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Yangtze River (Changjiang)

Central and eastern China, from headwaters to estuary, China

Rivers and surface water

Type
River or surface water

Largest river of China, an example of weathering-process-controlled transport: dissolved lithium decreases downstream (from 31.7 to 2.9 µg/L) while δ7Li increases, through adsorption onto suspended particles and sediments. Indicative coordinates (Wuhan).

δ7Li in ‰ (per mil) Values of the same system

Standard : L-SVEC, Non précisé dans la publication

ValueRangenMineral or matrixSource
7.6 / 21.3 ‰
Upstream-to-downstream increase quoted by the review after Wang et al. (2015), Geochimica et Cosmochimica Acta 151:117-132. Second-hand value, not checked in the original paper.
Song et al. (2025), The evolution of lithium resources and isotopic composition in salt l…
21.4 ‰1filtered river water (0.45 µm)
One analysis, Table 2. Sample CJ-W1 collected in the Jiangling Basin (July 2021); the sampling section calls it HJ-W1.
Yu et al. (2024), Factors controlling lithium accumulation in brines from Upper Cretaceou…

87Sr/86Sr isotope ratio, no unit Values of the same system

Standard : NIST SRM 987

ValueRangenMineral or matrixSource
0.7113361filtered river water (0.45 µm)
One analysis, Table 2. Sample CJ-W1 collected in the Jiangling Basin (July 2021); the sampling section calls it HJ-W1.
Yu et al. (2024), Factors controlling lithium accumulation in brines from Upper Cretaceou…

δ18O in ‰ (per mil) Values of the same system

Standard : V-SMOW

ValueRangenMineral or matrixSource
−7.7 ‰1filtered river water (0.45 µm)
One analysis, Table 2. Sample CJ-W1 collected in the Jiangling Basin (July 2021); the sampling section calls it HJ-W1.
Yu et al. (2024), Factors controlling lithium accumulation in brines from Upper Cretaceou…

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

Standard : V-SMOW

ValueRangenMineral or matrixSource
−57.2 ‰1filtered river water (0.45 µm)
One analysis, Table 2. Sample CJ-W1 collected in the Jiangling Basin (July 2021); the sampling section calls it HJ-W1.
Yu et al. (2024), Factors controlling lithium accumulation in brines from Upper Cretaceou…

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

Standard : JMC 3-0749L

ValueRangenMineral or matrixSource
0.37 / 0.83 ‰
Dissolved zinc; range compiled by the review from Little et al. (2014), Geochimica et Cosmochimica Acta 125:673-693.
Ding et al. (2024), Review on zinc isotopes in river systems: distribution and applicatio…

δ60Ni in ‰ (per mil) Values of the same system

Standard : NIST SRM 986

ValueRangenMineral or matrixSource
1.27 ± 0.08 ‰1.19 / 1.34 ‰3filtered river water (dissolved nickel)
Mean and standard deviation recalculated from 3 values. Chang Jiang upstream of Wuhan and at Wuhan (CJ-1, CJ-2, CJ-5): the heaviest river of the study. River heavier than continental silicate rocks, as for Cu and Zn: partitioning between dissolved phase and particles.
Cameron et Vance (2014), Heavy nickel isotope compositions in rivers and the oceans, Geoc…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Yangtze River (Changjiang), isotope signatures. https://www.isofind.tech/isotopes/en/sites/yangtse-changjiang/ (accessed 2026-10-13).

@misc{isofind2026yangtzeriverchangjiangisotope,
  title = {Yangtze River (Changjiang), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/yangtse-changjiang/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13