本文分析了节理的表面形貌特征，研究了不间形貌成分对节理剪切强度的不同作用，提出子能适用于3种不同表面形貌特征的节理剪切强度公式，并分3种情形建立了节理的闭合变形模型。对节理组合形貌含有周期性波纹度的节理的闭合变形模型也作了探讨。

This paper presents a study for quantifying both the joint topography characteristics and the load-closure deformation of a rock joint under normal compressive loading condition. The study covers (1) laboratory measurements of rock joint surface profiles using a profilometer designed and fabricated by the research team, (2) development of a mathematical method to identify the waviness and unevenness components in joint surface profiles and the associated composite topography, (3) development of a general load–closure deformation model by using both the waviness and unevenness components in the composite topography, (4) unconfined compressive testing of rock samples with joints for the experimental load-closure deformation of joints and, (5) verification of the general load-closure deformation model by the experimental load-closure deformation results. The study leads to the following four findings: (a) the mathematical method can be used to identify the waviness and unevenness components for joint surface profiles and its composite topography. The height characteristic parameters of the complete surface topography of a joint are mainly determined by the waviness component. The texture characteristic parameters of the complete surface topography of a joint are mainly determined by the unevenness component, (b) joints can be classified into the three contact state cases using the waviness and unevenness components for both the joint surface profiles and the associated composite topography. The load-closure deformation behavior of a joint is determined by the waviness and unevenness components of the composite topography for a specific contact state, (c) the general load–closure deformation model developed in this paper is applicable to the three contact state cases. The general load-closure deformation model uses the composite topography of a joint and can take into account the effects of the contact states, the initial aperture and the waviness and unevenness components; (d) parametric studies and verifications with the uniaxial compression test results show that the general load-closure deformation model gives reasonable estimations of the load-closure deformation behavior of rock joint under compressive loading and can be reduced to those given by other researchers in the relevant literature.

介绍了节理闭合试验技术和节理初始开度的测试方法，探讨了节理闭合时非线性和不可恢复变形的机理，研究了节理在不同接触状态下组合形貌的特征和闭合变形性质。得到了能反映节理接触状态和受载历史的包含有节理无量纲初始开度等节理组合形貌参数的法向力一法向变形本构方程。

在隧道与围岩介质相互作用的基础上，推导了岩石隧道温度应力的计算式，并给出了由温度应力引起的裂缝间距和宽度的计算公式；分析了影响温度应力的各种因素，探讨了由温度应力引起的裂缝的开展规律。

The influence of strain history on rock specimen deformation during multi-level loading and unloading cyclic uniaxial compression creep tests is studied with a creep testing machine. An experimental data processing method for such creep tests is suggested. The correction formulas to determine the rheological model parameters are derived for the case when load relaxation is considered. Creep and relaxation tests under uniaxial compression on four types of rocks are conducted using an electronic hydraulic servo-controlled stiff testing machine. The creep and relaxation laws of the different rocks are compared. The complete stress