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Biogeochemical Data for Mercury and other Constituents in Surface Sediment and Deep Cores from the Hells Canyon Reservoir Complex, Idaho and Oregon 2014-2018
The Hells Canyon Complex (HCC) is comprised of a series of three consecutive reservoirs (Brownlee, Oxbow, and Hells Canyon) along a 145 km reach of the Snake River bordered by Idaho to the east and Oregon to the west. Due to concerns regarding mercury (Hg) contamination within the HCC, in cooperation with Idaho Power Company, the U.S. Geological Survey has been leading an investigation into the sources, transport, microbial transformations, chemical speciation and bioaccumulation of Hg in this complex river-reservoir environment. This data release is focused on the sediment component of this larger effort and includes data collected between 2014 and 2018 from shallow surface sediment (≤ top 5 cm) and from sectioned deep cores ranging from 34 cm to 112 cm in length. While the majority of the data was collected from within the HCC, some limited additional data is included from a number of riverine bed sediment sites located in the watershed upstream of the HCC and from two additional reservoirs on the Boise River sampled as control sites (Anderson Ranch and Lucky Peak reservoirs). For shallow surface sediment, the list of mercury associated analytes reported in this dataset includes total mercury, methylmercury, and inorganic reactive mercury concentrations; as well as rate constants and calculated potential rates associated with microbial methylmercury production and degradation, derived from stable isotope amendment bottle incubations. The list of non-mercury analytes includes field measurements of temperature, oxidation-reduction potential and pH; percent dry weight; percent loss on ignition; wet bulk density; porosity; total reduced sulfur; and iron speciation. For a sub-set of the shallow sediment sampled there is additional data for: percent organic carbon (with isotopic 13C values), percent nitrogen (with isotopic 15N values), and grain size (percent < 64 µm). Of the eight sampling events conducted within the HCC, sediment porewater samples were collected from sediment-water interface cores on three occasions to estimate benthic-pelagic diffusive fluxes of a number of mercury and non-mercury constituents. The list of porewater analytes determined and reported herein include: total mercury, methylmercury, ortho-phosphate, ammonium, sulfide, dissolved organic carbon, dissolved organic matter specific ultra-violet absorption at 254 nm (SUVA254), acetate, sulfate, thiosulfate, nitrate, and elemental analysis of Al, As, B, Br, Ca, Cd, Cl, Cu, F, Fe, K, Mg, Mn, Mo, Na, Ni, P, Pb, Se, Si (as SiO2), U, and Zn. Of the eleven deep cores collected and sub-sectioned, all sediment samples were assayed for total mercury and percent loss on ignition, nine were assayed for methylmercury, and two were assayed for dry particle density and environmental radionuclides (137Cs, 210Pb and 226Ra) to assess sedimentation rates. This data release includes five data tables given both as Excel (*.xlsx) and machine readable 'comma-separated values' format (*.csv): 1) ‘T1_Data.Dictionary_HCC.2014-18’, the Data Dictionary, which provides definitions and details related to the other four data tables and includes analytical methods citations; 2) ‘T2_Shallow sed bulk_HCC.2014-18’, the shallow (bulk) sediment dataset; 3) ‘T3_Shallow sed porewater_HCC.2014-18’, the shallow sediment porewater dataset; 4) ‘T4_Deep cores_HCC.2014-18’, the deep core profile dataset; and 5) ‘T5_QA_HCC.2014-18’, quality assurance data summary for all major analyses. In addition, file ‘HCC 2014-18.kmz’ provides the sampling locations in a machine-readable geospatial file format (*.kmz).
