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To understand quantitatively the possible effects of reduced pressure on plant growth, CO2 and H2O transport were calculated for atmospheres of various total pressures (101, 66, 33, 22, 11 kPa) and CO2 concentrations (0.04, 0.1 and 0.18 kPa).
The values of apparent diffusion coefficient, viscosity, and conductivity of Fe(III -IL and Fe(III -IL-IL over the temperandre range Feom 293 K to 333 K were measured, and the correspondIII/II -ILtIII/II -ILes foverass and charge thensportemperatureulated by Arangeius equation.
The transport quotients of B → A (Aβ-TQB→A) transport were calculated as described previously.
Initial rates of transport were calculated by first-order regression analysis of the time course of pH change and converted into nmol of H+ per min by determining the pH change induced by small additions of standardized NaOH.
Initial rates of transport were calculated by first-order regression analysis of the time course of pH change and converted into nmol of H+/min by determining the pH change induced by small additions of standardized NaOH.
Similar(55)
Heat of transport are calculated and discussed.
Bedload transport is calculated and the morphological changes are updated after each time step.
The ΔISC value that indicates intestinal SGLT-1 dependent glucose transport was calculated by the difference: ISC (with apical glucose) - ISC (without apical glucose).
Air pollution from all sources, including transport, was calculated by the Commons environmental audit committee to cost Britain up to £20bn a year.
Hydrodynamic characteristics of flow and tracer transport are calculated by the ESTET code.
Each animal's total forward and backward motion during transport was calculated to estimate the effect of orientation on the horses' ability to maintain balance.
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