Loading...
HomeMy WebLinkAbout1403_FoothillsMSWLFLIned_ASD_DIN27386_20161104 PREPARED FOR: REPUBLIC SERVICES OF NORTH CAROLINA, LLC D.B.A. FOOTHILLS ENVIRONMENTAL 2800 CHERAW ROAD LENOIR, NORTH CAROLINA 28645 FOOTHILLS REGIONAL LANDFILL PERMIT NO. 14-03 ALTERNATE SOURCE DEMONSTRATION FOR COBALT AND REQUEST TO USE BACKGROUND AS THE GPS NOVEMBER 2016 PREPARED BY: 2211 WEST MEADOWVIEW ROAD, SUITE 101 GREENSBORO, NORTH CAROLINA 27407 NC LICENSE NUMBER C-0782 PHONE: (336) 323-0092 FAX: (336) 323-0093 JOYCE ENGINEERING PROJECT NO. 00890.1601.12 ______________________________________________________________________________ Alternate Source Determination for Cobalt Joyce Engineering Foothills Regional Landfill, Permit No. 14-03 November 2016 i Alternate Source Determination for Cobalt and Request to use Background as the GPS Foothills Regional Landfill, Permit No. 14-03 TABLE OF CONTENTS 1.0 INTRODUCTION..............................................................................................................1  1.1  Site Description and Background ................................................................................ 1  1.2 Compliance Monitoring History .................................................................................. 1  1.3 Hydrogeologic Setting ................................................................................................... 1  2.0 COBALT CONCENTRATIONS IN GROUNDWATER ..............................................2  21 Comparisons to Groundwater Standards ................................................................... 2  2.2 Statistical Evaluation of Background ......................................................................... 3  2.0 NATURAL SOURCES OF COBALT .............................................................................3  3.0 CONCLUSIONS ................................................................................................................4  4.0 REFERENCES ...................................................................................................................4  TABLE Table 1: Historical Cobalt Detections CHART Chart 1: Cobalt Concentrations vs. Time DRAWING Drawing 1: Potentiometric Surface Contour Map (July 2016) APPENDICES Appendix A: Statistical Analysis Worksheets & Summary Appendix B: Cobalt in NC Stream Sediments ______________________________________________________________________________ Alternate Source Determination for Cobalt Joyce Engineering Foothills Regional Landfill, Permit No. 14-03 November 2016 1 1.0 INTRODUCTION On behalf of Republic Services of North Carolina, LLC (Republic), Joyce Engineering (JOYCE) presents this Alternate Source Demonstration (ASD) for the Foothills Regional Landfill in accordance with 15A NCAC 13B .1633(c)(3). This ASD addresses recent and historic detections of cobalt above groundwater protection standards (GPS), as requested in a Letter from the NCDEQ to Republic dated August 8, 2016. 