eprintid: 1472611 rev_number: 22 eprint_status: archive userid: 608 dir: disk0/01/47/26/11 datestamp: 2015-11-16 14:19:55 lastmod: 2021-09-19 23:42:57 status_changed: 2015-11-16 14:19:55 type: article metadata_visibility: show creators_name: Suter, JL creators_name: Kabalan, L creators_name: Khader, M creators_name: Coveney, PV title: Ab initio molecular dynamics study of the interlayer and micropore structure of aqueous montmorillonite clays ispublished: pub divisions: UCL divisions: B04 divisions: C06 divisions: F56 note: © 2015 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/) abstract: Ab initio molecular dynamics simulations have been performed to gain an understanding of the interfacial microscopic structure and reactivity of fully hydrated clay edges. The models studied include both micropore and interlayer water. We identify acidic sites through dissociation mechanisms; the resulting ions can be stabilized by both micropore and interlayer water. We find clay edges possess a complex amphoteric behavior, which depends on the face under consideration and the location of isomorphic substitution. For the neutral (1 1 0) surface, we do not observe any dissociation on the timescale accessible. The edge terminating hydroxyl groups participate in a hydrogen bonded network of water molecules that spans the interlayer between periodic images of the clay framework. With isomorphic substitutions in the tetrahedral layer of the (1 1 0) clay edge, we find the adjacent exposed apical oxygen behaves as a Brönsted base and abstracts a proton from a nearby water molecule, which in turn removes a proton from an AlOH2 group. With isomorphic substitutions in the octahedral layer of the (1 1 0) clay edge the adjacent exposed apical oxygen atom does not abstract a proton from the water molecules, but increases the number of hydrogen bonded water molecules (from one to two). Acid treated clays are likely to have both sites protonated. The (0 1 0) surface does not have the same interfacial hydrogen bonding structure; it is much less stable and we observe dissociation of half the terminal SiOH groups (triple bond; length of mdashSisingle bondOsingle bondH → triple bond; length of mdashSisingle bondO− + H+) in our models. The resulting anions are stabilized by solvation from both micropore and interlayer water molecules. This suggests that, when fully hydrated, the (0 1 0) surface can act as a Brönsted acid, even at neutral pH. date: 2015-11-15 date_type: published official_url: http://dx.doi.org/10.1016/j.gca.2015.07.013 oa_status: green full_text_type: pub language: eng primo: open primo_central: open_green verified: verified_manual elements_id: 1076087 doi: 10.1016/j.gca.2015.07.013 language_elements: ENG lyricists_name: Coveney, Peter lyricists_name: Suter, James lyricists_id: PCOVE58 lyricists_id: JSUTE05 actors_name: Coveney, Peter actors_name: Gibson, Alice actors_id: PCOVE58 actors_id: AGIBS47 actors_role: owner actors_role: impersonator full_text_status: public publication: Geochimica et Cosmochimica Acta volume: 169 pagerange: 17-29 issn: 0016-7037 citation: Suter, JL; Kabalan, L; Khader, M; Coveney, PV; (2015) Ab initio molecular dynamics study of the interlayer and micropore structure of aqueous montmorillonite clays. Geochimica et Cosmochimica Acta , 169 pp. 17-29. 10.1016/j.gca.2015.07.013 <https://doi.org/10.1016/j.gca.2015.07.013>. Green open access document_url: https://discovery.ucl.ac.uk/id/eprint/1472611/1/1-s2.0-S0016703715004469-main.pdf