Oilwell Cement Clinkers

Christopher Hall , Karen L. Scrivener
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引用次数: 23

Abstract

X-ray microanalyses have been made on a suite of nine oilwell cement clinkers. Elemental data were obtained on alite, belite, and ferrite phases and, for two clinkers only, also on aluminate. The alite and belite compositions are broadly similar to those previously reported for other portland cements. Guest ion concentrations suggest that several charge-balancing substitutions occur. Bulk MgO and SO3 levels determine the Mg and S contents of both phases, but for Fe and Al the substitution levels are not strongly correlated with bulk composition. For ferrites, the data are generally consistent with the results of Bergstrom et al. (Adv Cem Res 1992,4, 141–147): the Mg content varies widely, is controlled by the bulk MgO, and is coupled with Si in a charge-balancing substitution for Fe. Estimates of the total phase assembly using the directly determined mineral compositions are compared with the predictions of a modified Bogue calculation (similar to that of Taylor, Adv Cem Res 1989, 2, 73–77). The agreement is variable and some refinements to the method of calculation are indicated.

油井水泥熟料
对9种油井水泥熟料进行了x射线显微分析。获得了阿利特相、白钨相和铁素体相的元素数据,仅对两种熟料,也获得了铝酸盐相的元素数据。alite和belite的组成与以前报道的其他硅酸盐水泥大致相似。客体离子浓度表明发生了几种电荷平衡取代。整体MgO和SO3水平决定了两相中Mg和S的含量,但Fe和Al的取代水平与整体组成的相关性不强。对于铁氧体,数据与Bergstrom等人(Adv Cem Res 1992,4,141 - 147)的结果基本一致:Mg含量变化很大,受大块MgO控制,并与Si耦合,以电荷平衡取代Fe。使用直接确定的矿物成分估算的总相组合与修正的Bogue计算的预测相比较(类似于Taylor, Adv Cem Res 1989, 2,73 - 77)。协议是可变的,并指出了对计算方法的一些改进。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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