The effect of B2O3 on the viscosity of haplogranitic liquids

D. B. Dingwell; R. Knoche; S. L. Webb; M. Pichavant

The effect of B₂O₃ on the viscosity of haplogranitic liquids

D. B. Dingwell
, R. Knoche
, S. L. Webb
, M. Pichavant

University of Bayreuth

科研成果: 期刊稿件 › 文章 › 同行评审

124 引用（Scopus）

摘要

The effect of B₂O₃ on the viscosity of a haplogranitic liquid has been determined at 1 atm pressure in the temperature interval of 600-1600°C. The viscosity of haplogranite liquid decreases with the addition of B₂O₃ at all temperatures investigated. The viscosity decrease is nonlinear, with the strongest decrease exhibited at low B₂O₃ concentration. The temperature dependence of the viscosity of all the investigated liquids is Arrhenian, in strong contrast to the case for B₂O₃ liquid. B must be considered as a fluxing agent in B-rich granitic and pegmatitic systems. -from Authors

源语言	英语
页（从-至）	457-461
页数	5
期刊	American Mineralogist
卷	77
期	5-6
出版状态	已出版 - 1992
已对外发布	是

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abstract = "The effect of B2O3 on the viscosity of a haplogranitic liquid has been determined at 1 atm pressure in the temperature interval of 600-1600°C. The viscosity of haplogranite liquid decreases with the addition of B2O3 at all temperatures investigated. The viscosity decrease is nonlinear, with the strongest decrease exhibited at low B2O3 concentration. The temperature dependence of the viscosity of all the investigated liquids is Arrhenian, in strong contrast to the case for B2O3 liquid. B must be considered as a fluxing agent in B-rich granitic and pegmatitic systems. -from Authors",

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AU - Dingwell, D. B.

AU - Knoche, R.

AU - Webb, S. L.

AU - Pichavant, M.

PY - 1992

Y1 - 1992

N2 - The effect of B2O3 on the viscosity of a haplogranitic liquid has been determined at 1 atm pressure in the temperature interval of 600-1600°C. The viscosity of haplogranite liquid decreases with the addition of B2O3 at all temperatures investigated. The viscosity decrease is nonlinear, with the strongest decrease exhibited at low B2O3 concentration. The temperature dependence of the viscosity of all the investigated liquids is Arrhenian, in strong contrast to the case for B2O3 liquid. B must be considered as a fluxing agent in B-rich granitic and pegmatitic systems. -from Authors

AB - The effect of B2O3 on the viscosity of a haplogranitic liquid has been determined at 1 atm pressure in the temperature interval of 600-1600°C. The viscosity of haplogranite liquid decreases with the addition of B2O3 at all temperatures investigated. The viscosity decrease is nonlinear, with the strongest decrease exhibited at low B2O3 concentration. The temperature dependence of the viscosity of all the investigated liquids is Arrhenian, in strong contrast to the case for B2O3 liquid. B must be considered as a fluxing agent in B-rich granitic and pegmatitic systems. -from Authors

UR - https://www.scopus.com/pages/publications/0026467816

M3 - 文章

AN - SCOPUS:0026467816

SN - 0003-004X

VL - 77

SP - 457

EP - 461

JO - American Mineralogist

JF - American Mineralogist

IS - 5-6

ER -

The effect of B2O3 on the viscosity of haplogranitic liquids

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The effect of B₂O₃ on the viscosity of haplogranitic liquids