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Each polygon shows analyte concentrations at a given depth below the sediment/water interface (SWI).
This new approach can transfer Lagrangian particle trajectories into an Eulerian form of particle concentrations at a given point, and thus provide the mean particle residence time.
Reduced groundwater recharge over B2-B3, and therefore slightly higher ages compared to B4-B5, could plausibly be inferred from the pattern of EM conductivity, the location of a large pond, and the major cation content of shallow groundwater, and would be consistent with As concentrations at a given depth that generally decline east of B2 (Fig. 5d).
The methodology seeks to predict pollution concentrations at a given site based on surrounding land use and traffic characteristics.
Previous studies show that iron deficiency increases erythrocyte survival and therefore disproportionately elevates HbA1c concentrations at a given glycemic level (5, 6).
In this simulation, kinetic constants of metabolic enzymes were introduced to allow for the computation of required enzyme concentrations at a given specific growth rate.
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The model predicted the experimental underflow solids concentration at a given flux.
This can violate an objective that limits the room noise level (resp. the CO2 concentration) at a given threshold.
Therefore, the chloride concentration at a given cover depth and time can be evaluated with this model.
If the concentration of gas molecules exceeds their maximum concentration at a given temperature, the excess of gas molecules leaves the gas under thermodynamic equilibrium.
From these subjective values of time and WTP were derived for reductions in the number of days of alert and hence the amount of pollutant concentration at a given location.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com