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Figure 5 — Drawdown in Observation Well 8 <br />840 <br />E 835 <br />c0 <br />c <br />00 830 <br />c <br />w <br />825 <br />a) <br />J <br />L <br />C 820 <br />> <br />815 <br />Drawdown in Observation Well 8 <br />-2400 feet from pumping well (Well 7) <br />October 19, 2019 <br />CO CO CO CO CO CO CO O CO CO CO CO CO CO O O N- O co O O CO 00 O COT- CO O CO CO 0 T- O CO O CO O M O O O O <br />71- 71-Lf) Li) Li) O O T- T N N 00 00 Li) Lf) Li) O LID O O O T- T- T- T N N 00 M M OD Li) Lf) Li) O O <br />.. CO.. .. .. .. .. .. .. .. .. .. .. .. .. <br />O co 00 00 O O f` Lf) In M M O) O) N- N- N- Ln LO O 00 7tN N N 0 0 0 00 00 00 O O O 7t,( N M T- <br />L00000MNNN OOOLOCOMNNN,-,-,-OOOLO00Lf) NNN OOOLf)00 <br />.. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. <br />f` 00 00 00 O d) O O O T- r T- N N 00 00 00 ,r O O O O LO LO O O O N- N- N- 00 00 00 d) d) O) O) d) O <br />N <br />Time <br />During the course of Well 7 pumping, Well 8 at a distance of 2,400 feet observed approximately 6 <br />to 9 feet of d rawdown . <br />The Theis equation predicts a cone of depression approximately 2,448 feet from pumping well 7. <br />Theis Equation for the City of Ramsey <br />Time = <br />0.5 <br />days <br />Theis W(u) Function <br />0.752 <br />unitless <br />Drawdown = <br />6 <br />ft <br />Transmissivity = <br />11493 <br />gpd/ft <br />Pumping Rate = <br />800 <br />gpm <br />Theis u variable = <br />0.390 <br />unitless <br />r2 = 4Ttu 4S <br />Storativity = <br />0.0002 <br />unitless <br />Radius rounded for <br />map <br />2400 <br />ft <br />These results indicate that a single well pumping at current well field spacing does not induce <br />mutual well interference. This 6-foot cone of depression is depicted on Figure 11. <br />However, complexities arise as present-day conditions see the use of 3 to 5 concurrent wells, <br />and a 2040 demand increasing up to a projected 500% daily maximum demand. In order to <br />model these scenarios and their resulting cone of depressions a groundwater model was <br />developed. <br />FEASIBILITY STUDY RAMSY 154354 <br />Page 22 <br />