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HomeMy WebLinkAboutNC0031879_Report_19820601Marion-Corpening Creek Study Plan Catawba River Basin June, 1982 Division of Environmental Management Water Quality Section Operations Branch Monitoring and Technical Services 'Mit I. Introduction The City of Marion has requested that the Division of Environmental Management review the effluent limits established for their Corpening Creek WWTP. Of special concern is the phosphorus limitation placed on this facility. Phosphorus limits were developed primarily as a product of limited work by the U.S. Environmental Protection Agency in the head- water lakes of the Catawba River. (Please see attached August 3, 1981 letter). This work was accomplished during 1973 and 1974. However, major changes have occurred in the Lake Rhodhiss drainage area which necessitates a re-evaluation of the impact of the Marion discharge. Significant among these changes was the introduction of several new domestic dischargers with design capacities greater than the Marion- Corpening Creek WWTP. The Marion facility presently has a design capacity of 3 MGD. II. Lake Models First, it would be of importance to ascertain the present loading of phosphorus to Lake Rhodhiss and the percentage of this loading contributed by Marion employing phosphorus removal. This would then be compared to the projected loading to the lake assuming no phosphorus removal by Marion. If a linear relationship is assumed between in -lake phosphorus concentration and phosphorus loading then the effect on Lake Rhodhiss of suspending Marion's phosphorus removal may be estimated. The impact that the Marion-Corpening Creek WWTP has on eutrophication in Lake Rhodhiss may also be analyzed by the use of several models. All of these models involve the estimation of nutrient loadings into the lake from both point sources and non -point source runoff. One of these models is the loading model proposed by Vollenweider (1975) where: L (P) = 100 + 10Z Tw 1000 L (P) = permissable phosphorus (P) loading rate (gmP/m2/yr) Z = mean depth of the body water (m) Tw = hydraulic residence time (yr) The permissable P loading reate indicates the maximum P loading level that a given water body can tolerate and still retain its oligotrophic or mesotrophic status. Vollenweider based most of his work on data from Canadian and Swiss lakes. In order to account for conditions in southeastern lakes and reservoirs which differ greatly from the lakes studied by Vollenweider, Marlar and Kutzman (1980) have proposed a refinement of the Vollenweider model. Marlar and Kutzman suggest computing the ratio of the actual P loading rate to the Vollenweider predicted dangerous P loading rate for the lake in question and for all lakes in the same region or area. The resulting dimensionless number can then be used to define that breakpoint for all lakes in the region at which higher values can be considered as predicting a eutrophic condition. This technique was used by EPA Region IV in their analysis of TVA reservoirs (EPA, 1980). Vollenweider (1976) also developed an approach for predicting an in -lake P concentration based on the actual P loading rate as follows: CP lake] = L (P)/qs 1 + (Tw)1/2 Where: [P lake] = in lake P level (ug/1) L (P) = actual P loading rate (mgP/m2/yr) qs = aereal water load = Z/Tw (m/yr) Tw = hydraulic residence time (yr) Z = mean depth (m) This approach was assessed and found to be satisfactory predictor of actual in -lake phosphorus levels in five TVA reservoirs (EPA 1980). Vollenweider's predicted in -lake phosphorus concentrations were adjusted for actual in -lake phosphorus levels. By the use of a regression equation the adjusted in -lake phosphorus concentration was then used to predicte summer mean chlorophyll a concentrations. Vollenweider's models have been developed using data taken largely from natural lakes where