3</sub> ·Cl-Na型,奧陶系灰?guī)r則為Cl-Na型,寒武系灰?guī)r呈現(xiàn)為 Cl?HCO<sub>3</sub>–Na 型,而2401采區(qū)的水質(zhì)則歸類(lèi)為 SO<sub>4</sub>?HCO<sub>3</sub>-Na 型。且隨著開(kāi)采深度的增加, Ca<sup>2+</sup>,Mg<sup>2+</sup>,Na<sup>+</sup>+K<sup>+</sup>,Cl 的濃度呈下降趨勢(shì), SO<sub>4</sub><sup>2-</sup> 的濃度則逐漸上升, H(O<sub>3</sub><sup>-</sup> 的濃度隨深度變化相對(duì)平穩(wěn)。【結(jié)論】太原組灰?guī)r含水層為直接充水含水層,奧陶系灰?guī)r為間接充水含水層。研究結(jié)果揭示了離子濃度及隨深度變化的規(guī)律,為制定針對(duì)性的礦井水害防治措施提供了科學(xué)依據(jù),有助于降低水害事故的風(fēng)險(xiǎn)。-龍?jiān)雌诳W(wǎng)" />

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新集二礦2401工作面灰?guī)r含水層水文地球化學(xué)特征研究

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關(guān)鍵詞:淮南煤田;灰?guī)r含水層;水文地球化學(xué)特征

中圖分類(lèi)號(hào):P641 文獻(xiàn)標(biāo)志碼:A 文章編號(hào):1003-5168(2025)13-0121-06

DOI:10.19968/j.cnki.hnkj.1003-5168.2025.13.024

Hydrogeochemical Characteristics ofLimestone Aquifer in 2401 Panel of Xinji No. 2 Mine

ZHOU PengjuLI Jibao (China Coal Xinji Energy Co.,Ltd.,Xinji No.2 mine,Huainan 232002,China)

Abstract: [Purposes] In view of the complex hydrogeological conditions of Huainan coalfield,this study systematicallyanalyzes the hydrogeochemical characteristics of groundwater incoal mines to identify the main water sources that pose a threat to coal mining.[Methods] Taking Xinji No.2 mine and 24Ol panel of Huainan City as a case study,Piper three-line analysis and major ion analysis methods were employed to systematically investigate the variation trend of hydrochemical types and ionic concentration gradients with depth acrosslimestone aquifers in the mining area.[Findings] According to the results of hydrochemical analysis,the water quality of Taiyuan Formation limestone is mainly HCO 3 ·Cl-Na type, the Ordovician limestone is Cl-Na type,while the Cambrian limestone is Cl ?? HCO NA type,and the wa3 ter quality of panel 24O1 is classified as SO 4 ·HCO 3 -Na type.With the increase of mining depth,the concentrations of Ca2+ , Mg2+ ,Na++K+and Cl- decreases,while concentration of SO progressively rises. The concentration of HCO3- remains relatively stable with the increase of mining depth.[Conclusions] The Taiyuan Formation limestone aquifer is a direct water-filling aquifer,while the Ordovician limestone is an indirect water-filling aquifer.Inaddition,the variation patterns of ion concentrations with depth is revealed, which provides a scientific basis for formulating targeted measures to prevent and control mine waterhazards,and thus helping to reduce the risk of water inrush accidents. Keywords:Huainan coal field; limestone aquifer; hydrogeochemical characteristics

0 引言

隨著淺部煤炭資源開(kāi)采的逐步完成,兩淮礦區(qū)的礦井作業(yè)重心逐步深人到更為復(fù)雜且深層的區(qū)域。(剩余6209字)

目錄
monitor