Loading...
HomeMy WebLinkAbout20042019 Ver 3_Staff Comments_20110125I RR- North Carolina Department of Environment and Natural Resources Division of Water Quality Beverly Eaves Perdue Coleen H. Sullins Dee Freeman Governor Director Secretary January 25, 2011 CERTIFIED MAIL: RETURN RECEIPT REQUESTED Mr. Brad Shaver, Acting Field Chief U.S. Army Corps of Engineers Wilmington Regulatory Field Office 69 Darlington Avenue Wilmington, North Carolina 28403 Subject Property: Anderson Creek Development Dear Mr. Shaver: DWQ Project # 04-2019, Ver. 3 Harnett County On behalf of the NC DWQ 401/Wetlands Permitting Unit, we again respectfully request that you consider the following comments within your review of the 404 Individual Permit request for the above referenced property: I . Applicant's Stated Purpose within the Public Notice states, "The purpose of the project is to construct a unique public recreational amenity within Anderson Creek to increase marketability. " yet, the Project Description located within 18. Nature ofActivity (Project Description) as part of the application, states the project is the development of Anderson Creek South (an expansion of the existing 773-acres Anderson Creek North residential Development) and requires the development of a road network, sewer outfalls, and an amenity to ensure the success of the development. It is unclear why the stated purpose does not include the residential development, road network and utility installation, since it would seem there would be no need for the recreational amenity were it not for the residential development to support it. Please clarify this inconsistency. Additionally, although the applicant's narrative attempts to convey the need for the "sailing" lake, the reader is left believing that the true need for the project in the area is the projected demand for reasonably priced housing due to the Base Relocation And Consolidation (BRAC). Our position regarding this understanding is further supported by enclosure of the letter from retired Brigadier General Paul R. Dordal to Ken Jolly of the USACE which states in the first paragraph, "this tremendous growth (at Fort Bragg) is straining our infrastructure and housing requirements, and we are encouraging developments, such as Anderson Creek South that meet the needs of military related growth while not encroaching on the installation." The second paragraph continues to discuss the need for housing in the area and ends with a comment regarding the applicant's avoidance and minimization of impacts to onsite wetlands for the project. It is not until the third paragraph in a four paragraph letter that the proposed "sailing lake" is mentioned. Therefore it is the opinion of this Office that the "sailing lake" should be regarded as an amenity to the residential and commercial development and not vice versa. 2. This project cannot be properly reviewed due to the lack of information contained in the Public Notice and the incredibly small scale of the submitted maps. Therefore, concerns regarding Wetlands, Buffers, Stormwater, Compliance and Permitting Unit (WeBSCaPe) 1650 Mail Service Center, Raleigh, North Carolina 27699-1650 Phone: 919-807-6301 1 FAX: 919-807-6494 Internet: hUp://pogal.ncdenr.org/web/wq/ws An Equal Opportunity lAffirmative Action Employer USACE Page 2 of 7 January 14, 2011 impacts to resources and water quality cannot be properly evaluated at this time. These deficiencies include: a. Lack of a map and tables describing the residential and commercial development, both proposed and existing within the project boundaries (specific map and data requests are cited later in this commenting letter). b. Lack of a map and tables describing roads and infrastructure, both proposed and existing within the project boundaries (specific map and data requests are cited later in this commenting letter). This should include road designs and traffic studies/justifications. 3. The compensatory mitigation plan included is not satisfactory. What was submitted is not even conceptual, but only speculative. 4. On page 2 of 6 of the Public Notice under 23. Avoidance, Minimization, and Compensation, the applicant states that the "we are of the opinion that any regulatory position that all ponds are detrimental to water quality and aquatic resources is based on subjective science that represents worst case scenarios... and believe that current technology can be employed to mitigate all practically foreseeable potential adverse impacts" (and yet the applicant offers no information to support their position). This Office very strongly disagrees with this statement. This Office recommends the applicant carefully read adjoining state Tennessee's study of the impact of small impoundments on stream (link: http://www.state.tn.us/environment/wpc/publications/pdf/isp report pdf ), and please carefully read DWQ's attached Selected Bibliography - Stream Impoundment Perspectives - 2008, and please consider the NC Dam Safety statewide dam assessment at this link: http://sections.asce.orWn carolina/ReportCard/dams pdf Additionally, a preimpoundment study conducted by Hayden M. Ratledge of the North Carolina Wildlife Resources Commission titled Preimpoundment Study of the French Broad River Watershed;1962: Anticipated Effects of the Presence of Ponds on Trout Streams in Transylvania and Henderson Counties North Carolina, concluded the following: a.) "It can be anticipated that the proposed flood control impoundments will increase the temperature below those impoundments approximately 13°F. This will make the water of the tributaries below the dams, and also of the main river, unsuitable for trout. " b.) "The construction of the proposed impoundments appears to be in contravention of the stated U.S. Forest Service Policy. " and c.) "The construction of the proposed impoundments appears to be in contravention of the N. C. State Stream Sanitation classifications so far as thermal pollution is concerned. " While this Office acknowledges this study was conducted in the mountains of the State, and the proposed "sailing lake" project is located within the Sandhills region of the state, the effect of impoundments on streams within either region of the State is comparable. Should you have any questions or need any clarification we will