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Volume 40 Issue 4
Aug.  2021
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Article Navigation >  CARSOLOGICA SINICA  > 2021  >  40(4): 555-564
ZHANG Cheng, XIAO Qiong. Study on dissolved inorganic carbon migration and aquatic photosynthesis sequestration in Lijiang River, Guilin[J]. CARSOLOGICA SINICA, 2021, 40(4): 555-564.
Citation: ZHANG Cheng, XIAO Qiong. Study on dissolved inorganic carbon migration and aquatic photosynthesis sequestration in Lijiang River, Guilin[J]. CARSOLOGICA SINICA, 2021, 40(4): 555-564.
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Study on dissolved inorganic carbon migration and aquatic photosynthesis sequestration in Lijiang River, Guilin

  • Institute of Karst Geology，CAGS/Key Laboratory of Karst Dynamics，MNR＆GZAR

  • Publish Date: 2021-08-25
    Abstract
  • Daily changes of dissolved inorganic carbon in river mainly are controlled by carbonate back-precipitation，aquatic photosynthesis and CO2 degassing at water-air interface. Dissolved inorganic carbon uptake by aquatic photosynthesis is a part of karst carbon sink，and the size of degassing proportion values acts as the determinant factor for carbon sink stability. To analysis of the loss of bicarbonate caused by aquatic photosynthesis and relevant calcite precipitation processes，high resolution monitoring for water chemistry and high-frequency water sampling in daily scale were conducted in a 15 km-long section between Shengli and Guanyan in middle course of Lijiang River. The results showed that the flux of photosynthesis uptake of dissolved inorganic carbon in monitoring section is about 859 kgC?d-1. DIC removal value by photosynthesis and calcite precipitation value are 2.06 t?（d?km）-1 and 0.78 t?（d?km）-1， respectively. CO2 degassing value accounts for 28.4 % of total carbon removal，namely，approximately 70% of carbon removal was converted into organic carbon and precipitated in riverbed in form of calcite，thus constitute a part of karst carbon sink. DIC removal accounts for about 6.0 % of total input，in which 1.7 % returned to the atmosphere in the form of CO2，indicating DIC uptake by aquatic photosynthesis during the summer low water level can restrain CO2 degassing process in air-water interface effectively during the day time. The low degassing proportion suggested that DIC in water body of Lijiang River is relatively stable.

     

