Characterization of Natural Consolidated Halloysite Nanotube Structures
Abstract
Halloysite is a unique 1:1 clay mineral frequently appearing with nanotubular morphology, and having surfaces of different polarity with interesting and important technological applications. HNTs can be consolidated naturally in the earth by pressure and thermal flows. In this study of natural consolidated HNTs, the strength and hardness of these materials were found to be dependent on the presence of impurities (gibbsite, alunite, quartz, and other silica minerals), which accounted for the increased stability of such samples. In the absence of impurities, the strength of consolidated HNTs was significantly lower. The first 3D mapping of the pore structure of natural consolidated HNT is provided. The contributions of the porosity within the nanotubes and between the nanotubes were delineated using a combination of non-invasive ultra-small and small-angle X-ray scattering (USAXS/SAXS) analyses, BET/BJH pore size analyses, and computed tomography studies. A total porosity of 40%, as determined by X-ray attenuation and He porosimetry, was found for the natural consolidated HNTs, of which about one-third was due to the inter-HNT porosity. Nano-X-ray computed tomography (nano-XCT) analyses also indicated that 76% of the inter-HNT pores were smaller than 150 nm in diameter. The intra-HNT pore size determined by combined USAXS/SAXS and BET/BJH was aboutmore »
- Authors:
- Publication Date:
- Research Org.:
- Univ. of Utah, Salt Lake City, UT (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Basic Energy Sciences (BES)
- OSTI Identifier:
- 1833113
- Alternate Identifier(s):
- OSTI ID: 1836664
- Grant/Contract Number:
- SC0019285
- Resource Type:
- Published Article
- Journal Name:
- Minerals
- Additional Journal Information:
- Journal Name: Minerals Journal Volume: 11 Journal Issue: 12; Journal ID: ISSN 2075-163X
- Publisher:
- MDPI AG
- Country of Publication:
- Switzerland
- Language:
- English
- Subject:
- 36 MATERIALS SCIENCE; halloysite; nanotube; porosity; hardness; spacing; wetting
Citation Formats
Jin, Jiaqi, Assemi, Shoeleh, Asgar, Hassnain, Gadikota, Greeshma, Tran, Thang, Nguyen, William, McLennan, John D., and Miller, Jan D. Characterization of Natural Consolidated Halloysite Nanotube Structures. Switzerland: N. p., 2021.
Web. doi:10.3390/min11121308.
Jin, Jiaqi, Assemi, Shoeleh, Asgar, Hassnain, Gadikota, Greeshma, Tran, Thang, Nguyen, William, McLennan, John D., & Miller, Jan D. Characterization of Natural Consolidated Halloysite Nanotube Structures. Switzerland. https://doi.org/10.3390/min11121308
Jin, Jiaqi, Assemi, Shoeleh, Asgar, Hassnain, Gadikota, Greeshma, Tran, Thang, Nguyen, William, McLennan, John D., and Miller, Jan D. Wed .
"Characterization of Natural Consolidated Halloysite Nanotube Structures". Switzerland. https://doi.org/10.3390/min11121308.
@article{osti_1833113,
title = {Characterization of Natural Consolidated Halloysite Nanotube Structures},
author = {Jin, Jiaqi and Assemi, Shoeleh and Asgar, Hassnain and Gadikota, Greeshma and Tran, Thang and Nguyen, William and McLennan, John D. and Miller, Jan D.},
abstractNote = {Halloysite is a unique 1:1 clay mineral frequently appearing with nanotubular morphology, and having surfaces of different polarity with interesting and important technological applications. HNTs can be consolidated naturally in the earth by pressure and thermal flows. In this study of natural consolidated HNTs, the strength and hardness of these materials were found to be dependent on the presence of impurities (gibbsite, alunite, quartz, and other silica minerals), which accounted for the increased stability of such samples. In the absence of impurities, the strength of consolidated HNTs was significantly lower. The first 3D mapping of the pore structure of natural consolidated HNT is provided. The contributions of the porosity within the nanotubes and between the nanotubes were delineated using a combination of non-invasive ultra-small and small-angle X-ray scattering (USAXS/SAXS) analyses, BET/BJH pore size analyses, and computed tomography studies. A total porosity of 40%, as determined by X-ray attenuation and He porosimetry, was found for the natural consolidated HNTs, of which about one-third was due to the inter-HNT porosity. Nano-X-ray computed tomography (nano-XCT) analyses also indicated that 76% of the inter-HNT pores were smaller than 150 nm in diameter. The intra-HNT pore size determined by combined USAXS/SAXS and BET/BJH was about 10 nm. This pore network information is essential for the utilization of natural consolidated HNTs as a model geomaterial to investigate the effects of surface characteristics on confined fluid flow.},
doi = {10.3390/min11121308},
journal = {Minerals},
number = 12,
volume = 11,
place = {Switzerland},
year = {Wed Nov 24 00:00:00 EST 2021},
month = {Wed Nov 24 00:00:00 EST 2021}
}
https://doi.org/10.3390/min11121308
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