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嘉陵江梯级水库群溶解无机碳同位素的时空变化特征
引用本文:李晓东,刘小龙,杨周,李亲凯,黄俊. 嘉陵江梯级水库群溶解无机碳同位素的时空变化特征[J]. 上海大学学报(自然科学版), 2015, 21(3): 286-293. DOI: 10.3969/j.issn.1007-2861.2015.01.009
作者姓名:李晓东  刘小龙  杨周  李亲凯  黄俊
作者单位:1. 中国科学院地球化学研究所环境地球化学国家重点实验室, 贵阳550002;2. 天津师范大学天津市水资源与水环境重点实验室, 天津300387;3. 中国科学院大学, 北京100049
基金项目:国家自然科学基金资助项目(41373136, 40703004)
摘    要:以嘉陵江流域及其梯级开发河段为研究对象, 通过在2008 年8 月(雨季) 及2009 年2 月(旱季) 进行密集采样, 分析测定了河水中溶解无机碳(dissolved inorganic carbon, DIC)含量及其同位素组成, 探讨了河水中DIC的来源及其季节与空间变化特征. 结果表明: 嘉陵江河水DIC 及其同位素13CDIC 组成的平均值, 雨季时为2 018 μmol/L 和−8.6‰, 旱季时为3 150 μmol/L 和−6.0‰, 二者均存在显著的季节变化; 嘉陵江水体13CDIC 的值旱季(枯水期) 高于雨季(丰水期), 与自然河流的季节变化特征相似, 而与水库、湖泊不同, 表明嘉陵江梯级水库群水体“湖沼学反应”并不明显.

关 键 词:嘉陵江  溶解无机碳同位素  时空变化  梯级水库  
收稿时间:2015-05-15

Spatial and seasonal variation of dissolved inorganic carbon isotope compositions in the cascade reservoirs of the Jialing River
LI Xiao-Dong,LIU Xiao-Long,YANG Zhou,LI Qin-Kai,HUANG Jun. Spatial and seasonal variation of dissolved inorganic carbon isotope compositions in the cascade reservoirs of the Jialing River[J]. Journal of Shanghai University(Natural Science), 2015, 21(3): 286-293. DOI: 10.3969/j.issn.1007-2861.2015.01.009
Authors:LI Xiao-Dong  LIU Xiao-Long  YANG Zhou  LI Qin-Kai  HUANG Jun
Affiliation:1. State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China;2. Tianjin Key Laboratory of Water Resources and Environment, Tianjin Normal University, Tianjin 300387, China; 3. University of Chinese Academy of Sciences, Beijing 100049, China
Abstract:The Jialing River and its cascade reservoirs were investigated. Wedensely collected water samples along the Jialing River in August 2008 (rain season) and February 2009 (dry season). We determine the contents and isotopic compositions of dissolved inorganic carbon (DIC), and discuss the sources and spatio-temporal variations of DIC. The results show that the average DIC and 13CDIC were 2 018 μmol/L and −8.6‰ in a rainy season, and 3 150 μmol/L and −6.0‰ in a dry season, showing obvious seasonal variations. The 13CDIC values in winter were heavier than in summer, similar to undammed rivers but different from lakes and reservoirs. This indicates that the hydro-geochemical characteristics of waters in the cascade reservoirs of Jialing River are similar to natural rivers
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