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Devineu, K., Bihannic, I., Michot, L., Villieras, F., Masrouri, F., Cuisinier, O., Fragneto, G. and Michau, N. (2006) In Situ Neutron Diffraction Analysis of the Influence of Geometric Confinement on Crystalline Swelling of Montmorillonite. Applied Clay Science, 31, 76-84.
https://doi.org/10.1016/j.clay.2005.08.006

has been cited by the following article:

• TITLE: Small Angle Neutron Scattering Investigation of Compressed Bentonite Plugs

  AUTHORS: Tomasz Blach, Heinz-Gerd Holl

  KEYWORDS: SANS, USANS, Bentonite, Porosity, Swelling Process

  JOURNAL NAME: Journal of Minerals and Materials Characterization and Engineering, Vol.7 No.5, September 11, 2019

  ABSTRACT: Bentonite plugs manufactured with and without a polymer binder were studied using Small Angle Neutron Scattering (SANS) and Ultra Small Angle Neutron Scattering (USANS) techniques. We have subjected the samples to hydration by evaporating water and then applied CD4 methane at a Zero Average Con-trast (ZAC) pressure (about 48.3 MPa/7000psi) to measure the accessible and inaccessible pores and channels. The data show that introduction of moisture has an immediate effect on the smallest pores, with swelling preventing access by the methane; however the larger network appears to be little affected by the addition of the moisture. The addition of a binder to the plug creates a greater number of open pores in the micron and above size regime, indicating that the polymer is vital in creating larger channels, which aids the movement of mois-ture throughout the plug, at the expense of sealing the smallest ones. This sug-gests that the polymer binder helps in the self-healing process in the clays and makes the structure more stable. The process of plug manufacturing and drying produces a chaotic system of aggregates in the sample, which forms packed clusters 130 nm in size. Addition of moisture destroys this structure. Addition of water to the dried plug material showed that at 18 weight% a dual layer of water has formed in the montmorillonite layer of the clay, separating the montmorillonite layers by 17 A. Increase to 33 weight% of water has added an extra layer with basal spacing of 19 A. The clay hydration with vapor and directly deposited liquid appear to delaminate some of the clay affecting the fractality index at the micron sizes. Mechanical compression had a significant effect on the polymerised sample, encouraging larger water-conducting channels to form.