Loading...
HomeMy WebLinkAboutB14_RoanokeBASIN 14 ROANOKE BASIN DESCRIPTION The Roanoke Basin in North Carolina comprises 3,530 square miles of the nearly 10,000 square mile Roanoke River Basin that straddles the North Carolina-Virginia border. The mainstem of the Roanoke begins in the Blue Ridge Mountains of Virginia and flows generally southeasterly to Albemarle Sound. The Dan and Hyco Rivers drain a stretch of land along the Virginia state line from northeastern Surry County to Kerr Lake in Granville County before they join the Roanoke. Leaving Kerr Lake the river flows into Lake Gaston and then Roanoke Rapids Lake. The water releases from all three lakes are used to generate electricity. Releases from Roanoke Rapids Lake are also managed to protect water quality and maintain aquatic habitat downstream as well as power generation. Below Roanoke Rapids the river regains its riverine characteristics and becomes a meandering coastal plain waterway. WATER USE Factors Affecting Water Demand This basin has about 4% of the state’s residents and contains all or part of 24 municipalities in 16 counties. One of the state’s 12 major metropolitan areas overlaps with the headwaters of this basin. From 1990 to 1997 year-round population in three counties in this basin grew by 10% or more. Over the same period, three counties in the lower basin had zero or declining population changes. Total Water Use in Basin Total water use in the basin was estimated at 77.6 million gallons per day (mgd), with about 56% coming from surface water sources. The U.S. Geological Survey’s (USGS) 1995 summary of water use estimated total basin population at 283,410, with total residential demand estimated at 17.3 mgd. Fifty-one percent of the residential demand was served by public water systems. Overall, public water systems supplied 25.8 mgd from surface water and 6.5 mgd from ground water for both residential and non-residential uses. The remaining residential water demand was met by 8.5 mgd of self-supplied ground water. An additional 36.7 mgd of self- supplied water was used for non-residential uses. Local Water Supply Plans (LWSPs) Units of local government that supply or plan to supply water to the public are required to develop a LWSP. The Division of Water Resources (DWR) reviews LWSPs and maintains a database of the LWSP information. This summary is based on data contained in the 1997 LWSPs. LWSPs were submitted by 36 public water systems using water from this basin. These systems supplied 29 mgd of water to 124,389 persons. The following discussion and table summarize the LWSP population served with water from the Roanoke basin and its water use for 1997. 1997 LWSP System Water Use from Basin (mgd) Sub-basin LWSP Population Residential Use Non-residential Use Total Use* Roanoke River 124,389 8.49 16.30 29.0 *Total Use includes unaccounted-for water and system process water. Residential uses accounted for 29% of water use in these systems while non-residential water use accounted for 56% and 12% was unaccounted-for water. Considerable growth in population and water use is expected in this basin. LWSP systems expect to supply water to171,132 persons by the year 2020, a 38% increase over 1997 levels. Their water demand is projected to increase from 29 mgd to 45 mgd by 2020, a 55% increase. In the 1997 LWSPs, two of the 36 systems using water from this basin reported that their peak demands will exceed their water treatment capacity by 2010. Water systems should maintain adequate water supplies and manage water demands to ensure that average daily use does not exceed 80% of their available supply. Data for 1997 indicated that five of the 36 LWSP systems in this basin had average demand above this threshold. By 2020, four systems project demand levels that will exceed 80% of their available supply. Self-supplied Water Not everyone gets water from a public water system. Many households and some commercial and industrial operations supply their own water. The USGS estimated that self-supplied users, excluding power generating facilities, accounted for 45 mgd of the 78 mgd total of water used from this basin, as shown in the