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    • References(32)
  • [1]
    Milliman J D， Syvitski J P M. Geomorphic/tectonic control of sediment discharge to the ocean： the importance of small mountainous rivers［J］.Journal of Geology，1992，100：525-544.
    [2]
    Pawellek F， Frauenstein F， Veizer J. Hydrochemistry and isotope geochemistry of the upper Danube River［J］. Geochimica et Cosmochimica Acta， 2002， 66： 3839-3854.
    [3]
    McAdams B C， Trierweiler A M， Welch S A， et al. Two sides to every range： Orographic influences on CO2 consumption by silicate weathering［J］. Applied Geochemistry， 2015， 63： 472-483.
    [4]
    Goldsmith S T， Lyons W B， Harmon R S， et al. Organic carbon concentrations and transport in small mountain rivers， Panama［J］. Applied Geochemistry， 2015， 63： 540-549.
    [5]
    Atekwana E A， Krishnamurthy R V. Seasonal variations of dissolved inorganic carbon and δ13C of surface waters： application of a modified gas evaluation technique［J］. Journal of Hydrology， 1998， 205：260-278.
    [6]
    Barth J A C， Cronin A A， Dunlop J， et al. Influence of carbonates on the riverine carbon cycle in an anthropogenically dominated catchment basin： evidence from major elements and stable carbon isotopes in the LaganRiver （N. Ireland） ［J］. Chemical Geology， 2003， 200：203-216.
    [7]
    Raymond P A， Cole J J. Increase in the export of alkalinity from North America’s largest river［J］. Science， 2003， 301：88-91.
    [8]
    Wachniew P. Isotopic composition of dissolved inorganic carbon in a large polluted river： The Vistula， Poland［J］. Chemical Geology， 2006， 233：293-308.
    [9]
    Kandu? T， Szramek K， Ogrinc N， et al. Origin and cycling of riverine inorganic carbon in the Sava River watershed （Slovenia） inferred from major solutes and stable carbon isotopes［J］. Biogeochemistry， 2007， 86：137-154.
    [10]
    Wu Y， Zhang J， Liu S M， et al. Sources and distribution of carbon within the Yangtze River system［J］. Estuarine Coastal and Shelf Science， 2007， 71：13-25.
    [11]
    Thomas J， Joseph S， Thrivikramji K P. Hydrochemical variations of a tropical mountain river system in a rain shadow region of the southern Western Ghats， Kerala， India［J］. Applied Geochemistry， 2015， 63： 456-471.
    [12]
    章程， 汪进良， 蒲俊兵. 2015. 地下河出口河流水化学昼夜动态变化：生物地球化学过程的控制［J］. 地球学报， 36： 197-203.
    [13]
    Parker S R， Poulson S R， Smith M G， et al. Temporal variability in the concentration and stable carbon isotope composition of dissolved inorganic and organic carbon in two Montana， USA rivers［J］. Aquatic Geochemistry， 2010， 16： 61-84.
    [14]
    Nimick D A， Gammons C H， Parker S R. Diel biogeochemical processes and their effect on the aqueous chemistry of streams： A review［J］. Chemical Geology， 2011， 283： 3-17.
    [15]
    Hayashi M， Vogt T， Mahler L. Diurnal fluctuations of electrical conductivity in a pre-alpine river： Effects of photosynthesis and groundwater exchange［J］. Journal of Hydrology， 2012， 450-451： 93-104.
    [16]
    Montety V de， Martin J B， Cohen M J. Influence of diel biogeochemical cycles on carbonate equilibrium in a karst river［J］. Chemical Geology， 2011， 283： 31-43.
    [17]
    Zhang C， Wang J L， Pu J B. Bicarbonate daily variations in a karst river： the carbon sink effect of subaquatic vegetation photosynthesis［J］. Acta Geologica Sinica （English Edition）， 2012， 86： 973-979.
    [18]
    章 程. 岩溶区河流水化学昼夜变化与生物地球化学过程［J］. 中国岩溶， 2015， 34（1）：1-8.
    [19]
    王奇岗， 肖 琼， 赵海娟， 等. 水生植物对岩溶区河水地球化学昼夜变化的影响：以漓江为例［J］. 中国岩溶， 2018， 37（4）： 501-514.
    [20]
    何若雪， 孙平安， 何师意，等. 漓江流域中下游无机碳通量动态变化及影响因素［J］.中国岩溶， 2017， 36（1）： 109-118.
    [21]
    缪钟灵. 漓江发育演化及与相邻流域关系［J］. 中国岩溶， 1998， （4）： 385-391.
    [22]
    Parkhurst D L， Appelo C A J. User’s guide to PHREEQC （Version 2）-A computer program for speciation， batch-reaction， transportone-dimensional， and inverse geochemical calculations［R］： US. Geological Survey Water-Resources Investigations Report 99-4259. 1999， p. 310.
    [23]
    J?hne B， Heinz G， Dietrich W. Measurments of the diffusion coefficients of sparingly soluble gases in water［J］. Journal of Geophysical Research， 1987， 92：10767-10776.
    [24]
    Broecker H C， Peterman J， Siems W. The influence of wind on CO2-exchange in a wind-wave tunnel， including the effects of monolayers［J］. Journal of Marine Research， 1978， 36：595-610.
    [25]
    Holley E H. Oxygen transfer at the air-water interface［C］. In： Gibbs RJ （ed） Transport processes in lakes and oceans. Proceedings of the symposium on transport processes in the ocean held at the 82nd Nat. Meet of the AICE， Atlantic City，N.J. Aug . 29-Sep. 1， 1976， Plenum Press. 1977， pp 117-150.
    [26]
    Mook W G. Stable carbon and oxygen isotopes of natural water in the Netherlands［R］. In Isotopic Hydrology， IAEA， 1970， pp 163-190.
    [27]
    Aucour A， Sheppard S M F， Guyomar O， et al. Use of 13C to trace origin and cycling of inorganic carbon in the Rh?ne river system［J］. Chemical Geology， 1999， 159： 87-105.
    [28]
    Richey J E， Hedges J I， Devol A H， et al. Biogeochemistry of carbon in the Amazon River［J］. Limnology and Oceanography， 1990， 35： 352-371.
    [29]
    Yang C， Telmer K， Viezer J. Chemical dynamics of the St-Lawrence riverine system： δDH2O， δ18OH2O， δ13CDIC， δ34Ssulfate， and dissolved 87Sr/86Sr［J］. Geochimica et Cosmochimica Acta， 1996， 60： 851-866.
    [30]
    McConnaughey T. Acid secretion， calcification， and photosynthetic carbon concentrating Mechanisms［J］. Canadian Journal of Botany， 1998， 76：1119-1126.
    [31]
    章程， 汪进良， 肖琼等. 桂林潮田河水溶解无机碳昼夜变化与通量［J/OL］．地球学报. https：//kns.cnki.net/kcms/detail/11.3474.P.20201104.0852.002.html.
    [32]
    章程， 肖琼， 苗迎， 等. 广西桂林漓江典型河段水化学昼夜动态变化及其对岩溶碳循环的影响［J］. 地球学报， 2018， 39： 613-621.
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