Author: Michael J. KleeschultePublisher:
ISBN:
Category : Mine drainage
Languages : en
Pages : 21
Book Description
Ground-water Levels in the Ozark Aquifer Along the Viburnum Trend, Southeastern Missouri, 2001-05
Author: Michael J. KleeschultePublisher:
ISBN:
Category : Mine drainage
Languages : en
Pages : 21
Book Description
Effects of Lead-zinc Mining on Ground-water Levels in the Ozark Aquifer in the Viburnum Trend, Southeastern Missouri
Author: Michael J. KleeschultePublisher:
ISBN:
Category : Lead mines and mining
Languages : en
Pages : 36
Book Description
Discharge of Ground Water Along the Ozark Escarpment in Southeastern Missouri and Northeastern Arkansas
Author: Thomas O. MeskoPublisher:
ISBN:
Category : Groundwater flow
Languages : en
Pages : 20
Book Description
Geohydrology of the Ozark Plateaus Aquifer System in Parts of Missouri, Arkansas, Oklahoma, and Kansas
Author: Jeffrey L. ImesPublisher:
ISBN:
Category : Aquifers
Languages : en
Pages : 140
Book Description
Water-resources Investigations Report
Author: Groundwater-Flow Model of the Ozark Plateaus Aquifer System, Northwestern Arkansas, Southeastern Kansas, Southwestern Missouri, and Northeastern Oklahoma
Author: U.S. Department of the InteriorPublisher: CreateSpace
ISBN: 9781496123930
Category : Reference
Languages : en
Pages : 68
Book Description
To assess the effect that increased water use is having on the long-term availability of groundwater within the Ozark Plateaus aquifer system, a groundwater-flow model was developed using MODFLOW 2000 for a model area covering 7,340 square miles for parts of Arkansas, Kansas, Missouri, and Oklahoma. Vertically the model is divided into five units. From top to bottom these units of variable thickness are: the Western Interior Plains confining unit, the Springfield Plateau aquifer, the Ozark confining unit, the Ozark aquifer, and the St. Francois confining unit. Large mined zones contained within the Springfield Plateau aquifer are represented in the model as extensive voids with orders-of-magnitude larger hydraulic conductivity than the adjacent nonmined zones.
From Precambrian Rift Volcanoes to the Mississippian Shelf Margin
Author: Kevin R. EvansPublisher: Geological Society of America
ISBN: 0813700175
Category : History
Languages : en
Pages : 166
Book Description
"Despite a long history of geologic investigations in the Ozarks, new studies and analyses continue to elucidate our understanding of the complex interconnection between the basement, extensive carbonate platforms, structural overprinting, mineralization, karstification, and hydrology. This guidebook volume highlights a few of these aspects as well as the connection to culture, history, and economic development of the Ozarks region."--Publisher's description.
Effects on Ground-water Levels in the Missouri River Alluvial Aquifer Caused by Changes in Missouri River Stage, Fremont and Monona Counties, Iowa
Author: Keith J. LuceyPublisher:
ISBN:
Category : Groundwater
Languages : en
Pages : 40
Book Description
Environmental and Hydrologic Setting of the Ozark Plateaus Study Unit, Arkansas, Kansas, Missouri, and Oklahoma
Author: Characterization and Modeling of the Ozark Aquifer in Southern Greene County, Missouri
Author: Bradley A. MitchellPublisher:
ISBN:
Category : Groundwater flow
Languages : en
Pages : 138
Book Description
The hydraulic properties of the Ozark aquifer and its upper confining unit were measured as part of the site characterization for the City Utilities Shallow Carbon Sequestration Demonstration Project. The goal was to delineate the cone of depression/capture zone (of any upward leaking CO2) produced by three onsite production wells above the CO2 injection zone and to model future changes in this cone due to increased pumpage in nearby municipal wells. A three month cessation of pumping in two of the three production wells allowed a unique opportunity to measure the aquifer response to the decreased pumping. Aquifer tests yielded limiting transmissivity values of 0.017 to 0.053 ft2/sec. with a median value of 0.029 ft2/sec. and a storativity value centered around 3 x 10-4. Digital model simulations of the steady potentiometric surface closely match measured levels with a calibrated transmissivity of 0.030 ft2/sec and a vertical hydraulic conductivity within the confining unit of 3 x 10-11 ft/sec. Thus, these calibrated values are very consistent with measured values and the calibrated model should provide reasonable estimates of the future capture zone under various pumping scenarios.