水布垭水库水体碳时空变化特征及其影响因素分析

doi:10.11870/cjlyzyyhj201702017

长江流域资源与环境 >> 2017, Vol. 26 >> Issue (02): 304-313.doi: 10.11870/cjlyzyyhj201702017

水布垭水库水体碳时空变化特征及其影响因素分析

赵登忠^1,3, 肖潇^1,3, 汪朝辉^1,3, 谭德宝^1,3, 陈永柏²

1. 长江水利委员会长江科学院, 湖北武汉 430010;
2. 中国长江三峡集团公司, 北京 100038;
3. 流域水资源与生态环境科学湖北省重点实验室, 湖北武汉 430010

收稿日期:2016-07-13 修回日期:2016-09-21 出版日期:2017-02-20
作者简介:赵登忠(1978~),男,高级工程师,博士,主要从事内陆水域碳循环与温室气体排放方面研究.E-mail:njuzhaodz@163.com
基金资助:
科技部软科学研究计划项目（2012GXS2B008）；中国长江三峡集团公司环境保护科研项目（0799562）；中国清洁发展机制基金赠款项目（2013015）；水利部中央级公益性科研院所基本科研业务费项目（CKSF2015018/KJ，CKSF2016263/KJ）

SPATIAL AND TEMPORAL DISTRIBUTION OF CARBON CONCENTRATION IN SURFACE WATER FROM THE SHUIBUYA RESERVOIR

ZHAO Deng-zhong^1,3, XIAO Xiao^1,3, WANG Zhao-hui^1,3, TAN De-bao^1,3, CHEN Yong-bo²

1. Changjiang River Scientific Research Institute(CRSRI), Wuhan 430010, China;
2. China Three Gorges Corporation, Beijing 100038, China;
3. Hubei Key Laboratory of Water Resources & Eco-Environment Science, Wuhan 430010, China

Received:2016-07-13 Revised:2016-09-21 Online:2017-02-20
Supported by:
Soft Science Research Project of Ministry of Science and Technology (2012GXS2B008);China Three Gorges Coorporation Environment Protection Project (0799562);China Clean Development Mechanism Fund Grant Program (2013015);Central Research Institutes of Basic Research and Public Service Special Operations for Ministry of Water Resources (CKSF2015018/KJ, CKSF2016263/KJ)

摘要/Abstract

摘要： 为了评估大型水库对河流碳循环的拦截作用，选择清江流域最上游水布垭水库为典型案例，采用德国元素公司vario TOC分析仪对定期采集水样进行分析，研究新建大型水库水体碳时空分布特征及其影响因素。结果表明，水布垭水库表层水体总碳、总无机碳、溶解有机碳和颗粒有机碳平均含量分别为26.665、24.089、2.141和0.438 mg/L，在水库年内蓄水阶段呈现显著的峰值，其空间分布格局在支流库湾和坝前典型断面表现出显著的差异，在水体碳中总无机碳占据主导地位，与湖泊水体碳时空分布特征极为相似。由于受到人类活动和自然环境的双重影响，水体无机碳则与水体电导率指标具有较强的相关性，溶解有机碳则与水体温度具有直接的关系，而数量最少的颗粒有机碳则与水体叶绿素含量具有弱相关关系。研究成果可以为理解水库碳循环过程机制提供数据支持，对于开展大坝建设的河流碳循环影响评估具有重要参考意义。

关键词: 清江流域, 水布垭水库, 水库碳循环, 水体碳, 时空变化特征

Abstract: The Shuibuya Reservoir over the Qingjiang River Basin was selected as a typical reservoir to analyze the spatial and temporal distribution of carbon cycle in large hydropower reservoir intercepting rive eco-system in this study. The spatial and temporal distribution of carbon in surface water were obtained by analyzing water sampling using vario TOC analyzer in laboratory and other aquatic environment parameters was attained by HACH hydro-lab multi-parameters water quality analyzer in field experiments. The results showed that the monthly mean concentration of total carbon, total inorganic carbon, dissolved organic carbon and particulate organic carbon in surface water from the Shuibuya Reservoir were 26.665 mg/L, 24.089 mg/L, 2.141 mg/L and 0.438 mg/L, respectively during measurement. The carbon concentrations peaked in spring and autumn, while valleyed in summer and winter. Inorganic carbon accounts for most of total carbon and the spatial variation of all carbon parameters mentioned above over the whole reservoir was very different at measurement stations, which is similar with that of lakes. The Shuibuya Reservoir was affected by both human activities and natural environment. Inorganic concentration was strongly related with water conductivity, dissolved organic carbon in water was strongly related with water temperature and chlorophyll concentration in surface water exerted more influences on the spatial and temporal heterogeneity of less particulate organic carbon in surface water over the Shuibuya Reservoir. This study is expected to provide more supports and in-situ data for understanding aquatic carbon cycle of reservoir and play a pivotal role to evaluate the effects of dam construction on aquatic ecosystem.

Key words: Qingjiang Basin, Shuibuya Reservoir, aquatic carbon cycle in reservoir, carbon in surface water, spatial and temporal distribution

中图分类号:

P342

赵登忠, 肖潇, 汪朝辉, 谭德宝, 陈永柏. 水布垭水库水体碳时空变化特征及其影响因素分析[J]. 长江流域资源与环境, 2017, 26(02): 304-313.

ZHAO Deng-zhong, XIAO Xiao, WANG Zhao-hui, TAN De-bao, CHEN Yong-bo. SPATIAL AND TEMPORAL DISTRIBUTION OF CARBON CONCENTRATION IN SURFACE WATER FROM THE SHUIBUYA RESERVOIR[J]. RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN, 2017, 26(02): 304-313.

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