TY - JOUR
T1 - Energy dissipation in sheared wet granular assemblies
AU - Kovalcinova, L.
AU - Karmakar, S.
AU - Schaber, M.
AU - Schuhmacher, A. L.
AU - Scheel, M.
AU - Dimichiel, M.
AU - Brinkmann, M.
AU - Seemann, R.
AU - Kondic, L.
N1 - Funding Information:
Stimulating discussions with Stephan Herminghaus are gratefully acknowledged. We further acknowledge the support by the German Research Foundation (DFG) via GRK-1276, Saarland University (S.K. and R.S.) and SPP 1486 “PiKo” under Grant No. HE 2016/14-2 (M.B.), by a start-up grant from Saarland University (A.L.S.), and by the NSF Grant No. DMS-1521717 and DARPA Contract No. HR0011-16-2-0033 (L.K. and L.K.).
Publisher Copyright:
© 2018 American Physical Society.
PY - 2018/9/19
Y1 - 2018/9/19
N2 - Energy dissipation in sheared dry and wet granulates is considered in the presence of an externally applied confining pressure. Discrete element simulations reveal that for sufficiently small confining pressures, the energy dissipation is dominated by the effects related to the presence of cohesive forces between the particles. The residual resistance against shear can be quantitatively explained by a combination of two effects arising in a wet granulate: (i) enhanced friction at particle contacts in the presence of attractive capillary forces and (ii) energy dissipation due to the rupture and reformation of liquid bridges. Coulomb friction at grain contacts gives rise to an energy dissipation which grows linearly with increasing confining pressure for both dry and wet granulates. Because of a lower Coulomb friction coefficient in the case of wet grains, as the confining pressure increases the energy dissipation for dry systems is faster than for wet ones.
AB - Energy dissipation in sheared dry and wet granulates is considered in the presence of an externally applied confining pressure. Discrete element simulations reveal that for sufficiently small confining pressures, the energy dissipation is dominated by the effects related to the presence of cohesive forces between the particles. The residual resistance against shear can be quantitatively explained by a combination of two effects arising in a wet granulate: (i) enhanced friction at particle contacts in the presence of attractive capillary forces and (ii) energy dissipation due to the rupture and reformation of liquid bridges. Coulomb friction at grain contacts gives rise to an energy dissipation which grows linearly with increasing confining pressure for both dry and wet granulates. Because of a lower Coulomb friction coefficient in the case of wet grains, as the confining pressure increases the energy dissipation for dry systems is faster than for wet ones.
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U2 - 10.1103/PhysRevE.98.032905
DO - 10.1103/PhysRevE.98.032905
M3 - Article
AN - SCOPUS:85053818679
SN - 1063-651X
VL - 98
JO - Physical Review E - Statistical Physics, Plasmas, Fluids, and Related Interdisciplinary Topics
JF - Physical Review E - Statistical Physics, Plasmas, Fluids, and Related Interdisciplinary Topics
IS - 3
M1 - 032905
ER -