Description Usage Arguments Details Value Note References Examples
Compute respiration flux from concentration data.
1 2 | compute_flux(time, gas_ppm, volume_cm3, tair_C, pressure_kPa = 101.325,
debug_plot = FALSE)
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time |
Time (typically in seconds); numeric vector |
gas_ppm |
Gas (e.g. CO2 or CH4) concentrations, ppmv; numeric vector |
volume_cm3 |
System volume, cm3; numeric |
tair_C |
Air temperature, C; numeric |
pressure_kPa |
Air pressure, kPa; numeric |
debug_plot |
Produce a plot of data and fitted model? Logical |
We derive the rate of concentration change via the slope of the linear regression of all data points of concentrations versus time. One problem with this method is that the linearity attributed to the regression is incorrect in a strict sense, since the gradients in water vapor and CO2 decrease over time in a closed chamber (see discussion in Steduto et al. below). This method should thus not be used for long measurement periods.
The gas flux, µmol per unit time.
The computed is not area- or mass-corrected.
Steduto et al. (2002), "Automated closed-system canopy-chamber for continuous field-crop monitoring of CO2 and H2O fluxes" AFM 111:171-186 http://dx.doi.org/10.1016/S0168-1923(02)00023-0.
Campbell and Normal (1998), An Introduction to Environmental Biophysics, ISBN 978-1-4612-1626-1. New York: Springer-Verlag, 286 pp.
LI-COR Biosciences (2015), Using the LI-8100A Soil Gas Flux System & the LI-8150 Multiplexer, 984-11123. 238 pp.
1 2 | # ten-second CO2 rise at room temperature
compute_flux(1:10, 401:410, volume_cm3 = 2000, tair_C = 20)
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