1.1 Site Description and Background The Foothills Regional Landfill is located approximately two miles northwest of Lenoir, North Carolina in Caldwell County at 2800 Cheraw Road. The landfill is bounded to the north and east by mainly wooded and agricultural properties, to the south by Cheraw Road, and to the west by rural residential/wooded properties and Abingdon Road. The location of the facility is shown on the inlay on Drawing 1. The facility is a lined Subtitle D municipal solid waste landfill which began operating in 1998 under Permit Number 14-03, issued by the North Carolina Department of Environmental Quality (NCDEQ). The approximately 230-acre facility is maintained and operated by Republic Services of North Carolina, LLC. 1.2 Compliance Monitoring History Groundwater monitoring at the facility was initiated in 1998 under the Detection Monitoring Program for municipal solid waste landfills. The facility’s current monitoring network is comprised of nine monitoring wells: MW-1R (background), MW-2R, MW-3R2, MW-4, MW-5, MW-6, MW-7, MW-8, and MW-10, which monitor the uppermost aquifer beneath the facility. In addition, four surface water sampling points are sampled semiannually: upstream surface point SW-1; and downstream surface points SW-2, SW-3, and SW-4. Two underdrains are also sampled semiannually: UD-1, the underdrain for Cell 1; and UD-2, the underdrain for Cells 4 and 8A. The locations of all sampling points are shown on Drawing 1. The facility was in an Assessment Monitoring Program in 2006. An Alternate Source Demonstration (ASD), for volatile organic compounds (VOCs) detected in wells MW-3 and MW-3R, was approved by NCDEQ on December 14, 2006, and the facility reverted to a Detection Monitoring Program. 1.3 Hydrogeologic Setting Geologically, the facility is located in the northwestern portion of the Inner Piedmont Belt of the Piedmont Physiographic Province, approximately 20 miles east of the thrust belt (Brevard Shear Zone) delineating the boundary between the westerly Blue Ridge Belt and the easterly Inner Piedmont Belt. The metamorphic rocks of the Inner Piedmont Belt generally group within the sillimanite facies of the amphibolite metamorphic sequence. Locally, the bedrock underlying the facility has been mapped as migmatitic granitic gneiss of the Ordovician and older Cambrian ______________________________________________________________________________ Alternate Source Determination for Cobalt Joyce Engineering Foothills Regional Landfill, Permit No. 14-03 November 2016 2 Periods. These rocks are described as ranging in composition from granitic to quartz dioritic with smaller biotite gneiss and amphibolite facies present locally. The unit as a whole exhibits a variable massive to foliated fabric (NCGS, 1985). The uppermost aquifer beneath the facility is present within weathered bedrock saprolite and fractured bedrock. The saprolite ranges in texture from clayey silt in the upper, most weathered sections to micaceous sandy silt in the lower sections. Immediately above the competent bedrock surface, a variable thickness transitional zone composed of highly weathered and degraded friable bedrock is present. The uppermost aquifer is laterally continuous across the site, with depth to water ranging from less than 31 feet in low-lying areas to greater than 77 feet beneath topographic highs. Groundwater in the uppermost