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Hydrolytic activity and metabolism of sediment and epilithon in streams draining mountaintop removal coal mining, West Virginia, U.S.A.
Citation:
FRITZ, K. M., B. R. JOHNSON, AND R. Price. Hydrolytic activity and metabolism of sediment and epilithon in streams draining mountaintop removal coal mining, West Virginia, U.S.A. Presented at Southeastern Water Pollution Biologists Association 2009 Annual Meeting, Frankfort, KY, October 20 - 22, 2009.
Impact/Purpose:
The goal of this research is to develop methods and indicators that are useful for evaluating the condition of aquatic communities, for assessing the restoration of aquatic communities in response to mitigation and best management practices, and for determining the exposure of aquatic communities to different classes of stressors (i.e., pesticides, sedimentation, habitat alteration).
Description:
Mountaintop removal and valley filling (MTR/VF) is a method of coal mining used in the Central Appalachians. Regulations require that potential impacts to stream functions must be considered when determining the compensatory mitigation necessary for replacing aquatic resources unavoidably lost or adversely affected by permitted mining activities. However, assessments of MTR/VF have only included structural measures. We measured sediment and epilithon metabolism and hydrolytic activity seasonally in ten streams. Sediment metabolism and hydrolytic activity were significantly higher in forested streams than in mined streams across all seasons. Epilithic metabolism was significantly higher in forested streams than in mined streams in October, but did not vary in February, April or July. Metabolism and hydrolytic activity were strongly correlated. The percent cover of fine sediments was negatively correlated with epilithic metabolsim and hydrolytic activity, where as the total upstream channel length was positively correlated with sediment metabolism and hydrolytic activity. All measures were negatively related to specific conductance. These results suggest that MTR/VF have negative effects on stream function by truncating stream networks, altering water chemistry, and increasing sedimentation. Combining functional measures with traditionally used structural measures will provide a more complete assessment of ecosystem integrity.