Toxicity Assay Data for Groundwater Contaminated by Petroleum Hydrocarbons near Bemidji, MN (2018)
공공데이터포털
Groundwater samples were collected in June 2018 from a background (reference) well located 200 m upgradient from the source and five wells along a flowline in the plume at 39, 68, 102, 125, and 254 m downgradient from the source. Before sampling, at least three times the water volume in the well casing was purged and field parameters (temperature, dissolved oxygen, specific conductance, and pH) were stable. Two samples from each well were collected into unpreserved 1 L amber bottles and shipped on ice overnight to a commercial lab. The two samples were extracted using dichloromethane (DCM; EPA Method 3510). One sample extract was treated with silica gel cleanup (SGC) column (USEPA method 3630C). Aliquots of the above two extracts were used for the high-throughput bioassays (Attagene Inc. Morrisville, NC).To ensure compatibility with the bioassays, DCM-total and DCM-SGC extracts were dried under nitrogen gas and, once dry, reconstituted in 1 mL of dimethysulfoxide (DMSO) resulting in 1000x concentration. A third water sample was collected from each well to perform Attagene bioassays on the organics obtained with the HLB solid phase extraction. These samples were kept on dry ice in the field and stored at 20C. Samples were processed before Aug 17, 2018 (within 22 days). They were filtered using a GF/F filter (1.0 μm); 250 mL of each filtrate was concentrated using OASIS hydrophilic-lipophilic balance (HLB) 5 cm3 200 mg cartridges (Waters, Milford, MA). The cartridges were eluted with 6 mL of methanol, followed by 6 mL of a 50:50 mixture of methanol and DCM, and brought to dryness under nitrogen gas at 20°C. The extracts were reconstituted with 0.5 mL dimethysulfoxide (DMSO) resulting in 500x concentration. The preparation method removes the volatile fraction. As a result, the toxicity assays performed in this study did not assess the effects of the volatile components in the plume as measured by the TPHg analyses. Extracts generated using DCM-total, DCM-SGC and HLB were tested in Attagene assays at 1x concentration relative to the groundwater (i.e. 1 µL of 1000x extract or 2 µL of 500x extract were added to 1 mL of growth media). Bioassays that evaluate activation of 46 molecular targets (CIS-FACTORIAL) were performed on these three extracts in duplicate (Attagene Inc. Morrisville, NC). The assay method was described by Romanov et al.38 and deployed for identification of molecular targets of interest in oil-contaminated groundwater samples 20 and a variety of surface waters39. Briefly, human hepatoma (HepG2) cells transfected with reporter constructs activated by transcription factors (TF) were used. The reporter transcript abundance was measured by isolating the produced RNA, reverse transcription, amplification, labeling and capillary electrophoresis. Abundance data are reported as the induction by sample of interest relative to abundance induced by a DMSO solvent control (abundance in environmental sample was divided by abundance in solvent control). Positive control assays were performed for a subset of molecular targets (Table S2) including AhR (6-Formylindolo [3,2-b] Carbazole) and PXR (Rifampicin).