aquifer generally flows from recharge areas associated with broad gently sloping topographic areas towards topographically lower areas that are generally delineated by the presence of stream channels, some of which are perennial receiving streams (groundwater discharge areas) and others of which are intermittent discharging streams. In the vicinity of the facility, the general groundwater flow direction is towards the south and west. Groundwater elevations obtained during the July 28, 2016, monitoring event are summarized in Table 1 and were used to prepare a potentiometric surface map presented as Drawing 1. The groundwater flow in the uppermost aquifer beneath the site is toward south and west in the direction of Abingdon Creek. The potentiometric surface map and interpreted flow directions are consistent with previously submitted potentiometric surface maps for this facility. 2.0 COBALT CONCENTRATIONS IN GROUNDWATER 21 Comparisons to Groundwater Standards For most constituents, the Groundwater Protection Standards (GPS) are the standards found in 15A NCAC 2L.0202 (NC2L Standards); however, the NCDEQ Solid Waste Section (SWS) has established alternate groundwater protection standards for constituents with no listed NC2L standard, referred to herein as the GWPS. The SWS has also established reporting limits for constituents, referred to as the Solid Waste Section Limits (SWSL), below which detections are considered estimated (not quantified). There is no NC2L standard established for cobalt. The SWS GWPS for cobalt is 1 µg/l; however, this is less than the SWSL of 10 µg/l. Estimated detections (below the SWSL) are not considered exceedances, so the effective GPS is the SWSL. Cobalt was detected in MW-4 above the GWPS and SWSL during the most recent (July 28, 2016) monitoring event with a concentration of 18.7 µg/l. No other inorganic constituents were detected at quantified concentrations above their respective NC2L or GWPS during the July 28, 2016, monitoring event. These results are consistent with historical detections of cobalt at the facility. The full results, including laboratory analytical reports, of the July 2016 sampling event ______________________________________________________________________________ Alternate Source Determination for Cobalt Joyce Engineering Foothills Regional Landfill, Permit No. 14-03 November 2016 3 have been presented in the Second Semiannual Water Quality Monitoring Report of 2016, dated September 2016. Cobalt in MW-4 has been consistently above the GWPS and SWSL, with the highest historical concentration of 27 µg/l in July 2009. Historically, there have also been periodic quantified exceedances for cobalt in UD-1 and UD-2. Table 1 presents all of the historical cobalt detections for the Foothills Landfill from August 1998 through July 2016, and Chart 1 shows a graph of the cobalt concentrations vs. time. There do not appear to be any consistent trends in the cobalt concentrations with time. 2.2 Statistical Evaluation of Background The data were evaluated through the use of the Shapiro-Wilk Test, Parametric Prediction Limits, Parametric Tolerance Intervals, Aitchison’s Adjustment, Non-parametric