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Banpo mine waters

Guizhou, Dushan County, Banpo mine, China

Acid mine drainage

Type
Acid mine drainage

Banpo antimony mine (Guizhou): 26 waters sampled in the Dajiagou Creek, which crosses the waste heaps, in the Chahe River, which receives the processing tailings, and in the Qisha tributary; Sb up to 1427 µg/L and sulfate up to 1926 mg/L. Dissolved sulfate δ34S follows Sb and sulfate in the Chahe (r = 0.68 and 0.89): a tracer of the pollution extent; isotope budget: about 59 % of the sulfur of the lower Chahe comes from the mine (Ning et al., 2011). Waters from the mine workings, the most sulfate-rich (322 to 1926 mg/L); δ34S close to stibnite. Coordinates not published.

δ34S in ‰ (per mil) Values of the same system

Standard : V-CDT

ValueRangenMineral or matrixSource
5.36 ± 2.24 ‰3.41 / 7.68 ‰4mine water
Mean and standard deviation recalculated from 4 analyses, +3.41 to +7.68 (W08 +7.68; W09 +3.47; W10 +6.86; W11 +3.41); 515 to 1377 µg/L Sb; together with the polluted Dajiagou, published mean of +5.04 ‰.
Ning et al. (2011), Antimony pollution and sulfur isotope study in the waters of an antim…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Banpo mine waters, isotope signatures. https://www.isofind.tech/isotopes/en/sites/eaux-d-exhaure-de-la-mine-de-banpo/ (accessed 2026-10-16).

@misc{isofind2026banpominewatersisotopesignatu,
  title = {Banpo mine waters, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/eaux-d-exhaure-de-la-mine-de-banpo/},
  note = {Accessed 2026-10-16}
}

Updated : 2026-10-16