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s) <br />Pearson Place <br />Ramsey, Minnesota <br />NTI Project No. 17.62064.100 <br />Redoximorphic soil features (soil staining) was obscured due to the heavy irrigation in the farm field. <br />We anticipate that the seasonal high groundwater would be comparable to this level, however, due to <br />the above average precipitation over the year as well as inputs from irrigation. <br />2.4 Laboratory Test Program <br />Our analysis and recommendations within this report are based upon our interpretation of the sampled <br />soils, laboratory test results, and experience with similar soils from other sites near the project. The <br />results of such tests are summarized on the boring logs or attached laboratory test reports. <br />2.5 Infiltration Test Results <br />In total, two (2) DRI tests were completed (see appendix for location). Test #1 was completed approximately <br />3 feet below existing grade, just below the agricultural till layer. In general accordance with the Minnesota <br />Pollution Control Agency Stormwater Manual, and the results of our DRI test, the design infiltration rate for <br />this test depth was found to be 0.25 inches per hour. Test #2 was completed approximately 5 feet below <br />existing grade. In general accordance with the Minnesota Pollution Control Agency Stormwater Manual, and <br />the results of our DRI test, the design infiltration rate for this test depth was found to be 1.5 inches per hour. <br />NTI perform an additional test on September 1, 2017. The design infiltration rate for that test was found to <br />be 2.75 inches per hour. The MPCA recommends using an average of values for tests in the same stratum. <br />The average would be approximately 2 inches per hour. <br />2.6 Low Floor Elevation <br />As mentioned above, we encountered groundwater at elevations of 848.5 and 849. Redoximorphic features <br />(soil staining) were obscured by the heavy irrigation that occurred during the farming process; however, due <br />to the relatively wet year and regular irrigation, we anticipate that this elevation will be similar to the <br />seasonal high water elevation. It is our opinion that a low floor elevation of 854 would provide a sufficient <br />buffer (at least 5 feet) against transient groundwater conditions. <br />Page 2 of 3 <br />