Prediction Limits, and Poisson Prediction Limits, as appropriate. Background data, tests for normality, outliers, Aitchison’s adjustment, tolerance interval, or prediction limits are used, as appropriate based on the background data. The statistical test by which downgradient data are compared to facility background data is based upon the nature of the data and the number of data values that are less than the laboratory limit of detection. All statistical tests are evaluated at the 0.05 level of significance, 95% confidence level, and are conducted as one-tailed tests. MW-1 was the upgradient background well for the facility from August 1998 through the July 2015 sampling event. MW-1, was abandoned in preparation for construction of Cell 5A and a new background well, MW-1R, was installed in October 2015. The data used for statistical analysis of the background consists of all the data available for both MW-1 and MW-1R from August 1998 through July 2016. Cobalt was detected in MW-4 at quantified concentrations above the GWPS during the July 28, 2016, monitoring event. The cobalt detections were statistically evaluated in accordance with the procedures outlined in 15A NCAC 13B.1632.(g) and (h) to determine if the quantified concentration exceeded the facility background concentration. Statistical analysis indicated a background level of 44.1 µg/l for cobalt. The statistical worksheets and summary table are presented in Appendix A. There have been no detections of cobalt above the statistical background in the history of the facility. 2.0 NATURAL SOURCES OF COBALT Cobalt is a common element occurring naturally in minerals commonly found in the bedrock, soil, and sediments in the North Carolina Piedmont. Appendix B presents a plate from A Geochemical Atlas of North Carolina (Reid, 1993), which shows the distribution of cobalt in stream sediments across the state. Caldwell County has been highlighted. Note that cobalt is found at concentrations as high as 10 mg/kg throughout Caldwell County; however there is a significant amount of variability. Metals in the soil and bedrock can easily leach into the groundwater, especially if the groundwater is acidic (pH < 7.0). The pH of groundwater samples ______________________________________________________________________________ Alternate Source Determination for Cobalt Joyce Engineering Foothills Regional Landfill, Permit No. 14-03 November 2016 4 from the Foothills Landfill during the July 2016 sampling event averaged 5.2, and the pH of the sample from MW-4, which had the highest cobalt concentrations, was 4.78. Also, since metals analyses required for the facility are for total metals, any suspended or dissolved sediment in the collected groundwater sample will be detected and included in the reported results. 3.0 CONCLUSIONS Cobalt is a naturally-occurring element if the bedrock, soil, and sediment in the region, and is therefore, expected to be naturally-occurring in the groundwater. The variations in cobalt concentrations in the groundwater are believed to reflect natural geologic variation at the site. Based on statistical evaluation, the cobalt detections at this facility are not statistically significant and are considered representative of historical background concentrations. The facility requests that the background value of 44.1 µg/l be considered the applicable groundwater protection standard for cobalt at the Foothills Landfill in accordance with 15A NCAC 13B.1634.