Abstract

Mountaintop mining and valley fill (MTM/VF) coal extraction, practiced in the Central Appalachian region, represents a dramatic landscape-scale disturbance. MTM operations remove as much as 300 m of rock, soil, and vegetation from ridge tops to access deep coal seams and much of this material is placed in adjacent headwater streams altering landcover, drainage network, and topography. In spite of its scale, extent, and potential for continued use, the effects MTM/VF on catchment hydrology is poorly understood. Previous reviews focus on water quality and ecosystem health impacts, but little is known about how MTM/VF affects hydrology, particularly the movement and storage of water, hence the hydrologic processes that ultimately control flood generation, water chemistry, and biology. This paper aggregates the existing knowledge about the hydrologic impacts of MTM/VF to identify areas where further scientific investigation is needed. While contemporary surface mining generally increases peak and total runoff, the limited MTM/VF studies reveal significant variability in hydrologic response. Significant knowledge gaps relate to limited understanding of hydrologic processes in these systems. Until the hydrologic impact of this practice is better understood, efforts to reduce water quantity and quality problems and ecosystem degradation will be difficult to achieve.

Highlights

  • Mountaintop removal mining and valley fill (MTM/VF) coal extraction, practiced in the CentralAppalachian region of the eastern United States, represents a dramatic change to the landscape

  • Protection Agency (EPA) estimates that MTM/VF will have impacted approximately 6.8% of the predominately forested Appalachian coalfield region of West Virginia, Kentucky, Tennessee, and Virginia with nearly 4000 km of headwater streams buried under valley fills [3] (Figure 1)

  • 2035, this decline is relatively minimal (−0.6%) indicating that the low-sulfur Appalachian coal extracted by cost effective MTM/VF practices will continue to be a significant component to the energy future of the United States [4]

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Summary

Introduction

Mountaintop removal mining and valley fill (MTM/VF) coal extraction, practiced in the Central. Appalachian region of the eastern United States, represents a dramatic change to the landscape. Surface mining represents the largest landuse/land cover change in the Central Appalachian region [2] and by 2012, the US Environmental. Protection Agency (EPA) estimates that MTM/VF will have impacted approximately 6.8% of the predominately forested Appalachian coalfield region of West Virginia, Kentucky, Tennessee, and Virginia with nearly 4000 km of headwater streams buried under valley fills [3] (Figure 1). 2035, this decline is relatively minimal (−0.6%) indicating that the low-sulfur Appalachian coal extracted by cost effective MTM/VF practices will continue to be a significant component to the energy future of the United States [4]. The large-scale alterations of catchment structure (e.g., topography, slopes, organization, volume, etc.), water chemistry, and land cover are likely permanent, having important health implications for aquatic and human communities linked to these streams

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