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A closer look as soil geochemical data demonstrates that geological forces shape the concentrations and occurrence patterns of the elements – even in densely populated (e.g., Berlin) and highly industrialised Central Europe[3].
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The elution curve had an asymmetrical shape, the concentration peak was attained in less than 5 min, and the concentration factor was 920.
This pore shape, the concentration of the electrolyte and its variation along pores, the rate of the transport of Al2 SO4 3, produced by the field assisted pore base oxide electrochemical dissolution and the purely chemical pore wall oxide dissolution, and the electrolyte conductivity inside pores were found to be of decisive importance for the growth of oxide beyond these times.
It is argued that for liquids with high surface tension, the shape of the concentration profiles and the behavior of diffusivity as a function of liquid content are both related to the shape of the cummulative pore size distribution of the porous solid under study due to the existence of efficient capillary flows induced by capillary suction.
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The shape of the concentration dependence of the activation energies is clearly modified in the vicinity of the concentration where the conductivity maximum occurs.
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Short-term exposure to ozone has been associated with asthma hospital admissions (HA) and emergency department (ED) visits, but the shape of the concentration-response (C-R) curve is unclear.
Since here the soil surface concentration is a function of time, the relative influence of the different rate-limited processes determining the shape of the concentration distribution at the slope outlet can be identified and analyzed.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com