be happy to assist you in any way we can. Finally, please note that because the DWQ has a very strong opinion on this issue and it is very important to us, we were awarded a US EPA grant this year to conduct a similar study to the one Tennessee performed. On page 5 of 6 of the Public Notice under 23. Avoidance, Minimization, and Compensation, the applicant states that the "amenity must be constructed to comply with local zoning requirements.", and on page 1 of 4 of your application narrative, under 20. Reason(s) for Discharge, the applicant states that "Development of size and scope of Anderson Creek legally and practically require amenities to make them marketable." Please provide documentation of this requirement and a contact name of an individual member of the local zoning board who would be available to discuss this requirement, and cite a source stating that Anderson Creek is legally required to have amenities. USACE Page 3 of 7 January 14, 2011 6. This Office was unable to locate an alternatives analysis for other properties that were considered for this project and would like the applicant to address this concern. 7. To DWQ's knowledge, a geotechnical study has not been performed within the area identified for the proposed "sailing lake." This Office has concerns regarding whether a lake is truly feasible in this area, and strongly encourages such a study be undertaken. 8. It is our understanding that several years ago DWQ had concerns that this lake was being proposed in an area that included an impressive stand of Atlantic white cedar. It is unclear if the current proposed "sailing lake" is located in the area that includes the aforementioned stand of Atlantic white cedar? 9. On page 3 of 6 of the application under 18. Nature ofActivity (Project Description), the applicant states, "Proposed amenities include a tennis center, small recreational parks, and a 40- acre public access lake to accommodate the establishment of a sailing school and beach areas." and on page 5 of 6 of the Public Notice under 23. Avoidance, Minimization, and Compensation, the applicant states "smaller more dispersed ponds are not conducive to providing organized swimming under the supervision ofli eguards. " The proposed lake is located in Class C waters which are, "waters protected for uses such as secondary recreation, fishing, wildlife, fish consumption, aquatic life including propagation, survival and maintenance of biological integrity, and agriculture. Secondary recreation includes wa ing, boating, and other uses involving human body contact with water where such activities take place in an infrequent, unorganized, or incidental manner. " Will the applicant be seeking a re-classification of the surface water to "B"? Class "B" waters are, "waters protected for all Class C uses in addition to primary recreation. Primary recreational activities include swimming skin diving water skiing and similar uses involving human body contact with water where such activities take place in an organized manner or on a frequent basis." 10. It is not clear to this Office why there is a need for a 40-acre "sailing lake" at the proposed location when Harris Lake and Jordan Lake, which are much larger than the proposed lake, and allow for sailing, are both located approximately one-hour from the project site. This position is further supported by our calculation that approximately five million gallons of water per month will be lost from this proposed lake through evaporation. This would be a significant concern in light of recent statewide droughts. 11. Are the proposed lakes to be located in streams that contain migrating or spawning fish? Please provide documentation of any studies or data collected that indicate that no fish species spawn in the stream segments proposed for impact. 12. We would like to hear from the applicant on how they propose to maintain water quality standards upstream from the impoundment, within the entire impoundment, and downstream of the impoundment. The explanation provided is insufficient. 13. Staff with the North Carolina Division of Water Resources have the following comments: Our major interest is the release from the dam forming the "amenity" lake and the resulting downstream flow regime. To evaluate this release the applicant will need to provide the drainage area, mean annual flow and 7Q10 flow for the dam site. The latter two flow statistics should be obtained from the USGS. USACE Page 4 of 7 January 14, 2011 The application should also provide a description of how downstream flows will be provided - both how a constant minimum flow will be maintained and how the dam structure will provide an outflow equal to the inflow to the lake (assuming that is how it will operate). The application should also indicate whether the lake will be used for irrigation or any other activity requiring withdrawal. If not, then the applicant should indicate through covenants or some other mechanism how this will be assured for the life of the project. If the lake will be used for withdrawals, then this will need to be incorporated in how the downstream release is made, and may require gauging of inflow so the release can match inflow prior to any loss of water via irrigation or other withdrawal 14. This Office will need to see the applicant's complete and comprehensive lake design and dam details. 15. Will the lake shoreline be a natural shoreline or an "armored" shoreline (having installed bulkheads/seawalls)? 16. This Office identified fourteen (14) ponds currently on the subject property. Are all of these too small for a "sailing school"? Could any be expanded or combined to accommodate the applicants "sailing lake"? 