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• <br /> Marton <br /> County <br /> OREGON <br /> Marion County Building Inspection <br /> 5155 Silverton Rd.NE <br /> Salem, Oregon 97383 <br /> Prepared For: <br /> Patrick Bartshe <br /> 127 Gates Hill Rd. SE <br /> Gates, Oregon 97383 <br /> 093E27DA01100 <br /> Winter Water Monitoring Summary <br /> Test Pits were observed on June 5 and June 12, 2018 in response to an application for a Site <br /> Evaluation at 127 Gates Hill Road SE, Gates. An observation concluded that the soil in the pits <br /> showed evidence of a permanent water table at a depth that was unable to be determined at the <br /> time. The site required winter water monitoring to ensure that the site was capable of septic <br /> approval. <br /> Methods Used: <br /> Ports approximately 12" in diameter were prepared and backfilled with gravel surrounding a 3" <br /> perforated length of pipe. The ports were approximately 5-6 feet deep and had risers above the <br /> surface open for inspection. The ports were within 6" of elevation difference. Twice a week, <br /> beginning in early November, 2018 and ending on April 29, 2019, an agent from Marion County <br /> observed the height of the water in the observation ports. Weather data was gathered from <br /> NOAA's weather.gov website and recorded in 72 hour increments preceding each visit. For <br /> further detail, please refer to the table and graph that accompany this report. The soil observed <br /> in the ports fell into Soil Group C, Per OAR 340-071-0220 table 5 (Silty Clay—Sandy Clay). <br /> Per OAR 340-071-0290(2)(b)(A)(iii),the permanent water table must have remained at a depth <br /> of 24" or greater for approval of any type. <br /> Conclusions: <br /> Aside from major precipitation events,the level of the water was not observed to be at denial <br /> depth in either port. Port#2 averaged a slightly deeper depth to the water by about 1.5 inches. <br /> The geographical area experienced slightly below average precipitation for the season, with peak <br /> events in late December and early April. This data allowed us to conclude that the permanent <br /> water table is evident around 30"below the surface, which correlates with the redoximorphic <br /> features originally observed in both test pits near similar levels. <br />