Hematite-goethite ratios at pH 2-13 and 25-170°C: A time-resolved synchrotron X-ray diffraction studyDOI: info:10.1016/j.chemgeo.2022.120995v. 606Elsevier
Chen, Si Athena, Heaney, Peter J., Post, Jeffrey E., Eng, Peter J., and Stubbs, Joanne E. 2022. "Hematite-goethite ratios at pH 2-13 and 25-170°C: A time-resolved synchrotron X-ray diffraction study." Chemical Geology, 606. https://doi.org/10.1016/j.chemgeo.2022.120995.