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典型岩溶区多介质中多环芳烃的环境存在特征——以广西大石围天坑群为例

孔祥胜 祁士华

中国岩溶2013,Vol.32Issue(2):182-188,7.
中国岩溶2013,Vol.32Issue(2):182-188,7.

典型岩溶区多介质中多环芳烃的环境存在特征——以广西大石围天坑群为例

The existing conditions of PAHs in multimedium in typical karst area:A case in the Leye Tiankeng Group, Guangxi

孔祥胜 1祁士华2

作者信息

  • 1. 中国地质科学院岩溶地质研究所/中国地质科学院岩溶生态系统与石漠化治理重点实验室/国土资源部、广西壮族自治区岩溶动力学重点实验室,广西桂林541004
  • 2. 中国地质大学(武汉)生物地质和环境地质国家重点实验室,湖北武汉430074
  • 折叠

摘要

Abstract

Based on the data of dry and wet atmospheric deposition,air,soil,groundwater and sediment samples gathered during the same term from 2007 to 2008 in a typical karst area-the Dashiwei Tiankeng,contrastive analysis is done in light of the component spectrums,the distribution features and the characteristic ratio as well as their chemical and physical properties of 16 kinds of PAHs.The results show that 4 kinds of PAHs with 4~6 rings (chrysenes,benzo[b]fluoranthene,benzo[k]fluoranthene and benzo[a]pyrene) are dominated in the annual dry and wet atmospheric deposition,soil and sediment of the underground river.And 4 kinds of PAHs with 2~3 rings (naphthalenes,fluorene,phenanthrene and anthracene) are dominated in dry and wet atmospheric deposition in autumn and winter,air and underground river water.The existing conditions of PAHs are of better consistency but also certain differences in each medium.By means of this method it is preliminary explained the sources or input of PAHs contaminant in soil,water and underground river sediment in karst area,and proved that the dry and wet atmospheric deposition is the main pollution source in soil and the underground river in remote karst mountain area.Therefore,it is suggested that the atmospheric dry and wet deposition should be taken as a PAHs source in the investigation of pollution sources.

关键词

多环芳烃/成分谱/环境介质/大石围天坑/岩溶地区

Key words

polycyclic aromatic hydrocarbons/ component spectrum/ environmental medium/ the Dashiwei Tiankeng/ karst area

分类

资源环境

引用本文复制引用

孔祥胜,祁士华..典型岩溶区多介质中多环芳烃的环境存在特征——以广西大石围天坑群为例[J].中国岩溶,2013,32(2):182-188,7.

基金项目

中国地质调查局项目(1212011121166)、中国地质科学院岩溶地质研究所所控项目(2009013) (1212011121166)

中国岩溶

OACSCDCSTPCD

1001-4810

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