Fiber-optic distributed temperature sensing data collected for improved mapping and monitoring of contaminated groundwater discharges along the upper Quashnet River, Mashpee and Falmouth, Massachusetts, USA 2020
Dates
Publication Date
2023-02-07
Start Date
2022-06-14
End Date
2022-06-20
Citation
Briggs, M.A., Rey, D., Johnson, C., Moore, H., Marble, K., Slater, L., and Iery, R., 2023, Fiber-optic distributed temperature sensing data collected for improved mapping and monitoring of contaminated groundwater discharges along the upper Quashnet River, Mashpee and Falmouth, Massachusetts, USA 2020: U.S. Geological Survey data release, https://doi.org/10.5066/P96KF0L2.
Summary
In summer in Massachusetts, USA, preferential groundwater discharge zones are often colder than adjacent streambed areas that do not have substantial discharge. Therefore, discharge zones can efficiently be identified and mapped over space using heat as a tracer. This data release contains fiber-optic distributed temperature sensing (FO-DTS) data collected along the streambed interface of the main channel and tributaries of the upper Quashnet River, within approximately 1 km of Johns Pond, from June 14 to June 20, 2020. For these deployments a Salixa XT-DTS control unit (Salixa Ltd, Hertfordshire, UK) was used, and measurements were made over several day increments at 0.508 m linear resolution. Specific locations for collected data [...]
Summary
In summer in Massachusetts, USA, preferential groundwater discharge zones are often colder than adjacent streambed areas that do not have substantial discharge. Therefore, discharge zones can efficiently be identified and mapped over space using heat as a tracer. This data release contains fiber-optic distributed temperature sensing (FO-DTS) data collected along the streambed interface of the main channel and tributaries of the upper Quashnet River, within approximately 1 km of Johns Pond, from June 14 to June 20, 2020. For these deployments a Salixa XT-DTS control unit (Salixa Ltd, Hertfordshire, UK) was used, and measurements were made over several day increments at 0.508 m linear resolution. Specific locations for collected data are located within the data files, and additional details are contained in the ‘readme’ files within each zipped data directory. Measured data in the form of Salixa instrument files are located in the 'Raw' data directory, including data collected along lengths of optical fiber that were not installed in the streams. The 'Processed' data directory contains data that have been aggregated from the original machine output files, spatially trimmed, and georeferenced. Additionally, simple summary streambed interface temperature statistics (mean, max, min, standard deviation) are listed by streambed location.
Temperature data were collected to infer where groundwater may be entering surface water through submerged preferential groundwater discharges. Groundwater temperature is typically unique from ambient surface water temperature in Massachusetts, USA in summer, and therefore seepage locations might be recognized via temperature anomalies and/or areas of buffered temperature change. Simple summary streambed interface temperature statistics are often used to indicate potential zones of preferential groundwater discharge that are then further investigated in the field with independent measurements of temperature, chemistry, and/or groundwater discharge flux. The ESRI shapefile contained in this release details the estimated spatial locations of preferential groundwater discharge zones as indicated by the FO-DTS data and from 'roving' handheld thermal infrared imaging. Thermal infrared data were not actually saved and preserved, rather thermal anomalies associated with potential discharge zones were identified in real time using the camera display screen.The shapefile data are included for demonstration purposes only and are not meant to represent an exhaustive spatial mapping of preferential groundwater discharge zones across the site.
Preview Image
Example map of average streambed interface temperature over the experiment.