(g).(5). 4.0 REFERENCES North Carolina Geologic Survey, 1985, Geologic Map of North Carolina; North Carolina Department of Natural Resources and Community Development, Geological Survey Section; scale 1:500,000. Reid, Jeffery C., 1993. A Geochemical Atlas of North Carolina. North Carolina Geological Survey, Bulletin 93. May 1991, Revised 1993. Table TA B L E 1 : H i s t o r i c a l C o b a l t D e t e c t i o n s Sa m p l e An a l y t e Da t e DL R L Co b a l t 08 / 1 0 / 9 8 -- - 10 ND -- - -- - -- - -- - -- - -- - -- - -- - -- - --------------------- 01 / 2 7 / 9 9 - - - 10 ND -- - -- - -- - -- - -- - -- - -- - -- - -- - --------------------- GW P S = 1 µ g / l 07 / 1 9 / 9 9 - - - 10 ND -- - ND -- - ND -- - -- - ND -- - -- - --------------------- 09 / 0 7 / 9 9 - - - 10 -- - -- - -- - -- - -- - -- - -- - -- - -- - -- - --------------------- SW S L = 1 0 µ g / l 09 / 0 9 / 9 9 - - - 10 ND -- - ND -- - ND -- - -- - ND -- - -- - --------------------- 10 / 1 2 / 9 9 - - - 10 -- - -- - ND -- - ND -- - -- - ND -- - -- - --------------------- Ba c k g r o u n d = 4 5 . 2 µ g / l 1 2 / 0 6 / 9 9 - - - 10 -- - -- - ND -- - ND -- - -- - ND -- - -- - --------------------- 01 / 2 5 / 0 0 - - - 10 ND -- - ND -- - ND -- - -- - ND -- - -- - --------------------- 07 / 2 1 / 0 0 - - - 10 ND -- - ND -- - ND -- - -- - ND -- - -- - ------------------ND 01 / 0 9 / 0 1 - - - 10 ND -- - ND -- - ND -- - -- - ND -- - -- - ------------------ND 07 / 1 7 / 0 1 - - - 10 ND -- - D r y - - - ND -- - -- - 10 . 0 -- - -- - ------------------ND 11 / 2 7 / 0 1 - - - 10 -- - -- - -- - -- - -- - -- - -- - -- - ND -- - --------------------- 01 / 2 2 / 0 2 - - - 10 ND -- - D r y - - - ND -- - -- - ND N D -- - ------------------ND 07 / 1 5 / 0 2 - - - 10 ND -- - D r y - - - ND -- - -- - 20 . 0 ND -- - ------------------ND 01 / 3 0 / 0 3 - - - 5 ND -- - -- - ND N D N D -- - 14 . 0 ND -- - ------------------ND 07 / 3 0 / 0 3 - - - 5 ND -- - -- - ND N D N D -- - 15 . 6 5. 6 6 - - - ------------------ND 01 / 1 5 / 0 4 - - - 10 ND -- - -- - ND N D N D -- - 16 . 0 ND -- - ------------------ND 07 / 1 6 / 0 4 - - - 10 ND -- - -- - ND N D N D -- - 15 . 8 10 . 7 - - - ------------------ND 01 / 2 8 / 0 5 - - - 10 ND -- - -- - ND N D N D -- - 1 3 . 4 B N D -- - ------------------ 3 1 . 6 0 07 / 2 1 / 0 5 - - - 10 ND -- - -- - ND N D N D -- - 17 . 7 ND -- - ------------------ND 10 / 2 1 / 0 5 - - - 10 -- - -- - -- - -- - -- - -- - -- - -- - -- - 17 . 1 --------------------- 01 / 1 8 / 0 6 - - - 10 ND -- - -- - ND N D N D -- - 15 . 4 ND N D ------------------ND 07 / 2 6 / 0 6 - - - 10 ND -- - -- - ND N D N D -- - 18 . 9 ND N D ------------------ND 08 / 2 1 / 0 6 - - - 10 -- - -- - -- - -- - -- - -- - ND -- - -- - -- - ------------------ND 10 / 0 3 / 0 6 - - - 10 -- - -- - -- - -- - -- - -- - ND -- - -- - -- - ------------------ND 01 / 2 3 / 0 7 -- - 10 ND -- - -- - ND -- - -- - ND 17 . 