Determination of pore structures and dynamics of fluids in hydrated cements and natural shales by various <sup>1</sup>H and <sup>129</sup>Xe NMR methods
Javed, Muhammad Asadullah; Komulainen, Sanna; Daigle, Hugh; Zhang, Boyang; Vaara, Juha; Zhou, Bing; Telkki, Ville-Veikko (2019-03-01)
Javed, M., Komulainen, S., Daigle, H., Zhang, B., Vaara, J., Zhou, B., Telkki, V. (2019) Determination of pore structures and dynamics of fluids in hydrated cements and natural shales by various 1H and 129Xe NMR methods. Microporous and Mesoporous Materials, 281, 66-74. doi:10.1016/j.micromeso.2019.02.034
© 2019 The Authors. Published by Elsevier Inc. This is an open access article under the CC BY license (http://creativecommons.org/licenses/BY/4.0/).
https://creativecommons.org/licenses/by/4.0/
https://urn.fi/URN:NBN:fi-fe2019041712678
Tiivistelmä
Abstract
Cements and shales play a vital role in the construction and energy sectors. Here, we use a set of advanced NMR methods to characterize the porous networks and dynamics of fluids in hydrated cement and shale samples. We compare the properties of cements from two different manufacturers, BASF and Portland, as well as shales brought from USA and China. 129Xe NMR spectra of xenon gas adsorbed in the samples indicate that the capillary mesopores are smaller and the exchange between free and confined gas is slower in the Portland than in the BASF cement samples. The pores probed by xenon in the shale samples from USA are significantly smaller than in the cement samples, partially in the micropore region. There is a substantial difference in between the 129Xe spectra of shales from USA and China. Whereas the latter show a clear signature of paramagnetic impurities by exhibiting large negative 129Xe chemical shifts (referenced to the free gas), the samples from USA lack the negative chemical shifts but feature large positive shift values, which may indicate the presence of micropores and/or paramagnetic defects. 1H NMR cryoporometry measurements using acetonitrile as probe liquid allowed the observation of mesopores in the shale samples as well, and T2-T2 relaxation exchange experiment enabled the quantification of the exchange rates between free and confined acetonitrile.
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