河流水-气界面碳交换研究进展及趋势

doi:10.3969/j.issn.1007-2861.2015.01.008

Abstract

Abstract: Gaseous carbon exchange between river water and air interface is an important link of regional and global carbon cycle. It is essential to the precious estimation of terrestrial carbon budget and optimization of carbon cycle model. In this paper, the importance and recent progress in the study of riverine CO₂/CH₄ exchange between water-air interface are introduced, and insufficiency in the related study is pointed out. In the future, more researches need to be carried out on CO₂/CH₄exchange between water-air interface of rivers under various geo-eco system and human impacts. Methods of paired carbon isotopes, stoichiometry, biomarker, etc., should be used to trace the sources of gaseous carbon (and other carbon forms) and their relative contributions, and to discover related carbon turn over processes. It is suggested that researches combining filed in-situ observing, traditional sample analysis, and laboratory experiments be conducted in the study of carbon exchange between multi-interfaces of soil-water, soil-air, sediment-water and water-air. Key factors that affect carbon exchange between water-air interface should be revealed. The study will provide abasis for related model development and watershed management.

Key words: carbon exchange between water-air interface, human disturbance, riverine carbon cycle, terrestrial carbon budget

CLC Number:

X 142

DING Hu, LIU Cong-Qiang, LANG Yun-Chao, LI Si-Liang, LI Xiao-Dong, WANG Fu-Shun. Recent advances in the research of gaseous carbon exchange between river water and air interface[J]. Journal of Shanghai University（Natural Science Edition）, 2015, 21(03): 275-285.

References

[1] Raymond P A, Hartmann J, Lauerwald R, et al. Global carbon dioxide emissions from inland waters [J]. Nature, 2013, 503(7476): 355-359.

[2] Wehrli B. Biogeochemistry: conduits of the carbon cycle [J]. Nature, 2013, 503(7476): 346-347.

[3] Richey J E, Melack J M, Aufdenkampe A K, et al. Outgassing from Amazonian rivers and wetlands as a large tropical source of atmospheric CO2 [J]. Nature, 2002, 416(6881): 617-620.

[4] Raymond P, Cole J. Gas exchange in rivers and estuaries: choosing a gas transfer velocity [J]. Estuaries, 2001, 24(2): 312-317.
[5] Wallin M B, ¨ Ouist M G, Buffam I, et al. Spatiotemporal variability of the gas transfer coefficient (KCO₂) in boreal streams: implications for large scale estimates of CO2 evasion [J].

Global Biogeochemical Cycles, 2011, 25(3): GB3025.

[6] Butman D, Raymond P A. Significant efflux of carbon dioxide from streams and rivers in the United States [J]. Nature Geoscience, 2011, 4(12): 839-842.

[7] Oquist M G, Wallin M, Seibert J, et al. Dissolved inorganic carbon export across the soil/stream interface and its fate in a boreal headwater stream [J]. Environmental Science &

Technology, 2009, 43(19): 7364-7369.

[8] Crawford J T, Lottig N R, Stanley E H, et al. CO2 and CH4 emissions from streams in a lake-rich landscape: patterns, controls, and regional significance [J]. Global Biogeochemical

Cycles, 2014: 2013GB004661.

[9] Jonsson A, Aerg J, Lindroth A, et al. Gas transfer rate and CO2 flux between an unproductive lake and the atmosphere in northern Sweden [J]. Journal of Geophysical Research:

Biogeosciences, 2008, 113(G4): G04006.

[10] Polsenaere P, Abril G. Modelling CO2 degassing from small acidic rivers using water pCO₂ , DIC and delta C-13-DIC data [J]. Geochimica Et Cosmochimica Acta, 2012, 91: 220-239.

[11] Frankignoulle M, Borges A, Biondo R. A new design of equilibrator to monitor carbon dioxide in highly dynamic and turbid environments [J]. Water Research, 2001, 35(5): 1344-1347.

[12] Lynch J K, Beatty C M, Seidel M P, et al. Controls of riverine CO₂over an annual cycle determined using direct, high temporal resolution pCO2 measurements [J]. Journal of Geophysical Research, 2010, 115(G3): G03016.

