T87 Achieving Groundwater Security across Local-to-Regional Scales in the Anthropocene
Monday, 16 October 2023
8:00 AM - 12:00 PM
319
MANAGEMENT OPTIONS TO SUSTAIN GROWTH WITHIN WATER-STRESSED SPRING CREEK WATERSHED, RIDGE AND VALLEY, CENTRE COUNTY, PENNSYLVANIA
Paper number: T87-13
Program: Technical Sessions
Time: 11:00 AM – 11:15 AM
Authors
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Byron ParizekPennsylvania State University, University Park, PA
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Katarin A. ParizekState College, PA
Abstract
The watershed is undergoing rapid development driven by Penn State's multi-billion dollar teaching, research and outreach budget that locally serves 46,000 students as well as economic activities made accessible and beneficial by I-99 and I-80 (e.g., growing medical, public and governmental services; research and development; construction). In support of this growth, high-quality limestone and aggregate are being mined and quarried at 4 locations below the water table.
Constrained by the Commission's low-flow protection policy, six options are available to sustain growing water demands:
· Import from adjacent watersheds
· Expansion of groundwater contributing areas by shifting 3 transient groundwater divides within local Ridge and Valley Appalachian karst aquifers
· Voluntary and mandated conservation during declared droughts. (e.g., Today, Penn State’s per student water use is ~45 gpd v 95 gpd nearly 20 years ago.)
· Management of stormwater flow enhanced by interconnected impervious surfaces and diverted from evapotranspiration.
· Wastewater reuse (e.g., Penn State's Living Filter returns 100% of its effluent to crops and forests; University Area Joint Authority’s 1 mgpd beneficial reuse system).
· Regional climate change between 1895 and 2017 includes +0.137°F/decade rise in temperature and +0.267 inches/decade precipitation increase. Patterns of increases in and intensity of flood events are driven by temperature and prevailing storm tracks, likely increasing the availability of stormwater for future harvest.
Given the will, a mix of these 6 options is a way forward to sustain growth within these headwaters and is supported by a well-understood hydrogeologic framework.
Geological Society of America Abstracts with Programs. Vol. 55, No. 6
doi: 10.1130/abs/2023AM-395757
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