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Temperature Mapping as an Indirect Characterization Method for Surface Water-Hyporheic Zone Exchange
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|Created:||Mar 16, 2020 at 9:40 p.m.|
|Last updated:|| May 13, 2020 at 3:42 p.m.
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The purpose of this part of the project is to compare hyporheic exchange measurement methods and evaluate feasibility of using fiber optic DTS in a small stream (East Fork Poplar Creek) in Tennessee. CTEMPS stand-alone high resolution temperature loggers and fiber optic DTS were used to measure temperature gradients between stream-bed sediments and a stream to estimate groundwater discharge to surface water across a small hyporheic zone. There are also in-stream piezometer, electrical resistivity, and in-stream tracer test data to compare with the temperature method.
Data will be available upon in September 2021.
Basic components of study
Site: East Fork Poplar Creek
DTS: Silixa XT
Cable: Kaiphone - armored, black jacket, 3 mm outside diameter, 2 multimode fibers, 2 km
Other: 10 RBR soloT temperature loggers
This resource was created using funding from the following sources:
|Agency Name||Award Title||Award Number|
|National Science Foundation||Collaborative Research: Facility Support: Center for Transformative Environmental Monitoring Programs - CTEMPs||1440506|
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
|CTEMPs OSU-UNR||CTEMPs||Nevada, US|
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/