[13] Johnson M S, Billett M F, Dinsmore K J, et al. Direct and continuous measurement of dissolved carbon dioxide in freshwater aquatic systems-method and applications [J]. Ecohydrology, 2010, 3(1): 68-78.

[14] Wang F, Cao M, Wang B, et al. Seasonal variation of CO₂diffusion flux from a large subtropical reservoir in East China [J]. Atmospheric Environment, 2015, 103: 129-137.

[15] Dinsmore K J, Billett M F, Dyson K E. Temperature and precipitation drive temporal variability in aquatic carbon and GHG concentrations and fluxes in a peatland catchment [J].

Glob Chang Biol, 2013, 19(7): 2133-2148.

[16] Campeau A, Lapierre J F, Vachon D, et al. Regional contribution of CO₂ and CH4 fluxes from the fluvial network in a lowland boreal landscape of Qu´ebec [J]. Global Biogeochemical

Cycles, 2014, 28(1): 57-69.

[17] Vachon D, Prairie Y T, Cole J J. The relationship between near-surface turbulence and gas transfer velocity in freshwater systems and its implications for floating chamber measurements of gas exchange [J]. Limnol Oceanogr, 2010, 55(4): 1723-1732.

[18] Giesler R, M¨oth C M, Karlsson J, et al. Spatiotemporal variations of pCO2 and 13C-DIC in subarctic streams in northern Sweden [J]. Global Biogeochemical Cycles, 2013, 27(1): 176-186.

[19] Koprivnjak J F, Dillon P J, Molot L A. Importance of CO2 evasion from small boreal streams [J]. Global Biogeochemical Cycles, 2010, 24(4): GB4003.

[20] Wang F S, Wang Y C, Zhang J, et al. Human impact on the historical change of CO₂degassing flux in River Changjiang [J/OL]. Geochemical Transactions, 2007, 8: 7[2007-08-09].

http://link.springer.com/article/10.1186/1467-4866-8-7. DOI: 10.1186/1467-4866-8-7.
[21] Rawlins B G, Palumbo-Roe B, Gooddy D C, et al. A model of potential carbon dioxide efflux from surface water across England and Wales using headwater stream survey data and

landscape predictors [J]. Biogeosciences, 2014, 11(7): 1911-1925.

[22] 唐文魁,高全洲. 河口二氧化碳水-气交换研究进展[J]. 地球科学进展, 2013, 28(9): 1007-1014.

[23] Aufdenkampe A K, Mayorga E, Raymond P A, et al. Riverine coupling of biogeochemical cycles between land, oceans, and atmosphere [J]. Frontiers in Ecology and the Environment,

2011, 9(1): 53-60.

[24] Wallin M B, Grabs T, Buffam I, et al. Evasion of CO2from streams-the dominant component of the carbon export through the aquatic conduit in a boreal landscape [J]. Glob Chang Biol, 2013, 19(3): 785-97.

[25] Alin S R, Rasera M F F L, Salimon C I, et al. Physical controls on carbon dioxide transfer velocity and flux in low-gradient river systems and implications for regional carbon budgets [J]. Journal of Geophysical Research, 2011, 116(G1): JG001398.

[26] Yao G R, Gao Q Z, Wang Z G, et al. Dynamics of CO2 partial pressure and CO2 outgassing in the lower reaches of the Xijiang River, a subtropical monsoon river in China [J]. Science of the Total Environment, 2007, 376: 255-266.

[27] Beaulieu J J, Shuster W D, Rebholz J A. Controls on gas transfer velocities in a large river [J]. Journal of Geophysical Research-Biogeosciences, 2012, 117(G2): JG001794.

[28] Billett M F, Palmer S M, Hope D, et al. Linking land-atmosphere-stream carbon fluxes in a lowland peatland system [J]. Global Biogeochemical Cycles, 2004, 18(1): GB1024.

[29] Cole J J, Caraco N F. Carbon in catchments: connecting terrestrial carbon losses with aquatic metabolism [J]. Marine and Freshwater Research, 2001, 52(1): 101-110.

