Microbial diversity of mine water at Zhong Tiaoshan copper mine, China

2007 ◽  
Vol 47 (6) ◽  
pp. 485-495 ◽  
Author(s):  
Zhiguo He ◽  
Xuehui Xie ◽  
Shengmu Xiao ◽  
Jianshe Liu ◽  
Guanzhou Qiu
Geofluids ◽  
2019 ◽  
Vol 2019 ◽  
pp. 1-17 ◽  
Author(s):  
Malin Bomberg ◽  
Jarno Mäkinen ◽  
Marja Salo ◽  
Päivi Kinnunen

Microbial communities of iron-rich water in the Pyhäsalmi mine, Finland, were investigated with high-throughput amplicon sequencing and qPCR targeting bacteria, archaea, and fungi. In addition, the abundance ofLeptospirillumandAcidithiobacilluswas assessed with genus-specific qPCR assays, and enrichment cultures targeting aerobic ferrous iron oxidizers and ferric iron reducers were established. The acidic (pH 1.4–2.3) mine water collected from 240 m, 500 m, and 600 m depth from within the mine had a high microbial diversity consisting of 63-114 bacterial, 10-13 archaeal, and 104-117 fungal genera. The most abundant microorganisms in the mine water were typical acid mine drainage (AMD) taxa, such as acidophilic, iron-oxidizingLeptospirillum,Acidiphilum,Acidithiobacillus,Ferrovum, andThermoplasma. The fungi belonged mostly to the phylum Ascomycetes, although a great part of the fungal sequences remained unclassified. The number of archaeal 16S rRNA genes in the mine water was between 0.3 and 1.2 × 107copies mL−1in the samples from 500 m and 600 m, but only 3.9 × 103at 240 m and archaea were in general not enriched in cultures. The number of fungal 5.8S rRNA genes was high only in the mine water from 500 m and 600 m, where 0.2–3.4 × 104spore equivalents mL−1were detected. A high number ofLeptospirillum16S rRNA genes, 0.6–1.6 × 1010copies mL−1, were detected at 500 m and 600 m depth and in cultures containing ferrous iron, showing the importance of iron oxidizers in this environment. The abundance of bacteria in general was between 103and 10616S rRNA gene copies mL−1. Our results showed a high microbial diversity in the acid- and iron-impacted waters of the Pyhäsalmi mine, whereLeptospirillumbacteria were especially prominent. These iron oxidizers are also the main nitrogen-fixing microorganisms in this ecosystem.


Extremophiles ◽  
2007 ◽  
Vol 12 (2) ◽  
pp. 225-234 ◽  
Author(s):  
Zhiguo He ◽  
Shengmu Xiao ◽  
Xuehui Xie ◽  
Yuehua Hu

Author(s):  
Rafał Siuda ◽  
Marek Łodziński ◽  
Marcin Syczewski ◽  
Łukasz Kruszewski ◽  
Jaroslav Pršek ◽  
...  

The presence of botallackite was recognized in an underground galery in the Polkowice-Sieroszowice copper mine. This mineral coexists with paratacamite, clinoatacamite, gypsum and halite. Botallackite crystallized from chloride-reach (3500 mg/dm3), warm (33°C) mine water. On the basis of microprobe analyzes, two types of botallackite were recognized. The first one contains only small amounts of Pb, Fe and Zn. These elements substitute Cu2+ ions in small proportions. Empirical formula of this botallackite is: (Cu1.94Pb0.02Fe0.02Zn0.02)S = 2.00Cl0.98(OH)3.02. The second type of the mineral were characterized by increased amounts of Pb, Fe, Zn. The empiric formula of this type of botallackite can be expressed as: (Cu1.85Pb0.09Fe0.04Zn0.02)S = 2.00Cl1.05(OH)2.95. The calculated unit-cell parameters of botallackite from Polkowice-Sieroszowice mine are as follows: a = 5.7165(2), b = 6.1362(2), c = 5.6325(2), b = 92.943(3). Botallackite is a least stable polymorph of Cu2Cl(OH)3 and finally transforms to more stable polymorphs. The botallackite recrystallization can be inhibit by high concentration of Ca2+ in the mine water. Substitution of Cu2+ ions by other divalent cations can slows the rapidity of recrystalization this mineral and prevent its further transformation also. The Polkowice-Sieroszowice mine is the first occurrence of botallackite in Poland.


