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The physical mechanism is expected to fault with the weathering of the bentonite while the chemical mechanisms have been only proved at 300 °C.
The theory was in good agreement with the measurements in the concentration range of 0.01 M ≤ n < 1 M for Kutch bentonite while the concentration range was 0.001 M ≤ n < 1 M for Barmer bentonite in NaCl solutions.
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The influence of pH on the dye adsorption onto bentonite was studied while the dye concentration, shaking time and amount of bentonite were fixed at 56.8 mg cm−3, 10 min and 0.05 g, respectively.
The bentonite samples were characterized by the main variable proportion of bentonite in the natural and intercalated forms (2, 5, 10, 15, 20, 25, 30, and 35%% by weight of cement) in the replacement mode whiles the amount of cementations material.
Model results attest the relevance of thermal osmosis and bentonite swelling for the geochemical evolution of the bentonite barrier while chemical osmosis is found to be almost irrelevant.
In the tests with functionalized bentonite the adsorption/absorption of water decreased as the POR substitution by functionalized bentonite increased.
Adsorption of malachite green onto bentonite followed the Langmuir isotherm.
Adsorption of methylene blue onto bentonite followed the Langmuir isotherm.
However, bentonite decreased the a* meat colour parameter (redness; P=0.004).
The inorganic additives used were lithiated bentonite and the nanocomposite PEO@bentonite with the same polymer used as matrix.
Open image in new window Fig. 3 FTIR spectrum of raw bentonite, Mn2+ bentonite and the F−-loaded Mn2+ bentonite clay.
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