17. On page 3 of 6 of the Public Notice under 23. Avoidance, Minimization, and Compensation, this Office believes there is an intent to dismiss several State regulations as "inappropriate" or "not applicable" based upon the assumption of natural condition. First, an impoundment is not a "natural condition". With that said, impoundments once completed, would be held to water quality standards in accordance with NC 15A NCAC .0213 and federal Clean Water Act provisions. One comment relating to applicability of a water quality standard notes that "the violation of the numerical water quality standard (temperature, pH, etc) would need to compromise the use before a violation is incurred: in other words, the violation would occur only after the water could no longer be able to support aquatic life (i.e. dead fish are floating on the lake), wildlife, or be used for recreation (i.e. can't sail a boat due to algae)." This statement is incorrect. An exceedence of a water quality standard that precludes "aquatic life propagation and maintenance of biological integrity" on a short or long term basis is indeed a violation of water quality standards. The regulations do not allow for fish to die before determining that a water body is not supporting its designated use, and in fact would defeat the purpose of water quality standards protecting wildlife and biology before mortality or extreme stress occurs. 18. This Office requests that the applicant please locate the project boundaries on the most recent bound and published Harnett County soil survey and the USGS 1:24,000 topographic map for the project. 19. This Office requests that the applicant please re-submit your site plans on full plan sheets at a scale of no smaller than 1"=50' with topographic contours shown. 20. This Office requests that the applicant please provide cross section details showing the provisions for aquatic life passage. 21. This Office requests that the applicant please provide building envelopes for all lots with wetlands and/or streams on the site plans. 22. This Office requests that the applicant please indicate all existing and proposed lot layouts as overlays on the site plan. Additionally, please indicate which lots are sold. USACE Page 5 of 7 January 14, 2011 23. This Office requests that the applicant please locate any planned sewer lines on the site plan. Additionally, please comment on whether there are any septic fields within the Anderson Creek development. 24. This Office requests that the applicant please indicate all proposed stream or wetland driveway crossings on your plan sheet (including future proposed). 25. This Office requests that the applicant please indicate all stream impacts including all fill slopes, dissipaters, and bank stabilization on the site plan. 26. This Office requests that the applicant please indicate all wetland impacts including fill slopes on the site plan. 27. This Office requests that the applicant please locate all isolated or non-isolated wetlands, streams, and other waters of the State as overlays on the site plan. 28. This Office requests that the applicant please provide a qualitative indirect and cumulative impact analysis for the project. Please see DWQ's policy for guidance on our website at: http://portal.ncdenr.oraJweb/wq/swp/ws/40 I/policies 29. This Office requests that the applicant please assess the need for a storm water management plan (SMP) on the site. Please comply with the requirements set forth below. In addition, the applicants shall follow the procedures explained in Protocol for Stormwater Management Plan (SMP) Approval and Implementation that is in place on the date of the submittal of the SMP. A. Project Density: Projects with SMPs that require 401 Oversight/ Express Unit approval shall be classified as either Low or High Density according to the criteria described below. 1. Low Density: A development shall be considered Low Density if ALL of the following criteria are shown to have been met. a. The overall site plan, excluding ponds, lakes, rivers (as specified in North Carolina's Schedule of Classifications) and saltwater wetlands (SWL), must contain less than 24% impervious surface area considering both current and future development. b. All stormwater from the entire site must be transported primarily via vegetated conveyances designed in accordance with the most recent version of the NC DWQ Stormwater BMP Manual. c. The project must not include a stormwater collection system (such as piped conveyances) as defined in NCAC 2B .0202. d. If a portion of project has a density greater than 24%, the project shall be considered low density as long as the higher density portion of the project complies with Items 1-3 above and the higher density area is located in upland areas and away from surface waters and drainageways to the maximum extent practicable. USACE Page 6 of 7 January 14, 2011 II. High Density: Projects that do not meet the Low Density criteria described above are considered to be High Density, requiring the installation of appropriate BMPs as described below. a. All stormwater runoff from the site must be treated by BMPs that are designed, at a minimum, to remove 85 percent of Total Suspended Solids (TSS). b. In addition to controlling 85 percent of TSS, projects requiring located in watersheds that drain directly to waters containing these supplemental classifications shall meet the following requirements: Water Quality Stormwater BMP Supplemental Classification Requirement §303(d) Project-specific conditions may be added by the Division to target the cause of the water quality impairment. NSW A minimum of 30 percent total phosphorus and 30 percent total nitrogen removal. Trout (Tr) A minimum of 30 percent total phosphorus and 30 percent total nitrogen removal; BMPs should also be designed to minimize thermal pollution. c. All BMPs must be designed in accordance with the most recent version of the NC Division of Water Quality Stormwater Best Management Practices Manual. Use of stormwater BMPs other than those listed in the Manual may be approved on a case-by-case basis if the applicant can demonstrate that these BMPs provide equivalent or higher pollutant removal. B. Vegetated Buffer: In areas that are not subject to a state Riparian Area Protection Rule, a 30-foot wide vegetated buffer must be maintained adjacent to streams, rivers and tidal waters as specified below. a. The width of the buffer shall be measured horizontally from: i. The normal pool elevation of impounded structures, ii. The streambank of streams and rivers, iii. The mean high waterline of tidal waters, perpendicular to shoreline. b. The vegetated buffer may be cleared or graded, but must be planted with and maintained in grass or other appropriate plant cover. c. The DWQ may, on a case-by-case basis, grant a minor variance from the vegetated buffer requirements pursuant to the procedures