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Evaluation of contamination of manganese in groundwater from overburden dumps of Lower Gondwana coal mines

机译:从较低煤层煤矿覆盖倒装地下水中锰污染的评价

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摘要

Inappropriate management of coal mine overburden (OB) dumps creates environmental hazards. In many countries, high concentration of Mn was observed in groundwater near the coal mine OB dump sites. Comparatively new coal mines in Barjora coalfield were chosen in this study to assess the impact of OB dumps in groundwater. Acid Digestion (AD), Toxicity Characteristics Leaching Procedure (TCLP) and Batch Leaching Test (BLT) were performed to estimate Mn concentration in OB dumps and its leaching behaviour. Shale present in OB dump has potential to leach high concentration of Mn. The aquifer in this region is mainly unconfined type and water table is very shallow. In situ soil is characterized by 44.3% sand, 37.5% silt and 18.2% clay with a saturated hydraulic conductivity of 5.58 cm/day. Column study and HYDRUS 1D numerical modelling were used to simulate the migration of Mn in vadose zone. Subsurface soil does not possess appreciable attenuating potential to retard the transport of Mn in vadose zone. HYDRUS 1D model explains that 1.6 m thick soil profile of the study area may release Mn in groundwater after 11(th) year and it can attain the complete breakthrough at 17(th) year. A groundwater contaminant transport model based on available hydrogeological data has been developed using VISUAL MODFLOW 2009.1 software. The movement of Mn in aquifer has been determined using MT3DMS code. It indicates similar or equal to 8 km(2) area around the two Open Cast Coal Mines (OCCMs) namely OCCM 1 and OCCM 2 may suffer groundwater contamination of Mn by 2050.
机译:煤矿覆盖物的不恰当管理(OB)倾倒会产生环境危害。在许多国家,在煤矿OB倾倒地点附近的地下水中观察到高浓度的Mn。在本研究中选择了Barjora Coalfield的相对较新的煤矿,以评估OB倾倒在地下水中的影响。进行酸消化(Ad),进行毒性特征浸出程序(TCLP)和批次浸出试验(BLT)以估计OB倾料及其浸出行为的Mn浓度。在OB倾卸地存在的页岩具有潜入高浓度的Mn。该地区的含水层主要是无纺布类型,水桌非常浅。原位土壤的特征在于44.3%的砂,37.5%淤泥和18.2%的粘土,饱和液压导电率为5.58厘米/天。柱研究和氢化1D数值建模用于模拟Mn在Vadose区中的迁移。地下土不具有可观的衰减潜力,可延缓延迟瓦糖区中的Mn运输。 Hydrus 1D模型解释说,在第11(Th)年后,研究区域的1.6米厚的土壤剖面可能在地下水中释放MN,并且可以在17年(第17岁)中获得完全突破。基于可用水文地质数据的地下水污染运输模型已经使用Visual Modflow 2009.1软件开发了。使用MT3DMS代码确定了Mn在含水层中的运动。它表明两个开放铸造煤矿周围的相似或等于8km(2)个区域,即CONCM 1,CONCM 2可能会遭受2050℃的地下水污染。

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