Monovalent ions (like K+) will also replace H+ ions, but they don't add any dGH. This is actually a 2 way process and those ions can be replaced by H+ ions etc and become available to the plant as the concentration of the ions change around the negatively - charged exchange sites of the clay mineral. This is the "LYOTROPIC SERIES":
most tightly bound H+ = Al3+ > Ca2+ > Mg2+ > K+ = NH4+ > Na+ least tightly bound. Adding large amounts of one cation will replace others, regardless of their position in the lyotropic series. For example Na+ could replace Ca2+ on the mineral's exchange sites if sufficient concentration of Na+ existed in tank water.