set forth in 15A NCAC 02B.0233(9)(h). d. Vegetated buffers and filters required by state rules or local governments may be met concurrently with this requirement and may contain coastal, isolated or 404 jurisdictional wetlands. USACE Page 7 of 7 January 14, 2011 C. Stormwater Flowing to Wetlands: Stormwater conveyances that discharge to wetlands must discharge at a non-erosive velocity prior to entering the wetland during the peak flow from the ten-year storm. D. Phased Projects: The DWQ will allow SMPs to be phased on a case-by-case basis, with a final SMP required for the current phase and a conceptual SMP for the future phase(s). If the current phase meets the Low Density criteria, but future phase(s) do not meet the Low Density criteria, then the entire project shall be considered to be High Density. Thank you for your attention. If you have any questions, please contact Ian McMillan in our Central Office in Raleigh at (919) 807-6301. Sincerely Ian McMillan, Acting Supervisor Acting Supervisor - Wetlands, Buffers, Stormwater, Compliance and Permitting Unit (WeBSCaPe) IJM Enclosure: Selected Bibliography - Stream Impoundment Perspectives - 2008 cc: Crystal Amschler, U.S. Army Corps of Engineers - Wilmington Regulatory Field Office Chad Turlington, DWQ Fayetteville Regional Office File Copy Chris Huysman, WNR, P.O. Box 1492, Sparta, NC 28675 Jim Mead, DWR Connie Brower, DWQ Jennifer Derby, Wetlands, Coastal, and Oceans Branch, Water Protection Division, U.S. Environmental Protection Agency, 61 Forsyth Street, SW, 15th Floor, Atlanta, GA 30303 Becky Fox, 1307 Firefly Road, Whittier, NC 28789 D.J. Gerken, SELL, 29 N. Market St., Suite 604, Asheville, NC 28801 Filename: 042019 Ver3AndersonCreekDevelopment(Hamett)IP_Commenting_Letter_USACE Selected Bibliography - Stream Impoundment Perspectives Compiled by North Carolina Division of Water Quality Staff June 2008 Introduction: Although Egyptians first constructed dams for the purpose of river regulation thousands of years ago (Smith, 1971), Man has only recently begun to understand and appreciate the dramatic and widespread effects of dams on river systems. The recent volume of work on impoundments, primarily published by environmental scientists in the United States and abroad in the last 50 years, suggests that the benefits associated with some impoundments (e.g. water supply, hydroelectric power, flood control, etc.) are accompanied by a great number of costs to nature, and ultimately, society. While far from comprehensive, the following summary document provides a good foundation on the many consequences of river impoundment. It is important to note that the literature uses the term "impoundment" to describe everything from large, water supply reservoirs to farm ponds created by small, earthen dams. It is also important to recognize that the summarized environmental, social, and economic effects will vary in magnitude depending on the impoundment's size and location. That said, the literature supports the following conclusions regarding the effects of river impoundment: Conclusions: 1. Impoundments negatively impact the physical, chemical, and biological characteristics of water (i.e. water quality) 2. Impoundments negatively impact ecological systems and native faunal/floral communities 3. Impoundments/dams create numerous maintenance and safety issues 4. Impoundments cause numerous hydrological, biological, and geomorphological impacts downstream due to changes in the flow regime and water quality Supporting Information: 1. Impoundments negatively impact the physical, chemical, and biological characteristics of water (i.e. water quality) a. Water temperature and dissolved oxygen When an impoundment is created, temperature and oxygen stratification may occur as water depth increases and flow velocity decreases. This process involves the in- flow of cooler, denser stream water to the bottom layer (hypolimnion) which pushes the water above it into the impoundment's top layer (epilimnion). Here, according to Maxted, McCready, and Scarsbrook (2005), the water warms and decreases in density as it is subject to "incoming solar radiation, unhindered by any of the topographic or vegetation shading characteristic of a stream channel". As the 2 suspended particles and substances in the epilimnion absorb solar radiation, the temperature in this shallow surface layer typically rises above the high daily maximum temperature of the inflowing stream. Maxted, McCready, and Scarsbrook observed temperature stratification in each of the six small ponds (ranging from 69-390 acres) they studied. Temperature (24° C) and dissolved oxygen (4 mg/L) were exceeded 46% and 86%, respectively, during a 40-day summer period. Maxted, McCready, and Scarsbrook also observed that thermoclines (i.e. zones of rapid temperature change) occurred above .5 meters in the small ponds. According to Higgs (2002), the hypolimnion and epilimnion seldom mix well enough to promote gas transfer from the highly-oxygenated surface water to the poorly-oxygenated bottom layer. As a result, the bottom water layer in an impoundment may become hypoxic and fail to support aquatic life. Depending on how water is released from the impoundment, these oxygen and temperature stratifications can lead to numerous problems downstream as well. In an attempt to preserve habitat for cold-water species such as trout, some dams release water from the cooler hypolimnion layer. However, while the temperature may be desirable for cold-water species, the lack of dissolved oxygen may still render the downstream habitat unsuitable. If the highly-oxygenated but warmer surface water is released downstream, cold-water fish may have adequate oxygen, but a "thermal block" is established which still prevents populations from reaching upstream spawning habitats (Higgs, 2002). Petts (1984) cites two field observations of seasonal dissolved-oxygen sags related to temperature stratification in upstream impoundments. The first, by Ingols (1959), occurred along the Holston River, below Cherokee Dam in east Tennessee. Ingols compared the dissolved-oxygen deficit in this location to be equivalent to that caused by the effluent from a town of 3,500,000 people. Petts' second example was from a study conducted by Walker et al. (1979) on the Murray River, below the Hume Dam in Australia. In this case, a dissolved oxygen sag attributed to lake stratification was observed for 100 km below the dam. b. Metal thresholds Metals can accumulate in impoundment sediments due to upstream pollution discharges, or from natural sources such as local soils. Problems associated with metals can be exacerbated by the aforementioned temperature and dissolved oxygen stratifications. For example, in Lake Toxaway in the Savannah River Basin of western North Carolina, researchers concluded that odor problems were emanating from manganese and iron concentrations that "increased significantly in response to increased hypoxic conditions near the bottom of the lake as summer progressed" (NC DENR, 2005). Metal concentrations exceeding state water quality standards have also been documented in impoundments in the Catawba, Yadkin, and Neuse river basins of North Carolina. 