completely mixed conditions are assumed. In impoundments, which tend to have hydrologic and morphologic characteristics which are gradients very different from natural lakes , significant longitudinal often exist. The empirical constants developed for natural lakes may not be applicable to impoundments. Higgins and Kim (1981) have presented a plug flow model for lakes and reservoirs which have significant longitudinal variation in phosphorus concentration at any point x along the reservoir phosphorus concentration at the inlet as well as between zero and x: Cx = Ci e ( - a ) concentration. Phosphorus is a function of the the residence time Where: Cx = phosphorus concentration at mile x Ci = phosphorus concentration at mile 0 which corresponds to lake inlet a = phosphorus sedimentation coefficient (an empirical constant) Tx = residence time between milepoint 0 and milepoint x Lake Rhodhiss is an impoundment which exhibits significant longitudinal variation (Anne'Witzig, personal communication). (1981) model should be applicable to this lake. Thus Higgins and Kim' s It should be noted that the above models all assume that the lake is phosphorus limited. Previous algal assay work had indicated the lake to be nitrogen limited; however in -lake data has shown that nutrient limitation vascillates between nitrogen and phosphorus depending on station and time of year (EPA, 1975). Algal nitrogen requirements are related to phosphorus requirements by a ratio of 15:1 by weight (Vollenweider, 1977). Therefore the phosphorus loading rates distinguishing the various trophic states (oligotrophic, mesotrophic, eutrophic) may be multiplied by a factor of 15 to obtain the corresponding nitrogen loading rates in a nitrogen limited environment. III. Trophic State In order to determine the necessity of requiring phosphorus removal for Lake Rhodhiss, a comparison of trophic state with and without phosphorus removal should be made. Using Marlar and Kutzman's (1980) refinement of the Vollenweider loading model, it can be determined whether or not a change in trophic state can be expected from allowing Marion to discontinue phosphorus removal. Using both Vollenweider's (1976) and Higgins and Kim's (1981) models average phosphorus concentrations may be estimated for Lake Rhodhiss both with and without phosphorus removal at the Marion Plant. These concentrations may then be used in the total phosphorus trophic state index (TSI) developed by Carlson (1977) whereby: TSI(TP) = 14.42 In TP + 4.15 The resulting dimensionless numbers may then be compared. Furthermore, it may be possible, using previous lake data, to develop a regression equation relating chlorophyll a concentrations to in -lake phosphorus concentrations. If this can be done, calculated phosphorus concentrations can then also be used to predict chlorophyll a concentrations. These chlorophyll a values can then also be inputted to another of Carlson's (1977) TSI equations.whereby: TSI (chlorophyll) = 9.81 In chla + 30.6 The resulting TSI values under the different phosphorus removal regimes may then be compared. IV. Existing Data Base The North Carolina ambient water quality network has stations which will help in the estimation of nutrient loadings entering Lake Rhodhiss from the Catawba River and major tributaries. In December, 1982, in order to facilitate the Lake Rhodhiss study the nutrient sampling frequency was increased on two existing ambient monitoring sites while three old secondary sites were reactivated. Sampling frequency was increased to monthly on these ambient stations. Table 1 lists the available data from these five stations as well as three other major ambient stations. The study area and the locations of these stations are indicated in Figure 1. Additional ambient monitoring data exists as well. USGS has estimates for average flow on all major tributaries entering Lake Rhodhiss. Daily flow records