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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Refining the estimation of metal loads dissolved in acid mine drainage by continuous monitoring of specific conductivity and water level
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Refining the estimation of metal loads dissolved in acid mine drainage by continuous monitoring of specific conductivity and water level

机译:通过连续监测比电导率和水位,改进对酸性矿山排水中溶解的金属负荷的估算

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The accurate estimation of metal loads transported by streams is necessary to calculate reliable mass transfers of metals between compartments, both at local and global scales. This estimation is particularly relevant in the case of the Tinto and Odiel Rivers (SW Spain) due to their significant contribution to the total metal transfer from continents to the ocean. At a local scale, the metal load transported by streams plays a key role in predicting the biogeochemical evolution of water reservoirs affected by Acid Mine Drainage (AMD). This work uses the relationships between specific conductivity (SC) and dissolved elements to calculate the metal load of the River Meca, a tributary of the Odiel. The SC and the water level were continuously monitored from April 2009 to June 2010. Water samples were also collected and measurements of the discharge were carried out manually once a month. The relationships between the SC and the concentration of dissolved elements are, in general, very good (R 2>0.90). However, some key elements such as Fe show a very poor correlation. A simple methodology based on the MIX code (a maximum likelihood method to estimate mixing ratios) was used to elucidate their different behaviours. During the dry period (April-December, 2009) the Fe concentration was lower than that deduced from the SC recorded value due to the precipitation of Fe-oxihydroxides, which also reduced the concentrations of As, Cr, Pb and, to a lesser extent, Cu. At the same time Na, Sr, Ca and Li were enriched because of the higher interaction with the riverbed materials. Correlations between the SC and the metal concentration improved significantly when each period was considered separately. A second dry period (April-June 2010) shows high SC values, although no dissolution/precipitation of solid phases is evidenced. This indicates that SC alone is not enough to predict the dissolved metal loads in Mediterranean AMD streams. The metal load transported by the River Meca was determined for the hydrological year 2009/10 as 1933±129 tonnes of Fe, 990±155 of Al and 378±41 of Zn.
机译:在局部和全球范围内,准确估算通过物流运输的金属负载对于计算隔室之间金属的可靠质量传递是必要的。对于Tinto河和Odiel河(西班牙西南部)而言,这一估算尤其重要,因为它们对从大陆到海洋的金属转移总量做出了重大贡献。在地方尺度上,由溪流输送的金属负载在预测受酸性矿山排水(AMD)影响的水库的生物地球化学演变中起着关键作用。这项工作利用比电导率(SC)与溶解元素之间的关系来计算Odiel支流Meca河的金属负荷。从2009年4月到2010年6月,对SC和水位进行了连续监测。还收集了水样,并每月一次手动测量排放量。通常,SC与溶解元素浓度之间的关系非常好(R 2> 0.90)。但是,某些关键元素(如铁)的相关性很差。使用基于MIX代码的简单方法(估计混合比的最大似然法)来阐明它们的不同行为。在干旱时期(2009年4月至12月),Fe的浓度低于从SC记录值中得出的值,这是由于Fe-羟基氧化物的沉淀,这也降低了As,Cr,Pb的浓度,并在较小程度上降低了浓度。 ,铜同时,由于Na,Sr,Ca和Li与河床物质之间的较高相互作用,使其富集。当分别考虑每个周期时,SC和金属浓度之间的相关性显着改善。第二个干燥期(2010年4月至6月)显示出较高的SC值,但未发现固相溶解/沉淀。这表明仅凭SC不足以预测地中海AMD流中的溶解金属负荷。在2009/10年度的水文年中,由梅卡河输送的金属负荷确定为1933±129吨铁,990±155铝和378±41锌。

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