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Disposal sites will be selected on a cut by cut basis for each pit to ensure the <br />depth of disposal is at least ten feet less than the depth to the maximum poten- <br />tial water table. 2iezometric surfaces within the pits will be evaluated during <br />future studies and disposal criteria may be modified to reflect this information. <br />Figure 4.3-22 depicts a situation where a backfilled pit cut has filled with water <br />until the water level reaches the elevation of the pit crest at its northern end. <br />At this point, the water will escape by a spring or seep. In actuality, the water <br />table may mound and somewhat exceed the pit crest elevation. The maximum poten- <br />tial extent of this mounding can be mathematically predicted. <br />A flow line passing from a more porous material (backfilled spoils) to a less por- <br />ous material (contiguous undisturbed geologic strata) will obey the law of inci- <br />dence and refraction given by: <br />K, tan a, <br />K tan a2 <br />where K = gpd/ft.2 <br />+ t +t++ +{+ F+ <br />++ ++ <br />} +++ .. <br />++ + <br />+a1 1+ } <br />+ + + <br />+ $}+ ++ + <br />+ +, + <br />K, > kz <br />Therefore, springs or seeps will only develop at .the north end of the pit cuts <br />where the recharge amount exceeds the conducting capacity of the high wall face. <br />7-8-82 <br />4-98 <br />potential ground water level in the lower <br />ends of the pits on the basis of topo- <br />graphy and the pitch of the coal. Figure <br />4.3-22 provides a <br />conceptualization of <br />this determination. As is evident from <br />the figure, spoil <br />trough disposal is <br />• <br />acceptable closer to the north end of the <br />pits than is spoil <br />bench disposal. In <br />turn, spoil bench disposal can be safely used closer to the lower <br />end of the pits <br />than bottom of the pit disposal can. <br />Disposal sites will be selected on a cut by cut basis for each pit to ensure the <br />depth of disposal is at least ten feet less than the depth to the maximum poten- <br />tial water table. 2iezometric surfaces within the pits will be evaluated during <br />future studies and disposal criteria may be modified to reflect this information. <br />Figure 4.3-22 depicts a situation where a backfilled pit cut has filled with water <br />until the water level reaches the elevation of the pit crest at its northern end. <br />At this point, the water will escape by a spring or seep. In actuality, the water <br />table may mound and somewhat exceed the pit crest elevation. The maximum poten- <br />tial extent of this mounding can be mathematically predicted. <br />A flow line passing from a more porous material (backfilled spoils) to a less por- <br />ous material (contiguous undisturbed geologic strata) will obey the law of inci- <br />dence and refraction given by: <br />K, tan a, <br />K tan a2 <br />where K = gpd/ft.2 <br />+ t +t++ +{+ F+ <br />++ ++ <br />} +++ .. <br />++ + <br />+a1 1+ } <br />+ + + <br />+ $}+ ++ + <br />+ +, + <br />K, > kz <br />Therefore, springs or seeps will only develop at .the north end of the pit cuts <br />where the recharge amount exceeds the conducting capacity of the high wall face. <br />7-8-82 <br />4-98 <br />