3 c. Sedimentation Sedimentation occurs when geologic or organic material falls out of suspension and accumulates in a given area. This phenomenon is common in impoundments for the following reasons: 1) inflowing streams/rivers slow down upon entering impoundments, and suspended soil particles settle out of the water column, 2) compared to natural streams and lakes, the water level in impoundments is regulated to be virtually constant. According to Nakashima, Yamada, and Tada (2007), nearly constant water levels may cause physical destabilization of impoundment shorelines, and 3) land-disturbing activities such as construction around the impoundment itself may lead to direct sedimentation. The sediment load of a stream is produced by sheet erosion of the surrounding landscape or by erosion of the stream bank itself (Baxter, 1977). Sedimentation is exacerbated when erosion increases upstream during storm events or as a result of construction, agriculture, or other land-disturbing activities. If flow rates decrease rapidly upon entering the impoundment, sediment may accumulate near this entry point, in the impoundment's upstream section. More often, however, sedimentation is a bigger concern further downstream in the impoundment, next to the dam. Sedimentation is a potential problem for water quality and aquatic life (e.g. sediment may carry potentially toxic materials, such as phosphorous, nitrogen, arsenic, chromium and copper), and it reduces the impoundment's water depth and water storage capacity. d. Turbidity Sediment or silt that remains suspended in the water column also causes physical and chemical changes in impoundments. In addition to detracting from a pond or lake's aesthetic value, high turbidity limits penetration of visible light, affects the heating and cooling rates of water, affects conditions on the bottom, and leads to the retention of organic matter (Ellis, 1936). By limiting the penetration of visible light, or by scattering light, turbidity can decrease the photosynthetic activity of plants and reduce the amount of dissolved oxygen. Additionally, suspended particles absorb heat from solar radiation causing the water to warm. Since oxygen cannot dissolve as easily in warm water, turbidity can further lower dissolved oxygen concentrations. High turbidity also leads directly to bottom effects as the silt or sediment begins to drop from suspension. Fish eggs and insect larvae are often blanketed and suffocated by silt, and gill structures can become clogged. e. Nutrient pollution The release of sewage effluent from point sources, such as wastewater treatment facilities, and storm water runoff from non-point sources, such as lawns and agricultural fields, to streams and tributaries, may cause nutrient pollution problems. As these waters flow into receiving water impoundments, the water may become eutrophic as elevated levels of phosphorus (P) and nitrogen (N) cause biological productivity to increase dramatically. This can lead to excessive algal 4 growth and decay, dissolved oxygen depletion, increased pH variation, and food- chain alterations. f. Algal blooms and Dissolved oxygen Nutrients are often the limiting factor for algae and other aquatic plant growth. If excess nutrients are present, such as the case in many impoundments, algae will grow until some other factor becomes limiting (HALMS, 2007). Algae have other significant growth advantages in impoundments as well, such as light intensity and elevated temperatures. Due to the lack of topological or vegetation shading and the aforementioned temperature stratification, algal photosynthesis can occur rapidly in impoundments. Although algal photosynthesis actually increases dissolved oxygen concentrations in the epilimnion, the algal bloom cycle can have far-reaching and potentially disastrous consequences in the hypolimnion of the impoundment, and downstream. Other aquatic plants may die during the bloom, and the algae itself will eventually crash as available nutrients are consumed. This dead organic matter eventually settles to the bottom and becomes a chief food source for heterotrophic bacteria. Heterotrophic bacteria will increase in number based on the available food source and, according to Petts (1984), "oxygen will be consumed in the hypolimnion, often to exhaustion". This cycle often results in massive fish and insect kills due to anoxic conditions, and the impoundment temporarily becomes a dead area (HALMS, 2007). Aside from these immediate ecological effects, algal blooms can also cause taste and odor problems in water supply impoundments, and release toxic metals from lake sediments as organic-matter decay becomes anaerobic (Fang et al., 2005). g. pH The pH of water can be altered by impoundment, and these changes often affect how chemicals dissolve in the impoundment and whether they affect resident flora and fauna. Impoundment eutrophication due to excess nutrients causes increased biological activity, such as algal photosynthesis, which tends to increase pH. Elevated pH may contribute to phosphorus release from the sediment and allow for additional biological productivity (Ceballos and Rasmussen, 2007). When nutrients are consumed, and dissolved oxygen drops, the water may become more acidic and contribute to the death of fish and other aquatic organisms. This pH variation is primarily a lake or impoundment phenomenon and not often observed in rivers or streams. 