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Mineralogical Characterization of Di Linh Bentonite, Vietnam: A Methodological Approach of X-ray Diffraction and Transmission Electron Microscopy

Hoang-Minh, Thao (författare)
Hanoi University of Science, Vietnam National University
Nguyen-Thanh, Lan (författare)
Institute of Geography and Geology, Ernst-Moritz-Arndt-University of Greifswald, Technical University of Darmstadt
Nguyen, Thuy-Duong (författare)
Hanoi University of Science, Vietnam National University
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Nguyen, Duc-Thanh (författare)
Vietnam Atomic Energy Institute
Lai, Le Thi (författare)
Institute of Geological Sciences, Vietnam Academy of Science and Technology
Thuyet, Nguyen Thi Minh (författare)
Hanoi University of Science, Vietnam National University
Kasbohm, Jörn (författare)
Institute of Geography and Geology, Ernst-Moritz-Arndt-University of Greifswald, University of Greifswald, GeoENcon Ltd
Pusch, Roland (författare)
Luleå tekniska universitet,Geoteknologi
Knutsson, Sven (författare)
Luleå tekniska universitet,Geoteknologi
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 (creator_code:org_t)
Hanoi : Vietnam National University Press, Hanoi, 2014
2014
Engelska.
Ingår i: Proceedings of 13th International Symposium on Mineral Exploration (ISME-XIII). - Hanoi : Vietnam National University Press, Hanoi. - 9786046215400 ; , s. 143-148
  • Konferensbidrag (refereegranskat)
Abstract Ämnesord
Stäng  
  • Vietnam has decided to establish nuclear power as further energy option. In order to develop a Vietnamese reference bentonite as potential barrier in a final repository for high radioactive waste, a detailed mineralogical investigation of Di Linh bentonite (Lam Dong province), lacustrine clay, was carried out by different methods especially transmission electron microscopy (TEM) linked with energy-dispersive X-ray (EDX). From a sample homogenized from 5 tones of the bentonite, mineral formulae of clay particles was calculated The calculation also focuses on randomly interstratifications of two and three members. The fraction <2 μm of Di Linh bentonite is composed mainly by montmorillonite (Ca0.06Mg0.03Na0.09K0.03Al1.39Fe0.25Mg0.26(OH)2 Si3.96Al0.04O10) and regular ordering (R1) illite-smectite interstratifications with K- and charge-deficiency (Ca0.04Mg0.07Na0.18K0.16Al1.76Fe0.08Mg0.16(OH)2Si3.62Al0.38O10). Additionally, Fe-poor kaolinite-smectite-vermiculite interstratifications and trace of Fe-rich chloritesmectite- vermiculite interstatifications were identified. TEM-investigations showed analytical proofs of the sedimentary character of smectite formation in the Di Linh deposit. Parent muscovite was weathered in several steps in two different environments: (i) K-leaching and layer-wise alteration into kaolinite; (ii) further edge- controlled alteration of mica into lathlike montmorillonite particles under dissolution of kaolinite layers from former kaolinite-mica intergrowths. Mineralogical composition of the Di Linh bentonite with mainly montmorillonite and illite-rich illite-smectite interstratifications shows that the Di Linh bentonite can be a suitable barrier candidate in final repositories.

Ämnesord

TEKNIK OCH TEKNOLOGIER  -- Samhällsbyggnadsteknik -- Geoteknik (hsv//swe)
ENGINEERING AND TECHNOLOGY  -- Civil Engineering -- Geotechnical Engineering (hsv//eng)

Nyckelord

Bentonite
Transmission electron microscopy
X-ray diffraction
Montmorillonite
Interstratification
Geoteknik
Soil Mechanics

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