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RESPONSE TO WRITTEN COMMENTS -3- <br /> City Of Stockton- Regional Wastewater Control Facility <br /> NPDES No. CA0079138 <br /> 26 April 2002 Board Meeting <br /> chronic (4-day and 7-day), Section 8.7 pathogen/disinfection considerations (7-day and 30- <br /> day), and Section 8.9 ammonia (1-day and 30-day)) <br /> • The available UVM data is from above average wet years (Fact Sheet, Section 8.2) <br /> • Tidal influences permit the receiving water to be dosed with effluent multiple times (Fact <br /> Sheet, Section 8.5) <br /> • The existing water quality models are inadequate to determine dilution (Finding 44 and <br /> Fact Sheet, Section 8.2). Detailed comments provided in Attachments A, B, and C. <br /> • The SJR is an impaired water body that is 303(d) listed for several contaminants and is <br /> inhabited by several threatened and endangered species (Findings 19 and 44, Fact Sheet @ <br /> 8and 13) <br /> • Minimal dilution may exist for certain averaging periods, but due to the severely impaired <br /> condition of the receiving water and the presence of threatened and endangered species, <br /> dilution has not been proposed in the tentative order. <br /> Stockton Comment No. LC (1): Contrary to the advice provided by experts in estuarine dynamics <br /> (e.g., Jones & Stokes reports), staff determined the available dilution solely as a ratio between the net <br /> river flow and the effluent flow. This approach is not applicable to tidal river systems as noted by <br /> EPA in the 1991 TSD. <br /> RWQCB Response: The models presented by the Discharger are inadequate and cannot be the basis <br /> for Regional Board decisions (detailed comments are presented in Attachments A, B, and Q. Even <br /> though using the net river flow to determine dilution may not be precisely accurate, there is enough <br /> actual data to make a decision on whether to grant dilution. <br /> Stockton Comment No. LC (1): The staff s conclusion regarding dilution and mixing during <br /> slack '.:des (i.e., flow stagnation equates to little or no dilution; Fact Sheet @ 12) is similarly <br /> misplaced. As noted by EPA, the available dilution occurring under the short slack tide event is <br /> governed by the receiving water volume and plume mixing dynamics, not the river velocity. The <br /> Findings did not cite any consideration of these factors to assess dilution and mixing near slack tide <br /> even though available studies confirmed that initial mixing followed this pattern. Prior studies <br /> submitted to the Board, which were confirmed by recent studies, showed at least 7:1 dilution from <br /> initial mixing at slack conditions (see Fact Sheet @ 7). Thus, the conclusion that very little dilution <br /> occurs during tide reversal is unsupported by fact, and is directly refuted by the available information. <br /> RWQCB Response: The 1993 dye study referred to in the City's comment was only performed <br /> during specific tidal conditions; ebb, low, and flood. Dye dosing was not continuous during the test; <br /> the dosing stopped for approxic two hours betwee: "des. The dosing connentration was <br /> increased prr ively frons i' condition to the ne .; to minimize possib. :.terference of dye <br />