2. Impoundments negatively impact ecological functioning and native faunal/floral communities Ecological systems and native faunal/floral communities within the impounded stream reach are negatively impacted due to water quality deterioration, habitat destruction, and effects on migration. For instance, sedimentation may cover existing rock and gravel 5 substrate, including riffles and breaks. This is especially detrimental to gravel-riffle spawners, such as channel catfish and smallmouth bass, that only deposit eggs where the water depth, current, temperature, clarity, dissolved oxygen content, and bottom types are suitable. Also, according to Higgs (2007), dams disrupt river connectivity and create physical and thermal barriers that prevent migrating fish and other wildlife from moving up- or downstream in a river system. He emphasizes that this is problematic for sea-run (anadromous and catadromous) fish as well as for residential fish that migrate up and down a river system. These physical and thermal barriers affect fish spawning, rearing, and foraging migrations, and also prevent re-colonization of other species following floods, droughts, or human disturbances. For instance, during the larval stage, mussels can attach to fish temporarily and move up- or downstream to re-colonize stream segments. Neves and Angermeier (1990) found that dams on the upper Tennessee River system (including parts of NC) have also altered habitat and adversely affected native fishes. Obligatory riverine fish species typically do not survive in these impoundments, and neither the reservoirs nor downstream areas receiving tailwaters provide suitable conditions for native fish reproduction. Neves and Angermeier concluded that the cumulative effects of dam-related stresses have significantly reduced the biological integrity of the rivers, including tailwaters areas where faunal diversity has not recovered. According to Mammoliti (2002), "a substantial body of literature indicates that construction of dams has a negative impact on native stream fishes. In general, an impoundment can reduce the quantity and quality of stream habitat, alter reproductive and feeding behavior or fishes, and increase the number and sizes of predatory fish within a stream system. These impacts suggest a negative relationship between impoundments and obligate stream species." Santucci, Gephard, and Pescitelli (2005) conducted an extensive study on the effects of low-head dams on a 171-km reach of a warmwater river in Illinois. The river system is fragmented by 15 dams that create an alternating series of deep-water and free-flowing river habitats. For each of the three indexes considered (i.e. the index for biotic integrity (IBI), the macroinvertebrate condition index (MCI), and the qualitative habitat evaluation index (QHEI)), scores for free-flowing sections were significantly higher than for impounded sections. In fact, the scores indicated alternating good-quality habitat (free- flowing sections) and severely-degraded habitats (impoundments). The researchers concluded, "From this large body of work, we know that dams can have dramatic effects on rivers and aquatic biota by altering water quality and habitat, disrupting nutrient cycling and sediment transport, and blocking fish and invertebrate movements". Furthermore, Santucci, Gephard, and Pescitelli (2005) cited dam removal as the best option to restore a river's ecological health. The Tennessee Department of Environment and Conservation (TDEC) sampled 75 streams below small impoundments and published a report in September 2006 (Amwine, Sparks, and James, 2006). Benthic macroinvertebrate communities were adversely affected in most of the streams sampled as only four passed biological criteria guidelines or were comparable to first order stream references. In fact, 96% of the streams sampled failed to 6 meet reference guidelines for the number of distinct Ephemeroptera, Plecoptera, and Trichoptera (EPT) taxa, and 86% had low EPT density. They also found that 39% of the dams with year-round (low-flow) discharge provided insufficient flow to supply adequate habitat for aquatic life during at least one season. Only about half of streams studied appeared to have relatively stable channel structures, and approximately 80% failed to meet regional expectations for sediment deposition. 3. Impoundments/dams create numerous maintenance and safety issues Aside from deleterious effects on water quality and ecological systems, impoundments also create numerous maintenance and safety issues. Even small, earthen dams installed to create amenity ponds eventually deteriorate as they are easily damaged by floods, wind, and ice. If maintenance activities are deferred or neglected, this deterioration can accelerate and eventually cause dam failure. Therefore, it is important to note that capital investment does not end when dam construction is complete. As with other critical infrastructure, such as roads, sewer lines, and bridges, a significant investment is essential to maintain dam structures and assure public health and safety (American Society of Civil Engineers (ASCE), 2008). In the past two years alone, 67 dam incidents, including 29 dam failures, were reported to the National Performance of Dams program by state and federal regulatory agencies and private dam owners (ASCE, 2008). According to ASCE, events such as large floods, earthquakes, and inspections that reveal dam deficiencies and/or safety concerns are recorded as incidents. However, ASCE estimates that the actual number of dam incidents and failures is likely to be higher due to non-reporting and understaffed state agencies. ASCE also reports that the number of high-hazard potential dams (dams whose failure would cause loss of human life) in the United States has increased from 9,281 in 1998, to at least 10,213 today. Regrettably, greater than 10% (1046) of all high-hazard potential dams are located in North Carolina. In their "2006 Infrastructure Report Card", the ASCE gave the state's dam infrastructure a grade of "D", and estimated that it will cost North Carolina approximately $400 million to "rehabilitate the most critical deficient structures" (ASCE, 2006). Regardless of dam size, it is critical to perform regular maintenance activities in order to reduce threats to downstream life and property. One of the many important dam maintenance activities is dredging. Many dams silt-in with eroded soil and lose water depth and storage capacity over time. Mahmood (1987) estimated that worldwide reservoir storage capacity decreases I% per year due to sedimentation. Evans et al. (1999) arrived at a similar conclusion in a study prompted by the failure of the IVEX dam on the Chagrin River in Ohio. They estimated that storage capacity loss due to sedimentation ranged from .37% to 1.72% per year. Even in carefully managed watersheds where sediment-loading is minimized due to strict sediment and erosion control measures (e.g. riparian buffers, silt fencing, stormwater retention ponds, etc.), continual maintenance dredging may be required (Newman, Perault, and Shahady, 2006). 