Theoretical modeling study demonstrates shear thinning and thickening transitions in dense granular suspensions, indicating that discontinuous thickening can trigger macro-viscous flow instabilities.
A unified constitutive framework is developed for dense fine-granular mixtures exhibiting apparent shear thinning and continuous or discontinuous shear thickening in the macro-viscous flow regime. The effective granular stress is decomposed into viscoplastic structural and suspension-stress contributions. The former is obtained from a hypoplastic model combined with a Herschel–Bulkley rheology, whereas the latter encompasses the μ (Iₘ) μ ( I m ) rheology and the Wyart–Cates frictional-contact transition, and shows stress-dependent jamming state. Benchmark calculations show that the proposed formulation captures the transition between shear-thinning and shear-thickening behaviour. A depth-averaged long-wave analysis further shows that non-monotonicity induced by discontinuous shear thickening may persist to promote instability in the macro-viscous flow regime.
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Wang et al. (2026) studied this question.
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