• norsk
    • English
  • norsk 
    • norsk
    • English
  • Logg inn
Vis innførsel 
  •   Hjem
  • Fakultet for naturvitenskap (NV)
  • Institutt for fysikk
  • Vis innførsel
  •   Hjem
  • Fakultet for naturvitenskap (NV)
  • Institutt for fysikk
  • Vis innførsel
JavaScript is disabled for your browser. Some features of this site may not work without it.

Intercalation Phenomena of Carbon Dioxide, Water or Ions in Smectite Clay

Miranda, Leander Edward Michels Brito
Doctoral thesis
Åpne
Fulltext not available (Låst)
Permanent lenke
http://hdl.handle.net/11250/2375060
Utgivelsesdato
2015
Metadata
Vis full innførsel
Samlinger
  • Institutt for fysikk [1805]
Sammendrag
Smectites, or swelling clays, are layered porous materials based on two-dimensional

stacks of inorganic layers. The non-equivalent substitutions of atoms generate a

negative charge on each layer surface which is balanced by exchangeable interlayer

cations. These cations are responsible for the differences in the physicochemical

behavior of smectites such as plasticity and swelling. The large scientific and

technological interest in smectites is connected to their ability to swell, most

commonly caused by their interactions with water (H2O) or carbon dioxide (CO2).

Smectites are rarely found in nature without H2O, that’s why understanding this

interaction is of paramount importance. While for CO2 the attracted interest in the

scientific community in recent years, is partly because clays, being cheap,

environmental friendly and abundant, can be used to capture anthropogenic CO2

and also because geological structures are used as storage sites.

This thesis contains experimental studies on intercalation of H2O and CO2 in

smectites. The study was systematically done in a synthetic smectite Mfluorohectorite,

with M referring to the interlayer cations Li+, Na+ and Ni2+. The main

objective of this work was to comprehend the role that the aforementioned cations

play in the intercalation process. More specifically, how these cations influence: (i)

the kinetics of intercalation of CO2 molecules when a fluorohectorite is exposed to

different sets of CO2 pressure and temperature conditions; (ii) water

intercalation/water vapor transport when a fluorohectorite is under different sets of

relative humidity and temperature. The physical processes and phenomena

described within this thesis were studied mainly by X-ray Diffraction.

The results show the strong cation dependence on intercalation of H2O and CO2. For

each cation-fluorohectorite system some unique features were observed, such as

kinetics of intercalation of CO2 and H2O stable hydration states.
Utgiver
NTNU
Serie
Doctoral thesis at NTNU;2015:319

Kontakt oss | Gi tilbakemelding

Personvernerklæring
DSpace software copyright © 2002-2019  DuraSpace

Levert av  Unit
 

 

Bla i

Hele arkivetDelarkiv og samlingerUtgivelsesdatoForfattereTitlerEmneordDokumenttyperTidsskrifterDenne samlingenUtgivelsesdatoForfattereTitlerEmneordDokumenttyperTidsskrifter

Min side

Logg inn

Statistikk

Besøksstatistikk

Kontakt oss | Gi tilbakemelding

Personvernerklæring
DSpace software copyright © 2002-2019  DuraSpace

Levert av  Unit