terms:exchange_cation
A positive ion that exists in the lattice or on a broken edge of some clay minerals which has the property of being easily replaced by another cation from a water solution that comes in contact with the clay. The most common exchange cations in clay materials are Ca++, Mg++, H+, K+, NH4+, and Na+.
terms/exchange_cation.txt · Last modified: 2023/11/22 08:40 by 127.0.0.1