2018
DOI: 10.12911/22998993/89658
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Water Reservoirs as an Element of Shaping Water Resources of Post-Mining Areas

Abstract: The aim of the study was to present the concepts of water reclamation and development of post-mining areas of the Adamów Lignite Mine following the termination of its excavating operation. The reclamation procedures will accelerate the process of restoring the devastated post-mining area to the natural environment and, above all, will contribute to the increase in local water resources. Several water reservoirs with different surface areas and capacities within the final excavations of opencasts were created. … Show more

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Cited by 9 publications
(12 citation statements)
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“…(approximately 60 years (Table 2, Figure 5) with an average net supply of 138.5 m 3 •d −1 (Table 2, Figure 4A), only slightly higher than the average calculated supply (101.8 m 3 •d −1 (Table 2, Figure 4A) from the physiographic direct catchment) points to difficult hydrogeological conditions (which are confirmed in the geological documentation of the deposit [112]) and the fact that the quarry is supplied with rainwater from a direct catchment with a non-existent groundwater supply. Considering the cubic capacity of the pit (~5.1 million m 3 , potentially~3.34 million m 3 of retained water), this confirms the cases featuring the spontaneous filling of an open excavation pit with water over several years to several decades, as discussed in the literature [3,25,36,54,59,70,91,117]. For example, it is prognosed that the natural filling of the water reservoirs in the Bełchatów mine may take about 60 years, and if additional water is supplied from outside the depression bowl, it may take 18 years [71].…”
Section: Resultssupporting
confidence: 78%
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“…(approximately 60 years (Table 2, Figure 5) with an average net supply of 138.5 m 3 •d −1 (Table 2, Figure 4A), only slightly higher than the average calculated supply (101.8 m 3 •d −1 (Table 2, Figure 4A) from the physiographic direct catchment) points to difficult hydrogeological conditions (which are confirmed in the geological documentation of the deposit [112]) and the fact that the quarry is supplied with rainwater from a direct catchment with a non-existent groundwater supply. Considering the cubic capacity of the pit (~5.1 million m 3 , potentially~3.34 million m 3 of retained water), this confirms the cases featuring the spontaneous filling of an open excavation pit with water over several years to several decades, as discussed in the literature [3,25,36,54,59,70,91,117]. For example, it is prognosed that the natural filling of the water reservoirs in the Bełchatów mine may take about 60 years, and if additional water is supplied from outside the depression bowl, it may take 18 years [71].…”
Section: Resultssupporting
confidence: 78%
“…The prognosed retention capacity of the Strzelin I granite quarry (~3.3 million m 3 ), as well as the capacity of the potential Strzelin quarry lake that would emerge as a result of connecting the Strzelin I and II pits (~6.6 million m 3 ) [23], correspond with the capacity of the water reservoirs that emerged in mines of solid rock materials [42,53,60] or pit lakes created in the Adamów lignite mine (i.e., smaller reservoirs created in the area) [71,117]. It should be noted that a major part of the pit lakes presented in the literature refers to coal and lignite mines, and the capacity of water retained in such lakes reaches 30-60 million m 3 [20,89], quite often exceeding 100 million m 3 [20,41,57,91,117], even up to 330-350 million m 3 [55,61]. The prognosed capacity of the water reservoirs that are planned to be created in the lignite mine "Bełchatów" after discontinuation of its operations is expected to reach 1.3 and 1.7 billion m 3 , and in the "Turów" lignite mine, 1.2 billion m 3 [70,71].…”
Section: Resultsmentioning
confidence: 99%
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