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The distributions of iodate, iodide and dissolved organic iodine (DOI) were determined in two deep sub-basins in the Chesapeake Bay, the shallow waters at the mouth of the Bay and the adjacent North Atlantic between the late spring and the early fall along the net flow-path of the water entering and exiting the Chesapeake Bay by using an improved analytical scheme designed for the quantitative recovery...
Dissolved organic iodine (DOI) in inshore waters was decomposed by solar irradiation. In the process, each mole of DOI was converted to about a mole of iodide. The disappearance of DOI and the formation of iodide were directly proportional to irradiation. The reaction could be expressed as a first-order reaction with respect to the concentration of DOI. The first-order rate constant ranged between...
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