“…Porosity changes are common in unsaturated porous media. Examples include industrial applications such as personal hygiene tissues (e.g., Sun et al 2015), absorbent polymers (e.g., Brandt et al 1987), cooling systems (e.g., Jo et al 2018), and many others. Geological systems with changing porosity are abundant and include mineral dissolution or precipitation in karst, geothermal, or hydrothermal systems (e.g., Evans and Lizarralde 2003;Waltham et al 2005;Ball et al 2015), thermal or mechanical stress, (e.g., Tsang 1999), bioturbation (e.g., Pérès et al 1998;Gingras et al 2012), diagenetic processes (e.g., Gluyas and Coleman 1992), simple compaction of deposits (Boudreau and Bennett 1999), and radiogenic waste in salt (e.g., Jordan et al 2015a, b, c;Bourret et al 2017).…”