Suggestions(1)
Exact(58)
As implied above, the equilibrium constants for exchange reactions change slightly with temperature.
Exchange reactions between river-borne clays entering seawater are particularly significant for sodium and calcium ions.
All ligand exchange reactions were performed under an argon atmosphere.
Figure 1 Kinetics of ion-isotopic exchange reactions.
The ligand exchange reactions could be monitored by cyclic voltammetry.
11.1 % of the boreholes were positive indicating the absence of base-exchange reactions but rather the existence of cation anion exchange reactions.
The decrease in ESP is attributed to the exchange reactions with calcium ions in the system.
Transport reactions and exchange reactions were added for metabolic network connectivity.
The ion exchange reactions occur by the exchange of H+ ions in the host rock.
Similar(2)
The reversibility of ion-exchange reactions greatly affects the behaviour of ion-exchange systems.
Steps 1A and 1B: ligand-exchange reactions.
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