UCL Discovery
UCL home » Library Services » Electronic resources » UCL Discovery

Ca isotope constraints on chemical weathering processes: Evidence from headwater in the Changjiang River, China

Chen, BB; Li, SL; Pogge von Strandmann, PAE; Sun, J; Zhong, J; Li, C; Ma, TT; ... Liu, CQ; + view all (2020) Ca isotope constraints on chemical weathering processes: Evidence from headwater in the Changjiang River, China. Chemical Geology , 531 , Article 119341. 10.1016/j.chemgeo.2019.119341. Green open access

[thumbnail of Manuscript-Chen_Chemical Geology.pdf]
Preview
Text
Manuscript-Chen_Chemical Geology.pdf - Accepted Version

Download (1MB) | Preview

Abstract

This study aims to clarify the relationship between chemical weathering of rocks and the carbon budget of rivers and better understand the weathering mechanisms of plateau watersheds. We chose to study the Jinsha River, which originates from the Tibetan Plateau and also is in the upper reaches of the Changjiang River. Analysis of hydrochemistry, radiogenic strontium isotope and stable calcium isotopes were conducted of the Jinsha River water samples, which were collected along its mainstream and main tributaries in the summer. The results show that the water chemistry of the mainstream waters is dominated by evaporite weathering, which have low 87Sr/86Sr values (0.7098–0.7108) and wide range of Sr contents (2.70–9.35 μmol/L). In contrast, tributaries of the Jinsha River have higher 87Sr/86Sr (0.7090–0.7157) and lower Sr contents (∼1 μmol/L). Moreover, the Ca isotopic compositions in the mainstream (0.87–1.11‰) are heavier than the tributaries (0.68–0.88‰) and could not be fully explained by the conventional mixing of different sources. We suggest that secondary carbonate precipitation fractionates Ca isotopes in the Jinsha River, and fractionation factors are between 0.99935 and 0.99963. At least 66% of Ca was removed in the mainstream of the Jinsha River through secondary mineral precipitation, and the average value is ∼35% in the tributaries. The results highlight that evaporite weathering results in more carbonate precipitation influencing Ca transportation and cycling in the riverine system constrained by stable Ca isotopic compositions and water chemistry.

Type: Article
Title: Ca isotope constraints on chemical weathering processes: Evidence from headwater in the Changjiang River, China
Open access status: An open access version is available from UCL Discovery
DOI: 10.1016/j.chemgeo.2019.119341
Publisher version: https://doi.org/10.1016/j.chemgeo.2019.119341
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
Keywords: Ca isotopes, Chemical weathering, Secondary carbonate precipitation, Isotope fractionation.
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: https://discovery.ucl.ac.uk/id/eprint/10087308
Downloads since deposit
58Downloads
Download activity - last month
Download activity - last 12 months
Downloads by country - last 12 months

Archive Staff Only

View Item View Item