摘要
墨西哥湾飓风促使本文作者再次反思渤海湾西岸的现状:海岸线由曲折转为平直的、以侵蚀为主的自然进程,人为活动为主因造成的潮间带变宽变缓的、以淤积为主的干扰进程,以及二者之间的交互作用。提出在海面上升、地面下沉伴随下,在淤积进程达到其顶点后、重归以侵蚀为主的自然进程的可能前景,届时的“沼泽化”威胁,将加剧目前以“封闭治理”理念为主导的防洪措施对环境的不良影响。
The Hurricanes, recently occurred in the Gulf of Mexico, spurred the writers to re-consider the current status of the Bohai Bay- naturally erosive process that changes zigzag to linear shoreline, interference accumulation proce- dure that widens and smoothes the intertidal zone, as being induced mainly by human activities, and interaction be- tween the two factors. Being corresponded by sea level rise and ground subsidence, coastal process will return to e- rosion after the culmination of muddy accumulation. On other hand, both rising sea and subsiding ground them- selves may trigger off a trend of paludification on the coastal lowland. This would exacerbate impact given by the current flood-control policy, being based on a “closed management” conception.
出处
《地质论评》
CAS
CSCD
北大核心
2007年第1期83-91,共9页
Geological Review
基金
中国地质调查局项目(编号0199201054
0100201094)
国家海洋局908专项的成果
关键词
渤海湾西岸海岸带
地质环境
变化与趋势
west coast of the Bohai Bay
geo-environment
changes and trend