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Riverbank vertical temperature profiler data and calculated groundwater discharge flux estimates from the Farmington River corridor, CT, USA
As the climate warms and dry periods become more extreme, shallow groundwater discharge is generally becoming a less reliable source of streamflow while deep groundwater discharge remains a more resilient source. The implications of shifts in the relative balance of shallow and deep groundwater discharge sources are profound in gaining streams. These different sources exert critical controls on stream temperature and water quality as influenced by legacy groundwater contaminant transport. Groundwater discharge flux rates over time were used for the inference of source groundwater characteristics to prominent riverbank groundwater discharge faces along the mainstem Farmington River, CT USA. To estimate groundwater discharge rates, we deployed sediment temperature loggers (iButton #DS1922L, Maxim Integrated, Inc., San Jose, CA, USA) in vertical profilers installed directly into mapped preferential groundwater discharge points across extensive riverbank discharge face features.Temperature data contained in this release were collected from June 24 to November 5, 2020, at 40 distinct discharge point riverbank locations, similar to those described by Barclay et al. (2022) and Briggs et al. (2022). Saturated sediment thermal conductivity and heat capacity were measured in-situ with a TEMPOS Thermal Property Analyzer (TEMPOS, Meter Group, Inc., Pullman, WA, USA) at multiple points across each riverbank discharge face to aid in estimating groundwater discharge flux rates. Barclay, J. R., Briggs, M. A., Moore, E. M., Starn, J. J., Hanson, A. E. H., & Helton, A. M. (2022). Where groundwater seeps: Evaluating modeled groundwater discharge patterns with thermal infrared surveys at the river-network scale. Advances in Water Resources, 160. https://doi.org/10.1016/j.advwatres.2021.104108 Briggs, M. A., Jackson, K. E., Liu, F., Moore, E. M., Bisson, A., & Helton, A. M. (2022). Exploring Local Riverbank Sediment Controls on the Occurrence of Preferential Groundwater Discharge Points. Water, 14(1). https://doi.org/10.3390/w14010011
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Streambank vertical temperature profile data collected along tributaries to Farmington River, CT, USA in 2021
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Groundwater is often supersaturated in greenhouse gases (GHGs; i.e. CO2, CH4, N2O) and delivers these gasses to stream channels where they are either emitted, consumed, or transported downstream. However, areas of relatively spatially-focused (‘preferential’) groundwater discharge may also be located above the waterline and be immediate sources of GHGs to the atmosphere before moving down the streambank and mixing with surface waters. The rate at which groundwater discharges from exposed streambanks may alter the amount of instantaneous emissions that occur at preferential groundwater discharge zones. To quantify vertical groundwater flux rates from exposed preferential groundwater discharge points along exposed streambanks, we deployed temperature loggers (iButton #DS1922L, Maxim Integrated, Inc., San Jose, CA, USA) in vertical profilers into thermally-identified groundwater discharge points along streambanks at two sites within the Farmington River watershed (northwestern CT and southwestern MA, USA) with varying streambank organic matter content. Stratton Brook is a 2nd order tributary to the Farmington River. The surficial sediments at this tributary include sand and gravel, with some areas being comprised of fines and thin and thick till deposits (Stone et al. 1992). Stratton Brook streambanks are composed of unconsolidated sediment with high organic matter deposits. Surrounding landcover include forest, forested wetlands, housing developments, and a public forested park . West Branch Salmon Brook is a 3rd order tributary to the Farmington River. Its local landcover includes forest, agriculture, a public park, and housing developments. Surficial sediments include a blend of alluvium atop of gravel and sand from postglacial deposits, thick and thin till, and coarse gravel deposits (Stone et al. 1992). Streambank sediment is poorly sorted, ranging from large cobbles to fine sand. Vertical temperature profiler (VTP) data were collected at 20 distinct preferential groundwater discharge points from September 9 to October 31, 2021. For West Branch Salmon Brook, the temperature data was collected at 20 distinct preferential groundwater discharge points from September 14 to October 31, 2021, for a total of 40 monitored locations. Stone, J. R., Schafer, J. P., London, E. H., & Thompson, W. B. (1992). Surficial materials map of Connecticut. Reston, VA: US Geological Survey. https://doi.org/10.3133/70046712
Thermal infrared images and direct temperature measurements of groundwater discharge zones throughout the Farmington River watershed (Connecticut and Massachusetts)
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Areas of groundwater discharge are hydrologically and ecologically important, and yet are difficult to predict at the river network scale. Thermal infrared imagery can be used to identify areas of groundwater discharge based on an observed temperature anomaly (colder during the late summer or warmer during the late winter). The thermal images, direct temperature measurements (11 cm depth) and discharge zone (seep) location information in this data release were collected as part of a study to evaluate and improve predicted spatial patterns of groundwater discharge. The data were collected during the late summer / early fall of 2017 along selected river reaches in the Farmington River watershed (Connecticut and Massachusetts). This dataset contains 4 files. 1) Images.zip is a zipped directory containing thermal infrared and real color images. 2) Image_Details.csv contains attribute information for each thermal image. 3) ScannedReaches.shp is a shapefile indicating the river reaches that were surveyed. 4) Seeps.shp is a shapefile of groundwater seep locations and attributes that were identified during the fieldwork.
