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Point sources in air (A), point sources in water with no background concentration (B), point sources in water with 0.1% background concentration (C), and point sources in water with 1% background concentration (D).
The investigations required the determination of the natural background concentration of chloride in groundwater.
After the background concentration, the most important pathway was the wet deposition.
Conceptual and statistical issues surrounding the estimation of a background concentration distribution for arsenic are reviewed.
Therefore, it is possible to specify the background concentration for all lithotypes.
After the release, Cl returns to background concentration starting from the release point.
These are the 15 to 1 signal to background concentration ratio images.
The concentrations increase upon release and return to background concentration when the release stops.
At the time when release stops, the precipitation even draws Ca concentration to below background concentration.
Furthermore, 60%% of the samples had nitrate concentrations above background concentration of 10 mg/l.
Additionally, 45%% of the samples had nitrate concentrations above background concentration of 10 mg/l.
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CEO of Professional Science Editing for Scientists @ prosciediting.com