Using the adjusted leads to Eq/kg and following the removal in the theoretical gypsum material (Eq. 7) an overview is provided of the individual ion content in all samples for every mixture type (Fig. four). In mixtures which might be part of form one the programs are mainly dominated by sodium and sulfate, accompanied by potassium and in lesser

When in mixtures Component of type 2 are usually additional hygroscopic, and therefore are dominated by nitrate, sodium, and chloride, followed by calcium and smaller sized quantities of potassium ions. Magnesium is in equally combination forms the least popular ion. The ions that dominate the mixture will drastically influence the mutual crystalli