7 Impoundments are also commonly afflicted with invasive aquatic plants like Hydrilla (Hydrilla verticillata), Creeping Primrose (Ludwigia peploides), and Parrot Feather (Myriophyllum aquaticum). At the least, these invasive plants are an intractable nuisance that may out-compete native aquatic flora, and inhibit recreational activities. At the worst, the presence of these aquatic plants may threaten public water supplies, and create conditions conducive to anopheles mosquitos, which carry malaria. According to NC DENR's Lake and Reservoir Assessments, Hydrilla covers approximately 625 acres of Mountain Island Lake (Catawba River Basin) and is also problematic on Lake Norman (NC DENR, 2005). In Lake Hickory, Parrot Feather has spread from the original 10 acre infestation to approximately 84 acres. Duke Energy and NC DENR are now working on a Parrot Feather management plan as it threatens to clog two drinking water intakes in the area. To address invasive species and algae problems, impoundment managers have drawn down water levels, introduced biological controls (e.g. grass carp), and treated water with chemicals such as copper sulfate, which may create a host of new water quality problems. Many small impoundments, such as farm ponds and amenity ponds associated with residential subdivisions, create complex and expensive management issues as well. However, these impoundments are seldom managed or maintained by experienced resource managers or civil engineers. In fact, many homeowners associations become dam "owners" upon completion of subdivision and dam construction activities. As such, they must assume the daunting maintenance and inspection responsibilities, as well as manage the aquatic resource. In fact, private companies have been created to capitalize on the demand for pond management services such as aeration, algae control, water quality improvement, odor reduction, and nuisance aquatic vegetation control. 4. Impoundments cause numerous geomorphological, hydrological, and biological impacts downstream due to changes in the flow regime and water quality The act of impounding streams affects more than just the impounded reach itself. In fact, some of the most harmful effects may occur well downstream from the impoundment. For instance, dams often decrease flow rates and prevent flow variations downstream, both of which can cause geomorphic changes. These changes might include bank instability, loss of sinuosity, disruption of bank vegetation, destruction of pool and riffle complexes, and tributary headcutting. As Mammoliti (2002) and Leopold (1997) note in separate studies, stream channel morphology is formed and maintained by natural flow variations, not by the steady flows associated with impounded streams. Higgs (2002) linked flow variation, and the movement of sediment and larger cobbles and boulders, to the creation of "new and more diverse habitat for aquatic species" downstream. Such transport cannot occur along impounded stream reaches however, because much of the sediment carried by the stream is deposited behind the dam. The resulting water releases from impoundments are characterized as "sediment-starved" or "clear-water releases". The downstream, sediment-deprived stream reaches "often regain sediments lost behind the dam by eroding deeper into the river channel and away at the stream banks" (Higgs, 2007). Evans et al. (1999) describe this bed and bank erosion as a "natural consequence of the stream adjusting to steepened gradients and low initial sediment load after exiting the reservoir". Low-flow rate and low-flow variability can negatively impact downstream habitats in other ways as well. The stream may be unable to transfer large particles, such as food sources, and water levels downstream may be too low to allow habitats to support aquatic life. In the event that some sediment has accumulated in the downstream reach, perhaps due to overland flow or sedimentation from an entering tributary, periodic scouring flows are important to maintaining the type and quality of downstream habitat. According to Mammoliti (2002), without scouring flow, sediments may "cover coarse substrates and prevent seepage or subsurface flow that maintains pool refugia during drought periods". Additionally, dams may reduce the ability of aquatic populations to recover following a drought if they cause low or no-flow events to increase in frequency and magnitude. According to Magilligan, Nislow, and Graber (2003), dams can cause other hydrological and biological changes by reducing out-of-bank flows and prolonging bank full flows. Over time this can "disconnect riparian zones from riverine influence" because floods greater than bankfull flow are essentially eliminated. They concluded that the 2-year interval discharge (bankfull discharge) decreased by approximately 60% as a result of impoundment. The lack of overbank inundation completely limits the transport of sediment, nutrients, and water to higher floodplain surfaces that work to sustain riparian habitat and species, and in-channel structure. Lake-induced water quality problems, as well as problem-management strategies (e.g. herbicides used to control invasive aquatic plants), often cause as many problems downstream as they do within the impoundment. For example, water released from impoundments often exhibits elevated temperatures compared to up- and downstream reaches. According