Zobrazeno 1 - 10
of 97
pro vyhledávání: '"Georgios D. Chryssikos"'
Autor:
George E. Christidis, Carlos Aldana, Georgios D. Chryssikos, Vassilis Gionis, Hussein Kalo, Matthias Stöter, Josef Breu, Jean-Louis Robert
Publikováno v:
Minerals, Vol 8, Iss 8, p 314 (2018)
A series of laponites and synthetic OH- and fluorinated hectorites prepared from hydrothermal and melting experiments at both industrial and laboratory scale were examined with XRD and FTIR (MIR and NIR) to determine their mineralogical composition a
Externí odkaz:
https://doaj.org/article/1ac46ba24c1343bcb91c797efbc68176
Publikováno v:
Clays and Clay Minerals. 70:796-807
Many kaolinites are known to exhibit limited intercalation capacity which affects their usage. Some reports have linked this lack of reactivity to particular structural features or to slow kinetics; others recommended increasing intercalation tempera
Publikováno v:
Applied Clay Science. 161:354-363
The aim of the present study was to test the applicability of the O-D method, a newly developed spectroscopic layer charge measurement technique, to measure the charge present on wettable surfaces of mixed-layer illite-smectite (I-S). The O-D method
Publikováno v:
Applied Clay Science. 160:81-87
The facile and accurate measurement of the layer charge of dioctahedral smectite has been demonstrated recently by means of the O-D method, an infrared-based technique capable of recording the exact position of a dangling O-D (O H) bond stretch of in
Autor:
Marek Szczerba, Eirini Siranidi, Zuzanna Ciesielska, Fevronia T. Andreou, Arkadiusz Derkowski, Vassilis Gionis, Georgios D. Chryssikos, Barbara Barylska
Publikováno v:
Applied Clay Science. 212:106209
The selective self-assembly of small molecules in the interlayer of kaolinite is a fundamentally important and technologically relevant process, typically studied ex situ by X-ray diffraction (XRD). Near-infrared (NIR) spectroscopy is now introduced
Autor:
Katja Emmerich, Constantinos Tsiantos, Vassilis Gionis, Arkadiusz Derkowski, Artur Kuligiewicz, Georgios D. Chryssikos, George E. Christidis
Publikováno v:
Clays and Clay Minerals. 63:443-456
Layer charge (LC) is a fundamental property of smectite but its measurement remains challenging and tedious to apply on a high-throughput basis. The present study demonstrates that the position of a sharp, high-energy O—D stretching band of adsorbe
Autor:
Vassilis Gionis, Georgios D. Chryssikos, Marek Szczerba, Arkadiusz Derkowski, Artur Kuligiewicz
Publikováno v:
Clays and Clay Minerals. 63:15-29
An overlap of bands produced by the O−H stretching vibrations of H2O (O–Hw) and structural OH (O−Hs) in smectite hampers the study by infrared spectroscopy (IR) of both their layer and interlayer structure. The present study re-evaluated the D2
Autor:
Maria Tsampodimou, Vanessa-Jane Bukas, Georgios D. Chryssikos, Vassilis Gionis, Elizabeth T. Stathopoulou
Publikováno v:
American Mineralogist. 100:195-202
Sepiolite is an industrially important clay mineral of the palygorskite-sepiolite group with alternating 2:1 ribbons and hydrated tunnels. Dry sepiolite, Mg 8 Si 12 O 30 (OH) 4 (OH 2 ) 4 , loses half of its OH 2 content upon further heating and under
Autor:
Paraskevi L. Tsiolaki, Stavros J. Hamodrakas, Vassiliki A. Iconomidou, Georgios D. Chryssikos, Vassilis Gionis, Fotis A. Baltoumas, Nikolaos N. Louros
Publikováno v:
Journal of structural biology. 199(2)
Human islet amyloid polypeptide (hIAPP) is the major protein component of extracellular amyloid deposits, located in the islets of Langerhans, a hallmark of type II diabetes. The underlying mechanisms of IAPP aggregation have not yet been clearly def
Autor:
Georgios D. Chryssikos, Artur Kuligiewicz, Andrey G. Kalinichev, Vassilis Gionis, Marek Szczerba, Arkadiusz Derkowski
Publikováno v:
Clays and Clay Minerals
Clays and Clay Minerals, Clay Minerals Society, 2016, 64 (4), pp.452-471. ⟨10.1346/ccmn.2016.0640409⟩
Clays and Clay Minerals, Clay Minerals Society, 2016, 64 (4), pp.452-471. ⟨10.1346/ccmn.2016.0640409⟩
International audience; Experimental studies have shown that a sharp, high-frequency IR band at ~3615 cm-1 (in H2O form) and at ~2685 cm-1 (in D2O form) is a common feature for all smectites, and its position correlates with layer charge. In order to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::07ac70b300e2b992ebe15076d779ffec
http://hal.in2p3.fr/in2p3-01577621/document
http://hal.in2p3.fr/in2p3-01577621/document