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PERMFILE55889
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PERMFILE55889
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Entry Properties
Last modified
8/24/2016 10:58:35 PM
Creation date
11/20/2007 4:48:10 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1999002
IBM Index Class Name
Permit File
Doc Date
6/18/1999
Doc Name
OBJECTORS EXHIBITS
Media Type
D
Archive
No
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. 1 ~ • <br />~~~ <br />graphical and hydraulic character of each unique project. Adoption of <br />standardized rules in some of the above areas appears to result in <br />inadequate protection in some cases and may cause undue restraint in <br />others. We recommend that MOE consider making chanyes in the review <br />process of items (1), (3), and (4) above. These changes are described <br />below. <br />6.5 Proposed Modifications to Present Rules and Procedures <br />6.5.1 Operatiny Fluid Levels; It is proposed that MUE consider <br />some modification of the methods it uses to determine the operatiny <br />pressures for individual infection wells. The maximum allowable operat- <br />iny fluid level is presently set at the elevation of the land surface at <br />the wellhead in the case of the two wells presently operating. A5 <br />described in Chapter 5, aliowiny this operating level may, in some <br />cases, involve some risk that injected or native brines could move <br />upward in conduits throuyn the confininy beds and into underground <br />sources of drinkiny water. (Insufficient data are available to deter- <br />mine if this is true at presently operatiny wells.) This rule does not <br />consider the density of the fluid in the wellbore, with the result that <br />the maximum allowable bottom-hole pressure corresponds to the pressure <br />that could be yenerated by a column of salt-saturated brine with a <br />specific yravity of approximately 1.2, or up to 2UX more pressure than <br />wouto exist at the base of a column of fresh to brackish water. <br />Since, in a worst-case situation, this operatiny level could yener- <br />I ate fluid levels in the disposal zone SU to lU0 feet (15 to 3U m) above <br />land surface, it is important to perform a more detailed analysis of <br />' local conditions to determine the likelihood that this could occur, and <br />in what size area, in order to yauye the possible effects on local <br />ground-water resources. We propose that the object of such an analysis <br />be the determination of the size of the "critical area" where water <br />1'l l <br />
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