Geochemical
Characteristics of the Acid Mine Drainage in the Sitai
Coalmine, North China
Zhiyuan
Cong, China University of Mining and Technology (Beijing),
Key Laboratory of Coal Resources, Ministry of Education,
P.R.C, XueYuan Road, Ding 11#, Haidian District, Beijing
100083, China, Fax: 86-10-62325016, Email: zhiyuancong@hotmail.com
Fenghua Zhao, China University of Mining and Technology
(Beijing), Key Laboratory of Coal Resources, Ministry of
Education, P.R.C, XueYuan Road, Ding 11#, Haidian
District, Beijing 100083, China, Fax: 86-10-62325016,
Email: zfh@cumtb.edu.cn
Acid
mine drainage (AMD) represents a serious environmental
problem for coal mining industry worldwide. Acid mine
drainage is generated when metal sulphides in coal and the
associated strata, particularly pyrite (FeS2),
react with water and oxygen in the presence of thiobacillus
bacteria to produce sulfuric acid and iron hydroxide or
iron sulphate. The low pH may result in further
dissolution of country rock and the subsequent leaching of
metals into water, and thereby adversely impact on aquatic
life and surrounding vegetation. In China, coal is the
most important energy sources and has been mined about
several hundreds of years. In the meanwhile, most of the
water systems in the vicinity of the coal mining areas
suffered from the water pollution, especially discharges
of untreated AMD.
In
this research, several water samples and sediments from
the Sitai coalmine were investigated to confirm the
mechanism of contamination and to identify the major
processes affecting the attenuations of heavy metals. The
analysis results show that the concentrations of major
constituents in AMD are tens to hundreds times high than
those in background stream. With the application of the
PHREEQCI program, predominant species of some toxic metals
were also determined. The saturation index of goethite was
pronounced positive. Furthermore, XRD analysis confirmed
the occurrence of goethite in ochrous precipitates.
Acid
Drainage from Rich-in-Pyrite Mining Wastes in a Uranium
Deposit
I.I.
Spasova, Department of Engineering Geoecology, University
of Mining and Geology, Studentski grad – Durvenitza,
Sofia 1700, Bulgaria, Tel: +359 2 687396, Fax: + 359 2
687396, Email: spasova@mgu.bg
F. Veglio, Department of Chemistry, Engineering Chemistry
and Materials, University of L’Aquila, L’Aquila,
Italy, Tel: + 34 862434223/4236, Fax: + 34 862434203,
Email: veglio@ing.univaq.it
M.V. Nicolova, Department of Engineering Geoecology,
University of Mining and Geology, Studentski grad –
Durvenitza, Sofia 1700, Bulgaria, Tel: +359 2 687396, Fax:
+ 359 2 687396. Email: mnikolova@mgu.bg
S.N. Groudev, Department of Engineering Geoecology,
University of Mining and Geology, Studentski
grad – Durvenitza, Sofia 1700, Bulgaria, Tel: +359 2
687396, Fax: + 359 2 687396
, Email:
groudev@mgu.bg
The
uranium deposit Curilo, Western Bulgaria, for a long
period of time was a site of intensive mining activities
including both the open-pit and underground mining
techniques as well as in situ leaching of uranium. The ore
was rich in pyrite and, apart from uranium, contained
several non-ferrous metals. The mining operations in the
deposit were ended in 1990 but since that time the dumps
consisting of mining wastes are, after rainfall, a large
source of acid drainage waters. These waters have pH in
the range of about 2 – 4 and contain radioactive and
heavy metals (uranium, radium, iron, manganese, copper,
zinc, cadmium, nickel, cobalt), arsenic and sulphates in
concentrations usually 2 – 10 times higher than the
relevant permissible levels for waters intended for use in
the agriculture and/or industry.
The
investigations carried out in the deposit revealed that
the generation of the polluted waters was connected with
the activity of the indigenous acidophilic
chemolithotrophic bacteria, which oxidized the pyrite,
other sulphides and uranium bearing minerals present in
the dumps. Acidithiobacillus ferrooxidans and
Leptospirilum ferrooxidans were the prevalent
microorganisms of this group and their number usually
exceeded 108 cells/g mining wastes. The growth
and activity of these bacteria markedly depended on some
essential environmental factors such as pH, temperature,
and water, oxygen and nutrient contents in the dumps.
These data will be used for development of technology to
inhibit the microbial growth and activity and in this way
to prevent the generation of polluted waters from the
dumps.
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