9 ND 10 . 9 ------------------ND 07 / 2 5 / 0 7 -- - 10 ND -- - -- - ND -- - -- - ND 19 . 5 ND 7. 0 0 J - - - ---------------ND 01 / 0 7 / 0 8 -- - 10 ND -- - -- - ND -- - -- - ND 8 . 7 J N D 6 . 9 0 J - - - ---------------ND 07 / 2 3 / 0 8 -- - 10 ND -- - -- - ND -- - -- - ND 10 . 2 ND 8 . 5 0 J - - - ---------------ND 08 / 1 1 / 0 8 -- - 10 -- - -- - -- - -- - -- - -- - -- - -- - -- - -- - ------------ 5 . 6 0 J - - - ND 01 / 0 6 / 0 9 -- - 10 ND -- - -- - ND -- - -- - ND 12 . 2 ND 5 . 4 0 J - - - ---------------ND 07 / 0 8 / 0 9 -- - 10 ND -- - -- - ND -- - -- - 1 . 6 2 J 27 . 0 ND 4 . 7 7 J - - - ---------26.3 ---ND 01 / 1 9 / 1 0 -- - 10 ND -- - -- - ND -- - -- - 0 . 5 6 J 22 . 6 ND 5 . 9 9 J - - - --------- 5 . 9 3 J - - - ND 06 / 0 2 / 1 0 -- - 10 -- - -- - -- - -- - -- - -- - -- - -- - -- - -- - 2.94 ---------------ND 07 / 2 7 / 1 0 -- - 10 ND -- - -- - ND -- - -- - ND 20 . 8 ND 2 . 6 0 J 1.46 --------- 5 . 9 8 J - - - ND 11 / 2 2 / 1 0 -- - 10 -- - -- - -- - -- - -- - -- - -- - -- - -- - -- - ND ---------------ND 01 / 2 4 / 1 1 -- - 10 ND -- - -- - ND -- - -- - ND 16 . 4 ND 4 . 0 6 J 2.51 --------- 9 . 3 0 J - - - ND 07 / 2 5 / 1 1 -- - 10 ND -- - -- - ND -- - -- - ND 23 . 8 ND 5 . 2 0 J 1.56 --------- 8 . 1 2 J - - - ND 01 / 0 5 / 1 2 -- - 10 . 0 ND -- - -- - ND -- - -- - 0. 2 J 18 . 2 ND 5 . 6 4 J 1.76 --------- 7 . 5 7 J - - - ND 07 / 0 3 / 1 2 -- - 10 . 0 ND -- - -- - ND -- - -- - 0 . 3 6 J 25 . 4 ND 4 . 4 8 J 1.56 ---------11.5 ---ND 01 / 3 0 / 1 3 -- - 10 . 0 ND -- - -- - ND -- - -- - 0 . 2 9 J 23 . 1 ND 4 . 3 2 J 0 . 9 9 ---------24.7 ---ND 04 / 1 0 / 1 3 -- - 10 . 0 -- - -- - -- - -- - -- - -- - -- - -- - -- - -- - ---7.32 J - - - ---------ND 05 / 0 9 / 1 3 -- - 10 . 0 -- - -- - -- - -- - -- - -- - -- - -- - -- - -- - --- 0 . 2 8 J - - - ---------ND 06 / 1 2 / 1 3 -- - 10 . 0 -- - -- - -- - -- - -- - -- - -- - -- - -- - -- - --- 1 . 5 5 J - - - ---------ND 07 / 1 5 / 1 3 -- - 10 . 0 ND -- - -- - 0 . 1 8 J - - - -- - 0 . 1 8 J 23 . 1 0. 1 2 J 4 . 3 8 J 3 . 6 6 J 6 . 0 4 J - - - ---26.2 ---ND 01 / 3 0 / 1 4 1 0 . 0 10 . 0 ND -- - -- - ND -- - -- - 0 . 6 0 J 22 . 6 ND 6 . 8 2 J 1 . 0 5 J 3 . 5 5 J - - - ---------ND 07 / 2 2 / 1 4 0 . 3 10 . 0 ND -- - -- - ND -- - -- - 1 . 8 4 J 21 . 2 ND 4 . 4 8 J 1 . 7 0 J 2 . 2 4 J - - - --- 7 . 1 0 J 11.9 ND 01 / 2 6 / 1 5 0 . 2 6 10 . 0 ND -- - -- - ND -- - -- - 0 . 3 9 J 19 . 0 ND 4 . 8 8 J 1 . 4 0 J 3 . 5 3 J - - - --- 7 . 3 4 J 16.0 ND 07 / 2 8 / 1 5 0 . 2 9 10 . 0 ND -- - -- - ND -- - -- - ND 19 . 0 ND 4 . 6 0 J 0 . 7 0 J 1 . 0 5 J - - - --- 6 . 9 6 J 16.0 ND 01 / 2 8 / 1 6 0 . 2 9 10 . 0 -- - 0 . 5 5 J - - - ND -- - -- - 0 . 3 7 J 19 . 1 ND 4 . 9 4 J 0 . 6 2 J 4 . 1 9 J - - - 1 . 8 5 J 10.3 8.9 J N D 07 / 2 8 / 1 6 0 . 2 9 10 . 0 -- - ND -- - ND -- - -- - ND 18 . 7 ND 5 . 0 1 J 1 . 1 1 J 1 . 6 6 J 1 . 8 1 J 0 . 5 4 J 2 . 