生态与农村环境学报 ›› 2018, Vol. 34 ›› Issue (6): 521-527.doi: 10.11934/j.issn.1673-4831.2018.06.006

• 区域环境与发展 • 上一篇    下一篇

红水河龙滩水库夏季CO2分压分布特征及影响因素

曹玉平, 邓飞艳, 焦树林, 袁热林, 张倩   

  1. 贵州师范大学地理与环境科学学院/贵州省山地资源与环境遥感应用重点实验室, 贵州 贵阳 550001
  • 收稿日期:2017-09-08 出版日期:2018-06-25 发布日期:2018-06-14
  • 通讯作者: 焦树林 E-mail:jiaoshulin@gznu.edu.cn
  • 作者简介:曹玉平(1993-),男,湖南怀化人,硕士生,研究方向为水文水资源与地理信息系统。E-mail:1329991949@qq.com
  • 基金资助:

    贵州省国内一流学科建设项目(黔教科研发[2017]85号);国家自然科学基金(41263011)

Research of Distribution Characteristics and Influencing Factors of pCO2 in Hong-shui River Longtan Reservoir in Summer

CAO Yu-ping, DENG Fei-yan, JIAO Shu-lin, YUAN Re-lin, ZHANG Qian   

  1. School of Geography and Environmental Science, Guizhou Normal University/Key Laboratory of Remote Sensing Application on Mountain Resources and Environment in Guizhou Province, Guiyang 550001, China
  • Received:2017-09-08 Online:2018-06-25 Published:2018-06-14

摘要:

为研究红水河龙滩水库的CO2浓度分布及影响因素,于2016年7月对红水河河段龙滩水库进行定点采样,测定水体理化参数并计算水体表层CO2分压(pCO2)。结果表明:坝前到红水河入库水体表层pCO2值分3个区间,坝前至库中在64.28~152.56 Pa之间,库中过渡带在161.57~257.57 Pa之间,入库水体在126.45~264.29 Pa之间,入库水体和过渡区的pCO2均高于坝前。相关分析表明:表层水体pCO2与电导率、总溶解固体物(TDS)、氧化还原电位(ORP)呈显著正相关,与pH值呈显著负相关,说明水生生物光合-呼吸作用、碳酸盐岩溶体系是影响水库pCO2变化的重要因素。水库CO2释放通量范围为9.06~78.80 mmol·m-2·d-1,均值为45.96 mmol·m-2·d-1,库区表层水体表现为大气CO2的源,呈现坝前CO2排放弱源过度到上游碳排放强源的空间变化特征,说明河流水体流经水库作用减缓了CO2释放。

关键词: 龙滩水库, CO2分压, CO2排放通量, 相关分析

Abstract:

For studying the CO2 emissions of Hongshui River Longtan Reservoir, the underway sampling was carried out to continuously survey the Longtan Reservoir of Hongshui River using a professional water sampler in July 2016. The partial pressure of CO2(pCO2) are calculated using the water-chemical balance and the Henry's law. The results show that the data of pCO2 values on the surface water were divided into three intervals because the data of pCO2 values on the surface from near the dam to the middle section ranged from 64.28 to 152.56 Pa, the transition zone of the middle section ranged from 161.57 to 257.57 Pa, as well as inflow waters ranged from 126.45 to 264.29 Pa, which was higher than that of pCO2 before the dam. There was a significant positive correlation on surface water pCO2 with its TDS, Cond and ORP, and a significant negative correlation on surface water pCO2 with pH, which suggests aquatic biosynthesis-respiration, carbonate karst system are important factors affecting the change of reservoir pCO2. Reservoir CO2 flux had a increasing trend from the dam to the end of the tail reservoir with the mean value of the CO2 flux being 45.96 mmol·m-2·d-1 and ranged from 9.06 to 78.80 mmol·m-2·d-1. Reservoir water showed an atmospheric CO2 source with an obvious variation characteristics changing from weak carbon source before the dam to strong carbon source to the upstream, which implies the river type reservoir would slow down the carbon emission of river water.

Key words: Longtan Reservoir, partial pressure of carbon dioxide, the CO2 emission flux, co-relationship analysis

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