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River and hyporheic zone water geochemical data from OsmoSamplers, East River Pumphouse, Colorado, Nov 2017-Sept 2018

Creators: Laura Lapham, Jessica Buser-Young, Andrew Thurber, Fredrick Colwell
Year: 2023
DOI: 10.15485/1766092
License: CC-BY 4.0
Location: This study took place at the U.S. Department of Energy’s Biological and Environmental Research (DOE BER) station located at East River (ER) in Crested Butte, CO, USA. OsmoSamplers were deployed at near the SFA pumphouse, 38.922°N 106.951°W
Temporal extent: 2017-11-01 to 2018-09-21
Bounding box: 38.922°N to 38.922°N, -106.951°W to -106.951°W
Publisher: RMBL
Tags: geochemistry, water temperature, methane, hyporheic, stable isotopes, temporal subsetting, biogeochemistry, Alpine & Subalpine Ecology, Hydrology & Watersheds, Groundwater, Weather & Atmospheric Science, Biogeochemical Cycling, RMBL & Gothic, Gunnison Basin, Research Programs

Description

This data package contains geochemical and river water temperature data from OsmoSamplers deployed at East River, Colorado pump house. There are three data files. The first one contains sulfate (SO4) and chloride (Cl) concentrations from riverwater and hyporheic zone (sediment water interface (SWI), 4 cm below seafloor (cmbsf), and 12 (cmbsf)). The second file contains methane concentrations, methane stable carbon isotope ratios and water isotopes from hyporheic zone porewaters. And the third is from a temperature logger during the deployment. Files are provided as .xls or .csv. This research was performed as part of the SBR funded project “Quantifying Subsurface Biogeochemical Variability in a High Altitude Watershed During Winter Isolation” DE-SC0018328. The novel part of this dataset is that we quantify these geochemical parameters throughout the winter isolation period, which is difficult to measure, as well as within the hyporheic zone. The data files were updated 3/1/2021 because the column label for the water isotopes was incorrect. Also, the csv files were also updated since they were not formatted correctly.

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