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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
Fields
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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" ~~~ <br />levels in piezometers or conduits would be above static water levels in <br />the overlying ground-water aquifer. Operating pressures can then be <br />stipulated which would limit this area to a size that presents accept- <br />ably small risks or is monitorable. <br />The size of the critical area should be determined by the methods <br />outlined in Chapter 5. An important requirement is the quantification <br />of the hydraulic properties of the disposal zone. The applicant would <br />be responsible for conducting tests to determine these properties. This <br />need not be done if the applicant is willing to accept a low operating <br />fluid level, such as the base of fresh water or lower, that could be <br />stipulated based on expectation of worst-case conditions. If the appli- <br />cant desires the maximum prudent operating fluid level or pressure, he <br />would accept the responsibility for gathering the data necessary for <br />determination of that limit in a technically sound manner. <br />Uell tests would have to be carefully conducted in order to define <br />the response of the disposal zone to injection. The parameters to be <br />determined include the storativity and flow capacity of the disposal <br />zone. Determination of the storativity will require use of one or more <br />observation wells during the test. The validity of measurements taken <br />in such a well should be confirmed by assuring that the response of the <br />observation well is representative of the reservoir using methods <br />described in Chapter 5. <br />If the hydraulic parameters of the disposal reservoir are known, an <br />initial set of curves of pressure versus distance from the injection <br />well can be constructed for various flow rates by assuming the aquifer <br />is of infinite areal extent. Next, curves can be constructed to depict <br />equivalent water levels for different fluid densities likely to occur in <br />possible conduits through the confining beds. Additional sets of curves <br />122 <br />
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