Thermal infrared images and direct temperature measurements of groundwater discharge zones throughout the Farmington River watershed (Connecticut and Massachusetts)
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Areas of groundwater discharge are hydrologically and ecologically important, and yet are difficult to predict at the river network scale. Thermal infrared imagery can be used to identify areas of groundwater discharge based on an observed temperature anomaly (colder during the late summer or warmer during the late winter). The thermal images, direct temperature measurements (11 cm depth) and discharge zone (seep) location information in this data release were collected as part of a study to evaluate and improve predicted spatial patterns of groundwater discharge. The data were collected during the late summer / early fall of 2017 along selected river reaches in the Farmington River watershed (Connecticut and Massachusetts). This dataset contains 4 files. 1) Images.zip is a zipped directory containing thermal infrared and real color images. 2) Image_Details.csv contains attribute information for each thermal image. 3) ScannedReaches.shp is a shapefile indicating the river reaches that were surveyed. 4) Seeps.shp is a shapefile of groundwater seep locations and attributes that were identified during the fieldwork.
Biogeochemical and source characteristics of preferential groundwater discharge in the Farmington River watershed (Connecticut and Massachusetts, 2017 - 2021)
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We used spatial data from previously mapped preferential groundwater discharges throughout the Farmington River watershed in Connecticut and Massachusetts (https://doi.org/10.5066/P915E8JY) to guide water sample collection at known locations of groundwater discharging to surface water. In 2017 and 2019 - 2021, samples were collected during general river baseflow conditions (July – November, <30.9 cms mean daily discharge (USGS gage 01189995, statistics 2010-2022) when the riverbank discharge points were exposed. We collected a suite of dissolved constituents and stable isotopes of water directly in the shallow saturated sediments of active points of discharge, and coincident stream chemical samples were also collected adjacent to locations of groundwater discharge. Data collected includes nutrients (NO3, NH4, Cl, SO4, PO4, dissolved organic carbon (DOC), and total nitrogen (TN)), greenhouse gases (CO2, CH4, and N2O), dissolved gases (N2, dissolved oxygen (DO)), conductivity, sediment characteristics, temperature, and spatial information. This dataset includes 2 main files: 1) Farmington_Chemistry_2017_2021.csv contains attribute information for each biogeochemical constituent collected at preferential groundwater discharges along the Farmington River network. 2)Farmington_Temporal_Cl_Rn_Iso_2020.csv contain attribute information for source characteristic data (Chloride, Radon, Isotope) collected at locations of repeat sampling at 5 groundwater seep faces along the Farmington River (Alsop and Rainbow Island).
