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Respiration and assimilation processes reflected in the carbon isotopic composition of atmospheric carbon dioxide

Treść / Zawartość
Identyfikatory
Warianty tytułu
Konferencja
Proceedings of the International Conference “2001 an Isotope Odyssey: New Application for a New Millenium", June 24-29, 2001, Zakopane, Poland
Języki publikacji
EN
Abstrakty
EN
This paper presents diurnal variations of concentration and carbon isotopic composition of atmospheric carbon dioxide caused by respiration and assimilation processes. Air samples were collected during early and late summer in 1998 in unpolluted area (village Guciow located near the Roztocze National Park, SE Poland) in three different environments: uncultivated field on a hill, a meadow in the Wieprz river valley and a forest. The effect is very strong during intensive vegetation growth on a sunny day and clear night. The largest diurnal variations in atmospheric CO2 concentration and its carbon isotopic composition in June above the meadow were about 480 ppm and 10‰, respectively.
Słowa kluczowe
Czasopismo
Rocznik
Strony
59--61
Opis fizyczny
Bibliogr. 14 poz., rys.
Twórcy
autor
  • Institute of Physics, M. Curie-Sklodowska University, 1 M. Curie-Sklodowska sq., 20-031 Lublin, Poland, Tel.: +48 81/ 5376221, Fax: +48 81/ 5376191
autor
  • Institute of Physics, M. Curie-Sklodowska University, 1 M. Curie-Sklodowska sq., 20-031 Lublin, Poland, Tel.: +48 81/ 5376221, Fax: +48 81/ 5376191
  • Institute of Physics, M. Curie-Sklodowska University, 1 M. Curie-Sklodowska sq., 20-031 Lublin, Poland, Tel.: +48 81/ 5376221, Fax: +48 81/ 5376191
Bibliografia
  • 1. Cerling TE, Solomon DK, Quade J, Bowman JR (1991) On the isotopic composition of carbon in soil carbon dioxide. Geochim Cosmochim Acta 55:3403–3405
  • 2. Ciais P, Tans PP, Trolier M, White JWC, Francey RJ (1995) A large northern hemisphere terrestrial CO2 sink indicated by the 13C/12C ratio of atmospheric CO2. Science 269:1098–1102
  • 3. Craig H (1954) Carbon 13 in plants and the relationship between carbon 13 and carbon 14 variations in nature. J Geol 62:115–149
  • 4. Denning AS, Fung IY, Randall D (1995) Latitudinal gradient of atmospheric CO2 due to seasonal exchange with land biota. Nature 376:240–243
  • 5. Farquhar GD, O’Leary MH, Berry JA (1982) On the relationship between carbon dioxide isotope discrimination and the intercellular carbon dioxide concentration in leaves. Aust J Plant Physiol 9:121–137
  • 6. Flanagan LB, Ehleringer AR (1998) Ecosystem-atmosphere CO2 exchange: interpreting signals of change using stable isotope ratios. Trends Ecol Evol 13:10–14
  • 7. Geyh MA, Schleicher H (1990) Absolute age determination. Physical and chemical dating methods and their application. English by Newcomb RC, Springer Verlag, Berlin Heidelberg
  • 8. Halas S, Krouse HR (1983) Isotopic analysis of nanomole gas samples by means of dynamic flow mass spectrometry. Rev Sci Instrum 54:437–443
  • 9. Halas S, Krouse HR (1984) Device for rapid transfer of condensable gases into capillary. Rev Sci Instrum 55:1160–1161
  • 10. Keeling CD (1958) The concentration and isotopic abundances of atmospheric carbon dioxide in rural areas. Geochim Cosmochim Acta 13:322–334
  • 11. Keeling CD, Chin LES, Whorf TP (1996) Increased activity of northern vegetation inferred from atmospheric CO2 measurements. Nature 382:666–670
  • 12. O’Leary MH (1981) Carbon isotopes in photosynthesis. Bioscience 38:328–336
  • 13. Park R, Epstein S (1960) Carbon isotope fractionation during photosynthesis. Geochim Cosmochim Acta 21:110–126
  • 14. Szaran J (1998) Seasonal variations of δ13C values and CO2 concentration in the air during vegetation growth. Isot Environ Health Stud 34:341–348
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ6-0006-0068
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