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BT is a multiplier of the basic flux rates.
We find distinct diurnal and annual cycles of flux rates.
Volcanic activity within these regions tends to be predominantly basaltic, with low flux rates.
Flux rates were greatest for WCA-1, followed by WCA-2 and WCA-3 (Table 3).
Filtrate flux rates for all solids loading displayed a negative dependency on axial velocity.
Capillary and methanotrophic final cover layers presented lower CH4 flux rates than the conventional layer.
Distance, soil temperature, moisture, and their interaction significantly influenced soil CO2 flux rates.
Acid flux rates from groundwater seepage were strongly positively correlated to effluent groundwater hydraulic gradients.
Grazing treatments exhibited only minor differences in overall ecosystem carbon flux rates compared to precipitation effects during our study period.
N2O concentrations in the soil profile and N2O flux rates were measured by gas chromatography.
However, they are often poorly understood due to low flux rates and difficulty in direct measurement.
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