摘要
通过研究典型的硅质碳酸盐Spratt石灰岩在LiOH溶液中的膨胀行为和产物形貌、组成,认为Spratt石灰岩既具有碱-硅酸反应活性,又具有碱-碳酸盐反应活性;通过研究碱-碳酸盐反应过程中离子的迁移,认为白云石晶体在碱的侵蚀下会发生解离,而解离出来的Ca2+和CO32-向外迁移,离开了它们原来的位置.
The expansion behavior of typical siliceous carbonate (Spratt limestone) autoclaved in LiOH solution were studied in this paper, the morphologies and chemical composition of the products produced by reaction of siliceous carbonate with LiOH were studied through SEM and EDS. The results show that Spratt limestone exhibits both alkali - silica and alkali - carbonate reactivity. Ion's migration in alkali - carbonate reaction process was revealed, dolomite crystal disintegrates because of alkali corrosion, Ca2+ and CO32- produced by dolomite crystal disintegration migrate out and leave original positions.
出处
《建筑材料学报》
EI
CAS
CSCD
2004年第4期379-383,共5页
Journal of Building Materials