Thermal infrared images of groundwater discharge zones in the Farmington and Housatonic River watersheds (Connecticut and Massachusetts, 2019)(ver. 3.0, January 2023)
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Locations of focused (or ‘preferential’) groundwater discharge to surface water are often hydrologically and ecologically important, yet our ability to predict the spatial distribution and water quality of preferential riverbank discharges is limited at the scale of river networks. To advance the understanding of the physical controls on riverbank groundwater discharge processes, discharge zones can be mapped efficiently using handheld and drone-based thermal infrared cameras. Groundwater discharge locations can be identified based on ‘anomalous’ thermal signatures, such as relatively cold riverbank zones in summer and warm riverbank zones in winter. Thermal infrared imaging can be combined with concurrent direct riverbank measurements to identify discharge zones with confidence and to evaluate local sediment properties, groundwater flux rates, and discharge water quality. The ground- and watercraft-based river data contained in this data release were collected from June through October during 2019, 2020, and 2021 to characterize the spatial distribution of riverbank groundwater discharges along river reaches within the Farmington and Housatonic River Watersheds. This data release contains GPS locations of mapped riverbank discharge zones, thermal infrared and visible-light image data, and direct riverbank measurements. This data release also contains bank soil parameters, temperature, and discharge water dissolved oxygen concentrations at a subset of groundwater discharges. This release also contains drone-based thermal infrared data collected over a wetland site in western Connecticut on 04/04/2019, and over a reach of the Farmington River in Farmington, Connecticut on 02/22/2019. These drone-based thermal image data should be interpreted as 'apparent'; potentially useful for qualitatively showing thermal contrast and anomalies but are not suited for more quantitative purposes without additional post-calibration steps. This updated dataset contains 12 main files: 1) SalmonBrook_FLIR.zip is a zipped directory containing thermal infrared and real color images collected by handheld cameras along Salmon Brook, a third-order stream located in the Farmington River Watershed. 2) SalmonBrook_Image_Details.csv contains attribute information for each thermal image in the Salmon Brook dataset that pertains to a mapped streambank preferential groundwater discharge locations. TIR image names and numbers are related to images in the SalmonBrook_FLIR.zip folder. 3) PDP_Images.zip is zipped directory containing thermal infrared and real color images collected along reaches of the mainstem Farmington and Housatonic Rivers. 4) PDP_2021_Main.csv contains attribute information for each thermal image and mapped riverbank preferential groundwater discharge location along the Farmington and Housatonic Rivers. 5) FldMsrmnts_11032021.csv contains attribute information of water and sediment characteristics at a subset of mapped riverbank groundwater discharge locations along the Farmington River. 6) FarmSN_PDPs.csv contains attribute information for characterizing lateral extent of groundwater discharges mapped along the Farmington River, along with bank locations were discharge zones were not identified at 1-m nominal resolution. 7) Hous_PDPs.csv contains attribute information for characterizing lateral extent of groundwater discharges mapped along the Housatonic River, along with bank locations were discharge zones were not identified at 1-m nominal resolution. 8) raw_drone_IR is a zipped directory of uncalibrated thermal infrared data collected via drone at two sites. 9) processed_drone_IR is a zipped directory of processed (apparent) thermal infrared orthomosaic images. 10) bank_discharge_locations_Farmington_TIR_2019_2021.shp is an ESRI shapefile of the groundwater discharge locations derived from the river field surveys for demonstration purposes. This shapefile indicates the lateral riverbank extent of mapped discharge zones along the
Geodatabase of Groundwater Discharge Estimates to Streams in the Upper Colorado River Basin
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The U.S. Geological Survey (USGS) as part of the Department of Interior WaterSmart Program compiled published estimates of groundwater discharge to streams in the Upper Colorado River Basin into a dataset and developed a geospatial database. For the purpose of this compilation, groundwater discharge to streams consists of base-flow, and may include contributions from groundwater discharge from various flow paths, lateral seepage, hyporheic flow, and irrigation return flow. Stream reaches from the National Hydrography Dataset (NHD) where there was groundwater discharge estimates were delineated in the geospatial database. Attributes describing the methods used for estimating groundwater discharge were created. Feature class attributes associated with each stream reach include: groundwater discharge (acre-ft/yr), method of measurement, report reference, defined reach, base flow index estimate (acre-ft/yr), and 8-digit HUC(s) (hydrologic unit code(s) for the reach). In addition, groundwater discharge estimates were calculated using attributes from a flow characteristics dataset (Wolock, 2003), the average annual base-flow index (BFI) value and the average daily streamflow value. The calculated groundwater discharge estimates were included in the database as separate attributes and were compared to reported estimates of groundwater discharge. Groundwater discharge estimates calculated using BFI were greater than reported groundwater discharge estimates. References cited: Wolock, D., 2003, Flow Characteristics at U.S. Geological Survey Streamgages in the Conterminous United States: U.S. Geological Survey Open-File Report 2003-146, accessed July 2, 2012 at https://water.usgs.gov/GIS/metadata/usgswrd/XML/qsitesdd.xml
