钠蒙脱土结合水的热分析定量研究方法

邓明毅; 刘洋洋; 谢刚; 赵洋

doi:10.3969/j.issn.1001-5620.2018.02.002

钠蒙脱土结合水的热分析定量研究方法

doi: 10.3969/j.issn.1001-5620.2018.02.002

邓明毅^1,2,
刘洋洋^1,2,
谢刚^1,2,
赵洋^1,2

1. 西南石油大学石油与天然气工程学院, 成都 610500;
2. 油气藏地质及开发工程国家重点实验室, 成都 610500

基金项目:

国家自然科学基金重点项目"基于多场耦合理论的页岩气水平井井壁失稳机理研究"（51574202）；国家自然科学基金项目"基于流-固-化耦合理论的欠平衡钻水平井井壁失稳机理研究"（51474186）。

详细信息

作者简介:
邓明毅,1960年生,副教授,主要从事油气井工作液力学与化学方面的研究。E-mail:185268106@qq.com。

中图分类号: TE254.1
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- 被引次数: 4
出版历程
- 收稿日期: 2017-12-30
- 刊出日期: 2018-03-30

A Thermoanalytic Quantitative Method for Studying the Bound Water of Sodium Montmorillonite

1. School of Oil & Natural Gas Engineering, Southwest Petroleum University, Chengdu, Sichuan 610500;
2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu, Sichuan 610500

摘要

摘要: 随着水化的进行，黏土矿物在不同的水化阶段所吸附的水有不同的结构和性质，可分为自由水和结合水，他们和黏土的连结形式不同。国内外相关学者更多地考虑不同结合水类型及含量的定性分析，而定量分析黏土吸附水、研究不同吸附水类型及含量对岩石力学参数的影响，可以为建立力-化学耦合模型提供定量化修正。在假设钠蒙脱土矿物颗粒为六面体的前提下，结合其微观吸水特性，建立钠蒙脱土结合水含量与总吸附含水量的幂函数关系模型。并用热失重分析法测定室温吸水样、风干含水样、室温吸附样及等温吸附样等钠蒙脱土含水样的吸附水类型及含量。将实验数据与模型求解数据拟合，结果表明，所建模型的相对误差之乘积与相对误差之几何平均值均近似等于1，因此所建立的模型有较高的预测精度。
- 钠蒙脱土 /
- 黏土水化 /
- 结合水 /
- 定量分析 /
- 热失重分析
Abstract: In hydration process, water molecules adsorbed by clay particles in different hydration stages have different structures and properties. The adsorbed water includes free water and bound water, which have different ways of being attached onto clay particles. Researchers both at home and abroad have paid more attention to qualitative analysis of the type and amount of the bound water, the quantitative analysis of bound water and research on the effects of the type and amount of bound water on rock mechanics, on the other hand, provides a quantitative correction method for the establishment of force-chemistry coupling model. Assume that the sodium montmorillonite particles are in a shape of hexahedron, a power function model describing the relationship between the amount of bound water and the total adsorbed water of sodium montmorillonite can be established taking into account the micro characteristics of water adsorption. The type and amount of water adsorbed by sodium montmorillonite can be measured with thermogravimetry, airdrying of clay, adsorption in room temperature and isotherm adsorption. The experimental data are then fitted with data from model calculation. The results show that the product of the relative errors and the geometric mean of relative errors of the established model are both approximately equal to 1, indicating that the established model has good precision of prediction.
- Sodium montmorillonite /
- Clay hydration /
- Bound water /
- Quantitative analysis /
- Thermogravimetric analysis

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参考文献(16)

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