Thermal decomposition study of crystalline limestone using P-wave velocity

被引：7

作者：

Kantiranis, N ^{[1
]}

Filippidis, A

Tsirambides, A

Christaras, B

机构：

[1] Aristotle Univ Thessaloniki, Sch Geol, Dept Mineral Petrol Econ Geol, GR-54124 Thessaloniki, Greece

[2] Aristotle Univ Thessaloniki, Sch Geol, Dept Geol, Lab Engn Geol & Hydrogeol, GR-54124 Thessaloniki, Greece

来源：

CONSTRUCTION AND BUILDING MATERIALS | 2005年 / 19卷 / 05期

关键词：

limestone; P-wave velocity; thermal decomposition;

D O I：

10.1016/j.conbuildmat.2004.08.002

中图分类号：

TU [建筑科学];

学科分类号：

0813 ;

摘要：

A high-calcium limestone was calcined in order to study its thermal decomposition using P-wave velocity. The onset of calcination is at approximately 750 degreesC, while its completion according to the size of the cubic specimens is noted between 1000 and 1150 degreesC. We found that P-wave velocities are a very good index for the study and estimation of calcination. P-wave velocity decreases due to a temperature rise from 650 to 1150 degreesC for the cubic specimens of 4, 6 and 8 cm mean edge, while for 1 and 2 cm cubic specimens mixed behavior is observed, with a considerable increase in velocities at calcination temperature higher than 1050 degreesC. (C) 2004 Elsevier Ltd. All rights reserved.

引用

页码：359 / 365

页数：7

共 31 条

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