本文選題：煤礦區(qū) + 水-巖作用�。� 參考：《水文地質(zhì)工程地質(zhì)》2017年05期

【摘要】：煤礦開采勢必破壞天然水化學環(huán)境,然而礦區(qū)多類含水層地下水系統(tǒng)水化學研究尚未從時空角度分析采動影響下水化學演化的本質(zhì)。以臨渙礦區(qū)為研究示范,基于歷年常規(guī)水化學數(shù)據(jù)開展主成分分析,揭示采動影響下水化學演化過程中的水-巖作用機制。其中,第1主成分代表碳酸鹽、硫酸鹽溶解及黃鐵礦氧化作用,第2主成分代表陽離子交替吸附及脫硫酸作用。采動影響下礦區(qū)主要突水含水層地下水碳酸鹽、硫酸鹽溶解及黃鐵礦氧化作用均逐漸減弱,減弱區(qū)域不盡相同;然而,陽離子交替吸附及脫硫酸作用的變化規(guī)律不明顯。研究成果為礦井突水水源識別和水資源保護與利用提供理論依據(jù)。
[Abstract]:Coal mining is bound to destroy the chemical environment of natural water. However, the hydrochemistry of groundwater system of many kinds of aquifers in mining area has not been analyzed from the point of view of time and space. Based on the conventional hydrochemical data over the years, principal component analysis (PCA) was carried out in Linhuan mining area to reveal the mechanism of water-rock interaction in the process of hydrochemical evolution affected by mining. Among them, the first principal component represents carbonate, sulfate dissolution and pyrite oxidation, and the second principal component represents cation alternating adsorption and desulfurization. Under the influence of mining, the carbonate of groundwater in main water-inrush aquifer of mining area, sulfate dissolution and pyrite oxidation are gradually weakened, and the weakening regions are different, however, the change law of cationic alternating adsorption and desulphuric acid is not obvious. The research results provide theoretical basis for mine water inrush source identification and water resources protection and utilization.
【作者單位】： 合肥工業(yè)大學資源與環(huán)境工程學院;
【基金】：國家自然科學基金項目(41372244、41773100) 中央高校基本科研業(yè)務費專項資金項目(JZ2016HGBZ0802)
【分類號】：P641.461

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