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Double-diffusive convection of a vertical through flow in a saturated porous layer by a power-law fluid with effect of variable gravity

Crossref DOI link: https://doi.org/10.1007/s11242-025-02273-2

Published Online: 2026-01-07

Published Print: 2026-02

Update policy: https://doi.org/10.1007/springer_crossmark_policy

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