首页 | 本学科首页   官方微博 | 高级检索  
     检索      

夏季汾河干流溶解无机碳同位素组成及其来源
引用本文:李云霄,黄潇,邹英杰,薛亮,樊文华,王改玲.夏季汾河干流溶解无机碳同位素组成及其来源[J].中国环境科学,2020,40(9):3871-3878.
作者姓名:李云霄  黄潇  邹英杰  薛亮  樊文华  王改玲
作者单位:1. 山西农业大学资源环境学院, 山西 太谷 030801;2. 南京信息工程大学环境科学与工程学院, 江苏 南京 210044;3. 潍坊生态环境监测中心, 山东 潍坊 261041;4. 自然资源部第一海洋研究所, 山东 青岛 266061
基金项目:山西省优秀博士来晋工作奖励资助项目(SXYBKY2018020);山西农业大学科技创新基金资助项目(2018YJ21)
摘    要:根据2019年8月对汾河干流水文参数和碳酸盐参数的调查,初步探讨了溶解无机碳(DIC)及同位素值(δ13CDIC)的沿程变化及其影响因素.结果显示,源头水DIC为2756μmol/kg,δ13CDIC为-9.6‰,土壤CO2输入和碳酸岩化学风化可能是其主要来源;在太原市区上游的水库影响区,较强的初级生产使得水体DIC(平均值为2377μmol/kg)和CO2分压(pCO2)(平均值为552μatm)偏低,δ13CDIC(平均值为-5.2‰)偏正,而在市区下游的水坝滞流影响区,城市污水的大量输入和有机物的降解使得DIC(>4900μmol/kg)和pCO2(>5000μatm)显著升高,δ13CDIC(<-10.3‰)偏负;在流经主要粮食产区的汾河下游,δ13CDIC偏正(~-8.0‰)于源头,可能与C4植被(如玉米)的存在有关.可见,人为干扰已成为影响汾河DIC沿程变化的重要因素,表现为大气CO2强源的城市下游水坝滞留区在今后需受到更多关注.

关 键 词:溶解无机碳(DIC)  δ13CDIC  好氧呼吸  初级生产  汾河  
收稿时间:2020-03-01

Isotopic composition of dissolved inorganic carbon and its source in the main stream of the Fenhe River during summer
LI Yun-xiao,HUANG Xiao,ZOU Ying-jie,XUE Liang,FAN Wen-hua,WANG Gai-ling.Isotopic composition of dissolved inorganic carbon and its source in the main stream of the Fenhe River during summer[J].China Environmental Science,2020,40(9):3871-3878.
Authors:LI Yun-xiao  HUANG Xiao  ZOU Ying-jie  XUE Liang  FAN Wen-hua  WANG Gai-ling
Institution:1. College of Resource and Environment, Shanxi Agricultural University, Taigu 030801, China;2. College of Environmental Science and Engineering, Nanjing University of Information Science and Technology, Nanjing 210044, China;3. Ecological Environmental Monitoring Center of Weifang, Weifang 261041, China;4. First Institute of Oceanography, SOA, Qingdao 266061, China
Abstract:Based on hydrographic and carbonate data collected from an investigation in the main stream of the Fenhe River in August 2019, the variations of dissolved inorganic carbon (DIC) and isotope value (δ13CDIC) along the river as well as their possible factors were preliminarily discussed. The results showed that the DIC concentration was 2756μmol/kg and the δ13CDIC value was -9.6‰ at the headstream, and CO2 input from soil and carbonate chemical weathering may be the main sources. In the upstream reservoir-affected area of Taiyuan downtown, due to strong primary production both DIC (the average value was 2377μmol/kg) and partial pressure of CO2 (pCO2) (the average value was 552μatm) were lower, and δ13CDIC (the average value was -5.2‰) was more positive compared to those at the headstream, whereas in the downstream dam stagnation affected area because of large amounts of municipal sewage inputs and degradation of organic matter both DIC (&ggt;4900μmol/kg) and pCO2 (>5000μatm) increased substantially, and δ13CDIC became more negative (<-10.3‰). In the lower reaches of the Fenhe River flowing through the main grain production areas, the δ13CDIC value (~-8.0‰) was more positive than that at the headstream of the river, possibly related to the existence of C4 plants such as corn. Overall, human disturbance had become a very important factor affecting the DIC variations along the Fenhe River. Moreover, the dam stagnation affected area at the downstream of the city, which acts as a strong CO2 source of the atmosphere, should be paid more attention in the future.
Keywords:dissolved inorganic carbon (DIC)  δ13CDIC  respiration  primary production  the Fenhe River  
本文献已被 CNKI 等数据库收录!
点击此处可从《中国环境科学》浏览原始摘要信息
点击此处可从《中国环境科学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号