Data release for Organic geochemistry and petrology of Devonian shale in eastern Ohio: implications for petroleum systems assessment (2018)
공공데이터포털
Recent production of light sweet oil from shallow (~2,000 ft) horizontal wells in the Upper Devonian Berea Sandstone of eastern Kentucky and historical oil production from conventional wells in the Berea of adjoining southern Ohio has prompted re-evaluation of Devonian petroleum systems in the central Appalachian Basin. Herein, we examined Upper Devonian Ohio Shale (lower Huron Member) and Middle Devonian Marcellus Shale organic-rich source rocks from eastern Ohio and nearby areas using organic petrography and geochemical analyses of solvent extracts. The data indicate the organic matter in the Ohio and Marcellus Shales was primarily derived from marine algae and its degradation products including bacterial biomass. Absence of odd-over-even n-alkane distributions in gas chromatograms and low gammacerane index values in Devonian source rocks are similar to properties reported for Devonian-reservoired oils in eastern Ohio, suggesting a strong oil-source rock correlation. However, petrographic and geochemical parameters presented here were unable to discriminate specific shale source rocks (e.g., Ohio Shale vs. Marcellus Shale) for the Devonian oils. Lower Paleozoic oils from eastern Ohio, in contrast, are characterized by the presence of odd-over-even n-alkane distributions and higher gammacerane values which clearly discriminate them from Devonian shale-derived oils. Measurements of solid bitumen reflectance (BRo) at the thermal maturity range of the samples (immature to peak oil conditions) tend to underestimate ‘true’ thermal maturity because solid bitumen has lower reflectance than co-occurring vitrinite. Because solid bitumen dominates the organic matter in Devonian shale and vitrinite is sparse, the value of reflectance as a thermal proxy is questionable and its use may lead to reports of ‘vitrinite reflectance suppression’ in early mature to oil window mature areas. For example, thermal maturity estimates from equilibrium(?) biomarker isomerization ratios may suggest some of the Devonian source rock samples are at middle to peak oil window conditions e.g., approximate vitrinite reflectance values of 0.8-0.9%, whereas solid bitumen reflectance is approximately 0.52-0.54% in the same samples. If correct, this observation may require that the predicted onset of oil generation from Devonian shale source rocks in eastern Ohio is moved farther westward. As a consequence, only local to short-distance (30-50 mi) migration would be necessary for emplacement of Devonian-sourced oils into Devonian reservoirs of eastern Ohio, rather than long-distance migration (>50 mi) from ‘deep in the Appalachian basin’, as suggested by previous workers, potentially impacting exploration and future assessments of undiscovered petroleum resources in the Berea Sandstone. However, biomarker isomerization ratios do not show consistent relationships to other thermal maturity parameters (BRo, Tmax), thereby preventing development of robust empirical calibrations for these thermal proxies in the Devonian of eastern Ohio.
Inorganic and organic chemical composition of groundwater collected from monitoring wells located at the National Crude Oil Spill Fate and Natural Attenuation Research Site, Bemidji, Minnesota, USA 2009-2023
공공데이터포털
This dataset contains information from groundwater monitoring wells at the National Crude Oil Spill Fate and Natural Attenuation Research Site near Bemidji, Minnesota, USA. The information includes field and laboratory methods, site locations, and inorganic and organic chemistry data. Samples were collected between 2009 and 2023, and analyzed for inorganic anions: F (fluoride), Cl (chloride), Br (bromide), NO3 (nitrate), PO4 (phosphate), SO4 (sulfate), and cations: Ca (calcium), Na, (sodium), Mg (magnesium), K (potassium), Si (silicon), Sr (strontium), Al (aluminum), Fe (iron), Mn (manganese), Ba (barium), B (boron), Li (lithium), Ag (silver), As (arsenic), Be (beryllium), Bi (bismuth), Cd (cadmium), Ce (cerium), Co (cobalt), Cs (cesium), Cr (chromium), Cu (copper), La (lanthanum), Mo (molybdenum), Ni (nickel), Pb (lead), Rb (rubidium), Sb (antimony), Se (selenium), Sn (tin), Th (thorium), Tl (thallium), U (uranium), V (vanadium), W (tungsten), and Zn (zinc). Additionally, samples were analyzed for benzene, toluene, ethylbenzene, o, m, p-xylene, total VHC (30 volatile hydrocarbons), NVDOC (non-volatile dissolved organic carbon), methane, ammonia as nitrogen, alkalinity as HCO3 (bicarbonate), and LMWOA (low molecular weight organic acids; lactate, acetate, propionate, formate, butyrate, pyruvate, and benzoate). The following analyses were performed during a select number of years: delta 13C of DIC (dissolved inorganic carbon) delta 13C of DOC, (dissolved organic carbon) and delta 2H in H2O, delta 18O in H2O. Field measurements for specific conductance, pH, and dissolved oxygen were measured daily. Water levels were measured during the sampling events. The supporting metadata files contain site information, field and laboratory methods, water chemistry, and quality-control results. There are three tables.