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Biogeochemical Data for Mercury and other Constituents in Surface Sediment and Deep Cores from the Hells Canyon Reservoir Complex, Idaho and Oregon 2014-2018
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The Hells Canyon Complex (HCC) is comprised of a series of three consecutive reservoirs (Brownlee, Oxbow, and Hells Canyon) along a 145 km reach of the Snake River bordered by Idaho to the east and Oregon to the west. Due to concerns regarding mercury (Hg) contamination within the HCC, in cooperation with Idaho Power Company, the U.S. Geological Survey has been leading an investigation into the sources, transport, microbial transformations, chemical speciation and bioaccumulation of Hg in this complex river-reservoir environment. This data release is focused on the sediment component of this larger effort and includes data collected between 2014 and 2018 from shallow surface sediment (≤ top 5 cm) and from sectioned deep cores ranging from 34 cm to 112 cm in length. While the majority of the data was collected from within the HCC, some limited additional data is included from a number of riverine bed sediment sites located in the watershed upstream of the HCC and from two additional reservoirs on the Boise River sampled as control sites (Anderson Ranch and Lucky Peak reservoirs). For shallow surface sediment, the list of mercury associated analytes reported in this dataset includes total mercury, methylmercury, and inorganic reactive mercury concentrations; as well as rate constants and calculated potential rates associated with microbial methylmercury production and degradation, derived from stable isotope amendment bottle incubations. The list of non-mercury analytes includes field measurements of temperature, oxidation-reduction potential and pH; percent dry weight; percent loss on ignition; wet bulk density; porosity; total reduced sulfur; and iron speciation. For a sub-set of the shallow sediment sampled there is additional data for: percent organic carbon (with isotopic 13C values), percent nitrogen (with isotopic 15N values), and grain size (percent < 64 µm). Of the eight sampling events conducted within the HCC, sediment porewater samples were collected from sediment-water interface cores on three occasions to estimate benthic-pelagic diffusive fluxes of a number of mercury and non-mercury constituents. The list of porewater analytes determined and reported herein include: total mercury, methylmercury, ortho-phosphate, ammonium, sulfide, dissolved organic carbon, dissolved organic matter specific ultra-violet absorption at 254 nm (SUVA254), acetate, sulfate, thiosulfate, nitrate, and elemental analysis of Al, As, B, Br, Ca, Cd, Cl, Cu, F, Fe, K, Mg, Mn, Mo, Na, Ni, P, Pb, Se, Si (as SiO2), U, and Zn. Of the eleven deep cores collected and sub-sectioned, all sediment samples were assayed for total mercury and percent loss on ignition, nine were assayed for methylmercury, and two were assayed for dry particle density and environmental radionuclides (137Cs, 210Pb and 226Ra) to assess sedimentation rates. This data release includes five data tables given both as Excel (*.xlsx) and machine readable 'comma-separated values' format (*.csv): 1) ‘T1_Data.Dictionary_HCC.2014-18’, the Data Dictionary, which provides definitions and details related to the other four data tables and includes analytical methods citations; 2) ‘T2_Shallow sed bulk_HCC.2014-18’, the shallow (bulk) sediment dataset; 3) ‘T3_Shallow sed porewater_HCC.2014-18’, the shallow sediment porewater dataset; 4) ‘T4_Deep cores_HCC.2014-18’, the deep core profile dataset; and 5) ‘T5_QA_HCC.2014-18’, quality assurance data summary for all major analyses. In addition, file ‘HCC 2014-18.kmz’ provides the sampling locations in a machine-readable geospatial file format (*.kmz).
Total mercury and methylmercury concentrations in biota from the Hells Canyon Reservoir Complex on the Snake River, Idaho and Oregon, USA
공공데이터포털
Comma-separated values (.csv) file containing data related to mercury in biota collected from the Hells Canyon Reservoir Complex on the Snake River, Idaho and Oregon.
Total mercury and methylmercury concentrations in biota from the Hells Canyon Reservoir Complex on the Snake River, Idaho and Oregon, USA
공공데이터포털
Comma-separated values (.csv) file containing data related to mercury in biota collected from the Hells Canyon Reservoir Complex on the Snake River, Idaho and Oregon.