2009 ◽  
Vol 15 (4) ◽  
pp. 237-249 ◽  
Author(s):  
Velizar Stankovic ◽  
Dragana Bozic ◽  
Milan Gorgievski ◽  
G. Bogdanovic

In this work the results on the batch and column adsorption of copper and some associated ions by employing linden and poplar sawdust as a low-cost adsorbent are presented. The mine water from a local abandoned copper mine, as well as synthetic solutions of those ions which are the main constituents of the mine water were both used as a model-system in this study. The adsorption ability of the chosen sawdust to adsorb heavy metal ions is considered as a function of the initial pH of the solution and kind of metal ions. At lower pH of solutions the adsorption percentage (AD %) decreases leading to a zero AD % at pH < 1.1. Maximum AD % is achieved at 3.5 < pH < 5. It was found that poplar and linden sawdust have both almost equal adsorption capacities against copper ions. The highest AD % ( ?80%) was achieved for Cu2+, while for Fe2+ it was slightly above 10%. The other considered ions (Zn2+ and Mn2+) were within this interval. The results obtained in the batch mode were verified through the column test by using the real mine water originating from an acid mine drainage (AMD) of the copper mine 'Cerovo', RTB Bor. The breakthrough curves are presented as a function of the aqueous phase volume passed through the column allowing having an insight into the column adsorption features. Breakthrough points were determined for copper, manganese and zinc ions. A very high adsorption degree - higher than 99% was achieved in these experiments for all mentioned ions. After completing the adsorption, instead of desorption, the loaded sawdust was drained, dried and burned; the copper bearing ash was then leached with a controlled volume of sulphuric acid solution to concentrate copper therein. The obtained leach solution had the concentration of copper higher than 15 g dm-3 and the amount of H2SO4 high enough to serve as a supporting electrolyte suitable to be treated by the electrowinning for recovery of copper. The technology process based on the column adsorption is proposed and discussed.


2017 ◽  
Vol 24 (6) ◽  
pp. 5908-5917 ◽  
Author(s):  
Tuanny S. Frantz ◽  
Nauro Silveira ◽  
Maurízio S. Quadro ◽  
Robson Andreazza ◽  
Amauri A. Barcelos ◽  
...  

Minerals ◽  
2019 ◽  
Vol 10 (1) ◽  
pp. 1 ◽  
Author(s):  
Chiara Boschi ◽  
Federica Bedini ◽  
Ilaria Baneschi ◽  
Andrea Rielli ◽  
Lukas Baumgartner ◽  
...  

Understanding low temperature carbon sequestration through serpentinite–H2O–CO2 interaction is becoming increasingly important as it is considered a potential approach for carbon storage required to offset anthropogenic CO2 emissions. In this study, we present new insights into spontaneous CO2 mineral sequestration through the formation of hydromagnesite + kerolite with minor aragonite incrustations on serpentinite walls of the Montecastelli copper mine located in Southern Tuscany, Italy. On the basis of field, petrological, and geochemical observations coupled with geochemical modeling, we show that precipitation of the wall coating paragenesis is driven by a sequential evaporation and condensation process starting from meteoric waters which emerge from fractures into the mine walls and ceiling. A direct precipitation of the coating paragenesis is not compatible with the chemical composition of the mine water. Instead, geochemical modeling shows that its formation can be explained through evaporation of mine water and its progressive condensation onto the mine walls, where a layer of serpentinite powder was accumulated during the excavation of the mine adits. Condensed water produces a homogeneous film on the mine walls where it can interact with the serpentinite powder and become enriched in Mg, Si, and minor Ca, which are necessary for the precipitation of the observed coating paragenesis. The evaporation and condensation processes are driven by changes in the air flow inside the mine, which in turns are driven by seasonal changes of the outside temperature. The presence of “kerolite”, a Mg-silicate, is indicative of the dissolution of Si-rich minerals, such as serpentine, through the water–powder interaction on the mine walls at low temperature (~17.0 to 18.1 °C). The spontaneous carbonation of serpentine at low temperature is a peculiar feature of this occurrence, which has only rarely been observed in ultramafic outcrops exposed on the Earth’s surface, where instead hydromagnesite predominantly forms through the dissolution of brucite. The high reactivity of serpentine observed, in this study, is most likely due to the presence of fine-grained serpentine fines in the mine walls. Further study of the peculiar conditions of underground environments hosted in Mg-rich lithologies, such as that of the Montecastelli Copper mine, can lead to a better understanding of the physical and chemical conditions necessary to enhance serpentine carbonation at ambient temperature.


2015 ◽  
Vol 1130 ◽  
pp. 606-609 ◽  
Author(s):  
Ana Laura Santos ◽  
D. Barrie Johnson

A low pH sulfate-reducing bioreactor was used to selectively recover copper from synthetic pH 5 mine water draining a copper mine in Brazil, and also to remove other transition metals from solution. The design of the system used meant that a single bioreactor could be used for the process. Over 99% of the copper present was recovered as CuS in an off-line reactor vessel, while other metals (Ni, Co and Zn) were precipitated in the bioreactor vessel.


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