首页|丰水及枯水期岩溶区水库总有机碳时空分异特征研究——以平班水库为例

丰水及枯水期岩溶区水库总有机碳时空分异特征研究——以平班水库为例

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为研究岩溶区水库有机碳的浓度水平和时空分布特征及影响因素,揭示岩溶区河道型水库的碳循环规律,分别于 2022 年丰水期和枯水期在平班水库进行水样采集及总有机碳质量浓度(ρTOC)和其他理化因子的测定,并对ρTOC和主要环境因子进行相关性分析.结果表明,平班水库ρTOC表现出明显的时空分异规律,范围为 1.899~8.057 mg·L-1,丰水期平均质量浓度为 5.215 mg·L-1,枯水期为 3.336 mg·L-1;丰水期库区ρTOC在空间上存在显著差异,靠近坝址的 1 号采样点ρTOC最高,上游入湖区浓度最低,枯水期全湖TOC分布稳定.平班水库表层温度(TW)、pH值、硝酸盐氮质量浓度ρ(NO-3-N)的空间差异较小,电导率(γCOND)、总溶解固体物质量浓度(ρTDS)的标准差较大,各点位数据离散程度明显;相关分析表明,ρTOC与TW,pH值,ρ(NO-3-N)及ρ(NO-2-N)显著正相关.研究发现,平班水库ρTOC与其他湖泊相比处于中等水平,这与库区水体面积、库容有一定关系;平班水库有机碳是径流携带营养盐入湖和浮游植物生长进行光合作用共同影响的结果.
Study on the Total Organic Carbon Characteristics of Reservoirs in Karst Areas during Abundant and Dry Season:Take the Pingban Reservoir as an Example
In order to study the concentration level,spatial and temporal distribution characteristics and influ-encing factors of organic carbon in Karst areas,and reveal the carbon cycle rules of river reservoirs in Karst areas,water samples were collected and ρTOC together with other physicochemical factors were determined in Pingban Reser-voir in July and December 2022,and the correlation analysis between ρTOC and main environmental factors was con-ducted.The results show that the concentration of ρTOC in Pingban reservoir shows obvious spatial and temporal differ-entiation,ranging from 1.899 to 8.057 mg·L-1,the average concentration are 5.215 mg·L-1 and 3.336 mg·L-1 during the wet and dry period,respectively.There were significant spatial differences in ρTOC in the reservoir area during the wet period,with the highest ρTOC distribution at sampling site 1 near the dam site and the lowest concentration in the upstream area into the lake.The ρTOCdistribution of the whole lake is stable during the dry season.The spatial difference of surface temperature(TW),pH,and nitrate nitrogen ρ(NO-3-N)is small,the standard deviation of conductivity(γCOND)and total dissolved solid(ρTDS)is large,and the dispersion of data at each point is obvious.The correlation analysis shows that ρTOC is significantly positively associated with TW,pH,ρ(NO-3-N),and ρ(NO-2-N).The study found that the ρTOC concentration of the Pingban reservoir is at the medium level compared with other lakes,which is related to the water area and storage capacity;the organic carbon of Pingban reservoir is the result of the joint influence of runoff carrying nutrient salt into the lake and phytoplankton growth for photosynthesis.

total organic carbonpluvial and dry seasonPingban reservoirspatial and temporal differentiation

李娟、焦树林、杨柳英、韦宗校

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贵州师范大学地理与环境科学学院/喀斯特研究院,中国 贵阳 550025

贵州省喀斯特山地生态环境国家重点实验室培育基地,中国 贵阳 550025

总有机碳 丰、枯水期 平班水库 时空分异

贵州省科技支撑项目

黔科合支撑[2023]一般214

2024

湖南师范大学自然科学学报
湖南师范大学

湖南师范大学自然科学学报

CSTPCD北大核心
影响因子:0.62
ISSN:1000-2537
年,卷(期):2024.47(2)
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