Na-relaxation and intermediate range structure in sodium-potassium silicate melts

被引：11

作者：

Kargl, F. ^{[1
]}

Meyer, A. ^{[2
]}

机构：

[1] Aberystwth Univ, Inst Math & Phys, Aberystwyth SY23 3BZ, Dyfed, Wales

[2] Deutsch Zentrum Luft & Raumfahrt, Inst Mat Phys Weltraum, D-51170 Cologne, Germany

来源：

CHEMICAL GEOLOGY | 2008年 / 256卷 / 3-4期

关键词：

Ternary silicates; Mixed alkali effect; Neutron scattering; Quasielastic; Melt; In situ; Intermediate range order;

D O I：

10.1016/j.chemgeo.2008.06.046

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

We report on the investigation of fast alkali-ion transport and its relation to microscopic structure for mixed Na-K silicate melts. Na2O K2O 4SiO(2), Na2O K2O 6SiO(2), and K2O 3SiO(2) are studied by means of quasielastic neutron scattering and the results are discussed in the context of results on Na2O 2SiO(2), Na2O 3SiO(2), and K2O 2SiO(2). The height and position of the prepeak in the elastic structure factor scales with the Na2O:K2O ratio between the binary alkali silicates. The addition of K2O to a binary sodium silicate melt appears to have no influence on the time scales of the Na self-relaxation. The data suggest the presence of two different subnetworks of percolation channels in the static structure for the two different alkali species Na and K. (C) 2008 Elsevier B.V. All rights reserved.

引用

页码：278 / 285

页数：8

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