CENTRAL POLAND) Z.M. Migaszewski [zmig@pu.kielce.pl] A. Gauszka, S. - - PowerPoint PPT Presentation

CHEMICAL AND ISOTOPIC VARIATIONS IN THE WIŚNIÓWKA MAŁA MINE PIT WATER, HOLY CROSS MOUNTAINS (SOUTH- CENTRAL POLAND)

Z.M. Migaszewski [zmig@pu.kielce.pl]

• A. Gałuszka, S. Dołęgowska, A. Michalik

(Pedagogical University, Kielce)

• S. Hałas, J. Dąbek

(Maria Curie-Skłodowska University, Lublin)

• P. Pasławski, E. Starnawska

(Polish Geological Institute, Warsaw)

Acid rock drainage/acid mine drainage

The oxidation of pyrite and iron-bearing sulfide minerals belongs to the most hazardous geogenic (geologic) and anthropogenic sources that can account for pollution of the environment. In 1989 about 19,300 km of streams and rivers,and 72,000 ha

• f lakes and reservoirs were seriously damaged by

mine effluents. The cessation of sulfide ore and brown coal mining

• perations leaves abandoned quarries and

underground workings usually filled in with water. Another source is mineral tailings. Most of the post-mining lakes and ponds are highlighted by a low pH (1 – 4) and raised levels of trace metals (in mgL-1 or gL-1).

The pyrite can undergo microbial oxidation by two natural oxidants, i.e. (1) oxygen and even more effective (2) ferric (Fe3+) ion: FeS2 + 3,5O2 + H2O  Fe2+ + 2SO4

2- + 2H+ (1)

FeS2 + 14Fe3+ + 8H2O  15Fe2+ + 2SO4

2- + 16H+ (2)

2Fe2+ + 1/2O2 + 2H+  2Fe3+ + H2O (3) Fe3+ + 3H2O  Fe(OH)3 + 3H+ (4) Chemolithotrophic acidophilic oxidizing bacteria, e.g. Acidithiobacillus ferrooxidans, A. thiooxidans, Leptospirillum ferrooxidans, catalyze all the stages of pyrite oxidation increasing reaction rates by several

• rders of magnitude.

Mining area of the Kielce Quartzite Mines ”Wiśniówka”

Bathymetric map of the Wiśniówka Mała pit lake

Wiśniówka Mała – eastern pond

Wiśniówka Mała – western pond

METHODS

Field measurements of water:

• pH, EC, T (pH-meter CP-103 and EC-meter CC-

101 Elmetron, Poland);

• concentrations of Fe2+, Fetotal, HCO3
• , SO4

2-

(spectrophotometer LF-205 Slandi, Poland). Chemical analyses of water:

• cations – 30 elements (including Hg)
• ICP-OES (multichannel spectrometer Jobin-

Yvon – model PANORAMA with horizontal plasma);

• ICP-MS (spectrometer ELAN DRC II, Perkin

Elmer);

• CV-AAS (Altec amalgam analyzer AMA 254).

• Anions – Br-, Cl-, F-, HPO4

2-), NO2

• , NO3
• (Waters

HPLC Ion Chrom); NH4

+ (Varian – Cary-1e);

Chemical analyses of sediment:

• 31 elements: XRF; spectrometer Philips PW

2400), ICP-MS, CV-AAS). Mineralogic study of sediment:

• polarizing microscope (Axilab Zeiss);
• scanning electron microscope (SEM/EDS LEO

1430/ISIS Detector (Oxford Instruments Ltd.).

• X-ray diffraction (diffractometer Philips X'Pert PW

3020) Isotopic analyses (mass spectrometer MI-1305):

• S and O isotopes (in soluble sulfates);
• O isotopes (in H2O).

Wiśniówka Mała lake

pH = 3.73; EC = 390 Scm-1 pH 4.36; EC = 293 Scm-1

Physico-chemical parameters, and S and O stable isotope ratios in the water of the Wiśniówka Mała pit lake in 2005

Parameter Western pond Eastern pond Depth of sampling (in m) 0.1 5.0 10.0 13.5 0.1 5.0 10.0 12.7 pH

3.75 3.78 3.37 3.38 4.40 4.27 4.26 4.27

EC Scm-1 450 450 672 656

231 235 231 231

T C

19.0 18.5 18.5 18.0 15.0 14.5 14.5 14.5

Fe2+ mgL-1

0.2 0.1 0.7 0.4 <0.1 <0.1 <0.1 <0.1

Fe3+ mgL-1

0.1 0.2 1.8 1.9 <0.2 <0.2 <0.2 <0.2

SO4

2- mgL-1

109 108 172 174 81 85 85 84

34S-SO4

2- ‰ -4.7

• 4.8
• 6.5
• 6.3
• 2.2
• 1.7
• 2.1
• 2.1

18O-SO4

2- ‰ -0.9 -1.69 -3.0

• 2.7
• 2.2
• 2.4
• 1.8
• 1.6

Physico-chemical parameters, and S and O stable isotope ratios in the water of the Wiśniówka Mała pit lake in 2006

Parameter Western pond Eastern pond Depth of sampling (in m) 0.1 5.0 10.0 15.6 0.1 5.0 10.0 14.0 pH

