Open File Studies - IGWS
Permanent link for this collectionhttps://hdl.handle.net/2022/159
Nonpeer-reviewed maps and reports constitute this series, each carrying a disclaimer that the data presented is “preliminary and does not necessarily conform to the Indiana Geological and Water Survey’s editorial standards for formal publication.” The series was intended primarily for annual deliverables and data summaries with minimal interpretation. These publications were either not ready to be formally published or needed to be quickly created. Open-file studies were approved by the director of the survey. Publications in the Open-File series have been inconsistently named using a variety of titles, including "Open-File Report," "Open-File Map," and "Open-File Study." Prior to 1994, a publication in this series was generally referred to as an "Open-File Report," with some exceptions. To reduce confusion, the IGWS began referring to every publication in the Open-File series as an "Open-File Study." When writing a bibliographic reference for a publication, one should use the series name and number on the publication.
Browse
Browsing Open File Studies - IGWS by Title
Now showing 1 - 20 of 274
- Results Per Page
- Sort Options
Item Abandoned Underground Mines and Hydrologic Conditions Around Cannelburg, Indiana(Indiana Geological & Water Survey, 1991) Harper, Denver; Hartke, Edwin J.; Olyphant, Greg A.Item Amendment to Quality Assurance Project Plan for Potential nonpoint Source Contamination of the Spring Mill Lake Drainage Basin(Indiana Geological & Water Survey, 2001) Hasenmueller, Nancy R.Item Anatomy of the Grainstone Shoal Facies of the Salem Limestone (Mississippian) of Southern Indiana (A Preliminary Report)(Indiana Geological & Water Survey, 1993) Thompson, Todd Alan; Dodd, J.; Petzold, DanielItem Ancient Fresh to Brackish Water Depositional Systems - A Guide to Three Outcrop Examples in Southern Indiana(Indiana Geological & Water Survey, 2000) Kvale, Erik; Mastalerz, MariaItem Aquifer Sensitivity Terrain, LaPorte and Porter Counties, Indiana(Indiana Geological & Water Survey, 1994) Bleuer, Ned K.; Frey, J. D.Item Assessment of levels of lead, arsenic, and other trace elements in the ground water from bedrock aquifers in southern Indiana(Indiana Geological & Water Survey, 1989) Branam, Tracy D.; Carpenter, Stanley H.; Comer, John B.; Ennis, Margaret V.; Hartke, Edwin J.; Hasenmueller, Nancy R.; Rybaczyk, JamesItem Assessment of the 3,000 ppm and 10,000 ppm Total Dissolved Solids Boundaries in the Mississippian and Pennsylvanian Aquifers of Southwestern Indiana(Indiana Geological Survey, 1993) Mitchell, William M.The Indiana Geological Survey (IGS), in cooperation with the Indiana Department of Natural Resources' Division of Oil and Gas, conducted a study of Mississippian and Pennsylvanian aquifers in southwestern Indiana to identify and depict the 3,000 and 10,000 ppm total dissolved solids (TDS) boundaries. Those boundaries, particularly the 10,000 ppm TDS level, are used to define the limits of aquifers denoted as Underground Sources of Drinking Water (USDW); under current federal regulations those aquifers are subject to protective measures to prevent contamination. The Indiana Division of Oil and Gas, as the primary state agency concerned with ensuring that USDWs are protected from contamination by the activity of the petroleum industry, has an ongoing interest to develop a regionally appropriate methodology. These data will facilitate the activity of the Division of Oil and Gas in the permitting and monitoring of various types of injection wells involved in secondary recovery and the subsurface disposal of oil field waters (Class II wells). Maps that show the structural configuration of the critical TDS boundaries within the petroleum-producing counties of southwestern Indiana, therefore, are highly useful. The TDS values for individual formations were obtained from two sources: actual brine samples, and from calculations utilizing resistivity and porosity readings from geophysical surveys that were run in petroleum industry wells. The data provided by over 2,500 oil and gas industry wells and approximately 10,000 individual-formation TDS calculations were used to make isosalinity maps. Maps depicting the elevations of the 3,000 and 10,000 ppm TDS boundaries were generated using the interpolated data from the log calculations and from brine samples. Five boreholes ranging from 449 ft to 609 ft were drilled and cored to calibrate the log evaluation techniques used. Each corehole was logged with a resistivity tool and a neutron/density device, which providing the same type of borehole evaluation data that was derived from petroleum industry wells used for calculation. TDS calculations were made from the logs on selected formations penetrated by the coreholes. The same zones were isolated by inflatable straddle packers, and actual samples of the formation waters were brought to the surface by a compressed-air operated pump. The water samples from 13 zones were analyzed using for TDS levels two different lab techniques and compared to log-derived calculated TDS values. None of the zones tested exceeded measured TDS levels of 2,000 ppm. The methodology was designed for saline fluids; the relatively low TDS levels and the presence of gas are though to be responsible for the reduced correlation found in the remaining fifty percent. The study demonstrated that TDS values derived from geophysical log can be used to predict salinity trends with reasonable reliability; however, exact TDS concentrations cannot be as reliably