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We calibrated the model using the measured concentrations of dissolved organic and inorganic carbon (C) in a young boreal hydroelectric reservoir, Eastmain-1 (EM-1), in northern Quebec, Canada.
Values were used to calculate the steady-state redox potential for GSH/GSSG (EhGSSG) and Cys/CySS (EhCySS) using the measured concentrations, the Nernst equation, and respective EoGSSG and EoCySS at pH 7.4 for plasma (−264 mV, −250 mV) and 7.0 for lung (−240 mV, −226 mV) [36], [37].
Aerosol acidities (strong acidity) were estimated based on charge balance using the measured concentrations of the three inorganic components.
Our most important conclusion is that eve expression in these nuclei can be correctly separated into two classes using the measured concentrations of various transcription factors alone.
In order to determine whether our model was applicable to experimental data, we have fitted our model using the measured concentrations of CTP in wild type and CTPsyn overexpressing human 293T cells.
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This is consistent with rapid decreases in concentrations of CPY in surface water after changes in patterns of use (see the 'Measured concentrations in surface waters' section).
The model was calibrated and verified using the measured BOD concentrations, and was used in test runs comparing performance under various vegetation, porous media size, temperature and HRT conditions.
The inoculum concentration for each experiment was determined by calculating the volume of preculture required to obtain the target initial concentration of each cell type using the measured biomass concentration in the shake flask media.
The SO3 decomposition percentage was determined using the measured O2 concentration in the exit gas stream.
In the next stage, the performance of SVM was evaluated using the measured and predicted concentrations.
The area under the plasma concentration time curve (AUC) was calculated according to the linear trapezoidal rule, using the measured concentration time values above the LLOQ.
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