3 J d r y N D No t e s : DL = M e t h o d D e t e c t i o n L i m i t . Al l c o n c e n t r a t i o n s a r e r e p o r t e d i n m i c r o g r a m s p e r l i t e r ( µ g / l ) . J = Estimated concentration above the DL but below the RL. RL = R e p o r t i n g L i m i t = P Q L p r i o r t o 2 0 0 7 a nd S W S L s t a r t i n g J a n u a r y 2 0 0 7 . ND = N o t d e t e c t e d a b o v e t h e D L . B = Blank-qualified data - analyte detected at a similar conentration in a quality-control blank. PQ L = P r a c t i c a l Q u a n t i t a t i o n L i m i t . Bl a n k s = H i g h e s t c o n c e n t r a t i o n d e t e c t e d i n f i e l d , t r i p a n d / o r m e t h o d b l a n k s . dry = insufficient water to sample. SW S L = N C - D E Q S o l i d W a s t e S e c t i o n L i m i t . Al l d a ta p r i o r t o 2 0 1 2 t a k e n f r o m p r e v i o u s r e p o r t s b y G o l d e r A s s o c i a t e s N C , I n c . --- = No data. NC 2 L = G r o u n d w a t e r S t a n d a r d es t a b l i s h e d i n 1 5 A N C A C 2 L . 0 2 0 2 Bold = Concentrations above the NC 2L or Groundwater Protecti on standards (GWPS). GW P S = N C D E Q S o l i d W a s t e S e c t i o n G r o u n d w a t e r P r o t e c t i on S t a n d a r d f o r c o n s t i t u e n t s w i t h n o l i s t e d N C 2 L . Blanks MW - 3 R M W - 3 R 2 M W - 4 M W - 5 M W - 6 M W - 7 M W - 8 M W - 9 M W - 1 0 U D - 1 U D - 2 MW - 1 M W - 1 R M W - 2 M W - 2 R M W - 3 Fo o t h i l l s R e g i o n a l L a n d f i l l Pe r m i t # 1 4 - 0 3 Joyce Engineering Chart Fo o t h i l l s R e g i o n a l L a n d f i l l Pe r m i t # 1 4 - 0 3 Joyce Engineering 05101520253035404550 J u l ‐ 9 9 J a n ‐ 0 0 J u l ‐ 0 0 J a n ‐ 0 1 J u l ‐ 0 1 J a n ‐ 0 2 J u l ‐ 0 2 J a n ‐ 0 3 J u l ‐ 0 3 J a n ‐ 0 4 J u l ‐ 0 4 J a n ‐ 0 5 J u l ‐ 0 5 J a n ‐ 0 6 J u l ‐ 0 6 J a n ‐ 0 7 J u l ‐ 0 7 J a n ‐ 0 8 J u l ‐ 0 8 J a n ‐ 0 9 J u l ‐ 0 9 J a n ‐ 1 0 J u l ‐ 1 0 J a n ‐ 1 1 J u l ‐ 1 1 J a n ‐ 1 2 J u l ‐ 1 2 J a n ‐ 1 3 J u l ‐ 1 3 J a n ‐ 1 4 J u l ‐ 1 4 Jan‐15 Jul‐15 Jan‐16 Jul‐16 C o b a l t   C o n c e n t r a t i o n     ( µ g / l ) Ch a r t  1:    Co b a l t  Co n c e n t r a t i o n s  vs .  Ti m e MW ‐3R2 MW ‐4 MW ‐6 MW ‐7 MW ‐8 MW ‐9 MW ‐10 UD ‐1 UD ‐2 GWPS SWSL Background Drawing Appendix A Statistical Analysis Work Sheets and Summary JOYCE Project:Foothills Regional Landfill Project No: 890.1601.12 Task No:02 Date: October 2016 Analyte:Cobalt Concentration RL Sample No. Sample Date Location (µg/L)(µg/L) 1 10-Aug-98 MW-1 ND 10 2 27-Jan-99 MW-1 ND 10 3 19-Jul-99 MW-1 ND 10 4 9-Sep-99 MW-1 ND 10 5 25-Jan-00 MW-1 ND 10 6 21-Jul-00 MW-1 ND 10 7 9-Jan-01 MW-1 ND 10 8 17-Jul-01 MW-1 ND 10 9 22-Jan-02 MW-1 ND 10 10 15-Jul-02 MW-1 ND 10 11 30-Jan-03 MW-1 ND 5 12 30-Jul-03 MW-1 ND 5 13 15-Jan-04 MW-1 ND 10 14 16-Jul-04 MW-1 ND 10 15 28-Jan-05 MW-1 ND 10 16 21-Jul-05 MW-1 ND 10 17 18-Jan-06 MW-1 ND 10 18 26-Jul-06 MW-1 ND 10 19 23-Jan-07 MW-1 ND 10 20 25-Jul-07 MW-1 ND 10 21 7-Jan-08 MW-1 ND 10 22 23-Jul-08 MW-1 ND 10 23 6-Jan-09 MW-1 ND 10 24 8-Jul-09 MW-1 ND 10 25 19-Jan-10 MW-1 ND 10 26 27-Jul-10 MW-1 ND 10 27 24-Jan-11 MW-1 ND 10 28 25-Jul-11 MW-1 ND 10 29 5-Jan-12 MW-1 ND 10 30 3-Jul-12 MW-1 ND 10 31 30-Jan-13 MW-1 ND 10 32 15-Jul-13 MW-1 ND 10 33 30-Jan-14 MW-1 ND 10 34 22-Jul-14 MW-1 ND 10 35 26-Jan-15 MW-1 ND 10 36 26-Jul-15 MW-1 ND 10 37 28-Jan-16 MW-1R 0.55 J 10 38 29-Jul-16 MW-1R ND 10 Number of Data: 38 Number of Truncated Data: 37 Percentage of Truncated Data: 97% Upper Poisson Prediction Limit: 44.1 µg/L All concentrations in micrograms