle Reaches of Changjiang River
