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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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 |
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ISSN: | 2151-7614 2151-7622 |
DOI: | 10.1109/ICBBE.2009.5163025 |