Sediment Temperature and Redox Potential As Confound Factors Controlling CO2 Flux Between Sediment and the Atmosphere in an Intertidal Zone
Variation in soil temperature can account for most of the seasonal and diel variation in soil CO 2 flux, but the temperature effect is not consistent in the intertidal zone, and other factors such as redox potential are known to influence CO 2 flux. The objectives of this research were to study the...
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