78-7 Surface water and groundwater interface controls on microbial N2O cycling in karst aquifers
Session: New Frontiers in Cave and Karst Science
Presenting Author:
Seonkyoo YoonAuthors:
Yoon, Seonkyoo1, Oh, Chamteut2, Martin, Jonathan B.3(1) Geological Sciences, University of Florida, Gainesville, FL, USA, (2) Environmental Engineering Sciences, University of Florida, Gainesville, FL, USA, (3) Geological Sciences, University of Florida, Geological Sciences, Gainesville, FL, USA,
Abstract:
Karst landscapes and aquifers have recently been identified as significant sources of nitrous oxide (N2O), the third most abundant greenhouse gas, with a global warming potential approximately 300 times greater than that of carbon dioxide. Despite this, the exact processes driving N2O production in karst systems remain poorly understood. In this research, we integrate field studies with microfluidic experiments to investigate how surface water–groundwater (SW-GW) interactions influence N2O cycling in karst aquifers. At SW-GW interfaces within a karst aquifer, we collected groundwater samples to measure N2O concentrations under different mixing conditions. In parallel, we used microfluidic devices that replicate karst environments to simulate SW-GW mixing and observe microbial N2O cycling. By connecting the outcomes of these laboratory experiments with field measurements, we demonstrate that inputs of dissolved oxygen from surface water into anoxic groundwater inhibit the completion of denitrification, consequently leading to the accumulation and atmospheric release of N2O from karst aquatic systems.
Geological Society of America Abstracts with Program. Vol. 57, No. 6, 2025
doi: 10.1130/abs/2025AM-10825
© Copyright 2025 The Geological Society of America (GSA), all rights reserved.
Surface water and groundwater interface controls on microbial N2O cycling in karst aquifers
Category
Topical Sessions
Description
Session Format: Oral
Presentation Date: 10/20/2025
Presentation Start Time: 09:50 AM
Presentation Room: HBGCC, 211
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