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contaminant source locations identified during the implementation of this WHPP will be verified by the <br />City with the assistance of the Wellhead Protection Consultant, if needed. <br />7.7.5.1 Source of Action <br />City staff. <br />7.7.5.2 Cooperators <br />City staff and the Wellhead Protection Consultant, if needed. <br />7.7.5.3 lime Frame <br />When new potential contaminant sources in the DWSMA are identified. <br />7.7.5.4 Estimated Cost <br />Approximately $500-$3,000. City staff time and Wellhead Protection Consultant costs, if needed. Actual <br />costs will depend upon the number of new potential contaminant source locations that must be verified <br />and in any update could be higher than the estimated range shown. <br />7.7.5.5 Goals Achieved <br />Verification of newly identified potential contaminant source locations within the DWSMAs will allow the <br />City to remain in compliance with the requirements of the State of Minnesota's Wellhead and Source <br />Water Protection Program. Verification of the newly identified locations will also ensure that the City uses <br />the most accurate data on type and location of potential contaminant sources as implementation of this <br />WHPP proceeds. <br />Success criterion: All potential contaminant source locations in the database are verified to the extent <br />possible. <br />7.7.6 Tritium and Indicator Parameter Sampling <br />In the April 4, 2019 Scoping Decision Notice (MDH, 2019b), the MDH recommended that the City should <br />sampling Wells 1, 3, 4, 6, and 7 for tritium and the indicator parameters ammonia, bromide, chloride, <br />nitrate and nitrite, and sulfate. Tritium (3H), a radioactive isotope of hydrogen, whose atmospheric <br />concentrations rose in the 1950s and early 1960s due to atmospheric hydrogen bomb testing. It has been <br />used extensively to date groundwater. Tritium activities peaked during atmospheric hydrogen bomb <br />testing of the 1950s and 1960s, and values of 3H in precipitation reached a maximum of approximately <br />10,000 TU (tritium units) in 1963 (Mazor, 2004). Natural production of 3H in the upper atmosphere <br />introduces approximately 5 TU to precipitation each year (Mazor, 2004). The presence of tritium at <br />concentrations above 1 tritium unit in a groundwater sample indicates the presence of a significant <br />fraction of post-1954 (i.e., recently infiltrated) water in the sample. The indicator parameters provide <br />additional information on the rate at which an aquifer recharges and can also provide evidence of impacts <br />to groundwater by human activities. <br />36 <br />