Chemical characterization of water and suspended sediment of the Snake River and Hells Canyon Complex (Idaho, Oregon) (ver. 3.0, November 2023)
공공데이터포털
This dataset includes laboratory analyses of surface water samples and sediment trap material collected from (1) locations upstream, downstream, and within the Hells Canyon Complex (Idaho, Oregon) of the Snake River, (2) tributaries of the Snake River, and (3) two reservoirs near Boise, Idaho, from 2014 to 2022. The study area spans approximately 232 river miles of the Snake River and includes: two sites on the main stem of the Snake River upstream of the Hells Canyon Complex (Snake River mile 447.6, 399.0, and 345.6), six sites within Brownlee Reservoir (Snake River mile 318, 314, 310, 305, 300, and 286), one site within Oxbow Reservoir (Snake River mile 273), two sites within Hells Canyon Reservoir (Snake River mile 252 and 248.1), reservoir outflow locations (Snake River mile 283.9, 269.9, and 246.9), one location downstream of the Hells Canyon Complex (Snake River mile 215.4), and over 20 tributary sites of waterways discharging into the Snake River. In addition, the Lucky Peak and Anderson Ranch reservoirs along the Boise River were sampled in June and September 2018. At sites on the main stem of the Snake River, reservoir inflow and outflow locations of the Hells Canyon Complex, and tributaries of the Snake River, whole water and filtered surface water samples were collected by using either a depth-integrated sampler from bridges or submerging a polyethylene terephthalate (PETG) bottle (details for each site provided in the metadata file). Within reservoirs, whole water and filtered water samples were collected in profile from the surface (2 meters) to approximately 5 meters above the sediment-water interface using either a peristaltic pump or a Van Dorn sampler. Further, water up to 1 meter above the sediment-water interface was obtained by collecting water in vertical subsections above an undisturbed sediment core. Water samples were processed (details provided in the metadata file) and analyzed for total suspended solids (TSS), particulate total mercury (p.THg), particulate methylmercury (p.MeHg), particulate iron (p.Fe), particulate manganese (p.Mn), particulate organic carbon (POC) content and stable isotopic composition, particulate nitrogen (PN) content and stable isotopic composition, filter-passing total mercury (f.THg), filter-passing methylmercury (f.MeHg), dissolved organic carbon (DOC) concentration and stable isotopic composition, dissolved organic matter composition (UV-vis absorption and fluorescence spectroscopy; ultrahigh resolution mass spectrometry), inorganic anions (chloride, nitrate, sulfate, thiosulfate), acetate, major and trace elements, inorganic sulfide, and chlorophyll a. Dissolved organic matter UV-vis absorption measurements included the specific ultraviolet absorbance at 254 nanometers (SUVA254), spectral slopes (at 275 to 295 nm and 350 to 400 nm), and the spectral slope ratio. Dissolved organic matter fluorescence indices include the fluorescence index, humification index, and freshness index. Concentrations of particulate and filter-passing inorganic divalent mercury (p.Hg(II), f.Hg(II)) were calculated by subtracting p.MeHg and f.MeHg concentrations from p.THg and f.THg concentrations, respectively. Aqueous – particulate distribution coefficients (Kd values) for inorganic divalent mercury and methylmercury were determined. Suspended sediment was collected in settling traps deployed at up to three depths at 4 locations within the Hells Canyon Complex (Snake River mile 318, 300, 286, and 248; 16 deployments from September 2016 to September 2018); the depths targeted discrete epilimnetic, metalimnetic, and hypolimnetic regions of reservoirs. Settling trap material was sieved (less than and greater than 243 µm) and analyzed for total mercury, methylmercury, loss on ignition, organic carbon content and stable isotopic composition, nitrogen content and stable isotopic composition, trace and major element content, and mineralogical composition. In addition, measurements of water properties
Chemical characterization of water and suspended sediment of the Snake River and Hells Canyon Complex (Idaho, Oregon) (ver. 3.0, November 2023)
공공데이터포털
