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基于微孔填充和毛细管凝聚理论的持水曲线模型 被引量:7
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作者 刘樟荣 叶为民 +3 位作者 崔玉军 朱合华 王琼 陈永贵 《岩土力学》 EI CAS CSCD 北大核心 2021年第6期1549-1556,共8页
持水曲线是研究非饱和土的渗透、强度和体变等水力-力学特性的重要工具。大多数既有持水曲线模型未能反映非饱和土的持水机制或形式较复杂,且对双峰或多峰形态的持水曲线模拟效果欠佳。在分析非饱和土持水机制的基础上,将持水曲线划分... 持水曲线是研究非饱和土的渗透、强度和体变等水力-力学特性的重要工具。大多数既有持水曲线模型未能反映非饱和土的持水机制或形式较复杂,且对双峰或多峰形态的持水曲线模拟效果欠佳。在分析非饱和土持水机制的基础上,将持水曲线划分为吸附和毛细持水域;再基于微孔填充理论,结合Kelvin定律,构建了吸附持水曲线模型;同时基于毛细管凝聚理论,结合Young-Laplace方程,构建了毛细持水曲线模型;然后通过吸附和毛细持水曲线模型的叠加,建立了全吸力范围内非饱和土的持水曲线模型。采用该模型对上海软土、西安黄土、南阳膨胀土、桂林红黏土、辽西风积土和内蒙古高庙子膨润土等6种代表性非饱和土的实测持水曲线进行了模拟。结果表明,该模型形式简单,参数物理意义明确,且反映了非饱和土的吸附和毛细作用持水机制,可适用于模拟不同条件不同类型土体的不同形状持水曲线。 展开更多
关键词 非饱和土 持水曲线 微孔填充 毛细管凝聚 持水模型
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FTIR-ATR chamber for observation of efflorescence and deliquescence processes of NaClO_(4) aerosol particles on ZnSe substrate 被引量:3
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作者 ZHANG Yunhong HU Yong'an DING Fei ZHAO Lijun 《Chinese Science Bulletin》 SCIE EI CAS 2005年第19期2149-2152,共4页
NaClO4 aerosol particles with diameter of 5―20 microns are deposited on the ZnSe substrate. An FTIR-ATR chamber on the ZnSe substrate is set up to ob-serve the structural changes of NaClO4 aerosol particles at crysta... NaClO4 aerosol particles with diameter of 5―20 microns are deposited on the ZnSe substrate. An FTIR-ATR chamber on the ZnSe substrate is set up to ob-serve the structural changes of NaClO4 aerosol particles at crystallization relative humidity (CRH) and deliquescence relative humidity (DRH). With the decrease of RH (relative humidity) from 96% to 24% in the efflorescence process, the absorbance of O-H stretching band of the aerosol solutions continuously decreases. A sudden decrease of the water peak is observed at RH20%, where solid particles form. Very small amount of residual interfacial water, with two weak peaks at 3602 and 3533 cm-1, can still be resolved in the FTIR-ATR spectra of the solid particles. In the deliquescence process of the same sample, little spectral changes are ob-served when the value of RH varies from 5% to 29%. Before the abrupt increase of the O-H stretching band at the DRH of about RH46%, a pre-deliquescence process is observed, i.e. in the RH range between 33% and 46%, there is really a slow absorbance increase for the peak area of O-H stretching band. The O-H stretching band shows an arciform O-H en-velope, totally different from not only the FTIR-ATR spectra of ClO4? solutions either under supersaturated state or in diluted state, but also the characteristic of the residually in-terfacial water discussed in the efflorescence process. Such kind of water is considered as pure water, indicating that small amount of water aggregates in the microspaces of solid aerosol particles due to the capillary cohesion effect. When the RH arrives at RH44%, two weak shoulders at 3384 and 3260 cm?1 can be resolved, and the solid NaClO4 particles begin to be dissolved by increasing capillary cohesion water. The spectral characteristic of the ν3-ClO4? band also shows the transition from solid particles to mainly solvated ClO4? ions. 展开更多
关键词 FTIR-ATR 气溶胶 毛细管凝聚 NaClO4 风化作用 潮解作用
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