table below. Industrial uses comprised 37% of self-supplied water used, followed by irrigation (32%), domestic (19%), livestock (11%), and commercial (1%) uses. 1995 USGS Estimated Self-supplied Water Use in mgd Sub-basin Domestic Livestock Industrial Commercial Irrigation Total Roanoke River 8.52 5.00 16.72 0.46 14.54 45.24 Registered Water Withdrawals Anyone withdrawing 1.0 mgd or more of surface or ground water for agricultural uses or 100,000 gallons per day for other uses is required to register that withdrawal with DWR. Registered withdrawals in this basin are summarized in the table below. Registered Water Withdrawals for 1999 Sub-basin Agricultural # mgd Non-agricultural # mgd Total # mgd Roanoke River 18 36.5 20 103 38 13945 *Excludes water use for power generation. All of the registered agricultural water use in this basin is for crop irrigation. The non-agricultural water users include one golf course, three mining operations, seven industries, and nine private water systems. The two largest industries used an average of 65 and 26 mgd of water. Three of the industrial users and the golf course are permittees in the existing Capacity Use Area #1. WATER AVAILABILITY Surface water is used to meet the majority of overall water needs in the Roanoke River Basin, especially in the upper basin. LWSPs indicate that eight water systems in this basin withdraw about 28 mgd of surface water. Surface water will continue to be the primary source of water for most of the residents of the basin. Local water supply plans show that six systems rely on reservoirs for all or part of their water supply. The combined demand on these reservoirs averaged about 14 mgd in 1997. The estimated available supply from these reservoirs is 64 mgd. Five of the surface water systems submitting local water supply plans have run-of-river intakes that supplied about 13.7 mgd of water in 1997. The available supply from these intakes, based on information reported in local water supply plans, is about 49 mgd. Ground water is an important water source for systems in the lower Roanoke Basin, which extends into the coastal plain. Sixteen LWSP systems supplied 2.7 mgd of ground water to their customers in 1997. The combined 12- hour yield reported by these systems is 7.2 mgd. The water-bearing geologic deposits of the coastal plain form a regional aquifer system that has historically provided plentiful, high-quality, low-cost water. However, ground water levels in some of the major aquifers have been declining because of over-pumping. To ensure that ground water remains a reliable long- term water source in the Coastal Plain, the Environmental Management Commission adopted rules in December 2000 establishing a Capacity Use Area for 15 counties in the Central Coastal Plain, including Martin and Washington. If approved by the legislature in 2002, permits would be required for all ground water withdrawals over 100,000 gallons per day within these counties. Pumping from the Black Creek and Upper Cape Fear aquifers would be limited or reduced in some areas. Affected water users will need to manage water demand and develop alternative sources of supply to offset these reductions. INTERBASIN TRANSFERS OF SURFACE WATER Across the state many water users and systems move water between sub-basins to meet their needs. Regulatory approval is generally needed for transfers of 2.0 mgd or more. The table below summarizes the identified interbasin transfers in 1997 associated with this basin. Estimated Interbasin Transfers based on 1997 data Sub-basin Number mgd OUT mgd IN Roanoke River 9 1.97 0.39 The most significant interbasin transfer out of the basin is not reflected in this table–the 60-mgd withdrawal from Lake Gaston by Virginia Beach, Virginia. Virginia Beach began pumping in 1998 following a very lengthy and contested Federal Energy Regulatory Commission approval process, during which North Carolina opposed the withdrawals. SUMMARY OF INFORMATION FROM 1997 LWSPs !Total per capita water use for the basin was 234 gallons per day (gpd) in 1997 and is projected to increase to 237 gpd by 2010. !24 systems are not connected to another water supply