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岩溶地下水补给的地表河流溶解无机碳昼夜变化与钙沉降
引用本文:汪进良,章程,裴建国,苗迎.岩溶地下水补给的地表河流溶解无机碳昼夜变化与钙沉降[J].地球与环境,2015,43(4):395-402.
作者姓名:汪进良  章程  裴建国  苗迎
作者单位:中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室, 广西桂林 541004
基金项目:国土资源部公益性科研行业专项(201111022,201311148);广西科学技术计划项目(桂科能1298018-6);中国地质调查局地质调查项目(12120113014200);国家自然科学基金项目(41202185)和IGCP/SIDA 598项目。
摘    要:溶解无机碳昼夜动态变化对河流水体碳通量的估算有重要影响。本文选择由地下水补给且富含水生植物的典型河流,开展高分辨率水文地球化学监测和高频率水样取样工作,分析了水化学的昼夜动态变化特征,钙与无机碳昼夜循环产生的生物地球化学控制机理,估算了钙与无机碳昼夜通量。结果表明,白天pH、SIC上升,产生钙沉降和水体无机碳(主要为HCO-3)含量的下降,夜间得到地下水的补给,Ca2+和HCO-3浓度回升。监测期间,官村地下河出口地表河流钙与溶解有机碳的流失或沉降量分别为69.04kg/d和168.68kg/d,即51.14g/(m·d)和124.95g/(m·d),分别占输入量的6.2%和4.7%。受水生植物光合作用和钙化作用控制,沿流程发生无机碳向有机碳转化,是真正意义上的自然碳汇。

关 键 词:岩溶地表河  溶解无机碳  昼夜变化  钙沉降  广西官村
收稿时间:2014/8/8 0:00:00
修稿时间:2014/12/18 0:00:00

Diel Changes of Dissolved Inorganic Carbon and Calcite Precipitation in a Typical Karst Spring-fed Stream
WANG Jingliang,ZHANG Cheng,PEI Jianguo,MIAO Ying.Diel Changes of Dissolved Inorganic Carbon and Calcite Precipitation in a Typical Karst Spring-fed Stream[J].Earth and Environment,2015,43(4):395-402.
Authors:WANG Jingliang  ZHANG Cheng  PEI Jianguo  MIAO Ying
Institution:Key Laboratory of Karst Dynamics, MLR/GZAR, Institute of Karst Geology, CAGS, Guilin, 541004, China
Abstract:Study on diel variation of dissolved inorganic carbon can help to estimate carbon flux in river water more precisely. Five-day monitoring with high resolution data logger and high frequency sampling with 1-hour interval were conducted in a typical karst spring-fed stream with abundant aquatic vegetation. Daily changes of hydrochemistry, especially diel cycling of calcium and dissolved inorganic carbon (DIC) were discussed and the influence of biogeochemical processes on diel cycling was analyzed. The diel fluxes of calcium and inorganic carbon were also estimated. Results show that the changes in aqueous chemistry are closely associated with biogeochemical processes and featured as diel cycling. During the daytime, pH value of water and the saturation index of calcite increase, thereby causing calcite to precipitate and removing Ca2+ and HCO3- from water. During the nighttime, concentrations of Ca2+ and DIC gradually increase due to the input of Ca and HCO3- by groundwater exchange. The daily loss of Ca2+ and DIC are estimated to be about 69.04 kg/d and 168.68 kg/d, respectively which represent about 51.14 g/(d·m) and 124.95 g/(d·m), respectively along the 1350m of the Guancun River. The study clearly shows that photosynthesis and calcite precipitation have strong influence on the chemistry of the spring-fed river. Diel DIC cycling downstream and their changes along the stream flow indicate that the river is losing inorganic carbon along its flowpath, and converting it into organic carbon, thus acts as an important DIC sink in small productive streams.
Keywords:spring-fed river  dissolved inorganic carbon  diel change  calcite precipitation  Guancun River  Guangxi Province
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