Analyses of Select Organic and Inorganic Data Collected from Lysimeters Installed at the Bemidji Crude Oil Spill Site, Minnesota, 2018, 2019, 2021
공공데이터포털
The U.S. Geological Survey (USGS) collected porewater samples from nine suction lysimeters in 2018, 2019, and 2021 for analysis of organic and inorganic constituents from the National Crude Oil Spill Fate and Natural Attenuation Research Site near Bemidji, MN. In August of 1979, approximately 1,700,000 L (liters), or 10,700 barrels, of crude oil spilled onto a glacial outwash aquifer. Sampled lysimeters included L310-1.5, L310-4.5, L1802-1.8, L9014-1.5, L9014-3.0, L9014-4.5, L9017-1.3, L9017-2.5, and L9017-3.7. This data release presents data on analytes that are important indicators of biodegradation processes. Some of these analytes, if present in elevated concentrations, can be a concern regarding potential effects on human health and the environment. There is one tabulated data set containing concentrations of non-volatile dissolved organic carbon (NVDOC), ammonium (NH3-N), orthophosphate, alkalinity as bicarbonate (HCO3-), major inorganic anions, cations, and trace elements. The supporting metadata file contains site information, field and laboratory methods, water chemistry, and quality-control results. Samples were analyzed in the Reston Biogeochemical Processes in Groundwater Laboratory (RBPGL) in Reston, VA, and by a contract lab, Meadowlands Environmental Research Institute (MERI) in Lyndhurst, NJ.
Analyses of Select Organic and Inorganic Data Collected from Lysimeters Installed at the Bemidji Crude Oil Spill Site, Minnesota, 2018, 2019, 2021
공공데이터포털
The U.S. Geological Survey (USGS) collected porewater samples from nine suction lysimeters in 2018, 2019, and 2021 for analysis of organic and inorganic constituents from the National Crude Oil Spill Fate and Natural Attenuation Research Site near Bemidji, MN. In August of 1979, approximately 1,700,000 L (liters), or 10,700 barrels, of crude oil spilled onto a glacial outwash aquifer. Sampled lysimeters included L310-1.5, L310-4.5, L1802-1.8, L9014-1.5, L9014-3.0, L9014-4.5, L9017-1.3, L9017-2.5, and L9017-3.7. This data release presents data on analytes that are important indicators of biodegradation processes. Some of these analytes, if present in elevated concentrations, can be a concern regarding potential effects on human health and the environment. There is one tabulated data set containing concentrations of non-volatile dissolved organic carbon (NVDOC), ammonium (NH3-N), orthophosphate, alkalinity as bicarbonate (HCO3-), major inorganic anions, cations, and trace elements. The supporting metadata file contains site information, field and laboratory methods, water chemistry, and quality-control results. Samples were analyzed in the Reston Biogeochemical Processes in Groundwater Laboratory (RBPGL) in Reston, VA, and by a contract lab, Meadowlands Environmental Research Institute (MERI) in Lyndhurst, NJ.
Nonvolatile dissolved organic carbon and diesel range organics concentrations measured in 2016 at the USGS crude oil study site near Bemidji, Minnesota, USA
공공데이터포털
The Bemidji crude oil spill site is a long-term USGS study site to understand the fate of crude oil in the shallow subsurface. A description of the site can be found at https://mn.water.usgs.gov/projects/bemidji. In 2014 concentrations of non-volatile dissolved organic carbon (NVDOC) were three times higher than diesel range organics (DRO) in the contaminant plume*. This is important because most of the NVDOC in the plume is composed of partial transformation products of compounds from the crude oil that are not reflected in a DRO analysis. In 2016 we conducted a campaign to determine if DRO values continue to reflect only a fraction of the NVDOC. These data are the results of that campaign. A total of 25 wells were sampled for DRO and NVDOC in August, 2016. Three wells with long term records were included in the sampling: 530B, 515B, and 9316D. Wells sampled in 2016 but not in 2014 include two wells located 14 m from a down gradient lake (1217B and 1217C) and one well in the zone sprayed by oil (956). *Bekins, B. A., Cozzarelli, I. M., Erickson, M. L., Steenson, R. A., and Thorn, K. A., 2016, Crude Oil Metabolites in Groundwater at Two Spill Sites: Groundwater, v. 54, no. 5, p. 681-691.