Continuous water adsorption states promoted by Ni2+ confined in a synthetic smectite

M.A.S. Altoé; L. Michels; E.C.D. Santos; R. Droppa; G. Grassi; L. Ribeiro; K.D. Knudsen; Heloisa Nunes Bordallo; J.O. Fossum; G.J. Silva

doi:10.1016/j.clay.2016.01.012

Continuous water adsorption states promoted by Ni2+ confined in a synthetic smectite

M.A.S. Altoé, L. Michels, E.C.D. Santos, R. Droppa, G. Grassi, L. Ribeiro, K.D. Knudsen, Heloisa Nunes Bordallo, J.O. Fossum, G.J. Silva

13 Citations (Scopus)

Abstract

The water adsorption isotherms of Ni-fluorohectorite have been obtained from the relative humidity dependence of X-ray diffraction intensities, and continuous transitions between the stable hydration states were observed. This behavior is significantly different from previous studies of Na-fluorohectorite and Li-fluorohectorite smectites. It was also observed that the environmental history of the clay mineral samples is important for the behavior displayed by these isotherms. In addition, based on thermogravimetric and differential scanning calorimetry measurements, it was observed that a complete Ni-fluorohectorite dehydrated state can only be reached at long times (several hours) at 70°C, or at shorter times (minutes) above 150°C. Our observations are consistent with the existence of various forms of Ni²⁺-H₂O complexes in Ni-fluorohectorite, and we suggest that the present results can be extended to other smectites with transition metals as interlayer charge compensating cations, and consequently have significant practical consequences in materials science and other areas.

Original language	English
Journal	Applied Clay Science
Volume	123
Pages (from-to)	83-91
ISSN	0169-1317
DOIs	https://doi.org/10.1016/j.clay.2016.01.012
Publication status	Published - 1 Apr 2016

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title = "Continuous water adsorption states promoted by Ni2+ confined in a synthetic smectite",

abstract = "The water adsorption isotherms of Ni-fluorohectorite have been obtained from the relative humidity dependence of X-ray diffraction intensities, and continuous transitions between the stable hydration states were observed. This behavior is significantly different from previous studies of Na-fluorohectorite and Li-fluorohectorite smectites. It was also observed that the environmental history of the clay mineral samples is important for the behavior displayed by these isotherms. In addition, based on thermogravimetric and differential scanning calorimetry measurements, it was observed that a complete Ni-fluorohectorite dehydrated state can only be reached at long times (several hours) at 70°C, or at shorter times (minutes) above 150°C. Our observations are consistent with the existence of various forms of Ni2+-H2O complexes in Ni-fluorohectorite, and we suggest that the present results can be extended to other smectites with transition metals as interlayer charge compensating cations, and consequently have significant practical consequences in materials science and other areas.",

author = "M.A.S. Alto{\'e} and L. Michels and E.C.D. Santos and R. Droppa and G. Grassi and L. Ribeiro and K.D. Knudsen and {Nunes Bordallo}, Heloisa and J.O. Fossum and G.J. Silva",

year = "2016",

month = apr,

day = "1",

doi = "10.1016/j.clay.2016.01.012",

language = "English",

volume = "123",

pages = "83--91",

journal = "Applied Clay Science",

issn = "0169-1317",

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TY - JOUR

T1 - Continuous water adsorption states promoted by Ni2+ confined in a synthetic smectite

AU - Altoé, M.A.S.

AU - Michels, L.

AU - Santos, E.C.D.

AU - Droppa, R.

AU - Grassi, G.

AU - Ribeiro, L.

AU - Knudsen, K.D.

AU - Nunes Bordallo, Heloisa

AU - Fossum, J.O.

AU - Silva, G.J.

PY - 2016/4/1

Y1 - 2016/4/1

N2 - The water adsorption isotherms of Ni-fluorohectorite have been obtained from the relative humidity dependence of X-ray diffraction intensities, and continuous transitions between the stable hydration states were observed. This behavior is significantly different from previous studies of Na-fluorohectorite and Li-fluorohectorite smectites. It was also observed that the environmental history of the clay mineral samples is important for the behavior displayed by these isotherms. In addition, based on thermogravimetric and differential scanning calorimetry measurements, it was observed that a complete Ni-fluorohectorite dehydrated state can only be reached at long times (several hours) at 70°C, or at shorter times (minutes) above 150°C. Our observations are consistent with the existence of various forms of Ni2+-H2O complexes in Ni-fluorohectorite, and we suggest that the present results can be extended to other smectites with transition metals as interlayer charge compensating cations, and consequently have significant practical consequences in materials science and other areas.

AB - The water adsorption isotherms of Ni-fluorohectorite have been obtained from the relative humidity dependence of X-ray diffraction intensities, and continuous transitions between the stable hydration states were observed. This behavior is significantly different from previous studies of Na-fluorohectorite and Li-fluorohectorite smectites. It was also observed that the environmental history of the clay mineral samples is important for the behavior displayed by these isotherms. In addition, based on thermogravimetric and differential scanning calorimetry measurements, it was observed that a complete Ni-fluorohectorite dehydrated state can only be reached at long times (several hours) at 70°C, or at shorter times (minutes) above 150°C. Our observations are consistent with the existence of various forms of Ni2+-H2O complexes in Ni-fluorohectorite, and we suggest that the present results can be extended to other smectites with transition metals as interlayer charge compensating cations, and consequently have significant practical consequences in materials science and other areas.

U2 - 10.1016/j.clay.2016.01.012

DO - 10.1016/j.clay.2016.01.012

M3 - Journal article

SN - 0169-1317

VL - 123

SP - 83

EP - 91

JO - Applied Clay Science

JF - Applied Clay Science

ER -

Continuous water adsorption states promoted by Ni2+ confined in a synthetic smectite

Abstract

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