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A Field-Based Aquatic Life Benchmark for Conductivity in Central Appalachian Streams (Final Report).

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Abstract

EXECUTIVE SUMMARY: This report uses field data to derive an aquatic life benchmark for conductivity that can be applied to waters in the Appalachian Region that are dominated by salts of Ca2+, Mg2+, SO42− and HCO3– at a circum-neutral to mildly alkaline pH. This benchmark is intended to protect the aquatic life in the region. It is derived by a method modeled on the EPA’s standard methodology for deriving water-quality criteria (i.e., Stephan et al., 1985). In particular, the methodology was adapted for use of field data. Field data were used because sufficient and appropriate laboratory data were not available and because high-quality field data were available to relate conductivity to effects on aquatic life. This report provides scientific evidence for a conductivity benchmark in a specific region rather than for the entire United States. The method used in this report is based on the standard methodology for deriving water-quality criteria, as explained in Stephan et al. (1985), in that it used the 5th centile of a species sensitivity distribution (SSD) as the benchmark value. SSDs represent the response of aquatic life as a distribution with respect to exposure. Data analysis followed the standard methodology in aggregating species to genera and using interpolation to estimate the centile. It differs primarily in that the points in the SSDs are extirpation concentrations (XCs) rather than median lethal concentrations (LC50s) or chronic values. The XC is the level of exposure above which a genus is effectively absent from water bodies in a region. For this benchmark value, the 95th centile of the distribution of the probability of occurrence of a genus with respect to conductivity was used as a 95th centile extirpation concentration. Hence, this aquatic life benchmark for conductivity is expected to avoid the local extirpation of 95% of native species (based on the 5th centile of the SSD) due to neutral to alkaline effluents containing a mixture of dissolved ions dominated by salts of SO42− and HCO3−. Because it is not protective of all genera and protects against extirpation rather than reduction in abundance, this level is not fully protective of sensitive species or higher quality, exceptional waters designated by state and federal agencies. This field-based method has several advantages. Because it is based on biological surveys, it is inherently relevant to the streams where the benchmark may be applied and represents the actual aquatic life use in these streams. Another advantage is that the method assesses all life stages and ecological interactions of many species. Further, it represents the actual exposure conditions for elevated conductivity in the region, the actual temporal variation in exposure, and the actual mixture of ions that contribute to salinity as measured by conductivity. The disadvantages of field data result from the fact that exposures are not controlled. As a result, the causal nature of the relationship between conductivity and the associated biological impairments must be assessed. Also, any variables that are correlated with conductivity and the biotic response may confound the relationship of biota to conductivity. Assessments of causation and confounding were performed and are presented in the appendices. They demonstrate that conductivity can cause impairments and the relationship between conductivity and biological responses apparently is not appreciably confounded. The chronic aquatic life benchmark value for conductivity derived from all-year data from West Virginia is 300 μS/cm. It is applicable to parts of West Virginia and Kentucky within Ecoregions 68, 69, and 70 (Omernick, 1987). It is expected to be applicable to the same ecoregions extending into Ohio, Pennsylvania, Tennessee, Virginia, Alabama, and Maryland, but data from those states have not been analyzed. This is because the salt matrix and background is expected to be similar throughout the ecoregions. The benchmark may also be appropriate for other nearby ecoregions, such as Ecoregion 67, but it has only been validated for use in Ecoregions 68, 69, and 70 at this time. This benchmark level might not apply when the relative concentrations of dissolved ions are not dominated by salts of Ca2+, Mg2+, SO42− and HCO3– or the natural background exceeds the benchmark. However, the salt mixture dominated by salts of SO42− and HCO3− is believed to be an insurmountable physiological challenge for some species.
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