per liter (µg/L). ND = Not detected above the method detection limit (truncated). J = Estimated concentration below the RL. RL = Reporitng Limit (PQL or SWSL). Joyce Project:Foothills Regional Landfill Project No: 890.1601.12 Task No: 02 Date: October 2016 Upper Poisson Prediction Limit Analyte:Cobalt Background Data Discrete Concentration RL Half Poisson Sample No. Sample Date Location (µg/l) (µg/l) RL Count 1 10-Aug-98 MW-1 ND 10 5 5 2 27-Jan-99 MW-1 ND 10 5 5 3 19-Jul-99 MW-1 ND 10 5 5 4 9-Sep-99 MW-1 ND 10 5 5 5 25-Jan-00 MW-1 ND 10 5 5 6 21-Jul-00 MW-1 ND 10 5 5 7 9-Jan-01 MW-1 ND 10 5 5 8 17-Jul-01 MW-1 ND 10 5 5 9 22-Jan-02 MW-1 ND 10 5 5 10 15-Jul-02 MW-1 ND 10 5 5 11 30-Jan-03 MW-1 ND 5 2.5 2.5 12 30-Jul-03 MW-1 ND 5 2.5 2.5 13 15-Jan-04 MW-1 ND 10 5 5 14 16-Jul-04 MW-1 ND 10 5 5 15 28-Jan-05 MW-1 ND 10 5 5 16 21-Jul-05 MW-1 ND 10 5 5 17 18-Jan-06 MW-1 ND 10 5 5 18 26-Jul-06 MW-1 ND 10 5 5 19 23-Jan-07 MW-1 ND 10 5 5 20 25-Jul-07 MW-1 ND 10 5 5 21 7-Jan-08 MW-1 ND 10 5 5 22 23-Jul-08 MW-1 ND 10 5 5 23 6-Jan-09 MW-1 ND 10 5 5 24 8-Jul-09 MW-1 ND 10 5 5 25 19-Jan-10 MW-1 ND 10 5 5 26 27-Jul-10 MW-1 ND 10 5 5 27 24-Jan-11 MW-1 ND 10 5 5 28 25-Jul-11 MW-1 ND 10 5 5 29 5-Jan-12 MW-1 ND 10 5 5 30 3-Jul-12 MW-1 ND 10 5 5 31 30-Jan-13 MW-1 ND 10 5 5 32 15-Jul-13 MW-1 ND 10 5 5 33 30-Jan-14 MW-1 ND 10 5 5 34 22-Jul-14 MW-1 ND 10 5 5 35 26-Jan-15 MW-1 ND 10 5 5 36 26-Jul-15 MW-1 ND 10 5 5 37 28-Jan-16 MW-1R 0.55 10 5 0.55 38 29-Jul-16 MW-1R ND 10 5 5 Note: All sample concentrations are micrograms per liter (µg/L) Using the background data, the upper Poisson Prediction Limit, y*, is determined by: y* = c y + [(t^2) c / 2] + t c [y (1 + (1/c)) + ((t^2) / 4)]^0.5 where: c = k / n y = Poisson count t = t(n-1, 0.95), Student's t-distribution n-1 = degrees of freedom (number of samples - 1) k = number of downgradient samples per event (7) .95 = confidence interval n = number of background samples For: c = 0.184 k = 7 = 7 d.g. MW's y = 180.55 t = 1.689 n = 38 y* = 44.1 µg/L Co n s t i t u e n t S W S L N C 2 L G W P S Da t a Di s t r i b u t i o n St a t i s t i c a l M e t h o d u s e d t o Es t a b l i s h B a c k g r o u n d Ca l c u l a t e d Ba c k g r o u n d Co n c e n t r a t i o n Sa m p l e Lo c a t i o n Sample Result SSI Co b a l t 1 0 N / E 1 9 7 % T r u n c a t e d U p p e r P o i s s o n P r e d i c t i o n L i m i t - I n t e r w e l l 4 4 . 1 M W - 4 1 8 . 7 N O No t e s : Co n c e n t r a t i o n s a r e i n m i c r o g r a m s p e r l i t e r ( µ g / L ) . SW S L = N C D E Q S o l i d W a s t e S e c t i o n R e p o r i t n g L i m i t . NC 2 L = N o r t h C a r o l i n a G r o u n d w a t e r S t a n d a r d e s t a b l i s h e d i n 1 5 A N C A C 2 L . 0 2 0 2 . GW P S = G r o u n d w a t e r P r o t e c t i o n S t a n d a r d e s t a b l i s h e d b y t h e D E N R - S W S . SS I = S t a t i s t i c a l l y s i g n i f i c a n t i n c r e a s e o v e r b a c k g r o u n d . N/ E = N o t e s t a b l i s h e d . Su m m a r y o f S t a t i s t i c a l B a c k g r o u n d A n a l y s e s Fo o t h i l l s R e g i o n a l L a n d f i l l Pe r m i t N o . 1 4 - 0 3 Joyce Engineering Appendix B Cobalt in NC Stream Sediments