# Crack formation and self-closing in shrinkable, granular packings

## TL;DR

This study investigates how shrinkable granular packings crack during drying, revealing that differential shrinkage can cause spontaneous crack self-closure or prevent cracking, with models explaining the interplay of physical factors.

## Contribution

It provides the first detailed analysis of cracking behavior in shrinkable granular packings, combining experiments and models to understand and control crack evolution.

## Key findings

- Differential shrinkage can cause cracks to self-close during drying.
- Cracking behavior can be controlled by the drying spatial profile.
- Models quantify the effects of shrinkage, poromechanics, and other factors.

## Abstract

Many clays, soils, biological tissues, foods, and coatings are shrinkable, granular materials: they are composed of packed, hydrated grains that shrink when dried. In many cases, these packings crack during drying, critically hindering applications. However, while cracking has been widely studied for bulk gels and packings of non-shrinkable grains, little is known about how packings of shrinkable grains crack. Here, we elucidate how grain shrinkage alters cracking during drying. Using experiments with model shrinkable hydrogel beads, we show that differential shrinkage can dramatically alter crack evolution during drying---in some cases, even causing cracks to spontaneously "self-close". In other cases, packings shrink without cracking or crack irreversibly. We developed both granular and continuum models to quantify the interplay between grain shrinkage, poromechanics, packing size, drying rate, capillarity, and substrate friction on cracking. Guided by the theory, we also found that cracking can be completely altered by varying the spatial profile of drying. Our work elucidates the rich physics underlying cracking in shrinkable, granular packings, and yields new strategies for controlling crack evolution.