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A kinetic multilayer model verifies that iodide depletion is happening not only within ozone's reactodiffusive depth, that is on the order of microns for environmental circumstances, but in addition much deeper in to the solution also. Most readily useful model-measurement arrangement arises whenever some degree of nondiffusive blending is happening when you look at the answer, moving iodide from deeper in the means to fix a thin, diffusively combined top level. If such blending does occ
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