[30] Abril G, Martinez J M, Artigas L F, et al. Amazon River carbon dioxide outgassing fuelled by wetlands [J]. Nature, 2014, 505(7483): 395-398.

[31] Battin T J, Luyssaert S, Kaplan L A, et al. The boundless carbon cycle [J]. Nature Geoscience, 2009, 2(9): 598-600.

[32] Abril G, Bouillon S, Darchambeau F, et al. Technical Note: large overestimation of pCO2 calculated from pH and alkalinity in acidic, organic-rich freshwaters [J]. Biogeosciences, 2015,

12(1): 67-78.

[33] Stets E, Raymond P A, Abril G, et al. Widespread positive bias in calculated carbon dioxide concentration: causes and implications for large-scale estimates of carbon dioxide efflux from freshwater ecosystems [M]. San Francisco: American Geophysical Union, 2013.

[34] Acu˜na V, Datry T, Marshall J, et al. Why should we care about temporary waterways? [J]. Science, 2014, 343(6175):1080-1081.

[35] Datry T, Larned S T,Tockner K. Intermittent rivers: a challenge for freshwater ecology [J]. BioScience, 2014, 64(3): 229-235.

[36] Neff J C, Asner G P. Dissolved organic carbon in terrestrial ecosystems: synthesis and a model [J]. Ecosystems, 2001, 4(1): 29-48.

[37] 丁虎, 刘丛强, 郎赟超, 等. 桂西北典型峰丛洼地降雨过程中地表水溶解性碳和13CDIC变化特征[J]. 地学前缘, 2011, 18(6): 182-189.
[38] Raymond P A, Saiers J E. Event controlled DOC export from forested watersheds [J]. Biogeochemistry, 2010, 100: 197-209.

[39] Bianchi T S, Garcia-Tigreros F, Yvon-Lewis S A, et al. Enhanced transfer of terrestrially derived carbon to the atmosphere in a flooding event [J]. Geophysical Research Letters, 2013,

40(1): 116-122.

[40] Rasera M F F L, Krusche A V, Richey J E, et al. Spatial and temporal variability of pCO2 and CO2 efflux in seven Amazonian Rivers [J]. Biogeochemistry, 2013: 1-19.

[41] Davidson E A, Figueiredo R O, Markewitz D, et al. Dissolved CO2 in small catchment streams of eastern Amazonia: a minor pathway of terrestrial carbon loss [J]. Journal of Geophysical Research, 2010, 115(G4): G04005.

[42] Mayorga E, Aufdenkampe A K, Masiello C A, et al. Young organic matter as a source of carbon dioxide outgassing from Amazonian rivers [J]. Nature, 2005, 436(7050): 538-541.

[43] Geldern R, Schulte P, Mader M, et al. Spatial and temporal variations of pCO2 , dissolved inorganic carbon, and stable isotopes along a temperate karstic watercourse [J/OL]. Hydrological Processes, 2015 [2015-03-24]. http://onlinelibrary.wiley.com/doi/10.1002/hyp.10457.

[44] Raymond P A, Bauer J E, Caraco N F, et al. Controls on the variability of organic matter and dissolved inorganic carbon ages in northeast US rivers [J]. Marine Chemistry, 2004, 92(1):

353-366.

[45] Griffith D R, Barnes R T, Raymond P A. Inputs of fossil carbon from wastewater treatment plants to US rivers and oceans [J]. Environmental Science & Technology, 2009, 43(15): 5647-5651.

[46] Raymond P, Bauer J. Riverine export of aged terrestrial organic matter to the North Atlantic Ocean [J]. Nature, 2001, 409(6819): 497-500.

[47] Mc Callister S L, Del Giorgio P A. Evidence for the respiration of ancient terrestrial organic C in northern temperate lakes and streams [J]. Proceedings of the National Academy of

Sciences of the United States of America, 2012, 109(42): 16963-16968.

[48] Dubois K D, Lee D, Veizer J. Isotopic constraints on alkalinity, dissolved organic carbon, and atmospheric carbon dioxide fluxes in the Mississippi River [J]. Journal of Geophysical Research, 2010, 115(G2): G02018.

