Chemical structure of cement aged at normal and elevated temperatures and pressures Part I.: Class G oilwell cement

被引:102
作者
Le Saout, G
Lécolier, E
Rivereau, A
Zanni, H
机构
[1] Ecole Super Phys & Chim Ind Ville Paris, UMR CNRS 7636, Phys & Mecan Milieux Heterogenes Lab, F-75231 Paris 05, France
[2] IFP Energies Nouvelles, F-92852 Rueil Malmaison, France
关键词
temperature; X-ray scattering; NMR; aging; oilwell cement;
D O I
10.1016/j.cemconres.2004.09.018
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The prime objective of the plug-and-abandon operations is to provide zonal isolation for infinite time. Cement-based materials are generally used as plugging materials. Therefore, it is important to understand the physical and chemical processes causing cement degradation in the downhole environment. In this study, we have characterised a Class G oilwell cement immersed for I year in brine at T=293 K, p=10(5) Pa and T=353 K, p=7x10(6) Pa using NMR and XRD techniques. In order to have a better understanding of the Al-27 NMR spectra, selective dissolution has been performed. The results show that after I year of immersion in brine at T=293 K, p=10(5) Pa, monosulfate is converted to Friedel's salt. Leaching. resulted in the disappearance of portlandite and the formation of calcite and a more polymerised calcium silicate hydrates (C-S-H). In the T-353 K, p=7x10(6) Pa mineralogy, ettringite is converted to hydrogrossular. (c) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:71 / 78
页数:8
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