determined from log-derived data alone when formation fluids having salinities less than 5,000 ppm are present. It was also demonstrated that the 3,000 and 10,000 TDS ppm surfaces form generally basinward dipping surfaces that are much more irregular than anticipated. The 3,000 and 10,000 TDS surfaces occur in southwestern Indiana at greater depths than expected. Numerous salinity anomalies and salinity reversals or inversions were observed to exist within the study are. Those salinity anomalies and inversions can indicate several conditions, including the upwelling of deep fluids, faulting, and/or the circulation of more shallow subsurface fluids, and perhaps even the mixing of surface waters and the subsequent introduction into deep aquifers that normally would contain fluids of higher TDS levels.Item Assessment of the 3000 ppm and 10000 ppm Total Dissolved Solids Boundaries in Mississippian and Pennsylvanian Bedrock Aquifers of Southwestern Indiana(Indiana Geological & Water Survey, 1994) Branam, Tracy D.; Comer, John B.; Ennis, Margaret V.Item Assessment of the Quality of Indiana Coals for Integrated Gasification Combined Cycle (IGCC) Performance(Indiana Geological & Water Survey, 2005) Drobniak, Agnieszka; Mastalerz, Maria; Rupp, John A.; Shaffer, Nelson R.Item Assessment of the quality of Indiana coals for integrated gasification combined cycle (IGCC) performance-final report(Indiana Geological & Water Survey, 2009) Drobniak, Agnieszka; Mastalerz, Maria; Rupp, John A.; Shaffer, Nelson R.Item Atlas of anthropogenic particles(Indiana Geological & Water Survey, 2006) Drobniak, Agnieszka; Mastalerz, MariaItem Atlas of Hydrogeologic Terrains and Settings of Indiana(Indiana Geological & Water Survey, 1995) Brown, Steven E.; Fleming, Anthony H.; Harper, Denver; Powell, Richard L.; Rupp, Robin F.; Herring, William C.; Bonneau, Philip; Grove, Glen; Lewis, Eric S.; Moeller, Angela J.; Reehling, Peter; Steen, WilliamItem The availability of the Seelyville Coal Member for mining in Indiana(Indiana Geological & Water Survey, 2001) Conolly, CarolItem The availability of the Springfield Coal Member for mining in Indiana(Indiana Geological & Water Survey, 1999) Conolly, Carol; Zlotin, AlexItem The Availibility of the Danville Coal Member for Mining in Indiana(Indiana Geological Survey, 2000-06) Conolly, Carol L.; Zlotin, AlexThis study assesses the resources of the Danville Coal Member in Indiana and identifies those resources that have the most favorable geologic and land use characteristics for mining. The tonnage of original coal in place, remaining coal after mining, coal unlikely to be mined due to geologic and land use factors, and available coal resources were calculated for the Danville Coal in Indiana. The geologic and land use factors which restrict the mining of the Danville Coal were identified through interviews with geologists and mining engineers mining the Danville Coal in Indiana and Illinois. These restrictions were applied to the tonnage of remaining Danville Coal resources in order to calculate the tonnage of available resources. The original, remaining, and available coal resources are reported in terms of potential method of mining, "surface" or "underground," coal thickness, "14-28 inches," "28-42 inches," or "greater than 42 inches," and overburden thickness, "0-200 feet," and "greater than 100 feet." Coal that lies between depths of 100 and 200 feet is considered minable by both surface and underground methods. Additionally, the resources are categorized by three levels of geologic assurance or reliability. The reliability categories express the degree of reliability of the resource estimate based on the density of coal thickness data points that are used to derive the resource estimate. The three reliability categories are: measured (0-0.5 miles from the data point), indicated (0.5-2.0 miles), and inferred (2.0-4.0 miles). The total volume of original Danville Coal resources in Indiana is calculated to be 6.55 billion short tons. Of the 6.55 billion short tons, 0.36 billion short tons have been removed by mining or lost in the mining process, thus leaving 6.19 billion short tons of remaining Danville resources. Technological and land use restrictions remove 5.36 billion short tons from potential mining, leaving 0.83 billion short tons (13% of the original resources or 13% of the remaining resources) available for mining in Indiana. Of the 0.83 billion short tons of total available resources, 0.52 billion tons (8% of the original resources or 63% of the total available resources) are available for underground mining, while 0.31 billion short tons (5% of the original resources or 37% of the total available resources) are available for surface mining.Item Bedrock Facies Controls on Potential Constituent Migration-Pathways and Barriers, Landfill and Sludge Application Sites(Indiana Geological & Water Survey, 1995) Kvale, ErikItem Bedrock geologic map of the Indianapolis 30 X 60 minute quadrangle, central Indiana(Indiana Geological & Water Survey, 2003) Hasenmueller, Walter A.; James, Christina L.Item Bedrock geologic map of the Lafayette 30 X 60 minute quadrangle, central Indiana(Indiana Geological & Water Survey, 2003) Hasenmueller, Walter A.; James, Christina L.Item Bedrock geologic map of the southwestern portion of the Wabash 30 X 60 minute quadrangle, Indiana(Indiana Geological & Water Survey, 2004) Hasenmueller, Walter A.Item Bedrock geologic map of the west half of the Muncie 30 X 60 minute quadrangle, central Indiana(Indiana Geological & Water Survey, 2003) Hasenmueller, Walter A.; James, Christina L.