海洋地质与第四纪地质2018，Vol.38Issue(1)：187-194,8.DOI:10.16562/j.cnki.0256-1492.2018.01.019
长江口低氧区的成因及过程
The origin and process of hypoxia in the Yangtze River Estuary
摘要
Abstract
The Yangtze Estuary is one of the most typical hypoxic regions in the world.The aggravation and expansion of the hypoxia are obvious in the past few years.This paper aims to synthetically analyze the origin of the hypoxia,its biogeochemical processes and its hazardous influence on the local ecological system.By comparing with other hypoxic areas in the world,the hypoxia of the Yangtze Estuary is found rather different geographically and oceanographically from those in the Gulf of Mexico,the Baltic Sea,the Black Sea and Tokyo Bay.The study of the case would greatly help the deeper research of marine ecology in this area.By briefly combining geochemistry,ecology,oceanography and other subjects,the necessity of developing hypoxia ecology is proposed by the authors to fill the blank in this field.关键词
长江口低氧区/富营养化/水体层化/低氧生态学Key words
the hypoxia zone of the Yangtze Estuary/eutrophication/stratification/hypoxia ecology分类
资源环境引用本文复制引用
刘贲,张霄宇,曾江宁,杜文..长江口低氧区的成因及过程[J].海洋地质与第四纪地质,2018,38(1):187-194,8.基金项目
国家自然科学基金“富稀土的含沸石深海黏土中稀土元素的物质来源研究”(41773005) （41773005）
国家自然科学基金“基于现场数据的CDOM光学属性和陆源输入DOC的定量关系研究”(40706057) （40706057）
国家海洋局第二海洋研究所基本科研业务费专项(JG1616,JG1312) （JG1616,JG1312）
海洋公益性行业科研专项(201505008-2) （201505008-2）
