2017
DOI: 10.1007/s10230-017-0505-x
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A Spatial Mixing Model to Assess Groundwater Dynamics Affected by Mining in a Coastal Fractured Aquifer, China

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Cited by 18 publications
(8 citation statements)
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“…Seawater and Quaternary water, which have a high hydraulic gradient, infiltrated the −375 m sublevel through bedrock fractures. Simultaneously, the F3 fault and the NW-oriented fractures opened due to mining-induced rock movement and stress redistribution [7,36]. M2 water samples that were affected by the F3 fault mainly received the vertical recharge of Quaternary water and partially received the lateral recharge of seawater.…”
Section: Results Of Multivariate Statistical Analysismentioning
confidence: 99%
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“…Seawater and Quaternary water, which have a high hydraulic gradient, infiltrated the −375 m sublevel through bedrock fractures. Simultaneously, the F3 fault and the NW-oriented fractures opened due to mining-induced rock movement and stress redistribution [7,36]. M2 water samples that were affected by the F3 fault mainly received the vertical recharge of Quaternary water and partially received the lateral recharge of seawater.…”
Section: Results Of Multivariate Statistical Analysismentioning
confidence: 99%
“…A field investigation revealed that the F3 fault, whose width of the fracture zone was approximately 15-35 m, was a deep fault, and in the -375 m sublevel, there were 471 fractures with three prior attitudes: 38° < 89°, 16° < 15°, and 120° < 83°. Above the -600 m sublevel, Quaternary water and seawater were dominant sources, and F3 and the NW-oriented fractures were the main channels for these sources for deeper parts of tunnels [7,36]. M1 water samples were recharged by Quaternary water through the F3 fault in the vertical direction, and M2 water samples were partly recharged by Quaternary water in the vertical direction through the F3 fault and mostly by seawater in the lateral direction through NW−NE fractures.…”
Section: Discussionmentioning
confidence: 99%
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“…Figure 8 shows the vertical displacement of the study area which is caused by settlement. The ground deformation suggests that a compressive zone is located at the center of the subsidence and a tensional zone is distributed around the compressive zone [40]. The horizontal fissures would be closed in the compressive zone because of the vertical stress.…”
Section: Discussion: the Potential Water Flow Channelmentioning
confidence: 99%
“…Thus, it was also reasonable to select 510-8-1 as an end-member at the −510-m sublevel. The reasons for the high content of HCO 3 − were that volatile components, including water, carbon dioxide, and methane, exist in the Sanshandao gold mine; beresite and lamprophyre are the main rocks containing carbonate minerals; and Quaternary water and freshwater containing CO 2 flow into the fractures [38].…”
Section: Choice Of End-members In the Pca And Hca Modelsmentioning
confidence: 99%