Geodatabase of Groundwater Discharge Estimates to Streams in the Upper Colorado River Basin
공공데이터포털
The U.S. Geological Survey (USGS) as part of the Department of Interior WaterSmart Program compiled published estimates of groundwater discharge to streams in the Upper Colorado River Basin into a dataset and developed a geospatial database. For the purpose of this compilation, groundwater discharge to streams consists of base-flow, and may include contributions from groundwater discharge from various flow paths, lateral seepage, hyporheic flow, and irrigation return flow. Stream reaches from the National Hydrography Dataset (NHD) where there was groundwater discharge estimates were delineated in the geospatial database. Attributes describing the methods used for estimating groundwater discharge were created. Feature class attributes associated with each stream reach include: groundwater discharge (acre-ft/yr), method of measurement, report reference, defined reach, base flow index estimate (acre-ft/yr), and 8-digit HUC(s) (hydrologic unit code(s) for the reach). In addition, groundwater discharge estimates were calculated using attributes from a flow characteristics dataset (Wolock, 2003), the average annual base-flow index (BFI) value and the average daily streamflow value. The calculated groundwater discharge estimates were included in the database as separate attributes and were compared to reported estimates of groundwater discharge. Groundwater discharge estimates calculated using BFI were greater than reported groundwater discharge estimates. References cited: Wolock, D., 2003, Flow Characteristics at U.S. Geological Survey Streamgages in the Conterminous United States: U.S. Geological Survey Open-File Report 2003-146, accessed July 2, 2012 at https://water.usgs.gov/GIS/metadata/usgswrd/XML/qsitesdd.xml
Geographic Data for the Estimation of Peak Flow Statistics for Illinois
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The U.S. Geological Survey Central Midwest Water Science Center completed a report (Over and others, 2023) documenting methods, results, and applications of an updated flood-frequency study for the State of Illinois. The study developed regional regression equations that relate the peak-flow quantiles and the basin characteristics of selected streamgages in Illinois, Indiana, and Wisconsin, based on data through water year 2017 (a water year is the period from October 1 to September 30 and is designated by the year in which it ends; for example, water year 2017 was from October 1, 2016, to September 30, 2017). The data provided through this data release are those digital datasets of basin characteristics that have been collected, tested, and ultimately selected for use in regional regression equations. These datasets consist of raster grid files for slope (slope100.zip), calculated from a published digital elevation model (DEM) (Schafer and Sharpe, 2023), soil slope (stats_slope100.zip) subsetted and resampled from Wolock (1997), a soil texture permeability index (texp_indx_rnd.zip) computed using data from Wolock (1997), land cover (nlcd16_22_23_24.zip) adapted from Yang and others (2018), a basin soil wetness measure (drclass1a.zip) computed from U.S. Department of Agriculture (USDA) (2013), and an urbanization fraction (urbthe2010.zip) computed from Theobald 2010 data (Theobald, 2005). Some basin characteristics are not included in this data release as they are easily derived from StreamStats basin delineations themselves, such as basin drainage area. The U.S. Geological Survey (USGS), in cooperation with the Illinois Center for Transportation (ICT) and the Illinois Department of Transportation (IDOT), prepared these digital datasets of basin characteristics for use in the Illinois StreamStats application (https://streamstats.usgs.gov/ss/). Two additional shapefiles are provided: a shapefile of the streamgages (IL_StreamStats_Gages.zip) and a shapefile of the associated delineated streamgage drainage basins (IL_StreamStats_DrainageBasins.zip) used in analysis (Over and others, 2023).
Precipitation, surface-water discharge, and groundwater elevation data for Fourmile Creek, Ankeny, Iowa, USA during October 1, 2013 to November 30, 2013
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Dataset includes continuous discharge at the USGS (Station ID: 05485605) Fourmile Creek near Ankeny, IA DS1 gage site (http://waterdata.usgs.gov/usa/nwis/uv?site_no=05485605) as well as daily precipitation and water level data in select groundwater piezometers recorded in 10 minute intervals during the period Oct 1, 2013 to November 30 2013. Latitude and longitude data are provided for groundwater piezometer locations.
Measurements of Discharge in Small, Low-Flowing Streams Using Multiple Techniques
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This dataset includes depth and position measurements to estimate the cross-sectional geometry at sites in small streams throughout the United States.