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Michelle A. Baker

Researcher at Utah State University

Publications -  63
Citations -  3354

Michelle A. Baker is an academic researcher from Utah State University. The author has contributed to research in topics: Dissolved organic carbon & Hyporheic zone. The author has an hindex of 27, co-authored 61 publications receiving 3003 citations. Previous affiliations of Michelle A. Baker include University of New Mexico & Centre national de la recherche scientifique.

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Dynamics of nitrate production and removal as a function of residence time in the hyporheic zone

TL;DR: In this paper, the authors measured solute concentrations (15 NO3, 15 N2 (g), as well as NO3, N H3, DOC, DO, Cl − ), and hydraulic transport parameters (head, flow rates, flow paths, and residence time distributions) of an instrumented gravel bar.
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Organic carbon supply and metabolism in a shallow groundwater ecosystem

TL;DR: In this paper, the influence on groundwater heterotrophic metabolism of DOC availability, inorganic nitrogen (N), inorganic phosphorus (P), temperature, and season were assessed using laboratory manipulations of aquifer sediments and seasonal measurements in field microcosms.
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Coupled biogeochemical and hydrological responses of streams and rivers to drought

TL;DR: In this article, the Palmer Drought Severity Index (PDSI) was used to measure the severity of severe or extreme droughts over a 105-year record from central New Mexico, U.S.A.
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Are rivers just big streams? A pulse method to quantify nitrogen demand in a large river.

TL;DR: It is found that the Upper Snake had surprisingly high biotic demand relative to smaller streams in the same river network for both ammonium (NH4+) and nitrate (NO3-), suggesting that large rivers may have similar bioticDemand for N as smaller tributaries.
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Biogeochemical and metabolic responses to the flood pulse in a semiarid floodplain

TL;DR: This article investigated how ecosystem responses to the flood pulse relate to forest IFI by quantifying nutrient and organic matter dynamics in the Rio Grande floodplain during three years of experimental flooding of disconnected floodplain and during a single year of natural flooding of the connected floodplain.