Sentence examples for clay components from inspiring English sources
Our study demonstrated how complex interaction between both the organic matter and clay components influences the leachability of HOCs in a compound-specific manner.
The degree of homogeneity and adhesion between the organic (polymer) and inorganic (clay) components can be improved using reactive organoclay, which results in greatly improved properties of the hybrid materials.
Other clay linked features include bands observed at 3696, 3668, 3654 and 3622 cm−1 that are assigned to the outer hydroxyl ions in the structures of the clay components [26, 28].
The clay components are indicated by the Si O Si strong broad band centered at 1041 cm−1, along with the Si O Al band expected at 1011 cm−1011
In earth pigments, the main chromophore responsible for imparting the colour can be a non-clay component like the oxides of iron (hematite, goethite, magnetite) or chromogenous elements (like Fe2+ or Fe3+) in the structure of the clay components, as is the case with green earth materials (glauconite, celadonite, smectites and chlorites) [20, 31].
It is concluded that most of the smectite clays in the weathered clay soils were inherited from the parent mudstone (with little or no transformation) and that these clay components were likely to have been present in the sediments from which the mudstone formed.
Those Harvey-Waroona soil stocks were long since gone and Maley's black-soil replacement looked OK to begin with (plenty of the vital clay component required) but was soon found to contain too much sodium.
The clay component of the clay/graphene composites could be leached out to obtain exfoliated graphite.
Namely, samples with a larger clay component were inferred to have higher absolute concentrations of REE but have less distinctive patterns.
MnAl hydrotalcite-like compound was used as the precursor of the active phase, while synthetic smectite Laponite RD, either in sodium form (Na-L) or as an organoclay, exchanged with cetyltrimethylammonium cations (CTA-L), served as the clay component.
Although kaolinite, illite, chlorite, and smectite are the principal clay mineral components of deep-sea sediments, their compositions vary from place to place.
