Infrared spectroscopy of ferrihydrite: evidence for the presence of structural hydroxyl groupsClay Minerals - Tập 14 Số 2 - Trang 109-114 - 1979
James Russell
AbstractIR spectroscopy has shown that adsorbed water is almost completely
removed from ferrihydrite by evacuation at room temperature. Absorption bands at
3615 and 3430 cm−1 appearing thereafter are interpreted as arising from OH
groups located respectively at the surface and deeper in the structure. These
groups are readily converted to OD on treatment with D2O vapour and this has
allowed the OH... hiện toàn bộ
The origin and formation of clay minerals in soils: past, present and future perspectivesClay Minerals - Tập 34 Số 1 - Trang 7-25 - 1999
M. J. Wilson
AbstractThe origin and formation of soil clay minerals, namely micas,
vermiculites, smectites, chlorites and interlayered minerals, interstratified
minerals and kaolin minerals, are broadly reviewed in the context of research
over the past half century. In particular, the pioneer overviews of Millot,
Pedro and Duchaufour in France and of Jackson in the USA, are considered in the
light of selected ... hiện toàn bộ
Magnetite in soils: I. The synthesis of single-domain and superparamagnetic magnetiteClay Minerals - Tập 22 Số 4 - Trang 411-422 - 1986
R. M. Taylor, Barbara A. Maher, Peter Self
AbstractA series of experiments has been carried out to investigate the possible
formation of magnetite, Fe3O4, under ambient soil-forming conditions. Rapid and
easy synthesis of magnetite was achieved through controlled oxidation of
Fe2+solutions at room temperatures and near neutral pH values. The synthetic
products were found to range in size between 0·01–0·07µm (mean diameter) and
hence span t... hiện toàn bộ
Chemically modified smectitesClay Minerals - Tập 38 Số 1 - Trang 127-138 - 2003
Peter Komadel
AbstractThis paper summarizes recent results obtained on chemical modifications
of smectites. These include replacement of exchangeable cations with protons, a
process connected with smectite autotransformation – attack of protons on the
layers and liberation of central atoms from the octahedral and tetrahedral
sheets, causing modification of the acid sites on the particles. More severe
modificati... hiện toàn bộ
Halloysite nanotubes as a new drug-delivery system: a reviewClay Minerals - Tập 51 Số 3 - Trang 469-477 - 2016
Muhammad Hanif, Fazila Jabbar, Sana Sharif, Ghulam Abbas, Athar Farooq, Mubashir Aziz
AbstractNew drug-delivery systems have remained a challenge for pharmaceutical
scientists due to the use of expensive polymers and the low loading capacity of
prepared nanoparticles. There is pressure to develop formulations that contain
not only cheaper materials but also have controlled-release properties.
Halloysite nanotubes (HNTs) are a naturally occurring clay mineral similar to
kaolin, poss... hiện toàn bộ
The adsorption of aliphatic alcohols by montmorillonite and kaoliniteClay Minerals - Tập 8 Số 2 - Trang 213-227 - 1969
William L. German, David A. Harding
Adsorption isotherms for an homologous series of primary aliphatic alcohols from
aqueous solution by montmorillonite and kaolinite saturated with either sodium
or calcium ions have been determined. The results show that adsorption is a
function of chain length and exchangeable cation in the case of the more
insoluble alcohols. Exchangeable cation does not affect the adsorption of the
soluble alcoh... hiện toàn bộ