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Middle Yangtze (Jingsha to Jiujiang)

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 ‰. Alluvial plain, Dongting Lake outlet and above Poyang, Wuhan. Indicative coordinates (middle of the reach).

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

Standard : NBS 28

ValueRangenMineral or matrixSource
2.04 ± 0.44 ‰1.5 / 2.7 ‰5filtered river water (dissolved silicon)
Mean and standard deviation recalculated from 5 values. Stations YZ-09 to YZ-13, dissolved silicon; whole-river mean +2.13 ‰ (n = 17).
Ding et al. (2004), Silicon isotope compositions of dissolved silicon and suspended matte…
−0.24 ± 0.18 ‰−0.5 / 0 ‰5suspended particulate matter
Mean and standard deviation recalculated from 5 values. Stations YZ-09 to YZ-13, 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). Middle Yangtze (Jingsha to Jiujiang), isotope signatures. https://www.isofind.tech/isotopes/en/sites/yangtse-moyen-de-jingsha-a-jiujiang/ (accessed 2026-10-13).

@misc{isofind2026middleyangtzejingshatojiujian,
  title = {Middle Yangtze (Jingsha to Jiujiang), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/yangtse-moyen-de-jingsha-a-jiujiang/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13