This dataset includes laboratory analyses of surface water samples and sediment trap material collected from (1) locations upstream, downstream, and within the Hells Canyon Complex (Idaho, Oregon) of the Snake River, (2) tributaries of the Snake River, and (3) two reservoirs near Boise, Idaho, from 2014 to 2022. The study area spans approximately 232 river miles of the Snake River and includes: two sites on the main stem of the Snake River upstream of the Hells Canyon Complex (Snake River mile 447.6, 399.0, and 345.6), six sites within Brownlee Reservoir (Snake River mile 318, 314, 310, 305, 300, and 286), one site within Oxbow Reservoir (Snake River mile 273), two sites within Hells Canyon Reservoir (Snake River mile 252 and 248.1), reservoir outflow locations (Snake River mile 283.9, 269.9, and 246.9), one location downstream of the Hells Canyon Complex (Snake River mile 215.4), and over 20 tributary sites of waterways discharging into the Snake River. In addition, the Lucky Peak and Anderson Ranch reservoirs along the Boise River were sampled in June and September 2018. At sites on the main stem of the Snake River, reservoir inflow and outflow locations of the Hells Canyon Complex, and tributaries of the Snake River, whole water and filtered surface water samples were collected by using either a depth-integrated sampler from bridges or submerging a polyethylene terephthalate (PETG) bottle (details for each site provided in the metadata file). Within reservoirs, whole water and filtered water samples were collected in profile from the surface (2 meters) to approximately 5 meters above the sediment-water interface using either a peristaltic pump or a Van Dorn sampler. Further, water up to 1 meter above the sediment-water interface was obtained by collecting water in vertical subsections above an undisturbed sediment core. Water samples were processed (details provided in the metadata file) and analyzed for total suspended solids (TSS), particulate total mercury (p.THg), particulate methylmercury (p.MeHg), particulate iron (p.Fe), particulate manganese (p.Mn), particulate organic carbon (POC) content and stable isotopic composition, particulate nitrogen (PN) content and stable isotopic composition, filter-passing total mercury (f.THg), filter-passing methylmercury (f.MeHg), dissolved organic carbon (DOC) concentration and stable isotopic composition, dissolved organic matter composition (UV-vis absorption and fluorescence spectroscopy; ultrahigh resolution mass spectrometry), inorganic anions (chloride, nitrate, sulfate, thiosulfate), acetate, major and trace elements, inorganic sulfide, and chlorophyll a. Dissolved organic matter UV-vis absorption measurements included the specific ultraviolet absorbance at 254 nanometers (SUVA254), spectral slopes (at 275 to 295 nm and 350 to 400 nm), and the spectral slope ratio. Dissolved organic matter fluorescence indices include the fluorescence index, humification index, and freshness index. Concentrations of particulate and filter-passing inorganic divalent mercury (p.Hg(II), f.Hg(II)) were calculated by subtracting p.MeHg and f.MeHg concentrations from p.THg and f.THg concentrations, respectively. Aqueous – particulate distribution coefficients (Kd values) for inorganic divalent mercury and methylmercury were determined. Suspended sediment was collected in settling traps deployed at up to three depths at 4 locations within the Hells Canyon Complex (Snake River mile 318, 300, 286, and 248; 16 deployments from September 2016 to September 2018); the depths targeted discrete epilimnetic, metalimnetic, and hypolimnetic regions of reservoirs. Settling trap material was sieved (less than and greater than 243 µm) and analyzed for total mercury, methylmercury, loss on ignition, organic carbon content and stable isotopic composition, nitrogen content and stable isotopic composition, trace and major element content, and mineralogical composition. In addition, measurements of water properties
Chemical characterization of water and suspended sediment of the Snake River and Hells Canyon Complex (Idaho, Oregon) (ver. 3.0, November 2023)
공공데이터포털