are available for the Catawba River near Marion and Lower Creek near Lenoir. It may thus be possible to extrapolate these records to the points where these tributaries enter Lake Rhodhiss and obtain flow weighted averages of nutrient concentrations. Where water quality data is lacking loading estimates may be made from existing land use patterns using literature values. Inputs from point sources may be estimated using monthly self -monitoring data. The monthly self -monitoring reports provide accurate data of daily flow. However, except for the Marion WWTP, no other dischargers monitor for phosphorus. In December 1981 Regional Office collect a 24-hour for all dischargers with a design Rhodhiss drainage area. This was V. Field Work it was requested that the Mooresville composite sample for nutrient analysis flow above 0:5 MGD entering the Lake to be taken by March 31, 1982. The Technical Services Unit is proposing to do additional field work on Lake Rhodhiss as well as on point and non -point sources entering its drainage area. This work is tentatively scheduled for late July 1982. The field work will include an accurate depth profile of the lake. Depth soundings will be taken on numerous cross -sections as well as in the center channel along the entire length of the lake. A reliable estimate of depth is essential for all lake models. Significant sedimentation has likely occurred since the lake was filled. In order to obtain additional information on loading. nutrient grab samples will be taken on all the major tributaries to Lake Rhodhiss. The tributary stations are listed in Table 2. The locations of these stations are shown in Figure 2. It is also desired to see how nutrients and chlorophyll a change longitudinally along the lake. Seven stations were chosen along the length of the lake in the center of the channel. Two sets of nutrient series will be taken at each station; one set will be an integrated sample from the euphotic zone, while the other will be taken from the hypolimnion. An integrated sample for chlorophyll a will be taken from the euphotic zone as well. D.O. and secchi disk depth will also be taken at each station. These stations are listed in Table 3 and their locations are indicated in Figure 3. Limited nutrient data is available for the dischargers entering the Lake Rhodhiss draiange area. As discussed previously. twenty-four hour composite samples for nutrients are being taken by the Regional Office on the eight dischargers with a design flow equal to or greater than 0.5 MGD. During the field survey, personnel from the Division will take grab samples for nutrient analysis from the same eight dischargers as well. These dischargers with their respective design flows are listed in Table 4. Their locations are shown in Figure 4. While still a limited data base, the grab samples will assist in giving a range of variability for effluent values. If the required monitoring equipment is available, 24-hour composite samples will be taken from the larger dischargers. In order to determine the limiting nutrient. it is also desired that algal assays be done on Lake Rhodhiss. The format for this work will be established in conjunction with Ron Raschke at EPA in Athens, Georgia. VI. Completion of Modeling Work It is expected that a preliminary analysis of the data utilizing the previously described lake models will be completed by mid October, 1982. Table 1 Major Ambient Monitoring Stations Storet # Location CTB028A Catawba R. @ SR 1147 Glen Alpine CTB029 Silver Cr. @ 70W C1250000 Catawba R. @ Morganton CTB031-01 Johns R. @ SR 1438 Oak Hill CTB032 Lower Cr. @ Hwy 321 CTB034 lA Lower Cr. @ SR 1501 nr Morganton Data Available Period of Record N + P, D.O. 740521-790828 811207-present* 811207-present* 750513-770126 770126-810225 750521-761129 770126-771027 771027-820405* 750529-770126 770126-810211 750521-770126 770126-820405* CTB034A L. Rhodhiss @ SR 1501 nr N + P, D.O. 740604-820330 Drexel Secchi CTB040A Lake Rhodhiss @ SR 1001 near Baton *active 730329-810803 8112.07-present* Sampling Frequency "every 3 mo monthly monthly every 3-4 mo every 1-2 mo "'every 4 mo every 2 mo almost monthly "'every 4 mo every 1-2 mo "'every 4 mo every 1-2 mo yearly occasionally more often yearly or more often monthly r ,.I • ti C ua —J v •, I ›- CD ':. l r • • Figure I Major_Ambient Monitoring Stations M��aw4lt Stream Table 2. Stream Stations Location Station # Muddy Creek Hwy. 70 S1 Silver Creek (CTB029) Hwy 70W S2 Warrior Fork SR 1440 S3 Johns River (CTB031-D1) SR 1438 S4 Lower Creek (CTB034-1A) SR 1501 S5 Catawba River (CTB028 A) SR 1147 S6 Catawba River NC 18 S7 Parametric Coverage: Nitrogen and Phosphorus series should be taken at the above stations. 0 W J •J • y 1 • ,;f _ \l • .yy j) ii_ i_J• h t. \ • 173. �• ,J g CC - L • ac 1 ' ; r 1 i .� /, Figure 2 Li l z \; Stream Stations \\ it '.. . •'rill/ • ) \,\ ) • ' ▪ •'>•) l Table 3. Lake Stations - Lake Rhodhiss Station # Location L1 (CTB034A) at SR 1501 L2 near mouth of Smoky Creek L3 by island just below mouth of Howard Creek L4 (CTB040A) SR 1001 LS by boat ramp just beyond mouth of Freemason Creek L6 where lake turns sharply to right below mouth of Hayes Mill Creek. L7 just above Rhodhiss Dam Parametric Coverage: Sampling will be performed at the center of the channel. Secchi disk depth and D.O. will be taken at each station such that the euphotic zone and hypolimnion may be determined. An integrated sample will be taken from the euphotic zone for analysis of N and P series and chlorophyll a. A sample for N + P series will also be taken from the hypolimnion. tf?l`!UP: •' ccoz G1yJ``,\ ` 0J .v \t\ ? ,,.I- :% l;1�• Figure 3 1 ' ' �' .�... •_ r ;� i ` Lake Stations Y.), \\\.) t) - �/ St'_---',- -< J ii.mf //tr,/t• + ��,� ,ter-J � / - oJ ;f �� l��YJ Q i�y° N....`'.ter • ~I� 1 a /�•., -- �� !",✓mil I. .` _ t i ,,f i l -L` F— s. '.. LW 1f CC ,�� .�� � - 0� _, • • • 1 J O ` Z 1 U.) C't II H..11'11 a it Free m a 'II r) //0 . � �1 tit 1 , : 1 (' / i r Table 4. Major* Dischargers in Lake Rhodhiss Drainage Area Discharger Design Flow 1. Morganton -Catawba River WWTP NC0026573 8.0 MGD 2. Valdese -Lake Rhodhiss WWTP NC0041696 7.5 MGD 3. Lenoir -Lower Creek WWTP NC0023981 6.0 MGD 4. Valdese-McGalliard Creek WWTP NC0020753 3.2 MGD 5. Marion-Corpening Creek WWTP NC0031879 3.0 MGD 6. Great Lakes Carbon -Silver Creek NC0005258 2.6 MGD 7. Valdese -Hoyle Creek WWTP NC0021199 1.0 MGD 8. Drexel WWTP-Howard Creek NC0021296 0.5 MGD *This list includes all dischargers.with a design flow equal to or greater than 0.5 MGD. Parametric Coverage: Grab samples for N and P series will be taken from the above dischargers. If required monitoring equipment is available, composite samples will be taken at the larger dischargers. \ r= CSS t�Irlit') �U" .11 Y 1 �r Figure 4 Major Dischargers in Lake Rhodhiss Drainage Area •1,94 . -Jo \LaJ Q \,11i, ..... fir ] ly \CC `J 1,Q rt • c9 .CC ) ` Figure 4 Cont'd • • ` 0 Li I.11lit' • nut 1. 1k 03 il2.704.31 �_ (•► /r// )/ l• Cr—IC:2 a dim tot I`v /? / ( )J `8104, 011 _ 03 113 G1,--3-_ Q� I NC fro i CU •,J \ /tlair (/ r-1 ra tl- r('('1%ii�.\Ilii r • 1 ` • Ifi t3 r3 l,cr' —t.1 1 it/(l1•'r, 14t: 1► i + ;�/• • a • REFERENCE CITED Carlson, R.E., "A Trophic State Index for Lakes", Limnol. Oceanogr. Vol. 22:361-369, 1977. EPA, "Report on Rhodhiss Lake, Burke and Caldwell Counties, North Carolina", EPA Region IV, National Eutrophication Survey, Working Paper No. 388, June, 1975. EPA, "Eutrophication Analysis of the Proposed Columbia Reservoir - Duck River Basin, Tennessee", Water Qaulity Standards Section, Water Quality Management Branch, Water Division, EPA -Region IV, July 30, 1980. Higgins, J.M. and Kim, B.R., "Phosphorus Retention Models for Tennessee Valley Authority Reservoirs", Water Resources Research, Vol. 17, No. 3: 571-576, 1981. Marler, J. and