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<br />o <br />l\) <br />l\.) <br />--l <br /> <br />SUMMARY (Continued) <br /> <br />. <br /> <br />Problem identification and quantification activities were directed <br />at determining the nature and volume of salt loading from Meeker Dome. <br />From data collected during the problem identification and quantification <br />activities, it was hypothesized that an insufficient plug and deteri- <br />orated casing in one of the wells allowed saline water to move verti- <br />cally into near surface aquifer( s) in the Morrison Formation. The <br />saline water moved laterally by gravity flow along the Morrison and <br />Dakota Formations and surfaced in springs and seeps where the Dakota is <br />exposed by the White River. <br /> <br />. <br /> <br />To investigate the flow-mechanism hypothesis, a verification pro- <br />gram was initiated in 1980. The program included the installation of a <br />monitoring network and the cleaning, testing, and plugging of three of <br />the abandoned oil wells. After the last of the three oil wells had been <br />plugged, a significant reduction in ground water levels and flows of <br />springs occurred. Analysis of the monitoring data indicates that the <br />plugging operations conducted in the three wells impeded the hydraulic <br />connection that existed between the shallow and deep aquifers. Further- <br />more, the continuing decline in water levels in the observation wells <br />provides strong evidence that the well plugs are still intact. The <br />effect of well plugging is depicted on the following page. <br /> <br />The verification activities confirmed that deep exploratory oil <br />wella provided the corridors through which saline water under pressure <br />was escaping to surface formations and flowing into the White River. <br />The first year after completion of verification activities, salt load- <br />ing from the dome was reduced about 74 percent from preplugging levels, <br />with a total reduction of 15,800 tons. This salt loading reduction <br />represents a decrease in salinity of the Colorado River at Imperial Dam <br />of about 1.6 milligrams per liter (mg/L) at an annual cost of $149,000 <br />per mg/L. The cost effectiveness of the Meeker Dome Unit is compared <br />with the Grand Valley and Lower Gunnison Basin Units in the table on <br />page S-4. <br /> <br />. <br /> <br />Before the 1981 plugging of the three wells, the salt loading from <br />the area was estimated at 21,400 tons annually with a 2.2-mg/L effect at <br />Imperial Dam. After plugging, the salt loading was reduced to 5,600 <br />tons per year or a salinity effect of 0.6 mg/L. The salinity reduction <br />value of 1.6 mg/L attributed to the Meeker Dome Unit is the difference <br />between the 2.2-mg/L prep lugging level and the O.6-mg/L postplugging <br />level. It is possible that had the 1981 plugging not been undertaken, <br />the salt loading from the dome would have eventually returned to the <br />pre-1968 condition when salt loading from the dome was estimated at <br />about 57,000 tons annually with a salinity effect of about 5.8 mg/L. If <br />the 1981 plugging proves totally effective and the annual salt loading <br />value becomes 0, then it could be argued that the combined effect of <br />both plugging efforts (1968 and 1981) could be 57,000 tons with a reduc- <br />tion in salinity at Imperial Dam of 5.8 mg/L. <br /> <br />., <br /> <br />Costs of the Meeker Dome investigations were $2,870,000 through <br />fiscal year (FY) 1983. It is estimated that an additional $160,000 will <br />be needed to complete monitoring activities and a final report. The <br /> <br />5-2 <br />