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suitable material is loaded and hauled around the ends of the pit and is placed on the unsuitable <br />material as a cap, (see Sections 2.05.4(2)(c) Backfilling and Grading and 2.05.4(2)(d) Topsoil <br />Redistribution). The separation of materials (suitable and unsuitable) will help prevent the runoff <br />from more toxic un -oxidized backfill materials from contaminating surface water and place the <br />more toxic percolating ground water (leachate of un -oxidized backfill) below the root zone. <br />It is not anticipated that NHN will transfer ownership or use of any wells completed within NHN <br />permit area. Bore holes, shafts, wells, and auger holes will be cased and/or sealed to prevent <br />possible ground water degradation from the mixing of waters of different quality within the bore <br />holes and acid or toxic surface runoff entering the bore holes. A specific plan for sealing of bore <br />holes, exploration holes, auger holes, wells, and shafts is presented in Section 2.05.6(3)(b)(v), <br />Hydrologic Reclamation Plan. <br />Ground Water Quantity Typical backfilling methods largely involve the use of dozers and <br />trucks (see Section 2.05.4(2)(c), Backfilling and Grading). Replaced spoil materials exhibit <br />greater porosities and hydraulic conductivities because of increased void volumes, regardless of <br />how the spoil material is replaced in the pits. Seepage from the irrigation network has provided <br />an artificial source of recharge to the undisturbed shallow ground water system. Spoil <br />replacement (backfilling) using methods outlined in Section 2.05.4(2)(c), Backfilling and <br />Grading, will allow the infiltration and percolation of storm event water and irrigation water <br />through the backfill. Due to the structural attitude, it is unlikely that the backfill will ever be re - <br />saturated over time. The NHN permit area is located in a semi -arid climate which averages about <br />12.5 inches of precipitation annually, (see Section 2.04.8 Climatological Information). <br />Evapotranspiration rates in the vicinity are relatively high (see Section 2.04.7, Hydrology <br />Description). Textural analyses performed on potential backfill materials generally indicate that <br />sandy clay loam materials will be replaced in the pits (see Section 2.04.6, Geology Description). <br />Consequently, infiltration rates in reclaimed areas are expected to be slow to moderate which <br />will help water retention in the topsoil and sub -soil. However, the upstream and downstream <br />(above and below the 2nd Park Lateral diversion) irrigation ditches and laterals will continue to <br />recharge the bedrock zones. Again, the irrigation network has provided an artificial source of <br />recharge to the Dakota Formation coal strata bedrock zones in the NHN permit area. <br />Overburden and topsoil handling, reconditioning, and revegetation methods (outlined in Sections <br />2.05.4(2)(d), Topsoil Redistribution, and 2.05.4(2)(e), Revegetation,) will maximize the potential <br />for establishing reclaimed areas that will exhibit infiltration rates and capacities adequate for <br />insuring at least pre -mining rates and capacities. Timely reseeding and mulching of redistributed <br />topsoil will augment the retention and eventual downward infiltration of soil moisture. Textures <br />of topsoil material will generally range from sandy loam to loam, and topsoil material will <br />exhibit moderate infiltration rates. Deep ripping of re -graded backfill material, followed by <br />topsoil placement, chisel plowing, and disking will improve the infiltration potential of the <br />Section 2.05.6(3) Page 3 April 2016 (PR -01) <br />