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三峡水库支流水文情势差异对水-气界面二氧化碳释放通量特征的影响

程瑶1,2,3*,王雨春2,3,胡明明2,3#br#   

  1. 1河北工程大学, 河北邯郸 056001; 2中国水利水电科学研究院, 北京 100038; 3中国水利水电利学研究院流域水循环模拟与调控国家重点实验室, 北京 100038)
  • 出版日期:2017-01-10 发布日期:2017-01-10

Influence of different water regimes of tributaries in Three Gorges Reservoir on airwater interface CO2 fluxes.

CHENG Yao1,2,3*, WANG Yu-chun2,3, HU Ming-ming2,3#br#   

  1. (1 Hebei University of Engineer, Handan 056001, Hebei, China; 2 China Institute of Water Resources and Hydropower Research, Beijing 100038, China; 3State Key Laboratory of Simalation and Regulation of water Cycle in River Basin, Beijin 100038, China).
  • Online:2017-01-10 Published:2017-01-10

摘要: 选取三峡水库支流朱衣河、草堂河及其毗邻干流为研究区域,于2015年3月开展了春季水华易发期水气界面温室气体及相关环境因子的动态观测。结果表明:该时段内,三峡水库干流总体表现为释放CO2的“源”,其通量为85.01 mmol·m-2·d-1;在受干流泄水影响较小的朱衣河回水区,表现为强烈吸收CO2的“汇”,其通量变化范围为-73.26~-30.38 mmol·m-2·d-1;而因“狭管效应”受干流强烈影响的草堂河支流回水区,则表现为相对较弱的CO2释放“源”,其通量变化范围为81.43~36.72 mmol·m-2·d-1。相关分析表明,三峡水库干支流不同水域CO2释放通量与浮游植物初级生产力呈显著相关关系。由于受到工程调度影响,干流、支流回水区不同水域水文情势的差别,导致了浮游植物生物量和碳转换利用强度的空间差异,可能是形成三峡水库水气界面CO2“源、汇”特征分布高度异质性的重要原因。

Abstract: Zhuyi River, Caotang River, two tributaries of Three Gorges Reservoir (TGR), and its adjacent mainstream were selected as survey area. In the spring algal bloom period, the airwater interface greenhouse gas fluxes in relation to environmental factors were observed in March, 2015. The results showed that during this period, the mainstream of TGR was a source of CO2 and its flux was 85.01 mmol·m-2·d-1. Zhuyi River, slightly influenced by the mainstream, was a sink of CO2, and its flux ranged from  -73.26 to -30.38 mmol·m-2·d-1. However, Caotang River, intensely influenced by the mainstream, was a weak source of CO2, and its flux ranged from 81.43 to 136.72 mmol·m-2·d-1. Correlation analysis showed that the CO2 fluxes of different areas in TGR had a significant correlation with primary productivity of plankton. Influenced by the TGR operation, the difference of water regimes in different water areas in mainstream and tributaries resulted in spatial difference of biomass of plankton and intensity of carbon conversion and utilization, which would be the main factor for the high heterogeneity in the source or sink for airwater interfaces CO2 in TGR.