Acta Montanistica Slovaca (Mar 2001)

The viscosity measurement of molten rocks

  • Rybár Pavol,
  • Kyse¾ová Katarína

Journal volume & issue
Vol. 6, no. 1
pp. 1 – 4

Abstract

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This paper deals with the viscosity measurtement of molten rocks. The reason of such investigation was due to the solving of SC No. 95/135/059 LITHO-JET. Technology of thermic rock melting for trenching of tenous vertical works. One task in the scope of above investigation was to experimentally verify the properties of melts of various types of works. An important moment in the trenching of tenuous vertical works by rock melting is the ability of melt to penetrate into the rock cracks. From this point of view an important physical property of molten rock is its viscosity. There are various methods how to measure viscosity but for the continuous measurements just some of them are suitable. The most suitable is rotary viscosimeter because it is simple in its construction, it allows to measure the viscosity as a function of temperature, concentration of wide class of sub stances with different rheologic properties. Hence, it allows to measure structural viscosity of the chemical reaction systems. The viscosity of molten nefelitic basanite as the function of temperature is studied in this paper. Viscosity of the nefelinitic basanite taken at locality Konrádovce was measured using rotary viscosimeter HAAKE ROTOVISKO. Eperimental conditions shown, that rising of the temperature vs. viscosity is in reverse order. Measurement is realised in scale 1370-1550°C. Under 1370°C was sample very viscous and measurement was impossible. Viscosity is the function of the temperature, pressure and gas components of rock.Though the viscosity measurements was carried out at atmospheric pressure, what does not fully conform real condition during trenching, it is still possible to express the effect of pressure. Other conditions, which take effect of viscosityof molten rocks in nature conditions will be subject of future investigation.

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