LAKE ENVIRONMENTAL CHARACTERISTICS RECOREDED BY ISOTOPES IN SEDIMENTS OF DAPU AREA IN LAKE TAIHU: LAKE ENVIRONMENTAL CHARACTERISTICS RECOREDED BY ISOTOPES IN SEDIMENTS OF DAPU AREA IN LAKE TAIHU

Longsheng Xu, Jing-lu Wu
{"title":"LAKE ENVIRONMENTAL CHARACTERISTICS RECOREDED BY ISOTOPES IN SEDIMENTS OF DAPU AREA IN LAKE TAIHU: LAKE ENVIRONMENTAL CHARACTERISTICS RECOREDED BY ISOTOPES IN SEDIMENTS OF DAPU AREA IN LAKE TAIHU","authors":"Longsheng Xu, Jing-lu Wu","doi":"10.3724/SP.J.1140.2013.02137","DOIUrl":null,"url":null,"abstract":"Through the determinations of δ13C,δ15N,total organic C,total N,total P in sediments of Dapu area in the Taihu Lake,this paper analyzed the eutrophication process of this area.The results showed that δ13C,δ15N in sediments had a significant change in patferns with the water evolution from low nutrition to eutrophication.Before 1950s,primary productivity of the lake was low and the water environment was good.Moreover,the impact of human activities was weak,and the lake sediments record showed a high value of δ13C and low values of δ15N,TOC,TN,TP.In 1990s,the lake environment changed significantly and the primary productivity increased substantially.As the result,the water environment deteriorated and the nutrition level increased rapidly resulting in eutrophication.Accordingly,the value of δ13C decreased rapidly,but δ15N increased,and the correlation showed significant reverse(R=-0.81).However,the correlation between δ13C and δ15N was significantly positive(R=0.96).This phenomenon reflected that the isotopic elements of different lakes responded differently to environmental changes,and the eutrophication patterns of grass-type lake and algae-type lake were initially established.","PeriodicalId":18188,"journal":{"name":"海洋地质与第四纪地质","volume":"33 1","pages":"137-142"},"PeriodicalIF":0.0000,"publicationDate":"2014-03-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"海洋地质与第四纪地质","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.3724/SP.J.1140.2013.02137","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Through the determinations of δ13C,δ15N,total organic C,total N,total P in sediments of Dapu area in the Taihu Lake,this paper analyzed the eutrophication process of this area.The results showed that δ13C,δ15N in sediments had a significant change in patferns with the water evolution from low nutrition to eutrophication.Before 1950s,primary productivity of the lake was low and the water environment was good.Moreover,the impact of human activities was weak,and the lake sediments record showed a high value of δ13C and low values of δ15N,TOC,TN,TP.In 1990s,the lake environment changed significantly and the primary productivity increased substantially.As the result,the water environment deteriorated and the nutrition level increased rapidly resulting in eutrophication.Accordingly,the value of δ13C decreased rapidly,but δ15N increased,and the correlation showed significant reverse(R=-0.81).However,the correlation between δ13C and δ15N was significantly positive(R=0.96).This phenomenon reflected that the isotopic elements of different lakes responded differently to environmental changes,and the eutrophication patterns of grass-type lake and algae-type lake were initially established.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
太湖大浦地区沉积物同位素记录的湖泊环境特征:太湖大浦地区沉积物同位素记录的湖泊环境特征
通过对太湖大浦地区沉积物中δ13C、δ15N、总有机C、总N、总P的测定,分析了该地区富营养化过程。结果表明:沉积物中δ13C、δ15N随水体由低营养向富营养化的演化有显著的变化规律;20世纪50年代以前,湖泊初级生产力较低,水环境较好。人类活动的影响较弱,湖泊沉积物的δ13C值较高,δ15N、TOC、TN、TP值较低。90年代湖泊环境变化明显,初级生产力显著提高。其结果是水环境恶化,营养水平迅速上升,导致水体富营养化。δ13C值迅速下降,δ15N值上升,呈显著负相关(R=-0.81)。δ13C与δ15N呈显著正相关(R=0.96)。这一现象反映了不同湖泊的同位素元素对环境变化的响应不同,初步建立了草型湖泊和藻型湖泊的富营养化格局。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
CiteScore
0.10
自引率
0.00%
发文量
4176
期刊介绍:
期刊最新文献
南海琼东上升流区过去1900年海洋生产力记录 GENETIC TYPES OF GAS HYDRATE IN THE WORLD AND THEIR MAIN CONTROLLING FACTORS: GENETIC TYPES OF GAS HYDRATE IN THE WORLD AND THEIR MAIN CONTROLLING FACTORS Rb/Sr GEOCHEMISTRY OF LOESS DEPOSITS IN THE HORQIN DUNEFIELD, NORTHEASTERN CHINA, AND ITS IMPLICATIONS FOR CLIMATE CHANGE DURING LATE QUATERNARY: Rb/Sr GEOCHEMISTRY OF LOESS DEPOSITS IN THE HORQIN DUNEFIELD, NORTHEASTERN CHINA, AND ITS IMPLICATIONS FOR CLIMATE CHANGE DURING LATE QUATERNARY LAKE ENVIRONMENTAL CHARACTERISTICS RECOREDED BY ISOTOPES IN SEDIMENTS OF DAPU AREA IN LAKE TAIHU: LAKE ENVIRONMENTAL CHARACTERISTICS RECOREDED BY ISOTOPES IN SEDIMENTS OF DAPU AREA IN LAKE TAIHU ADVANCES IN NUMERICAL MODELING OF GAS HYDRATE FORMATION IN MARINE SEDIMENTS: ADVANCES IN NUMERICAL MODELING OF GAS HYDRATE FORMATION IN MARINE SEDIMENTS
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1