Author: Edward Joseph Harvey
Publisher:
ISBN:
Category : Artificial groundwater recharge
Languages : en
Pages : 76
Book Description
Average ground-water conditions have not changed significantly in the Springfield-Salem plateaus section of southern Missouri and northern Arkansas in the past 25 years except in the vicinity of well fields. The amount of ground water pumped is approximately 200 cubic feet per second, which is about 5 percent of the total discharge at the 80 percent point on flow-duration curves for major streams. Ground-water recharge is variable and occurs through sinkholes by infiltration in upland areas of good permeability, and through streambeds that lose flow. Main waterbearing zones lie in the Potosi Dolomite and the lower dolomite and sandstone of the Gasconade Dolomite. Cavernous connections from ground surface to depths as great as 1,500 feet occur in the West Plains area, Mo., and result in deep circulation of water. Municipal well-water in the area often becomes turbid after rainstorms, despite well depths of 1 ,500 feet and 950 to 1,000 feet of pressure-grouted casing. Ground-water movement is generaly north and south from the crest of the Springfield-Salem plateaus, which extend across southern Missouri from the St. Francois Mountains to the southwest. Interbasin diversion of surface- and ground-water flow is common.
Ground Water in the Springfield-Salem Plateaus of Southern Missouri and Northern Arkansas
Author: Edward Joseph Harvey
Publisher:
ISBN:
Category : Artificial groundwater recharge
Languages : en
Pages : 76
Book Description
Average ground-water conditions have not changed significantly in the Springfield-Salem plateaus section of southern Missouri and northern Arkansas in the past 25 years except in the vicinity of well fields. The amount of ground water pumped is approximately 200 cubic feet per second, which is about 5 percent of the total discharge at the 80 percent point on flow-duration curves for major streams. Ground-water recharge is variable and occurs through sinkholes by infiltration in upland areas of good permeability, and through streambeds that lose flow. Main waterbearing zones lie in the Potosi Dolomite and the lower dolomite and sandstone of the Gasconade Dolomite. Cavernous connections from ground surface to depths as great as 1,500 feet occur in the West Plains area, Mo., and result in deep circulation of water. Municipal well-water in the area often becomes turbid after rainstorms, despite well depths of 1 ,500 feet and 950 to 1,000 feet of pressure-grouted casing. Ground-water movement is generaly north and south from the crest of the Springfield-Salem plateaus, which extend across southern Missouri from the St. Francois Mountains to the southwest. Interbasin diversion of surface- and ground-water flow is common.
Publisher:
ISBN:
Category : Artificial groundwater recharge
Languages : en
Pages : 76
Book Description
Average ground-water conditions have not changed significantly in the Springfield-Salem plateaus section of southern Missouri and northern Arkansas in the past 25 years except in the vicinity of well fields. The amount of ground water pumped is approximately 200 cubic feet per second, which is about 5 percent of the total discharge at the 80 percent point on flow-duration curves for major streams. Ground-water recharge is variable and occurs through sinkholes by infiltration in upland areas of good permeability, and through streambeds that lose flow. Main waterbearing zones lie in the Potosi Dolomite and the lower dolomite and sandstone of the Gasconade Dolomite. Cavernous connections from ground surface to depths as great as 1,500 feet occur in the West Plains area, Mo., and result in deep circulation of water. Municipal well-water in the area often becomes turbid after rainstorms, despite well depths of 1 ,500 feet and 950 to 1,000 feet of pressure-grouted casing. Ground-water movement is generaly north and south from the crest of the Springfield-Salem plateaus, which extend across southern Missouri from the St. Francois Mountains to the southwest. Interbasin diversion of surface- and ground-water flow is common.
Ground Water in the Springfield-Salem Plateaus of Southern Missouri and Northern Arkansas
Ground Water in the Springfield-Salem Plateaus of Southern Missouri and Northern Arkansas
Geohydrology of the Ozark Plateaus Aquifer System in Parts of Missouri, Arkansas, Oklahoma, and Kansas
Author: Jeffrey L. Imes
Publisher:
ISBN:
Category : Aquifers
Languages : en
Pages : 140
Book Description
Publisher:
ISBN:
Category : Aquifers
Languages : en
Pages : 140
Book Description
Water-resources Investigations
Environmental and Hydrologic Setting of the Ozark Plateaus Study Unit, Arkansas, Kansas, Missouri, and Oklahoma
Selected Water Resources Abstracts
Monthly Catalog of United States Government Publications
Geraghty & Miller's Groundwater Bibliography, Fifth Edition
Author: Frits van der Leeden
Publisher: CRC Press
ISBN: 1000674657
Category : Technology & Engineering
Languages : en
Pages : 526
Book Description
This bibliography reflects the tremendous growth of interest in groundwater, which has occurred in recent years, dealing with a particular aspect of the field of hydrogeology. It will be helpful to those searching for information on management and protection of the groundwater resource.
Publisher: CRC Press
ISBN: 1000674657
Category : Technology & Engineering
Languages : en
Pages : 526
Book Description
This bibliography reflects the tremendous growth of interest in groundwater, which has occurred in recent years, dealing with a particular aspect of the field of hydrogeology. It will be helpful to those searching for information on management and protection of the groundwater resource.