In the past 10 years, we have been using the isotope doping method from the field of chemistry and biology together with newly available non-traditional stable isotopes to advance the near-equilibrium reaction kinetics.
(Uundergraduate, Ggraduate, PDpostdoc authors supervised by Zhu; *corresponding author)
- Schott J, Saldi GD, Zhu C, Gong L and Chen KY (2024) Albite dissolution and precipitation kinetics as a function of departure from equilibrium in 29Si spiked aqueous solutions at 150 and 180° C: Direct evidence for the decrease of the forward dissolution rate and the reactive surface area with the reaction progress. Geochimica et Cosmochimica Acta. DOI.
- Chen MK, Gong L, Jacques Schott, Lu P, Song YC, Chen KY, Yuan HL, Sun J, Apps J and Zhu C. Coupled feldspar dissolution and secondary mineral precipitation in batch systems: 6. labradorite dissolution and calcite and clay precipitation. Submitted to Geochimica et Cosmochimica Acta. June 20, 2024.
- GChen MK, Lu P, Song YC and Zhu C (2023) Geochemical modeling to aid experimental design for multiple isotope tracer studies of coupled dissolution and precipitation reaction kinetics, Acta Geochimica, accepted October 27, 2023.
- GKang JT, Bracco JN, Rimstidt JR, Zhu GH, Huang F and *Zhu C (2022). Ba attachment and detachment fluxes to and from barite surfaces in 137Ba-enriched solutions with variable [Ba2+]/[SO42-] ratios near solubility equilibrium. Geochimica et Cosmochimica Acta. v317,180-200. DOI.
- *Zhu C, GZhang YL, Rimstidt JD, Gong L, UBurkhart, JA, Chen KY and Yuan HL (2021) Testing hypotheses of albite dissolution mechanisms at near-equilibrium using Si isotope tracers. Geochimica et Cosmochimica Acta. v303, 15-37. DOI.
- *Zhu C, Rimstidt JD, GZhangYL, GKangJT, Schott J and Yuan HL (2020) Decoupling feldspar dissolution and precipitation rates at near-equilibrium with Si isotope tracers: Implications for modeling silicate weathering. Geochimica et Cosmochimica Acta. v271, 132-153. DOI.
- Gong L, Rimstidt JD†, GZhang YL, Chen KY and *Zhu C (2019) Unidirectional kaolinite dissolution rates at near-equilibrium and near-neutral pH conditions. Applied Clay Science v182. DOI.
- GZhang YL, Gong L, Chen KY, UBurkhart J, Yuan HL and *Zhu C (2020) A method for Si isotope tracer kinetics experiments: Using Q-ICP-MS to obtain 29Si/28Si ratios in aqueous solutions. Chemical Geology v531. DOI;
- *Zhu C, PDLiu ZY, PDWang C, USchaefer A, GLu P, GZhang GR, GZhang YL, Georg RB, Rimstidt JD and Yuan HL (2016) Measuring silicate mineral dissolution rates using Si isotope doping. Chemical Geology, 445: 146-163. DOI
- PDLiu ZY, GZhang YL, Yuan HL, Rimstidt JD and *Zhu C (2016) A stable isotope doping method to test the range of applicability of detailed balance. Geochemical Perspective Letters 2(1): 78-86. DOI
- Gruber C, Zhu C, Georg, RB, Zakon J and Ganor J (2014) Resolving the gap between laboratory and field rates of feldspar weathering. Geochimica et Cosmochimica Acta 147: 90–106. DOI.
- Gruber C, Harpaz L, Zhu C, Bullen TD and Ganor J (2013) A new approach for measuring dissolution rates of silicate minerals by using silicon isotope. Geochimica et Cosmochimica Acta 104: 261-280. DOI.