U.S. Department of EnergyOffice of Scientific and Technical Information
Groundwater level elevation and temperature across Meander C at the Lower Montane in the East River Watershed, Colorado.
Abstract
This groundwater level elevation and temperature data package is aimed at improving the predictive understanding of hydro-biogeochemical processes at the lower montane site in the East River Watershed, Colorado. The dataset is obtained using pressure transducers placed in shallow wells in the floodplain. This dataset contains data from wells ER-CPA1 to ER-CPA6 (six wells with SFA Location ID's). Each file contains the water level elevation and the water temperature. Water level elevation have been obtained using the barometric pressure from the pressure transducer (Hobos sensor) in the well, barometric pressure from a sensor in air located at the same site (lower montane), depth from top-of-casing (TOC) to sensor measurement point, and TOC elevation. Data have been checked with a few measurements of water table depths. A real-time kinematic (RTK) global positioning system (GPS) has been used to survey the TOC (data in file WellLocation_WLdataArchive2018). The water level elevation is given in UTM13N Geoid2012AB. While depth to water level is not present in the data files, it can be easily calculated with the TOC and distance to ground provided in the GPS coordinate file (WellLocation_WLdataArchive2018). The dataset quality is discussed in Collection/Analysis section of the methods. Time-series of measurements will bemore »
- Publication Date:
- Other Number(s):
- paf_357
- Research Org.:
- Environmental System Science Data Infrastructure for a Virtual Ecosystem (ESS-DIVE) (United States); Watershed Function SFA
- Sponsoring Org.:
- U.S. DOE > Office of Science > Biological and Environmental Research (BER)
- Subject:
- 54 ENVIRONMENTAL SCIENCES
- Keywords:
- elevations; table; water; EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER; groundwater level; groundwater temperature; EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > GROUND WATER FEATURES > WATER TABLE; EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER > GROUNDWATER CHEMISTRY
- Geolocation:
- 39.034,-106.88|38.88,-106.88|38.88,-107.05|39.034,-107.05|39.034,-106.88
- OSTI Identifier:
- 1647041
- DOI:
- https://doi.org/10.15485/1647041
- Project Location:
-
Citation Formats
Dafflon, Baptiste, Malenda, Helen, and Dwivedi, Dipankar. Groundwater level elevation and temperature across Meander C at the Lower Montane in the East River Watershed, Colorado.. United States: N. p., 2020.
Web. doi:10.15485/1647041.
Dafflon, Baptiste, Malenda, Helen, & Dwivedi, Dipankar. Groundwater level elevation and temperature across Meander C at the Lower Montane in the East River Watershed, Colorado.. United States. doi:https://doi.org/10.15485/1647041
Dafflon, Baptiste, Malenda, Helen, and Dwivedi, Dipankar. 2020.
"Groundwater level elevation and temperature across Meander C at the Lower Montane in the East River Watershed, Colorado.". United States. doi:https://doi.org/10.15485/1647041. https://www.osti.gov/servlets/purl/1647041. Pub date:Wed Jan 01 00:00:00 EST 2020
@article{osti_1647041,
title = {Groundwater level elevation and temperature across Meander C at the Lower Montane in the East River Watershed, Colorado.},
author = {Dafflon, Baptiste and Malenda, Helen and Dwivedi, Dipankar},
abstractNote = {This groundwater level elevation and temperature data package is aimed at improving the predictive understanding of hydro-biogeochemical processes at the lower montane site in the East River Watershed, Colorado. The dataset is obtained using pressure transducers placed in shallow wells in the floodplain. This dataset contains data from wells ER-CPA1 to ER-CPA6 (six wells with SFA Location ID's). Each file contains the water level elevation and the water temperature. Water level elevation have been obtained using the barometric pressure from the pressure transducer (Hobos sensor) in the well, barometric pressure from a sensor in air located at the same site (lower montane), depth from top-of-casing (TOC) to sensor measurement point, and TOC elevation. Data have been checked with a few measurements of water table depths. A real-time kinematic (RTK) global positioning system (GPS) has been used to survey the TOC (data in file WellLocation_WLdataArchive2018). The water level elevation is given in UTM13N Geoid2012AB. While depth to water level is not present in the data files, it can be easily calculated with the TOC and distance to ground provided in the GPS coordinate file (WellLocation_WLdataArchive2018). The dataset quality is discussed in Collection/Analysis section of the methods. Time-series of measurements will be added to this data package, so please check back for updates. If you have questions, please contact the author.},
doi = {10.15485/1647041},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Wed Jan 01 00:00:00 EST 2020},
month = {Wed Jan 01 00:00:00 EST 2020}
}