<?xml version="1.0" encoding="UTF-8"?><rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcq="http://purl.org/dc/terms/"><records count="1" morepages="false" start="1" end="1"><record rownumber="1"><dc:product_type>Journal Article</dc:product_type><dc:title>Uncovering the hidden world of riverbed sediments: The role of sediment heterogeneity and cross-bar channel fills in the hydrogeochemical dynamics of the hyporheic zone</dc:title><dc:creator>McGarr, Jeffery T; Li, Pei; Ford, Robert G; Kleman, Teagan; Fields, Colton; Hobbs, Julie; Lupton, Lydia; Poston, Emma; Marsh, Thomas; Trutschel, Leah; Fritz, Ken M; Rowe, Annette; Wallace, Corey D; Ward, Dylan; Sturmer, Daniel M; Dietsch, Craig; Naber, Margaret; Lien, Bob K; Soltanian, Mohamad Reza</dc:creator><dc:corporate_author/><dc:editor/><dc:description>Groundwater-surface water interaction (hyporheic exchange) is critical in numerous hydrogeochemical processes; however, hyporheic exchange is difficult to characterize due to the various spatial (e.g., sedimentary
architecture) and temporal (e.g., stage fluctuations) variables that influence it. This interdisciplinary study
brings forth novel insights by integrating various methodologies including geophysical surveys, physical
and chemical sediment characterization, and water chemistry analysis to explore the interplay of the
numerous facets governing hyporheic zone processes within a compound bar deposit. The findings reveal
distinct sedimentary facies and geochemical zones within the compound bar, driven by the sedimentary
architecture. Cross-bar channel fills are identified as critical structures influencing hydrogeochemical dynamics,
acting as baffles to groundwater flow and modulating nutrient transformations. Geophysical imaging and
hydrogeochemical analyses highlight the complex interplay between sediment characteristics and subsurface
hydraulic connectivity, emphasizing the role of sediment heterogeneity in controlling hyporheic exchange and
solute mixing. The study concludes that sediment heterogeneity, particularly the presence of cross-bar channel
fills, plays a pivotal role in the hydrogeochemical dynamics of the hyporheic zone. These structures significantly
influence hyporheic flow paths, solute residence times, and nutrient cycling, underscoring the necessity to
consider the fine-scale sedimentary architecture in models of hyporheic exchange. The findings contribute to a
deeper understanding of riverine ecosystem processes, offering insights that can inform management strategies
for water quality and ecological integrity.</dc:description><dc:publisher>Elsevier</dc:publisher><dc:date>2024-11-01</dc:date><dc:nsf_par_id>10548345</dc:nsf_par_id><dc:journal_name>Journal of Hydrology</dc:journal_name><dc:journal_volume>644</dc:journal_volume><dc:journal_issue>C</dc:journal_issue><dc:page_range_or_elocation>132062</dc:page_range_or_elocation><dc:issn>0022-1694</dc:issn><dc:isbn/><dc:doi>https://doi.org/10.1016/j.jhydrol.2024.132062</dc:doi><dcq:identifierAwardId>2048452</dcq:identifierAwardId><dc:subject>Hyporheic exchange
Solute mixing
Geochemical hotspots
Riverbed
Geophysical imaging</dc:subject><dc:version_number/><dc:location/><dc:rights/><dc:institution/><dc:sponsoring_org>National Science Foundation</dc:sponsoring_org></record></records></rdf:RDF>