This dataset includes laboratory analyses of surface water samples and sediment trap material collected from (1) locations upstream, downstream, and within the Hells Canyon Complex (Idaho, Oregon) of the Snake River, (2) tributaries of the Snake River, and (3) two reservoirs near Boise, Idaho, from 2014 to 2022. The study area spans approximately 232 river miles of the Snake River and includes: two sites on the main stem of the Snake River upstream of the Hells Canyon Complex (Snake River mile 447.6, 399.0, and 345.6), six sites within Brownlee Reservoir (Snake River mile 318, 314, 310, 305, 300, and 286), one site within Oxbow Reservoir (Snake River mile 273), two sites within Hells Canyon Reservoir (Snake River mile 252 and 248.1), reservoir outflow locations (Snake River mile 283.9, 269.9, and 246.9), one location downstream of the Hells Canyon Complex (Snake River mile 215.4), and over 20 tributary sites of waterways discharging into the Snake River. In addition, the Lucky Peak and Anderson Ranch reservoirs along the Boise River were sampled in June and September 2018. At sites on the main stem of the Snake River, reservoir inflow and outflow locations of the Hells Canyon Complex, and tributaries of the Snake River, whole water and filtered surface water samples were collected by using either a depth-integrated sampler from bridges or submerging a polyethylene terephthalate (PETG) bottle (details for each site provided in the metadata file). Within reservoirs, whole water and filtered water samples were collected in profile from the surface (2 meters) to approximately 5 meters above the sediment-water interface using either a peristaltic pump or a Van Dorn sampler. Further, water up to 1 meter above the sediment-water interface was obtained by collecting water in vertical subsections above an undisturbed sediment core. Water samples were processed (details provided in the metadata file) and analyzed for total suspended solids (TSS), particulate total mercury (p.THg), particulate methylmercury (p.MeHg), particulate iron (p.Fe), particulate manganese (p.Mn), particulate organic carbon (POC) content and stable isotopic composition, particulate nitrogen (PN) content and stable isotopic composition, filter-passing total mercury (f.THg), filter-passing methylmercury (f.MeHg), dissolved organic carbon (DOC) concentration and stable isotopic composition, dissolved organic matter composition (UV-vis absorption and fluorescence spectroscopy; ultrahigh resolution mass spectrometry), inorganic anions (chloride, nitrate, sulfate, thiosulfate), acetate, major and trace elements, inorganic sulfide, and chlorophyll a. Dissolved organic matter UV-vis absorption measurements included the specific ultraviolet absorbance at 254 nanometers (SUVA254), spectral slopes (at 275 to 295 nm and 350 to 400 nm), and the spectral slope ratio. Dissolved organic matter fluorescence indices include the fluorescence index, humification index, and freshness index. Concentrations of particulate and filter-passing inorganic divalent mercury (p.Hg(II), f.Hg(II)) were calculated by subtracting p.MeHg and f.MeHg concentrations from p.THg and f.THg concentrations, respectively. Aqueous – particulate distribution coefficients (Kd values) for inorganic divalent mercury and methylmercury were determined. Suspended sediment was collected in settling traps deployed at up to three depths at 4 locations within the Hells Canyon Complex (Snake River mile 318, 300, 286, and 248; 16 deployments from September 2016 to September 2018); the depths targeted discrete epilimnetic, metalimnetic, and hypolimnetic regions of reservoirs. Settling trap material was sieved (less than and greater than 243 µm) and analyzed for total mercury, methylmercury, loss on ignition, organic carbon content and stable isotopic composition, nitrogen content and stable isotopic composition, trace and major element content, and mineralogical composition. In addition, measurements of water properties
Geochemical data including mercury for subsamples of deep cores from the Cache Creek Settling Basin, Yolo County, California
공공데이터포털
Sediment cores were collected in the Cache Creek Settling Basin (CCSB), Yolo County, California, during October 2011 at 10 locations (borehole sites) and during August 2012 at 5 other locations. Total core depths ranged from approximately 4.6 to 13.7 meters (15 to 45 feet), with penetration to about 9.1 meters (30 feet) at most locations. Detailed subsampling (3-centimeter intervals) was done at total of seven locations: six along an east-west transect in the southern part of the Cache Creek Settling Basin and at one in the northern part of the basin for analyses of total mercury; organic content; and cesium-137, which was used for dating. This data release reports results of the analyses of each subsample of these sediment cores, including associated quality-assurance and quality-control data.
