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River downstream of the Fanjia-Caiyuan confluence (Xiaozhaizi)

Duyun, Qiannan, Guizhou, China

Rivers and surface water

Type
River or surface water

Niujiaotang zinc mine, mined on a large scale, in carbonate karst terrain. Waters stay alkaline (pH 8.6 to 9.0): mine drainage matters little, anthropogenic zinc mainly travelling with fine tailings dust dispersed by wind (19.5 % on average). Sites 7 and 8, below the confluence. Indicative coordinates.

δ66Zn in ‰ (per mil) Values of the same system

Standard : IRMM-3702

ValueRangenMineral or matrixSource
−0.2 ± 0.01 ‰−0.2 / −0.19 ‰2
Mean and standard deviation recalculated from 2 samples, Table 4. Filtered river water (W7 and W8).
Xia et al. (2020), Zinc isotope revealing zinc's sources and transport processes in karst…
−0.26 ± 0.01 ‰−0.26 / −0.25 ‰2
Mean and standard deviation recalculated from 2 samples, Table 4. Bed sediments (S7 and S8).
Xia et al. (2020), Zinc isotope revealing zinc's sources and transport processes in karst…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). River downstream of the Fanjia-Caiyuan confluence (Xiaozhaizi), isotope signatures. https://www.isofind.tech/isotopes/en/sites/riviere-en-aval-de-la-confluence-fanjia-caiyuan-xiaozhaizi/ (accessed 2026-10-13).

@misc{isofind2026riverdownstreamofthefanjiacai,
  title = {River downstream of the Fanjia-Caiyuan confluence (Xiaozhaizi), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/riviere-en-aval-de-la-confluence-fanjia-caiyuan-xiaozhaizi/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13