Research news on compaction

Compaction, as a physical phenomenon, refers to the reduction of volume and increase in bulk density of a particulate or porous material under applied stress, typically due to mechanical loading, overburden pressure, or confining forces. It involves rearrangement of grains, expulsion of pore fluids or gases, and progressive reduction of porosity, often accompanied by deformation or crushing of particles at higher stresses. In geological and engineering contexts, compaction governs consolidation of sediments, evolution of mechanical and hydraulic properties (e.g., permeability), and stress–strain behavior, and is described by constitutive relationships linking effective stress, void ratio, and time-dependent creep or consolidation processes.

3D architecture of genome enables cells to remember their past

A French research team led by CNRS scientists has discovered that cells are able to retain a memory of a previous perturbation within the 3D structure of their genome, independently of their DNA sequence. When they are exposed ...

Plants use engineering principles to push through hard soil

Across the globe, soil compaction is becoming an ever more serious challenge. Heavy vehicles and machinery in modern agriculture compress the soil to such an extent that crops struggle to grow. In many regions, the problem ...

3D X-ray study reveals how rock grains move and stress builds

A team of Johns Hopkins researchers is using an innovative X-ray imaging approach to reveal how compression reshapes the tiny spaces and stresses within sandstone—findings that could predict how this common rock used for ...