Laserfiche WebLink
Ms.Kaie Pickford <br />Division Of Minerals and Geology <br />October 8, 2003 <br />Page 3 oj4 <br />Wells identified as domestic use are located east and southwest of the' existing permit <br />boundary. However, wells listed as domestic use in this particular area are not typically used <br />for drinking water purposes since other domestic water supplier taps are available. <br />Additionally, it is believed that the local groundwater gradient is towards the north and the <br />Cache la Poudre River. Domestic wells near the future groundwater lake are, therefore, <br />up-gradient or cross-gradient from the lake. <br />4. Since the stormwater drain is not yet constructed, no surface water runoff is available for <br />analysis. The potential surface water runoff quality collected by the drainage system was <br />evaluated in the text of TR-005. Based on City of Greeley programs and practices For <br />stormwater quality protection, the watershed characteristics, and the design of the stormwater <br />channel itself, it is anticipated that stonnwater delivered to the future groundwater lake will <br />not significantly impact surface water or groundwater quality. <br />The City of Greeley recently applied for coverage under the Colorado Phase II Municipal <br />Stormwater Discharge Permit. The measures under this permit include public education and <br />outreach, public participation/involvement, illicit discharge detection and elimination, <br />construction site stormwater runoff control, post-construction stormwater management, and <br />pollution prevention/good housekeeping for municipal operations. Once applied, these <br />measures have been shown to significantly reduce most pollutant concentrations in urban <br />runoff. It should also be noted that the City of Greeley operates separate stormwater and <br />domestic sewer systems. Therefore, during major storm events, there is no possibility of <br />domestic sewer overflow into the stonnwater channel entering the site. <br />Additionally, the groundwater lake will only receive stormwater flows that exceed the 5-year <br />stormwater runoff event (please reference the North Eagleview Regional Detention Pond <br />Concept Phase Report). Base flows from the stormwater drain system and flows from more <br />frequent minor stonnwater events would not flow irito the future groundwater lake. These <br />base flows and frequent minor stormwater flows typically contain the highest concentrations <br />of potential contaminants. During major stormwater events, such as those that would be <br />expected to reach the future groundwater lake, the concentration of potential contaminants in <br />stormwater runoff is significantly reduced by the large volume of stormwater produced. <br />During major stonnwater events, stonnwater flows entering the future groundwater lake will <br />be passed through the lake. The lake is not intended to provide a major source of <br />groundwater recharge: It is predicted that during the 100-year stormwater event, the lake <br />surface will only rise 2.5 feet and will return to the normal surface elevation within days <br />(please reference the North Eagleview Regional Detention Pond Concept Phase Report and <br />North Eagleview Regional Detention Pond Design Report). The limited amount of time that <br />the lake surface elevation is above the surrounding groundwater table will significantly limit <br />the amount of surface water recharging the local groundwater from the lake. <br />5. Adjacent landowners are provided on the attached Figure l . <br />