[49] Raymond P A, Cole J J. Increase in the export of alkalinity from North America’s largest river [J]. Science, 2003, 301(5629): 88-91.

[50] Barnes R T, Raymond P A. The contribution of agricultural and urban activities to inorganic carbon fluxes within temperate watersheds [J]. Chemical Geology, 2009, 266(3/4): 318-327.

[51] Moore S, Evans C D, Page S E, et al. Deep instability of deforested tropical peatlands revealed by fluvial organic carbon fluxes [J]. Nature, 2013, 493(7434): 660-663.

[52] Interlandi S J, Crockett C S. Recent water quality trends in the Schuylkill River, Pennsylvania, USA: a preliminary assessment of the relative influences of climate, river discharge and

suburban development [J]. Water Research, 2003, 37(8): 1737-1748.
[53] Baker A, Cumberland S, Hudson N. Dissolved and total organic and inorganic carbon in some British rivers [J]. Area, 2008, 40(1): 117-127.
[54] Regnier P, Friedlingstein P, Ciais P, et al. Anthropogenic perturbation of the carbon fluxes from land to ocean [J]. Nature Geoscience, 2013, 6(8): 597-607.

[55] Bastviken D, Tranvik L J, Downing J A, et al. Freshwater methane emissions offset the continental carbon sink [J]. Science, 2011, 331(6013): 50.

[56] Sawakuchi H O, Bastviken D, Sawakuchi A O, et al. Methane emissions from Amazonian Rivers and their contribution to the global methane budget [J]. Glob Chang Biol, 2014, 20(9):

2829-2840.

[57] Ding H, Lang Y C, Liu C Q, et al. Chemical characteristics and 34S-SO2−4 of acid rain:anthropogenic sulfate deposition and its impacts on CO2 consumption in the rural karst area of

southwest China [J]. Geochemical Journal, 2013, 47(6): 625-638.

[58] Li S L, Liu C Q, Li J, et al. Geochemistry of dissolved inorganic carbon and carbonate weathering in a small typical karstic catchment of Southwest China: isotopic and chemical

constraints [J]. Chemical Geology, 2010, 277: 301-309.

[59] Marce R, Obrador B, Morgui J A, et al. Carbonate weathering as a driver of CO2 supersaturation in lakes [J]. Nature Geosci, 2015, 8(2): 107-111.

[60] Ford D C, Williams P D. Karst hydrogeology and geomorphology [M]. New York: Wiley,2007.

Recent advances in the research of gaseous carbon exchange between river water and air interface

PDF

Knowledge

Cited

Abstract

Cite this article

share this article

References

Related Articles 4

Recommended Articles

Metrics

Comments

[1]	LIU Xiao-Long, WANG Fu-Shun, BAI Li, LI Si-Liang, WANG Bao-Li, LIU Cong-Jiang, WANG Zhong-Liang. Impact of cascade reservoir development on N₂O emissions in the Wujiang River [J]. Journal of Shanghai University（Natural Science Edition）, 2015, 21(03): 301-310.
[2]	WU Xue-Qian, CAO Man, FU Jia-Nan, WEI Hao-Bin, JIA Xiao-Bin, DENG Bing, WANG Fu-Shun. Partial pressure and diffusion flux of dissolved carbon dioxide in the main stream of the Three Gorge Reservoir and the Caotang River in summer [J]. Journal of Shanghai University（Natural Science Edition）, 2015, 21(03): 311-318.
[3]	WANG Bao-Li, LIU Cong-Jiang, WANG Fu-Shun, LIU Xiao-Long, PENG Xi, ZHAO Yan-Chuang. Carbon and nitrogen coupled biogeochemical cycle in cascade reservoirs of the Wujiang River [J]. Journal of Shanghai University（Natural Science Edition）, 2015, 21(03): 294-300.
[4]	LI Xiao-Dong, LIU Xiao-Long, YANG Zhou, LI Qin-Kai, HUANG Jun. Spatial and seasonal variation of dissolved inorganic carbon isotope compositions in the cascade reservoirs of the Jialing River [J]. Journal of Shanghai University（Natural Science Edition）, 2015, 21(03): 286-293.