Geochemical data including mercury for subsamples of deep cores from the Cache Creek Settling Basin, Yolo County, California
공공데이터포털
Sediment cores were collected in the Cache Creek Settling Basin (CCSB), Yolo County, California, during October 2011 at 10 locations (borehole sites) and during August 2012 at 5 other locations. Total core depths ranged from approximately 4.6 to 13.7 meters (15 to 45 feet), with penetration to about 9.1 meters (30 feet) at most locations. Detailed subsampling (3-centimeter intervals) was done at total of seven locations: six along an east-west transect in the southern part of the Cache Creek Settling Basin and at one in the northern part of the basin for analyses of total mercury; organic content; and cesium-137, which was used for dating. This data release reports results of the analyses of each subsample of these sediment cores, including associated quality-assurance and quality-control data.
Chemical characterization of water and suspended sediment of the Snake River and Hells Canyon Complex (Idaho, Oregon)
공공데이터포털
This dataset includes laboratory analyses of surface water samples and sediment trap material collected from (1) locations upstream, downstream, and within the Hells Canyon Complex (Idaho, Oregon) of the Snake River, (2) tributaries of the Snake River, and (3) two reservoirs near Boise, Idaho, from 2014 to 2019. The study area spans approximately 232 river miles of the Snake River and includes: sites on the main stem of the Snake River upstream of the Hells Canyon Complex (Snake River mile 447.6 and 345.6), four primary sites within Brownlee Reservoir (Snake River mile 318, 310, 300, and 286), one site within Oxbow Reservoir (Snake River mile 273), two sites within Hells Canyon Reservoir (Snake River mile 252 and 248.1), reservoir outflow locations (Snake River mile 283.9, 269.9, and 246.9), one location downstream of the Hells Canyon Complex (Snake River mile 215.4), and over 20 tributary sites of waterways discharging into the Snake River. In addition, the Lucky Peak and Anderson Ranch reservoirs along the Boise River were sampled in June and September 2018. At sites on the main stem of the Snake River, reservoir inflow and outflow locations of the Hells Canyon Complex, and tributaries of the Snake River, whole water and filtered surface water samples were collected by using either a depth-integrated sampler from bridges or submerging a polyethylene terephthalate (PETG) bottle (details for each site provided in the metadata file). Within reservoirs, whole water and filtered water samples were collected in profile from the surface (2 meters) to approximately 5 meters above the sediment-water interface using either a peristaltic pump or a Van Dorn sampler. Further, water up to 1 meter above the sediment-water interface was obtained by collecting water in vertical subsections above an undisturbed sediment core. Water samples were processed (details provided in the metadata file) and analyzed for total suspended solids (TSS), particulate total mercury (p.THg), particulate methylmercury (p.MeHg), particulate iron (p.Fe), particulate manganese (p.Mn), particulate organic carbon (POC) content and stable isotopic composition, particulate nitrogen (PN) content and stable isotopic composition, filter-passing total mercury (f.THg), filter-passing methylmercury (f.MeHg), dissolved organic carbon (DOC) concentration and stable isotopic composition, dissolved organic matter composition (UV-vis absorption and fluorescence spectroscopy; ultrahigh resolution mass spectrometry), inorganic anions (chloride, nitrate, sulfate, thiosulfate), acetate, major and trace elements, and inorganic sulfide. Dissolved organic matter UV-vis absorption measurements included the specific ultraviolet absorbance at 254 nanometers (SUVA254), spectral slopes (at 275 to 295 nm and 350 to 400 nm), and the spectral slope ratio. Dissolved organic matter fluorescence indices include the fluorescence index, humification index, and freshness index. Concentrations of particulate and filter-passing inorganic divalent mercury (p.Hg(II), f.Hg(II)) were calculated by subtracting p.MeHg and f.MeHg concentrations from p.THg and f.THg concentrations, respectively. Aqueous – particulate distribution coefficients (Kd values) for inorganic divalent mercury and methylmercury were determined. Suspended sediment was collected in settling traps deployed at up to three depths at 4 locations within the Hells Canyon Complex (Snake River mile 318, 300, 286, and 248; 16 deployments from September 2016 to September 2018); the depths targeted discrete epilimnetic, metalimnetic, and hypolimnetic regions of reservoirs. Settling trap material was sieved (less than and greater than 243 µm) and analyzed for total mercury, methylmercury, loss on ignition, organic carbon content and stable isotopic composition, nitrogen content and stable isotopic composition, trace and major element content, and mineralogical composition. There are 4 files (*.csv) provided in this product: 1) Table 1, site
