scholarly journals Integrated treatment of acid mine drainage using cryptocrystalline magnesite and barium chloride

2017 ◽  
Vol 12 (3) ◽  
pp. 727-736 ◽  
Author(s):  
Vhahangwele Masindi

This study endeavours to report the efficiency of a hybrid approach in the treatment of acid mine drainage. Cryptocrystalline magnesite was used to pre-treat acid mine drainage and barium chloride was used to remove the residual sulphate through the formation of barium sulphate. Batch experimental approach was adopted and the documented optimum conditions for both cryptocrystalline magnesite and barium salts were used. This was 60 mins for pre-treatment and 60 mins for polishing the residual sulphate. Water quality was assessed using ICP-MS and IC. Mineralogical composition was done using XRD, elemental composition with XRF, morphology with SEM and transmission electron microscope. Magnesite removed >99% of heavy metal species and 40% sulphate except for base cations. Barium managed to remove 99% of residual sulphate from an aqueous system. This indicate that the water meet the industrial, discharge and irrigation standards as stipulated by the water quality guidelines. As such, it can be concluded that this integrated approach can be used to treat acid mine drainage to useable standards as defined in the water quality guidelines. This will be a pragmatic approach for mining houses to curtail the impact of acid mine drainage by using natural and locally available materials such as cryptocrystalline magnesite and polish the water with barium salts.

2017 ◽  
Vol 17 (2) ◽  
pp. 17-31
Author(s):  
A. Ewusi ◽  
B. Y. Apeani ◽  
I. Ahenkorah ◽  
R. S. Nartey

The quality of water in mining communities is uncertain since metals associated with acid mine drainage are known to saturate these waters. Previous studies in Tarkwa, an area noted for gold and manganese extraction, have reported large concentrations of aluminium, arsenic, cadmium, copper, lead, manganese and mercury in water samples. This research aimed at investigating the chemistry of groundwater with special focus on the contamination status of trace elements. It also compared levels of metal concentration with those that were determined in previous research works, to identify changes that might have occurred. Thirty-eight water samples from boreholes, hand-dug wells and streams, within the Tarkwa area were obtained and analysed. Results show that 90 % of water in the area is acidic and Eh was determined to be positive, depicting oxidizing conditions. Mean groundwater temperature was 28.9 ºC. Thirty-two samples had either temperature or pH values falling outside the range recommended by the World Health Organisation (WHO). Thirty samples had at least one metal concentration exceeding the WHO guideline values. Among the list of elements that exceeded the guideline, arsenic, manganese, nitrate, nitrite and iron were the most predominant. The dominant ions in the samples were sodium and bicarbonate. High concentrations of Fe and SO42- in some parts of the study area point to the influence of acid mine drainage (AMD). Comparisons of results of metal concentrations with findings from previous research in the area showed a reduction in concentration. Hydrochemical modelling with PhreeqC attributed this reduction to sorption processes. Comparison of levels of metal concentration in the different water supply facilities (borehole, hand-dug well and stream) showed no significant variations. Keywords: Water Quality, Drinking Water, Hydrochemical Modelling, Heavy Metals


2017 ◽  
Vol 37 (1) ◽  
pp. 88-97 ◽  
Author(s):  
Soledad Chamorro ◽  
Carlos Barata ◽  
Benjamín Piña ◽  
Marta Casado ◽  
Alex Schwarz ◽  
...  

2009 ◽  
Vol 24 (12) ◽  
pp. 2301-2311 ◽  
Author(s):  
Manuel A. Caraballo ◽  
Tobias S. Rötting ◽  
Francisco Macías ◽  
José Miguel Nieto ◽  
Carlos Ayora

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