Main Factors Impacting the CO2 Flux Between Sediment and the Atmosphere in an Intertidal Zone, Qingdao

Using a Li-8100 automated soil CO 2 flux system (Licor, Lincoln, Nebraska, USA), we measured the in situ diurnal CO 2 flux from the sediment to the atmosphere in a temperate intertidal zone in northern China in 19 days during April 24 to July 26 of 2006, with average CO 2 flux of 0.09 mumol m -2 s -...

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Bibliographische Detailangaben
Hauptverfasser: Longjun Zhang, Pengjin Yang
Format: Tagungsbericht
Sprache:eng
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Zusammenfassung:Using a Li-8100 automated soil CO 2 flux system (Licor, Lincoln, Nebraska, USA), we measured the in situ diurnal CO 2 flux from the sediment to the atmosphere in a temperate intertidal zone in northern China in 19 days during April 24 to July 26 of 2006, with average CO 2 flux of 0.09 mumol m -2 s -1 . The CO 2 flux varied with redox potential and temperature. When the redox potential was
ISSN:2151-7614
2151-7622
DOI:10.1109/ICBBE.2009.5163025