*This material is partly based upon work supported by National Science Foundation under Grant No. EAR1225733
| Title | Cited by | Year |
|---|---|---|
Decoupling feldspar dissolution and precipitation rates at near-equilibrium with Si isotope tracers: Implications for modeling silicate weathering. Zhu C, Rimstidt JD, ‡Zhang YL, ‡Kang JT, Yuan HL. Geochimica et Cosmochimica Acta. 271:132-153. DOI | N/A | 2020 |
Unidirectional kaolinite dissolution rates at near-equilibrium and near-neutral pH conditions. Gong, L., Rimstidt, J.D.†, ‡Zhang, Y.L., Chen K.Y. and Zhu, C. Applied Clay Science 183. DOI | N/A | 2020 |
Measuring silicate mineral dissolution rates using Si isotope doping. Zhu C, Liu ZY, Wang C, Scheafer A, Lu P, Zhang GR, Zhang YL, Georg RB, Rimstidt JD and Yuan H. Chemical Geology DOI. | 16 | 2006 |
*A stable isotope doping method to test the range of applicability of detailed balance. Liu, Z.Y., Zhang, Y.L., Yuan, H.L., Rimstidt, J.D. and Zhu, C. Geochemical Perspective Letters 2:78-86. | 11 | 2016 |
Coprecipitation in the barite isostructural family: 1. Binary mixing properties. Zhu, C. Geochimica et Cosmochimica Acta 68(16): 3327-3337 | 73 | 2004 |