“…Predicting these changes has a wide practical importance in applied sciences and materials engineering, especially for hydraulically conductive materials where reactive transport takes place ( Figure 1 ): hydrothermal alterations may weaken geological fractures [ 1 ] and fault zones up to their reactivation [ 2 ], chemical degradation of cements may influence the integrity of wells [ 3 , 4 ] and mineral dissolution can lead to significant weakening of geological reservoirs [ 5 , 6 ]. Hence, the quantification of this direct chemical–mechanical interaction is of substantial relevance within the context of risk assessment for most applications related to geological subsurface utilisation such as geothermal energy systems [ 7 , 8 , 9 ], enhanced oil recovery [ 10 , 11 ], radioactive waste disposal [ 12 , 13 ], underground coal gasification [ 14 , 15 , 16 ] and CO 2 or geological energy storage [ 17 , 18 , 19 ].…”