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Exact(4)
Cations (Ca2+ and Mg2+) are exchanged on the mineral surface by a substitution mechanism.
The adsorption of collector on mineral surface by MD method indicates that the combination processes of collectors with mineral crystal are exothermic, and THCA has the greatest difference in binding energy between diaspore and aluminosilicate.
We hypothesise that this chain of events involves a penetration of the water film covering the mineral surface by small relatively hydrophilic polar organic molecules which physisorb to reduce mineral surface polarity, followed by an adsorption of apolar organic molecules on the thus preconditioned surface.
The adsorption mode of three collectors on mineral surface by MD method indicates that the combination processes of collectors with mineral are exothermic, and the higher the binding energy, the firmer the collector adsorbs on the mineral surface and the higher collecting capacity.
Similar(56)
Thus, we explained the higher OC coverage on mineral surfaces by complex association between clay minerals, iron oxides and SOM in paddy soils.
The results for SSA corresponded to changes in surface specific parameters like cation exchange capacity (CEC), surface enthalpy and the fractional coverage of mineral surfaces by SOM.
The enhancement in the oil-solid separation was mainly ascribed to the interfacial alteration at the oil and mineral surfaces by the TrpBF4/U, including lowering the interfacial tension and increasing solid wettability.
They consider the complex with the shorter Cs O distance to be an outer sphere complex, fully hydrated and therefore separated from mineral surfaces by water molecules, while the complex with the longer Cs O distance is thought to be an inner sphere complex, partially dehydrated and directly associated with a mineral surface.
Cyclohexane and carbazole form discrete organic phases removed from the mineral surfaces by a water film; phenol and acetic acid show a sufficient water solubility to penetrate through these films to compete with the water molecules for mineral surface adsorption sites.
Activated osteoclasts can detach bonded bisphosphonates from bone mineral surfaces by generating a local acidic environment [ 29].
This led to 'trenching' of silicate mineral surfaces by AM and EM fungi, with EM gymnosperms and angiosperms releasing calcium from basalt at twice the rate of AM gymnosperms.
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