Alejandro
Fernandez-Martinez
*a,
Jinhui
Tao
b,
Adam F.
Wallace
*c,
Ian C.
Bourg
*d,
Mark R.
Johnson
e,
James J.
De Yoreo
bf,
Garrison
Sposito
g,
Gabriel J.
Cuello
e and
Laurent
Charlet
a
aUniversité Grenoble Alpes, Université Savoie Mont Blanc, CNRS, IRD, IFSTTAR, ISTerre, 38000 Grenoble, France. E-mail: Alex.Fernandez-Martinez@univ-grenoble-alpes.fr
bPhysical and Computational Sciences Directorate, Pacific Northwest National Laboratory, Richland, Washington 99352, USA
cDepartment of Earth Sciences, University of Delaware, Newark, DE 19716, USA
dDepartment of Civil and Environmental Engineering, Princeton Environmental Institute, Princeton University, Princeton, New Jersey 08544, USA
eInstitut Laue Langevin, 71 Rue de Martyrs, 38000 Grenoble, France
fDepartment of Materials Science and Engineering, University of Washington, Seattle, Washington 98195, USA
gDepartment of Environmental Science, Policy, and Management, University of California, Berkeley, California 94720, USA
First published on 2nd September 2020
Correction for ‘Curvature-induced hydrophobicity at imogolite–water interfaces’ by Alejandro Fernandez-Martinez et al., Environ. Sci.: Nano, 2020, DOI: 10.1039/d0en00304b.
The corrected Acknowledgements section is shown below:
“Barry Bickmore and Kideok K. Kwon are gratefully acknowledged for enriching discussions. Diana Alvarez Fernandez (Alcoa Corp.) is thanked for providing the gibbsite sample. Loïc Vidal (Inst. Sciences des Matériaux de Mulhouse, France) is thanked for TEM analyses. A. F.-M. acknowledges the Région Rhône-Alpes for the financial support received through an Explora'DOC fellowship for a 6 months stay at the University of California, Berkeley. 2PT analysis was performed by A. F. W. with support of the U.S. Department of Energy (DOE), Office of Science, Office of Basic Energy Sciences (BES), Chemical Sciences, Geosciences, & Biosciences (CSGB) Division, under Award Number DE-SC0018439. I. C. B. was supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, Geosciences Program under Award DESC0018419. Molecular dynamics simulations were performed using resources of the National Energy Research Scientific Computing Center (NERSC), which is supported by the U.S. Department of Energy, Office of Science, under Award DE-AC02-05CH11231. The DFS experiment (by J. T.) was performed at the Molecular Foundry, Lawrence Berkeley National Laboratory which is supported by the Office of Science, Office of Basic Energy Sciences, US Department of Energy under Contract DE-AC02-05CH11231. The DFS data analysis (J. T. and J. J. D.) was supported by U.S. Department of Energy, Office of Science, Basic Energy Sciences, Division of Materials Sciences and Engineering, under Award KC020105-FWP12152. Pacific Northwest National Laboratory (PNNL) is operated by Battelle for the Department of Energy under contract No. DE-AC05-76RLO1830.”
The Royal Society of Chemistry apologises for these errors and any consequent inconvenience to authors and readers.
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