3.93 4.33 3.94 3.72 4.59 4.44 4.69 4.47

EC Scm-1 417 445 323 563

322 322 328 331

T C

24.0 21.7 22.0 24.6 25.3 24.3 22.5 26.5

Fe2+ mgL-1

0.3 0.5 1.0 2.7 <0.1 <0.1 <0.1 <0.1

Fe3+ mgL-1

0.0 0.0 0.0 0.3 <0.2 <0.2 <0.2 <0.2

SO4

2- mgL-1

147 117 160 192 95 88 100 96

34S-SO4

2- ‰ -4.9

• 4.6
• 5.2
• 5.4
• 1.4
• 1.1
• 0.9
• 1.4

18O-SO4

2- ‰ -0.6

• 0.5
• 0.8
• 2.3
• 1.6
• 2.3
• 2.9
• 1.4

Selected trace metals in the water of the Wiśniówka Mała pit lake in 2006

Parameter Western pond Eastern pond Depth of sampling (in m) 0.1 5.0 10.0 15.6 0.1 5.0 10.0 14.0 Ba mgL-1 38 32 34 31 64 62 71 73 Cd mgL-1 0.41 0.37 0.46 0.46 0.33 0.30 0.58 0.30 Co mgL-1 40 41 45 54 32 30 32 31 Cu mgL-1 78 83 94 126 49 49 52 50 Ni mgL-1 46 47 51 60 36 34 36 34 Pb mgL-1 1.53 3.20 1.31 1.20 0.64 1.48 1.33 0.67 U mgL-1 1.31 1.54 1.76 2.65 0.50 0.56 0.57 0.58 Zn mgL-1 76 75 80 88 48 47 54 49

As – <2 gL-1, Hg – <0.3 gL-1

Selected trace metals in the sediment

• f the Wiśniówka Mała pit lake in 2006

Parameter Western pond Eastern pond CaO % 0.11 0.10 Fe2O3 % 2.08 2.26 As mgkg-1 43 40 Ba mgkg-1 843 958 Cu mgkg-1 14 16 Hg mgkg-1 2.38 1.96 Ni mgkg-1 7 10 Pb mgkg-1 16 18 U mgkg-1 3.30 4.65 Zn mgkg-1 27 26

Cd – <3 mgkg-1, Co – <5 mgkg-1

Saturation indices for selected minerals calculated with PHREEQC program for Windows

Minerals Western pond Eastern pond Depth of sampling (in m) 0.1 5.0 10.0 15.6 0.1 5.0 10.0 14.0 Al(OH)3(a)

• 2.60 -1.53 -2.60 -2.88 -0.98 -1.56 -0.88 -1.28

Ca-smectite 5.00 7.69 5.20 4.49

8.70 7.26 8.86 7.83

Fe(OH)3(a)

• 6.07 -4.83 -5.62 -5.82 -4.53 -5.04 -4.39 -5.01

Goethite

• 0.22 0.94

0.16 0.05 1.38 0.83 1.41 0.93

Hematite

1.53 3.88 2.32 2.11 4.76 3.66 4.83 3.88

Illite

2.06 5.01 2.25 1.38 6.22 4.65 6.46 5.26

Quartz

1.96 1.98 2.02 2.02 1.89 1.88 1.86 1.85

SEM images of the sediment

Eastern pond Western pond

Clay minerals Hydrous ferric oxides and hydroxides

Hydrous ferric oxides and hydroxides

5 µm 5 µm

Gorceixite BaAl3H[(OH)6(PO4)2]

Hydrous ferric oxides and hydroxides

5 µm 100 µm

18Osulfate = Xoxygen (18Ooxygen + oxygen) + Xwater (18Owater + water)

18O-SO4

2- = -1.4‰

Precipitation Soils + wastes!! 34S-SO4

2- = 4.5‰

18O-H2O = -8.5‰ 34S-FeS2 = -11.6‰?

Dissolved O2 18O = 23.5‰

34S-SO4

2- = -5.6‰

Oxygen path (87.5% O2) (12.5% H2O) Iron path (Fe3+)

Precipitation Soils + wastes 18O-SO4

2- = 7 to 17‰

Unique chemistry of the Wiśniówka Mała pit lake water

Locations of mine pits pH SO4

2- Fetot. Fe2+

mgL-1 Wiśniówka Mała lake – western pond 3.73 156 1.0 0.6 Wiśniówka Mała lake – eastern pond 4.36 90 <0.2 <0.1 Podwiśniówka mine pond 2.90 131 5.6 3.0 Lusatia (eastern Germany) 2.54 2.87 3.25 1160 1559 2006 – – – – – – Mynydd Parys (G.B.) – copper mine 2.5 3100 650 650 Sverdrupbyen (Norway) – coal dumps 2.7 1077 179 – Wheal Jane (G.B.) – tin mine 3.6 350 130 130

Conclusions

• 1. The principal source of soluble sulfates in the

Wiśniówka Mała pit lake is the oxidation of pyrite and iron oxidation/hydrolysis reactions with some influxes of sulfates from: (i) soils, weathered wallrocks and tailings piles and subordinate (ii) atmospheric deposition.

• 2. The pit lake reveals different chemistry and

isotopic composition within two separated ponds. The western pond is notable for the lower pH and higher concentrations of most elements.

• 3. Compared to other areas impacted by acid mine

drainage, the water examined shows distinctly low concentration of sulfates, iron and other trace metals.