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Weathering rates, natural organic matter and global climate change : are they related ?

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
Czasopismo
Rocznik
Tom
Strony
49--50
Opis fizyczny
Bibliogr. 18 poz.
Twórcy
  • Colorado School of Mines, Golden, CO 80401 USA
  • Department of Chemistry and Geochemistry, Colorado School of Mines, Golden, CO 80401 USA
  • Norwegian Geological Survey (NGU), Trondheim, Norway
Bibliografia
  • Anderson, S.P.,Drever,J.I.,Frost,C.D.,Holden,P., 2000. Chemical weathering in the foreland of a retreating glacier,Geochim. Cosmochim. Acta,64: 1173–1189.
  • Antweiler,R.C.,Drever,J.I.,1983. The weathering of a late Tertiary volcanic ash: Importance of organic solutes. Geochim. Cosmochim. Acta,47: 623–629.
  • Benner, R.,Benitez-Nelson, B.,Kaiser, K.,Amon, R.M.W.,2004. Export of young terrigenous dissolved organic carbon from rivers to the Arctic Ocean,Geophys. Res. Lett.,31,L05305, doi:10.1029/2003GL019251.
  • Frey,K.E.,Smith,L.C.,2005. Amplified carbon release from vast west Siberian peatlands by 2100, Geophys. Res. Lett.,32,L09401,doi:10.1029/2004GL022025.
  • Hinzman,L.D.,et al. 2005. Evidence and implications of recent climate change in northern Alaska and other arctic regions,Clim. Change,72, doi:10.1007/s10584-005-5352-2.
  • Jardine,P.M.,Wilson,G.V.,McCarthy,J.F., Luxmoore,R.J., Tayler,D.L.,Zelazny,L.W.,1990. Hydrogeochemical processes controlling transport of dissolved organic carbon through a forested hillslope. J. Contam. Hydrol., 6: 3–19.
  • Jardine,P.M.,Wilson,G.V.,Luxmoore, R.J.,Mc - Carthy,J.F.,1989b. Transport of inorganic and natural organic tracers through an isolated pedon in a forest watershed. Soil Sci. Soc. J.,53: 317–323.
  • Jardine,P.M.,Weber,N.L.,McCarthy,J.F.,1989a. Mechanisms of dissolved organic carbon adsorption on soil. Soil Sci. Soc. Am. J., 53: 1378–1385.
  • Kawahigashi, M.,Kaiser,K.,Kalbitz,K.,Rodionov, A. Guggenberger,G., 2004. Dissolved organic matter in small streams along a gradient from discontinuous to continuous permafrost,Global Change Biol., 10: 1576–1586.
  • McCarthy, J.F.,Gu,B.,Liang,L.,Mas-Pla,J.,Williams,T.M.,Yeh,T.-C.J.,1996. Field tracers tests on the mobility of natural organic matter in a sandy aquifer. Water Resources Res., 32(5): 1223–1228.
  • McCarthy,J.F.,Williams,T.M., Liang,L., Jardine, P.M.,Palumbo,A.V.,Jolley,L.W. Cooper,L.W. Taylor,D.L.,1993. Mobility of natural organic matter in a sandy aquifer. Environ. Sci. Technol., 27: 667–676.
  • Michaelson, G.J.,Ping,C.L.,Kling,G.W.,Hobbie, J.E.,1998. The character and bioactivity of dissolved organic matter at thaw and in the spring runoff waters of the Arctic tundra north slope, Alaska,J. Geophys. Res.,103(D22),28,939– 28, 946.
  • Ranville,J.,Macalady,D.,1997. Natural organic matter in catchments in Saetther. In: Geochemical Processes,Weathering and Groundwater Recharge in Catchments,O.M., de Caritat,Patrice, (eds.), Balkema, Rotterdam, pp. 263–297.
  • Rauland-Rasmussen,K., Borggaard, O.K., Hansen, H.C.B.,Olsson,M.,1998. Effect of natural organic soil solutes on weathering rates of soil minerals. Eur. J. Soil Sci., 49: 397–406.
  • Raymond,P.A., Cole,J.J. 2003. Increase in the export of alkalinity from North America’s largest river, Science 301: 88–91. DOI: 10.1126/science. 1083788.
  • Striegl,R.G.,Aiken,G.R.,Dornblaser, M.M.,Ray - mond,P.A.,Wickland,K.P.,2005. A decrease in discharge-normalized DOC export by the Yukon River during summer through autumn,Geophys. Res. Lett.,32,L21413,doi: 10.1029/2005GL024413.
  • Striegl,R.G.,Dornblaser,M.M.,Aiken,G R. Wickland,K. P.,Raymond, P.A.,2007. Carbon export and cycling by the Yukon,Tanana,and Porcupine rivers,Alaska,2001–2005,Water Resour. Res., 43, W02411, doi: 10.1029/2006WR005201.
  • Velbel,M.A. 1993. Temperature dependence of silicate weathering in nature: How strong a negative feedback on long-term accumulation of atmospheric CO2 and global greenhouse warming? Geology, 21: 1059–1062.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-935cfedc-7a68-4728-8d60-c473447a0755
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