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Upper Yangtze (Yibin to Fuling)

Yangtze basin, China

Rivers and surface water

Type
River or surface water

Main channel of the Yangtze sampled from 14 to 22 July 1996 (high water). Dissolved silicon 97 to 121 µmol/L, suspended matter with 52 to 57 % SiO2; dissolved silicon is heavier than suspended matter by 1.0 to 3.7 ‰. Sichuan Basin reach, before the Min, Tuo, Jialing and Wu confluences. Indicative coordinates (middle of the reach).

δ30Si in ‰ (per mil) Values of the same system

Standard : NBS 28

ValueRangenMineral or matrixSource
1.25 ± 0.49 ‰0.7 / 1.9 ‰4filtered river water (dissolved silicon)
Mean and standard deviation recalculated from 4 values. Stations YZ-01 to YZ-04, dissolved silicon; whole-river mean +2.13 ‰ (n = 17).
Ding et al. (2004), Silicon isotope compositions of dissolved silicon and suspended matte…
−0.3 ± 0.08 ‰−0.4 / −0.2 ‰4suspended particulate matter
Mean and standard deviation recalculated from 4 values. Stations YZ-01 to YZ-04, suspended matter; whole-river mean -0.34 ‰ (n = 17).
Ding et al. (2004), Silicon isotope compositions of dissolved silicon and suspended matte…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Upper Yangtze (Yibin to Fuling), isotope signatures. https://www.isofind.tech/isotopes/en/sites/yangtse-amont-de-yibin-a-fuling/ (accessed 2026-10-13).

@misc{isofind2026upperyangtzeyibintofulingisot,
  title = {Upper Yangtze (Yibin to Fuling), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/yangtse-amont-de-yibin-a-fuling/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13