The efflorescence mineralogy showed a vertical distribution and changes over time.
The mineral distribution is from interaction of RH diurnal changes and capillary flow.
Over nine years the efflorescence developed after the intervention had reached the pre-intervention composition.
Also simple salts, we found humberstonite, darapskite, konyaite and aphthitalite.
Saline ions came mainly from groundwater and airborne particles.