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Fig. 11 shows spatial interpolation map of chloride.
Open image in new window Fig. 4 Spatial distribution map of chloride.
Open image in new window Fig. 5 Spatial distribution map of chloride and sulphate.
Open image in new window Fig. 8 Spatial distribution map of chloride concentrations at various depths in relation to geomorphic units.
Spatial distribution map of chloride concentrations (Fig. 8) at various depths show that concentration is comparatively low in FDP, but it gradually increases towards south, i.e., in the FTDP as it approaches the coastal plain.
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The spatial distribution map of the chloride ion is given in Fig. 4.
In fact 1,25(OH)2D3 can rapidly stimulate phosphoinositide metabolism, cytosolic calcium levels, cGMP levels, PKC, MAP kinases, and the opening of chloride channels (reviewed in [34]).
A previously developed four parameter model of chloride deposition as a function of distance from the coast for Australia was used as the basis for producing a continental scale chloride deposition map.
The temporal variability in chloride deposition on a decadal scale was investigated in the Murray-Darling Basin, this highlighted the need for long-term monitoring of chloride deposition if the uncertainty of the continental scale map is to be reduced.
The uncertainty in the chloride deposition map was quantified as the 5th and 95th percentile of 1000 calibrated models produced via Null Space Monte Carlo analysis and the spatial variability of chloride deposition across the continent was consistent with landscape morphology.
A technician then measures the concentration of chloride in the pad.
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