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Refining the estimation of metal loads dissolved in acid mine drainage by continuous monitoring of specific conductivity and water level
Authors:Laura Galván  Manuel Olías  Carlos Ruiz Cánovas  Ester Torres  Carlos Ayora  José Miguel Nieto  Aguasanta Miguel Sarmiento
Institution:1. Department of Geodynamics and Palaeontology, University of Huelva, Avda. Fuerzas Armadas s/n, 21071 Huelva, Spain;2. Department of Physical, Chemical and Natural Systems, University Pablo de Olavide, Carretera de Utrera, km 1, 41013 Sevilla, Spain;3. Institute of Environment Assessment and Water Research (IDAEA), CSIC, C/Jordi Girona 18, 08034 Barcelona, Spain;4. Department of Geology, University of Huelva, Avda. Fuerzas Armadas s/n, 21071 Huelva, Spain
Abstract: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 (R2 > 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.
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