Kutzman, J'., "A Holistic Lake System Assessment", A Paper presented at the National Water Quality Management Conference, Atlanta, Georgia, June 4-6, 1980. Vollenweider, R., "Input - Output Models, with Special Reference to the Phosphorus Loading Concept in Limnology", Schweiz. Z. Hydrol., Vol. 33:53-83, 1976. Vollenweider, R., Personal Communication found in Rast, W. and Lee, G., "Summary Analysis of the North American (US Portion) OECD Eutrophication Project: Nutrient Loading - Lake Response Relationships and Trophic State Indices", U.S. EPS Ecological Research Series, January, 1978, EPA-600/3-78-008, communication transmitted January 20, 1977. DIVISION OF EMMENTAL MANAGEMENT August 3e 1981 Mr. Howard Ze1 lery Acting Director Enforcement Division U. S. Environmental Protection icy Region Iv 345 Cot rtland Strut, N.E. At1 an to s Georgia 35365 Subject: 'i•: i uesi-fer...Nedi fication �„,, 44. �� Dischar Permit' Carpeting Creek Wastewater Treatment •' Plant City of Marlon 1 licDwell CotaiQy s North Cat i na Dear Mr. . Zeller: The City of Marion has rutted that -Division of Envi ron:r tal t review the effittent limits contained as a part of tones mi- t:harp Permit Colo. PIC0031879 to determine if the . lintitations placed upon phosphons and oxygen consuming waste are valid in -11 girt of present day standards and allocation methodology. Limitations for oxygen consv1ng taste were the result of a modified Level it evaluation waning limited field work specific to C rpening Cry was utilized for purposes of developing constants for use in the modified Streeter -Phelps Equation. P osphor= l imi is were ,,', velopad pri sari ly a a pr 3dtct of limited work by the!:o S. Envi ron ental Protection Agency t n the headwater lakes of the Catawba River. The City of itsrion ha$ ex- pound interest in gaining sow relief from pint final effluent limns for the reason that tva experience City might thereby experiensavil ;, in opera- tional costs at its Coriling Creek Wastarater Treatment Plant. The Division of En vi tal Manegemant is i h 1 n g to inert time in saking the doter nation as to whether conditions as they exist today in Lake Rhodi ss or as they exist in the near future raight al l aw nods fi ca- tion of the phosphors limits for the C orrpening Comic Wastewater Treatment Plante Addltlonallya the Division of Environmental f nt is willing to invest its mammas in the conduct of a Laval C sty of Corpen1ng C:,s f `� Creek which would include In intensive spy with slug sapling tor �. mina if the present permit limits for o,ypn consuming avast .are in ...,:_ ,S i.; . of modification. Obvilys the inmost of time and ray in effort by the Division Of FAVimmental itnagacesst mold not be 3. , fib'- ",, �. if the U. S. Environmental Protection Agency would not allow role certain 1irdts should the above scribed star demonstrate that Quality Standards would be protected in Corpon1ng Creek by the disci` r y 6.„ „ • wastewater of a lesser -quality then presently described .in the City -11P ES . Ord Zeller Page 2 August 31, 1981 Permit. Cbviauslyo effluent lints could be no less stringent the quh d by applicable effluent guidelines. The State of North Carolina would be in- terested in giving this relief to the City of Harlon if justified so that the City 10 turn et ght be in a position to experience cost savings as a re- sult of Tess stringent effluent requirements. I would appraciate your giving this Should 1t be helpful to you 1n arriving pose' further0 please contact Kr. L. P. Section at 919-7. 3 c 5083. cc: Vit. L. P. Banton 0 Jr. a Chief Water Quality Secct1 cat Mr. J. Earl Daniels:, Manager C1 Qy of fir! ae matter your careful consideration. at a decision to discuss this pro - Benton:, Chief of the war Qual 1 ty Sincerely yourss9 Original Signed By POB€RT F. HELMS Robert F. Wel = 81 rear Kr. Heath P. Dobsa 9 Regional Engineer Water Quality Section a Asheville \iv)