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Numerical simulation of non-isothermal flows in dikes

Periodic variations in flow rate with different influx intensities Qin. At large Qin eruption continues with relatively small variations in flow rates. Small Qin correspond to large repose periods and intense discharge. At Qin > 13 m3/s eruption stabilizes. SEMINARIO: Speaker: Oleg MelnikAffiliation: University Grenoble Alpes,…

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