Bentonite swelling pressure response to temperature change

IF 5.3 2区 地球科学 Q2 CHEMISTRY, PHYSICAL
Jari Martikainen , Teemu Laurila , Sirpa Kumpulainen , Olivier X. Leupin
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引用次数: 0

Abstract

In the proposed Swiss repository location at Nördlich Lägern, in an Opalinus Clay formation, at the depth of about 850–900 m, the ambient temperature due to geothermal gradient is expected to be about 45–50 °C.

In this study, constant-volume swelling pressure experiments were performed to assess the effect of such elevated temperatures (25 - 60 °C) on granular Wyoming bentonite performance around designed buffer dry density of 1450 kg/m3. Bentonite was hydrated with a saline solution closely simulating reference Opalinus clay groundwater, and the bentonite dry density was varied between 1300 kg/m3 and 1600 kg/m3 to evaluate density dependency. Tests included isothermal, as well as increasing (incremental) and decreasing (decremental) temperature programs following different thermo-hydraulic paths: full saturation-first and complete heating-first. The dependency of swelling pressure on both bentonite density and temperature was analyzed by pressure-temperature slope (kPa/°C) and obtained results were compared to previous similar tests with Wyoming bentonite at different bentonite densities.

Overall conclusion is that granular Wyoming-type bentonite swelling pressure response to elevated temperature at designed dry density of 1450 kg/m3 is small (−6.5 ± 2.0 kPa/°C), and robust against changes in the thermo-hydraulic path or in the density.

膨润土膨胀压力对温度变化的响应
在位于 Nördlich Lägern 的拟议瑞士储存库位置,在约 850-900 米深处的 Opalinus 粘土层中,地热梯度导致的环境温度预计约为 45-50 °C。
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来源期刊
Applied Clay Science
Applied Clay Science 地学-矿物学
CiteScore
10.30
自引率
10.70%
发文量
289
审稿时长
39 days
期刊介绍: Applied Clay Science aims to be an international journal attracting high quality scientific papers on clays and clay minerals, including research papers, reviews, and technical notes. The journal covers typical subjects of Fundamental and Applied Clay Science such as: • Synthesis and purification • Structural, crystallographic and mineralogical properties of clays and clay minerals • Thermal properties of clays and clay minerals • Physico-chemical properties including i) surface and interface properties; ii) thermodynamic properties; iii) mechanical properties • Interaction with water, with polar and apolar molecules • Colloidal properties and rheology • Adsorption, Intercalation, Ionic exchange • Genesis and deposits of clay minerals • Geology and geochemistry of clays • Modification of clays and clay minerals properties by thermal and physical treatments • Modification by chemical treatments with organic and inorganic molecules(organoclays, pillared clays) • Modification by biological microorganisms. etc...
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