“…For example, factors that influence diagenetic phase transitions and reactive surface area for each Wentworth size class of SWL-derived particles can now be tested using controlled experimentation of urine-stone-microbe-renal tissue interactions within microfluidic testbeds such as the GeoBioCell 38 – 42 , 79 . Of specific utility is the small size of SWL-derived particles, which fit easily into GeoBioCell microfluidic flow chambers and channels, and therefore permit real-time quantitative tracking of diagenetic phase transitions controlled by a wide variety of interacting physical, chemical, and biological processes 41 , 93 , 95 . Potential examples include 39 , 42 : (1) real-time systematic analysis of the effect of microbiome- and host human-derived protein catalysis by promotional and inhibitory macromolecules (i.e., anionic proteins and glycosaminoglycans) on crystal aggregation and cell attachment 10 , 11 , 31 , 42 , 51 , 96 ; (2) controls on crystal growth morphology, mineralogy, chemistry, aggregation, layering, dissolution, and recrystallization; and (3) the influence of organic acids such as citric, oxalic and formic acids excreted by specific bacteria and fungi entombed in CaOx kidney stones on stone dissolution.…”