Jesse Radolinski
Affiliation confirmed via AI analysis of OpenAlex, ORCID, and web sources.
Assistant Professor
Also affiliated: Universität Innsbruck (2020–2026); Max Planck Institute for Biogeochemistry (2023); Arkansas Department of Agriculture (2026); University of Maryland, College Park (2024–2025); Virginia Tech (2017–2022)
Faculty Researcher
Research Areas
Biomedical Subjects
Links
Biography and Research Information
OverviewAI-generated summary
Jesse Radolinski investigates soil science, focusing on water movement, solute transport, and the impact of agricultural practices on soil and water quality. His research examines how preferential flow paths in soil influence the mobility of substances, including antibiotic resistance genes and chemicals associated with manure application. Radolinski also studies the effects of environmental factors such as drought, warming temperatures, and elevated carbon dioxide on grassland ecosystems, specifically looking at water use by vegetation and soil water dynamics. His work has explored methodologies for analyzing water in the Critical Zone and employed computational approaches like Markov Chain Monte Carlo simulations to model soil water retention parameters. Radolinski has published 38 papers, accumulating 310 citations, with an h-index of 9.
Metrics
- h-index: 9
- Publications: 38
- Citations: 321
Selected Publications
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Synergistic effects of warming and elevated CO <sub>2</sub> intensify drought impacts on grassland carbon and water fluxes (2026)
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Data and code from the journal article "Synergistic effects of warming and elevated CO2 intensify drought impacts on grassland carbon and water fluxes" (2026)
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Data and code from the journal article "Synergistic effects of warming and elevated CO2 intensify drought impacts on grassland carbon and water fluxes" (2026)
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Drought soil legacies and grassland responses to subsequent drought (2026)
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A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water (2026)
Collaboration Network
Top Collaborators
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- Drought soil legacies and grassland responses to subsequent drought
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- A warmer, more CO2-rich climate amplifies hydrological disconnections within soil water
- Drought soil legacies and grassland responses to subsequent drought
- Drought soil legacies and grassland responses to subsequent drought
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