Evaluating the role of flow and specific conductivity on stream metabolism across a mining-induced salinity gradient in the Appalachian Coalfield

dc.contributor.authorMeehan, Caleigh Elizabethen
dc.contributor.committeechairHotchkiss, Erin R.en
dc.contributor.committeechairMcLaughlin, Daniel L.en
dc.contributor.committeememberBarrett, John E.en
dc.contributor.departmentBiological Sciencesen
dc.date.accessioned2026-03-03T09:00:28Zen
dc.date.available2026-03-03T09:00:28Zen
dc.date.issued2026-03-02en
dc.description.abstractFreshwater salinization is a notable concern for headwater streams in Appalachia with the history of resource extraction in the region. Mountaintop removal/valley fill mining techniques in Appalachia result in the burial of headwater streams and mobilization of ions, specifically SO42-, Ca, and Mg into waters, raising specific conductivity (SpC). Organismal responses to salinization have been well documented in freshwater ecosystems, but there are few measurements assessing how salinity effects on organisms influence whole-ecosystem processes, specifically stream metabolism. Understanding how gross primary production (GPP) and ecosystem respiration (ER) respond to salinity, stream flow, and their association is needed to characterize the consequences of salinization on stream processes. To assess the role of salinization and discharge on metabolism, we recorded high-frequency SpC, discharge, and dissolved oxygen data in three headwater streams in the Appalachian (U.S.) coalfields, where mining has resulted in widespread headwater stream salinization. Sites included a reference stream (REF) with SpC ranging from 0.2 - 57.69 μS/cm, a mid-salinity site (MID; 2.03- 594.7 μS/cm), and a high-salinity site (HI; 84.6-1920 μS/cm) with similar flow regimes, helping to characterize these covarying and potentially interacting drivers of metabolism. Across all sites, SpC decreased with increased discharge and with significant breakpoints. This study did not find a clear relationship between SpC and ecosystem metabolism. All streams, regardless of SpC levels, were heterotrophic (|ER|>GPP). Our high salinity site had the highest GPP and ER, suggesting salt may subsidize ecosystem metabolism, though differences in canopy cover complicate this. While we saw no consistent effect of SpC on metabolism, deviation in patterns at mining-impacted sites from expected discharge-metabolism patterns at our reference sites suggests some impact of salinity. This study reinforces the need for research across diverse ecosystems and salinization sources to characterize the role of freshwater salinization on ecosystem metabolism, as mediated by discharge.en
dc.description.abstractgeneralSurface coal mining operations in the Appalachian Coalfield region have resulted in decreased water quality and increased salt levels (measured as specific conductance; SpC) in small, headwater streams. Declines in aquatic biodiversity have been documented with increases in SpC, but little work has been done to address impacts on broader stream processes such as ecosystem metabolism, which represents organic carbon fixation and breakdown by gross primary production (GPP) and ecosystem respiration (ER), respectively. High stream flows are a known driver of both ecosystem metabolism and SpC concentrations in headwater streams; however, minimal work has been conducted to connect the roles of these interacting drivers (flow and SpC) on metabolism. This study measured metabolism across three headwater streams in the Appalachian Coalfield of varying salinity and flow regimes from August 2024 to August 2025. We found no relationship between ecosystem metabolism and SpC across our sites. Increases in GPP and ER at our high SpC site suggest a subsidy effect, although small sample sizes and the potential for increased light availability complicate this interpretation. While we found no consistent effect of SpC on metabolism across our sites, variation in flow-metabolism relationships from reference conditions at salinized sites suggests salts exhibit a potential effect on ecosystem processes. We encourage continued work on connecting ecosystem metabolism and freshwater salinization across flow regimes in headwater streams.en
dc.description.degreeMaster of Scienceen
dc.format.mediumETDen
dc.identifier.othervt_gsexam:45755en
dc.identifier.urihttps://hdl.handle.net/10919/141636en
dc.language.isoenen
dc.publisherVirginia Techen
dc.rightsIn Copyrighten
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en
dc.subjectFreshwater Salinizationen
dc.subjectEcosystem Metabolismen
dc.subjectFlowen
dc.subjectSpecific Conductivityen
dc.subjectHeadwatersen
dc.subjectAppalachian Coalfielden
dc.subjectMountain Top Removal/Valley Fillen
dc.titleEvaluating the role of flow and specific conductivity on stream metabolism across a mining-induced salinity gradient in the Appalachian Coalfielden
dc.typeThesisen
thesis.degree.disciplineBiological Sciencesen
thesis.degree.grantorVirginia Polytechnic Institute and State Universityen
thesis.degree.levelmastersen
thesis.degree.nameMaster of Scienceen

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