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Finally, the kinetic of sodium chloride release in water was analyzed in order to attain a preliminary evaluation of the durability of the anti-icing effects.
Chloride release is an important indicator for the degradation of chlorinated molecules.
The results in Figure 3 show that about 25% of the eaq − reactions induce chloride release.
The mechanism suggested for chloride release is shown in Scheme 2, Reaction (12).
We investigated the question whether the O2 −/HO2 pair directly induces chloride release.
The G-values of chloride release are between 0.07 − 0.15 μmol J−1 (two Cl-atom elimination).
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If most of the degassing of primary volatile substances from the Earth's interior occurred early, the chloride released by the reaction of hydrochloric acid with rock minerals would be found in the oceans or in evaporite deposits, and the oceans would have a salinity and volume comparable to that of today.
If most of the degassing of primary volatile substances from Earth's interior occurred early, the chloride released by reaction of hydrochloric acid with rock minerals would be found in the oceans and seas or in evaporite deposits, and the oceans would have a salinity and volume comparable to those that they have today.
Chloride released in groundwater system through various physicochemical reactions like ion exchange.
The ratio of chloride released per unit of 2-CP removed was then close to the theoretical value but still higher than that expected from complete dechlorination.
Salt increased the microbe-killing capacity of the immune cells, the team reports; the macrophages exposed to high levels of sodium chloride released significantly more microbicidal molecules than those that grew in a culture medium without salt.
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