Leslie D. Arihood (Former Employee)
Science and Products
Filter Total Items: 32
Hydrogeology and paths of flow in the carbonate bedrock aquifer, northwestern Indiana Hydrogeology and paths of flow in the carbonate bedrock aquifer, northwestern Indiana
The U.S. Geological Survey (USGS) is assessing the ground.water resources of the carbonate bedrock aquifers in Indiana and Ohio as part of their Regional Aquifer Systems Analysis program. Part of this assessment includes the determination of unknown aspects of the hydraulic characteristics, boundaries, and flow paths of the carbonate aquifer. To accomplish this, the USGS drilled three...
Authors
Leslie D. Arihood
Method for estimating low-flow characteristics of ungaged streams in Indiana Method for estimating low-flow characteristics of ungaged streams in Indiana
Equations for estimating the 7-day, 2-year and 7oday, 10-year low flows at sites on ungaged streams are presented. Regression analysis was used to develop equations relating basin characteristics and low-flow characteristics at 82 gaging stations. Significant basin characteristics in the equations are contributing drainage area and flow-duration ratio, which is the 20-percent flow...
Authors
Leslie D. Arihood, Dale R. Glatfelter
Sedimentation in Versailles Lake, Ripley County, southeastern Indiana, 1956-88 Sedimentation in Versailles Lake, Ripley County, southeastern Indiana, 1956-88
Sedimentation has affected the storage capacity and surface area of Versailles Lake. The lake was constructed by damming Laughery Creek in 1956. At the dam, the drainage area of Laughery Creek is 168 square miles. Locations where the largest amount of sediment has accumulated for the 32-year period 1956-88, are in the upper end of the lake where Laughery Creek enters and in the middle...
Authors
D.E. Renn, L. D. Arihood
Evaluation of a watershed model to simulate sediment transport in a small agricultural watershed in Indiana Evaluation of a watershed model to simulate sediment transport in a small agricultural watershed in Indiana
The streamflow and sediment components of the watershed model, ' Hydrologic Simulation Program-Fortran ', were evaluated using 2 years and 9 months of data from a 2.7-sq mi agricultural watershed in Indiana. Hydrographs of simulated sediment concentration generally have smaller peaks and longer recessions than do hydrographs of measured data. The attenuation of simulated peaks was partly...
Authors
L. D. Arihood
Preliminary analysis of the shallow ground-water system in the vicinity of the Grand Calumet River/Indiana Harbor Canal, northwestern Indiana Preliminary analysis of the shallow ground-water system in the vicinity of the Grand Calumet River/Indiana Harbor Canal, northwestern Indiana
The shallow groundwater system in the vicinity of the Grand Calumet River-Indiana Harbor Canal, Indiana was analyzed from June 1985 to May 1986. This analysis was done to obtain detailed information about the physical characteristics of the Calumet aquifer and the shallow groundwater flow system. 36 shallow wells were installed and sediment samples were collected at 26 sites. Water level
Authors
Lee R. Watson, R. J. Shedlock, K. J. Banaszak, L. D. Arihood, P. K. Doss
Science and Products
Filter Total Items: 32
Hydrogeology and paths of flow in the carbonate bedrock aquifer, northwestern Indiana Hydrogeology and paths of flow in the carbonate bedrock aquifer, northwestern Indiana
The U.S. Geological Survey (USGS) is assessing the ground.water resources of the carbonate bedrock aquifers in Indiana and Ohio as part of their Regional Aquifer Systems Analysis program. Part of this assessment includes the determination of unknown aspects of the hydraulic characteristics, boundaries, and flow paths of the carbonate aquifer. To accomplish this, the USGS drilled three...
Authors
Leslie D. Arihood
Method for estimating low-flow characteristics of ungaged streams in Indiana Method for estimating low-flow characteristics of ungaged streams in Indiana
Equations for estimating the 7-day, 2-year and 7oday, 10-year low flows at sites on ungaged streams are presented. Regression analysis was used to develop equations relating basin characteristics and low-flow characteristics at 82 gaging stations. Significant basin characteristics in the equations are contributing drainage area and flow-duration ratio, which is the 20-percent flow...
Authors
Leslie D. Arihood, Dale R. Glatfelter
Sedimentation in Versailles Lake, Ripley County, southeastern Indiana, 1956-88 Sedimentation in Versailles Lake, Ripley County, southeastern Indiana, 1956-88
Sedimentation has affected the storage capacity and surface area of Versailles Lake. The lake was constructed by damming Laughery Creek in 1956. At the dam, the drainage area of Laughery Creek is 168 square miles. Locations where the largest amount of sediment has accumulated for the 32-year period 1956-88, are in the upper end of the lake where Laughery Creek enters and in the middle...
Authors
D.E. Renn, L. D. Arihood
Evaluation of a watershed model to simulate sediment transport in a small agricultural watershed in Indiana Evaluation of a watershed model to simulate sediment transport in a small agricultural watershed in Indiana
The streamflow and sediment components of the watershed model, ' Hydrologic Simulation Program-Fortran ', were evaluated using 2 years and 9 months of data from a 2.7-sq mi agricultural watershed in Indiana. Hydrographs of simulated sediment concentration generally have smaller peaks and longer recessions than do hydrographs of measured data. The attenuation of simulated peaks was partly...
Authors
L. D. Arihood
Preliminary analysis of the shallow ground-water system in the vicinity of the Grand Calumet River/Indiana Harbor Canal, northwestern Indiana Preliminary analysis of the shallow ground-water system in the vicinity of the Grand Calumet River/Indiana Harbor Canal, northwestern Indiana
The shallow groundwater system in the vicinity of the Grand Calumet River-Indiana Harbor Canal, Indiana was analyzed from June 1985 to May 1986. This analysis was done to obtain detailed information about the physical characteristics of the Calumet aquifer and the shallow groundwater flow system. 36 shallow wells were installed and sediment samples were collected at 26 sites. Water level
Authors
Lee R. Watson, R. J. Shedlock, K. J. Banaszak, L. D. Arihood, P. K. Doss