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HomeMy WebLinkAboutNC0024112_Wasteload Allocation_19840703DIVISION OF ENVIRONMENTAL MANAGEMENT July 3, 1984 MEMORANDUM TO: Russell Radford FROM: Trevor Clements 11l THROUGH: Randy Williams Steve Tedder SUBJECT: Summary In -Stream Assessment Thomasville WWTP - Hambys Creek Davidson County The Tbwn of Thomasville is seeking permission to add 141,300 gpd of, domestic wastewater to their effluent. According to self -monitoring data, the Thomasville WWTP is operating out of compliance with their final limits for BOD5 and NH3-N. They are, however, within compliance of their interim limits which apply until June 30th of this year. A level C Qual-II modeling analysis was performed using both Thomasville's 1983 summer period average wasteflow of 2.455 MGD and the projected flow of 2.55 MGD. The additional wasteflow did not result in a significant impact. However, a minimum DO of 2.2 mg/1 was predicted to occur under each scenario along with a projected degraded zone (D.O. less than 5 mg/1) of 5.5 miles. Analysis and Results Thomasville discharges to Hambys Creek, a class "C" stream, 6.8 miles above its confluence with Rich Fork Creek. Thomasville is permitted with final limits of: Summer Winter Wasteflow 4.0 MGD 4.0 MGD BOD5 5 mg/1 10 mg/1 NH3-N 2 mg/1 3 mg/1 DO 5 mg/1 5 mg/1 TSS 30 mg/1 30 mg/1 fecal coliform 1000/100 ml 1000/100 ml pH 6-8.5 SU 6-8.5 SU Russell Radford May 14, 1984 - page two - They do have interim limits of: BOD5 20 mg/1 NH3-N 12 mg/1 According to self -monitoring data recorded between April and October of 1983, Thomasville's effluent has the following characteristics: Wasteflow 2.55 MGD BOD5 15.1 mg/1 NH3-N 2.7 mg/1 DO 7.9 mg/1 TSS 10.7 mg/1 fecal coliform 5/100 ml These characteristics were input to a Level C Qual-II model. The model was run at the existing and proposed wasteflow levels. Under both wasteflows; a DO minimum of 2.2 mg/1 was predicted to occur 6 miles downstream of the outfall. A degraded zone (DO 5.0 mg/1) was predicted to occur for a 5.5 mile stretch. Since the downstream monitoring station for Thomasville is located only 2.1 miles below the outfall, information obtained there cannot be used to support these modeling conclusions. JTC:cs cc: L. Page Benton, Jr. Dean Cunningham