to Maxted, McCready, and Scarsbrook (2005), "elevated temperatures were observed for hundreds of meters downstream owing to the slow rate of cooling (1 ° C/100 m), expanding the extent of adverse effects well beyond the footprint of the pond". They also concluded that water quality criteria exceedences (i.e. temperature and dissolved oxygen) significantly decreased invertebrate community richness and diversity for hundreds of meters downstream. Saila, Poyer, and Aube (2005) reached similar conclusion after studying 5 impoundments ranging from 8-10 feet in height and 112-358 feet in length. They found that the small dams increased temperatures 4-5 C° at the source, and the water did not recover from the warming effects (i.e. recover to 17° C) until 5 miles downstream of the dam. Here are some examples of how water quality problems in impoundments affect downstream segments: • Heavy metal accumulations in the hypolimnion may be released during anaerobic organic-matter decay, and cause toxicity in downstream aquatic life • Nutrient-rich water may create algal colonies that render substrates unusable for colonization by aquatic fauna 9 pH fluctuations may cause regulatory failure and/or an inability to molt among aquatic insects Herbicides and pesticides (commonly introduced as a management strategy in impoundments) may be highly toxic to fish and aquatic invertebrates (e.g. copper sulfate) From the works cited above and other materials collected during this literature review, it is evident that the scientific community is progressing towards a consensus on the subject of river impoundment. River impoundments negatively impact water quality and ecological systems, cause undesirable hydrological and geomorphological changes, and create costly maintenance and safety issues for society. While river impoundment can provide benefits such as public water supply, hydroelectric power, and flood control, the practice should be avoided if possible based on the likely environmental, economic, and social consequences. 10 Works Cited American Society of Civil Engineers (ASCE). 2006. Dams - 2006 North Carolina Infrastructure Report Card. Available online at: htt p://sections.asce.org carolina/ReportCard/dams.pdf American Society of Civil Engineers (ASCE). 2008. Report Card for America's Infrastructure. Available online at: http://www.asce.org/reportcard/2005/page.cfm?id=23 Arnwine, D.H., Sparks, K.J., and R.R. James. 2006. Probabilistic Monitoring of Streams Below Small Impoundments in Tennessee. Tennessee Department of Environment and Conservation (TDEC), Division of Water Pollution. Baxter, R.M. 1977. Environmental Effects of Dams and Impoundments. Annual Reviews Ecological Systems; 1977.8:255-283. Available from arjoumals.annualreviews.org. Accessed 2008 May 30. Ceballos, E., and Rasmussen, T. 2007. Internal Loading in Southeastern Piedmont Impoundments. Warnell School of Forestry and Natural Resources, The University of Georgia. Ellis, M.M. 1936. Erosion Silt as a Factor in Aquatic Environments. Ecology 17(1): 29-42. Accessed 2008 February 6. Evans, J.E., Mackey, S.D., Gottgens, J.F., and W.M. Gill. 1999. Lessons from a Dam Failure. Ohio Journal of Science 100(5): 121-131, 2000. Fang, T., Liu, J.T., Xiao, B.D., Chen, X.G. and X.Q. Xu. 2005. Mobilization potential of heavy metals: A comparison between river and lake sediments. Water, Air and Soil Pollution 161 (1- 4):209-225. Higgs, Stephen. 2002. The Ecology of Dam Removal: A Summary of Benefits and Impacts. American Rivers; 2002 February. Ingols, R.S. 1959. Effect of impoundment on downstream water quality, Catawba River, S.C. Journal of the American Water Works Association, 51, 42-6. Leopold, L.B. 1997. Waters, rivers, and creeks. University Science Books, Sausalito, California, 185 pp. Magilligan, F., Nislow, K., and B. Graber. 2003. Scale-independent assessment of discharge reduction and riparian disconnectivity following flow regulation by dams. Geology 31(7): 569- 572. Mahmood, K. 1987. Reservoir Sedimentation: Impact, Extent, and Mitigation. World Bank Technical Paper Number 71. The World Bank, Washington, D.C. 11 Mammoliti, C.S. 2002. The Effects of Small Watershed Impoundments on Native Stream Fishes: A Focus on the Topeka Shiner and Hornyhead Chub. The Kansas Academy of Science 105(3-4), 2002, 219-231. Maxted, J.R., McCready, C.H., and M.R. Scarsbrook. 2005. Effects of small ponds on stream water quality and macroinvertebrate communities. New Zealand Journal of Marine and Freshwater Research 39:1069-1084. Nakashima, S., Yamada, Y., and K. Tada. 2007. Characterization of the water quality of dam lakes on Skikoku Island, Japan. Limnology (2007) 8:1-22 Neves, R.J. and Angermeier, P.L. 1990. Habitat alteration and its effects on native fishes in the upper Tennessee River system, east-central U.S.A. Journal of Fish Biology 37(Supplement A), 45-52. Newman, D.J., Perault, D.R., and T.D. Shahady. 2006. Watershed development and sediment accumulation in a small urban lake. Lake and Reservoir Management. 22(4): 303-307. North American Lake Management Society (HALMS). 2007. Bluegreen Initiative - Overview. Basic Information on cyanobacteria. Last modified: 2007 March 21. North Carolina Department of Environment and Natural Resources (NC DENR). 2005. Lake & Reservoir Assessments - Savannah River Basin. Available from: Division of Water Quality (DWQ), Environmental Sciences Section, Intensive Survey Unit. Petts, G.E. 1984. Impounded Rivers: Perspectives for Ecological Management. Department of Geography, University of Technology, Loughborough, Leicestershire, UK. John Wiley & Sons, 1984. Saila, S.B., Poyer, D., and D. Aube. 2005. Small dams and Habitat Quality in Low Order Streams. Wood-Pawcatuck Watershed Association, Hope Valley, RI. Santucci, V.J., Gephard, S.R., and S.M. Pescitelli. 2005. Effects of Multiple Low-Head Dams on Fish, Macroinvertebrates, Habitat, and Water Quality in the Fox River, Illinois. North American Journal of Fisheries Management 25:975-992, 2005. Smith, N. 1971. A History of Dams. Peter Davies, London: xiv + 279 pp., illustr. Walker, K.F., Hillman, T.J., and W.D. Williams. 1979. The effects of impoundment on rivers: an Australian case study. Verhandlungen Internationale Vereinigung fur Theoretische and Angewandte Limnologie, 20,1695-701. 12