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在他的专著《论岩浆熔体的粘度》中提出了计算岩浆熔体的粘度的半经验简易方法.该法与实验测定的精度相比,尚有误差.其方程式是:lg·η＝(a-bK)10~3/4.576T－3.5＋a(P总压-PH_2O)式中,η—粘度(泊);P—压力(MPa);T—温度(K);a= -5.02·10_(-4)MPa,对于“干的”熔体-1.2·10_(-3)MPa,对于不饱和水的熔体K—结构化学参数,熔体的结构比学参数K用下式计算:K=O_(-1)O_0=2(O-2M)/M×100式中,O_-—非桥氧;O~0—桥氧;O—熔体内氧的离子总和;M—成网阳离子(Si~(4+)、Al~(3+)、Fe~(3+)、P~(5+))的离子总和(单位均以moi计).参数K可根据岩石的化学成分计算,例子见《岩浆熔体的粘度》.
In his monograph “On the Viscosity of Magma Melts”, a semi-empirical and simple method for calculating the viscosity of magma melt is proposed, which is still inaccurate compared with the accuracy of the experimental determination. The equation is: lg · η = ( a-bK) 10-3 / 4.576T-3.5 + a (P total pressure -PH_2O) where η- viscosity (poise); P- pressure (MPa); T- temperature (K); a = -5.02 · 10_ (-4) MPa. For the “dry” melt -1.2 · 10_ (-3) MPa, for the melt K-structure chemical parameters of the unsaturated water, the structure specific parameter K of the melt is calculated using the following formula: K = O _ (- 1) O_0 = 2 (O-2M) / M × 100 wherein O _ - non-bridging oxygen; O ~ O-bridge oxygen; O-ions in the melt oxygen; M-network cations (3), Fe (3 +), P ~ (5+)) ions (units are moi) .The parameter K can be calculated according to the chemical composition of the rock, See for example “Viscosity of Magma Melts.”