system capable of supply water in an emergency. !15 water systems purchased a total of 5.265 mgd of water from this basin. Two of these systems had no purchase contract. !Nine systems rely on purchase water as their sole supply. !The systems used 28 mgd from surface water and 2.7 mgd of ground water. !The reported raw water supply was 113 mgd of surface water and a 12-hour groundwater supply of 7.2 mgd. !There are five county-wide systems and two regional water supply systems. !Nine systems were planning additional supplies totaling 11 mgd in the 1997 LWSPs. !The systems are projecting significant growth, 38% in population and 55% in demand, by 2020. !About 0.4 mgd of additional water supply will be needed by water systems to ensure that water demands in 2010 do not exceed 80% of available supply. !Systems reporting high Demand-to-Supply Ratios: 1997 2010 Demand exceeds available supply 1 1 Demand exceeds 80% of available supply 5 4 January 2001 State Water Supply Plan Division of Water Resources, DENR ROANOKE RIVER BASIN (14) 1997 and 2010 Population and Water Use as reported by LWSP systems using water from this basin. Water systems showing "Demand as % of Supply" above 80% should be actively managing demand and pursuing additional supplies.mgd = million gallons per day Water Systems by County Water Source or Supplier 1997 2010 1997 2010 1997 2010 1997 2010 BERTIE BERTIE CO RWS Upper Cape Fear Aquifer 6076 8870 0.294 0.539 1.131 2.139 26%25% KELFORD Upper Cape Fear & Beaufort Aquifers 189 210 0.014 0.021 0.058 0.058 24%36% LEWISTON-WOODVILLE Upper Cape Fear Aquifer 1022 980 0.121 0.119 0.216 0.216 56%55% ROXOBEL Upper Cape Fear Aquifer 290 315 0.023 0.024 0.043 0.043 53%56% WINDSOR Upper Cape Fear & Black Creek Aquifers 2450 2800 0.387 0.477 0.9 0.9 43%53% CASWELL MILTON Bedrock Wells 179 189 0.017 0.017 0.108 0.108 16%16% YANCEYVILLE County Line Cr. Res. 2421 2540 0.231 0.55 6.3 6.3 4%9% GRANVILLE OXFORD KERR LAKE RWS 10000 15000 0 0 2 3 67%66% STOVALL Bedrock Wells 500 700 0.026 0.053 0.092 0.092 28%58% HALIFAX ROANOKE RAPIDS SD Roanoke Rapids Lake 22271 23492 5.517 6.3 12.5 12.5 44%50% WELDON Roanoke River 1508 1588 0.786 1.197 14 14 6%9% MARTIN (in proposed Central Coastal Plain Capacity Use Area) HAMILTON Upper Cape Fear Aquifer 544 618 0.05 0.061 0.324 0.324 15%19% JAMESVILLE Black Creek Aquifer 632 645 0.055 0.062 0.252 0.252 22%25% MARTIN CO WSD 1 HAMILTON, Ground water, WILLIAMSTON 0 2535 0 0.183 0 0.81 0%23% MARTIN CO WSD 2 Ground water, BEAR GRASS, WILLIAMSTON 0 3619 0 0.432 0 1.15 0%32% WILLIAMSTON Black Creek, Beaufort, & UCape Fear Aquifers 6274 9477 0.923 1.788 1.674 2.394 55%75% NORTHAMPTON JACKSON Lower Cape Fear Aquifer 664 620 0.097 0.12 0.216 0.216 45%56% NORTHAMPTON-GASTON ROANOKE RAPIDS SD 900 1050 0.132 0.204 0.142 0.292 93%70% NORTHAMPTON-LAKE GASTON Lower Cape Fear Aquifer 1800 2400 0.087 0.082 0.191 0.191 46%43% NORTHAMPTON-PROGRESSIVE Upper Cape Fear Aquifer / WELDON 684 875 0 0 0.151 0.151 37%44% PERSON ROXBORO Stories, Satterfield,S.Hyco Creeks & Lake Roxboro 10847 11625 3.464 4.18 11 11 32%38% ROCKINGHAM EDEN Dan River 15500 17310 12.544 13.322 24.17 24.17 52%55% MADISON Dan River 2482 2678 0.512 0.704 15 15 3%5% MAYODAN Mayo River 2553 2900 1.665 3.566 10 10 17%36% STONEVILLE MAYODAN 1107 1200 0.184 0.209 1.008 1.008 18%21% STOKES DANBURY Bedrock Wells 175 220 0.029 0.041 0.072 0.072 41%56% STOKES C0 SE MADISON 0 0 0 0 0 0 0%0% WALNUT COVE Bedrock Wells 1147 2000 0.203 0.399 0.198 0.198 106%202% VANCE HENDERSON KERR LAKE RWS 16639 19256 2.66 6.09 6 9 44%68% KERR LAKE RWS Kerr Lake 0 0 4.628 11.137 20 20 23%56% KITRELL WA KERR LAKE RWS 1000 1200 0.078 0.093 0.079 0.116 100%80% WARREN NORLINA WARREN CO 1034 1100 0.19 0.198 0.2 0.2 95%99% WARREN CO KERR LAKE RWS 500 4900 0.708 1.301 2 2 35%65% WARRENTON WARREN CO 2650 2757 0.346 0.37 0.4 0.4 87%93% WASHINGTON (in proposed Central Coastal Plain Capacity Use Area) PLYMOUTH Castle Hayne & Yorktown Aquifer 4328 4921 0.471 0.405 1.675 1.675 28%24% WASHINGTON CO CRESWELL / ROPER / PLYMOUTH 5523 7070 0.353 0.468 0.532 1 66%47% Year-round Service Population Average Daily Demand (mgd)Available Supply (mgd)Demand as % of Supply