Chemical characterization of water and suspended sediment of the Snake River and Hells Canyon Complex (Idaho, Oregon)
공공데이터포털
This dataset includes laboratory analyses of surface water samples and sediment trap material collected from (1) locations upstream, downstream, and within the Hells Canyon Complex (Idaho, Oregon) of the Snake River, (2) tributaries of the Snake River, and (3) two reservoirs near Boise, Idaho, from 2014 to 2019. The study area spans approximately 232 river miles of the Snake River and includes: sites on the main stem of the Snake River upstream of the Hells Canyon Complex (Snake River mile 447.6 and 345.6), four primary sites within Brownlee Reservoir (Snake River mile 318, 310, 300, and 286), one site within Oxbow Reservoir (Snake River mile 273), two sites within Hells Canyon Reservoir (Snake River mile 252 and 248.1), reservoir outflow locations (Snake River mile 283.9, 269.9, and 246.9), one location downstream of the Hells Canyon Complex (Snake River mile 215.4), and over 20 tributary sites of waterways discharging into the Snake River. In addition, the Lucky Peak and Anderson Ranch reservoirs along the Boise River were sampled in June and September 2018. At sites on the main stem of the Snake River, reservoir inflow and outflow locations of the Hells Canyon Complex, and tributaries of the Snake River, whole water and filtered surface water samples were collected by using either a depth-integrated sampler from bridges or submerging a polyethylene terephthalate (PETG) bottle (details for each site provided in the metadata file). Within reservoirs, whole water and filtered water samples were collected in profile from the surface (2 meters) to approximately 5 meters above the sediment-water interface using either a peristaltic pump or a Van Dorn sampler. Further, water up to 1 meter above the sediment-water interface was obtained by collecting water in vertical subsections above an undisturbed sediment core. Water samples were processed (details provided in the metadata file) and analyzed for total suspended solids (TSS), particulate total mercury (p.THg), particulate methylmercury (p.MeHg), particulate iron (p.Fe), particulate manganese (p.Mn), particulate organic carbon (POC) content and stable isotopic composition, particulate nitrogen (PN) content and stable isotopic composition, filter-passing total mercury (f.THg), filter-passing methylmercury (f.MeHg), dissolved organic carbon (DOC) concentration and stable isotopic composition, dissolved organic matter composition (UV-vis absorption and fluorescence spectroscopy; ultrahigh resolution mass spectrometry), inorganic anions (chloride, nitrate, sulfate, thiosulfate), acetate, major and trace elements, and inorganic sulfide. Dissolved organic matter UV-vis absorption measurements included the specific ultraviolet absorbance at 254 nanometers (SUVA254), spectral slopes (at 275 to 295 nm and 350 to 400 nm), and the spectral slope ratio. Dissolved organic matter fluorescence indices include the fluorescence index, humification index, and freshness index. Concentrations of particulate and filter-passing inorganic divalent mercury (p.Hg(II), f.Hg(II)) were calculated by subtracting p.MeHg and f.MeHg concentrations from p.THg and f.THg concentrations, respectively. Aqueous – particulate distribution coefficients (Kd values) for inorganic divalent mercury and methylmercury were determined. Suspended sediment was collected in settling traps deployed at up to three depths at 4 locations within the Hells Canyon Complex (Snake River mile 318, 300, 286, and 248; 16 deployments from September 2016 to September 2018); the depths targeted discrete epilimnetic, metalimnetic, and hypolimnetic regions of reservoirs. Settling trap material was sieved (less than and greater than 243 µm) and analyzed for total mercury, methylmercury, loss on ignition, organic carbon content and stable isotopic composition, nitrogen content and stable isotopic composition, trace and major element content, and mineralogical composition. There are 4 files (*.csv) provided in this product: 1) Table 1, site