淤泥质潮滩地貌演变中的水动力及生物过程研究进展  

Hydrodynamic and biological processes that control the morphodynamic evolution of mudflats: an overview

作　　者：王宁舸 龚政 张长宽[1] 赵堃[1] 耿亮[1] 

机构地区：[1]河海大学海岸灾害及防护教育部重点实验室,江苏南京210098 [2]江苏省海岸海洋资源开发与环境安全重点实验室,江苏南京210098

出　　处：《海洋工程》2016年第1期104-116,共13页The Ocean Engineering

基　　金：国家自然科学基金资助项目(51379003);国家自然科学基金资助项目(51179067);新世纪优秀人才支持计划(NCET-12-0841)

摘　　要：淤泥质潮滩对于海岸防护、增加土地资源、保持生物多样性等具有重要作用。从淤泥质潮滩演变的主要驱动因子——潮流、波浪、生物作用及地下过程四个方面回顾和总结了潮滩演变动力地貌过程的相关研究进展,提出应关注潮滩短期演变规律、波浪与浮泥作用机理、生物生长与潮滩演变定量关系,以及地下过程作用机理等。Mudflats play an important role in coast protection,increasing the availability of land resources and keeping biodiversity. An overall study was conducted to review and summarize the contributions of tide,waves,biological effects and subsurface processes to the morphodynamic evolution processes of mudflats. Further interests were proposed including the short-term evolution of tidal flats,interplay mechanisms between wave and fluid mud,quantitative relationship between biological growth and tidal flat evolution,and mechanisms of subsurface process.

关 键 词：淤泥质潮滩 动力地貌过程 潮流 波浪 生物作用 土壤固结 

分 类 号：P737.12[天文地球—海洋地质] P753[天文地球—海洋科学]