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李海祥,曹志国,王路军,等. 台格庙矿区地下水水化学特征与演变规律研究[J]. 煤炭科学技术,2023,51(9):284−291

. doi: 10.12438/cst.2022-1439
引用本文:

李海祥,曹志国,王路军,等. 台格庙矿区地下水水化学特征与演变规律研究[J]. 煤炭科学技术,2023,51(9):284−291

. doi: 10.12438/cst.2022-1439

LI Haixiang,CAO Zhiguo,WANG Lujun,et al. Study on chemical characteristics and evolution law of groundwater in Taigemiao Mining Area[J]. Coal Science and Technology,2023,51(9):284−291

. doi: 10.12438/cst.2022-1439
Citation:

LI Haixiang,CAO Zhiguo,WANG Lujun,et al. Study on chemical characteristics and evolution law of groundwater in Taigemiao Mining Area[J]. Coal Science and Technology,2023,51(9):284−291

. doi: 10.12438/cst.2022-1439

台格庙矿区地下水水化学特征与演变规律研究

Study on chemical characteristics and evolution law of groundwater in Taigemiao Mining Area

  • 摘要: 台格庙矿区煤炭资源丰富,但水资源匮乏、生态环境脆弱,利用水文地球化学方法,开展矿区全流域地下水化学特征与演变规律研究,能为矿区绿色开采提供科学支撑。利用Piper三线图分析白垩系地下水、侏罗系地下水、河水和湖水类型,其水化学特征满足湖水由河水和不断演变的地下水混合后形成的条件;通过Gibbs图分析得出,白垩系和侏罗系地下水在循环演变过程中受岩石和蒸发作用控制;离子比值端元法进一步表明,白垩系和侏罗系地下水受硅酸岩盐和岩盐控制为主,同时伴随离子交换;最后通过质量平衡模拟得出,白垩系地下水循环演变过程中溶解白云岩、石膏、岩盐矿物质,吸收CO2,析出方解石,伴随离子交换,可与不同比例河水混合形成湖水,但侏罗系地下水只能混合少量河水或不混合河水。河水占红碱淖湖水补给量83%,侏罗系地下水不能为其主要补给来源,红碱淖湖水主要来源白垩系地下水和河水。结合矿区水文地质条件,将矿区地下水流系统分为南侧白垩系地下水流系统、北侧的白垩系地下水流系统和深部的侏罗系地下水流系统,煤炭开采直接影响侏罗系地下水流系统,在保障两个白垩系地下水流系统不被破坏的前提下,当采煤排水只袭夺侏罗系边界流出水量或少量侏罗系补给红碱淖水量时,采煤对红碱淖及周边河流的影响降至最小。

     

    Abstract: Taigemiao Mining Area is rich in coal resources, but water resources are scarce and the ecological environment is fragile, and the use of hydrogeochemical methods to carry out research on the chemical characteristics and evolution law of groundwater in the whole basin of mining areas can provide scientific support for green mining in mining areas. Piper three-line diagram was used to analyze the types of Cretaceous groundwater, Jurassic groundwater, river water and lake water, and the water chemical characteristics met the characteristics of lake water mixed by river water and evolving groundwater; through Gibbs diagram analysis, it is concluded that the Cretaceous and Jurassic groundwater in the cyclic evolution process It is controlled by rock and evaporation; the ion ratio endmember method further shows that the Cretaceous and Jurassic groundwater is dominated by silicate rock salt and rock salt, accompanied by ion exchange; finally, the mass balance simulation shows that the Cretaceous groundwater circulation During the evolution process, dolomite, gypsum, and rock salt minerals are dissolved, CO2 is absorbed, and calcite is precipitated. With ion exchange, it can be mixed with different proportions of river water to form lake water, but Jurassic groundwater can only be mixed with a small amount of river water or not mixed with river water. The river water accounts for 83% of the water supply of Hongjiannao Lake. Jurassic groundwater cannot be the main source of water supply. The main sources of water in Hongjiannao Lake are Cretaceous groundwater and river water. Combined with the hydrogeological conditions of the mining area, the groundwater flow system of the mining area is divided into the Cretaceous groundwater flow system in the south, the Cretaceous groundwater flow system in the north and the Jurassic groundwater flow system in the deep. Coal mining directly affects the Jurassic groundwater flow system. On the premise of ensuring that the two Cretaceous groundwater flow systems are not damaged, when coal mining drainage only captures the outflow water from the Jurassic boundary or a small amount of Jurassic replenishment to Hongjiannao, coal mining will affect Hongjiannao and surrounding rivers. impact is minimized.

     

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