My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WSP01088
CWCB
>
Water Supply Protection
>
Backfile
>
1001-2000
>
WSP01088
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 12:29:17 PM
Creation date
10/11/2006 10:09:51 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8112.600
Description
Arkansas White Red Basins Interagency Committee - AWRBIAC -- Reports
Basin
Arkansas
Water Division
2
Date
6/1/1977
Title
Specific Problem Analysis Summary Report - 1975 National Assessment of Water and Related Land Resources - Part 2 of 2
Water Supply Pro - Doc Type
Report/Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
84
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br />I <br />I <br /> <::> <br />II (-, <br />-' <br />N <br />W <br /> "'-I <br />I N <br />I <br />I' <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />for private wells in the area. Wells range in depth from less than <br />100 to 400 feet. Recharge is direct through soil and limestone bed- <br />rock, as well as through sinkholes and losing stretches of streambeds. <br /> <br />The "deep" aquifer is separated from the shallow aquifer by <br />a layer of silts and shales which retard the downward movement of <br />water and acts as thp. u~ppr r0~fi~i~g l~y~r tG the d~~p aquif~L. <br />The deep aquifer is OVer 1000 feet thick and consists mainly of <br />dolomites. In only a few places is this deep squifer exposed at <br />the surface. Water recharging the deep aquifer must either pass <br />first through the shallow aquifer, then slowly through the confin- <br />,ing layer of silts and clays by lateral movement in the deep aquifer. <br /> <br />The quality 09 the groundwater and surface water in the area <br />is generally good. <br /> <br />Springfield utilizes stream impoundments and a spring in the <br />Sac River Basin for most of its domestic supply. Municipal wells, <br />owned by the City of Springfield, and industrial wells in and <br />adjacent to Springfield have maximum depths of 1400 feet. Yields <br />in excess of 1000 g.p.m. with no more than 100 feet of drawdown <br />are common. Table 8 shows water use in the area. <br /> <br />Industries, municipalities, public-water-supply districts, <br />subdivisions, and rcral homes in the Springfield area are all <br />dependent in some measure upon water from wells Or springs. <br /> <br />Missouri uses the Riparian Rights, modified by reasonable <br />use and natural flow as the basis for ground and surface water <br />administration. To protect shallow and deep groundwater forma- <br />tions, the stste requires wells to be cased. Private (residential) <br />wells are to be cased to a depth of'at least 80 feet with schedule <br />40 plastic pipe, 6", 13 Ib./ft. steel casing, or equivalent. Rock <br />wells producing over 30 g.p.m. must be constructed to stated stan- <br />dards which includes the use of 19# per foot steel pipe or equiva- <br />lent casing installed to a depth determined for each well by the <br />Division of Geology and Land Survey, Department of Natural Resources. <br />The casing must be pressure grouted through total length. <br /> <br />State law requires water supply facility plsns and designs <br />be approved by the Department of Natural Resources before con- <br />struction. <br /> <br />Application of Public Law 92-500, the Federal Water Quality <br />Act Amendment of 1972, and the Missouri Clean Water Law of 1972, <br />seek to reduce, if not eliminate, effluent discharges which <br />cause water to be less than suitable for swimming and fish habitat. <br /> <br />88 <br />
The URL can be used to link to this page
Your browser does not support the video tag.