Research output: Contribution to journal › Article › peer-review
Evaporation of droplets on inclined biphilic surfaces. / Starinskaya, E. M.; Miskiv, N. B.; Rodionov, A. A. et al.
In: International Journal of Heat and Mass Transfer, Vol. 256, No. Part 1, 127978, 03.2026.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Evaporation of droplets on inclined biphilic surfaces
AU - Starinskaya, E. M.
AU - Miskiv, N. B.
AU - Rodionov, A. A.
AU - Nazarov, N. A.
AU - Kargina, A. M.
AU - Starinskiy, S. V.
AU - Terekhov, V. V.
AU - Tonini, S.
AU - Conti, P.
AU - Cossali, G. E.
AU - Sazhin, S. S.
N1 - This research was supported by the Ministry of Science and Higher Education of the Russian Federation (grant 075-15-2025-007, https://megagrant.ru/labs/lab_rus_1082740/), (contributions by E.M. Starinskaya, S.V. Starinskiy, N.B. Miskiv, A.A. Rodionov, V.V. Terekhov and S.S. Sazhin, Sections 1, 3–6), the Russian Science Foundation (RSF) (grant 19-79-30075, https://rscf.ru/project/19-79-30075/), (contribution by N.A. Nazarov, development of the algorithms for the 3D droplet shape reconstruction, Section 2), and the University of Bergamo (S.S. Sazhin’s short-term incoming visiting professorship, grant n.ST_69 2023). The research presented in this paper was initiated by work on a project supported by the Royal Society (UK) (grant IEC 192007).
PY - 2026/3
Y1 - 2026/3
N2 - The evaporation of droplets on biphilic surfaces inclined at angles of 0°, 45°, 90°, 135°, and 180°, is studied experimentally. The fastest evaporation was observed for droplets on vertical surfaces, and the slowest was observed for sessile droplets on surfaces inclined at an angle of 45°. A pendant droplet evaporating on a surface at an angle of 180° had the highest temperature. Numerical and analytical/numerical models are applied to the analysis of the experimental data. The first is based on ANSYS Fluent, while the second is based on the earlier developed variable density model. Function Φ, used in the second model, is inferred from the numerical solution of the Laplace equation by COMSOL Multiphysics. The numerical model can take into account or ignore the effect of natural convection on droplet evaporation. This effect is ignored in the analytical/numerical model. The predictions of the numerical model are shown to be reasonably close to the experimental data. A very small difference between the results predicted by the numerical and analytical/numerical models in the absence of gravity is considered to be a verification of both models. It is shown that the evaporation rates of the droplets on inclined surfaces are mainly controlled by the re-direction of the flow around them driven by natural convection and not by their deformation and changes in their surface areas.
AB - The evaporation of droplets on biphilic surfaces inclined at angles of 0°, 45°, 90°, 135°, and 180°, is studied experimentally. The fastest evaporation was observed for droplets on vertical surfaces, and the slowest was observed for sessile droplets on surfaces inclined at an angle of 45°. A pendant droplet evaporating on a surface at an angle of 180° had the highest temperature. Numerical and analytical/numerical models are applied to the analysis of the experimental data. The first is based on ANSYS Fluent, while the second is based on the earlier developed variable density model. Function Φ, used in the second model, is inferred from the numerical solution of the Laplace equation by COMSOL Multiphysics. The numerical model can take into account or ignore the effect of natural convection on droplet evaporation. This effect is ignored in the analytical/numerical model. The predictions of the numerical model are shown to be reasonably close to the experimental data. A very small difference between the results predicted by the numerical and analytical/numerical models in the absence of gravity is considered to be a verification of both models. It is shown that the evaporation rates of the droplets on inclined surfaces are mainly controlled by the re-direction of the flow around them driven by natural convection and not by their deformation and changes in their surface areas.
KW - Biphilic surfaces
KW - Evaporation
KW - Inclined surfaces
KW - Mathematical model
KW - Sessile and pendant droplets
UR - https://www.scopus.com/pages/publications/105022148158
UR - https://www.mendeley.com/catalogue/9e11315b-2151-3051-9707-d1f2313fc32a/
U2 - 10.1016/j.ijheatmasstransfer.2025.127978
DO - 10.1016/j.ijheatmasstransfer.2025.127978
M3 - Article
VL - 256
JO - International Journal of Heat and Mass Transfer
JF - International Journal of Heat and Mass Transfer
SN - 0017-9310
IS - Part 1
M1 - 127978
ER -
ID: 72217623