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. Author manuscript; available in PMC: 2023 Nov 24.
Published in final edited form as: Phys Rev X. 2022 Aug 17;12(3):031027. doi: 10.1103/physrevx.12.031027

FIG. 4. Capillary forces increase aggregate internal pressure.

FIG. 4.

(A) A schematic describing the decomposition of forces and pressures at A=A0 on deformable substrates. (B) Effective surface tension as a function of substrate stiffness when measured from monolayer stress (red), and active elasto-capillary deformations (blue) (N=10 samples per data point). Effective elasto-capillary length as a function of substrate stiffness calculated from experimental data (solid grey) and under assumption that surface tension stays constant (dashed grey). lc and Ec are the critical elasto-capillary length and critical substrate stiffness, respectively, where the transition between modes of migration occurs. (C) Aggregate spreading rate as a function of the aggregate surface tension on a 0.7 kPa substrate (N=27). Surface tension as a function of aggregate size (inset). (D) Pressure on top and bottom section of an aggregate at 0.7 kPa and 8.6 kPa (inset). The dashed black line represents the minimum pressure, Pmin=135.8±4.4Pa, required to overcome traction. The dashed blue line is basal pressure, P0=109.6±6.2Pa, for largest aggregates. Error bars are error propagated from measurements of lmax and zmax. (E) Mean pressure on top and bottom sections as a function of substrate stiffness (N=9 for 0.7 and 8.6 kPa each). Error bars are mean ± standard deviation.