为探究羟基纤维素对预崩解炭质泥岩工程特性的改良效果,开展了无侧限抗压强度、干湿循环以及理化特性的试验,以分析掺量、养护时间、干湿循环次数对预崩解炭质泥岩力学和理化特性的影响,并结合扫描电子显微镜(scanning electron microsc...为探究羟基纤维素对预崩解炭质泥岩工程特性的改良效果,开展了无侧限抗压强度、干湿循环以及理化特性的试验,以分析掺量、养护时间、干湿循环次数对预崩解炭质泥岩力学和理化特性的影响,并结合扫描电子显微镜(scanning electron microscope,SEM)技术揭示了羟基纤维素改良预崩解炭质泥岩的微观机制。结果表明:在养护时间相同的情况下,改良后的预崩解炭质泥岩的无侧限抗压强度随羟基纤维素掺量的增加呈现出先增大后减小的趋势,且当掺量为4%时,其无侧限抗压强度达到最大值;当羟基纤维素的掺量保持不变时,随着养护时间的增加,改良后的预崩解炭质泥岩的无侧限抗压强度也随之增加,并在养护14 d后趋于稳定;在干湿循环作用下,经羟基纤维素改良后的预崩解炭质泥岩的无侧限抗压强度变化符合指数函数规律;改良后的预崩解炭质泥岩的pH基本保持不变,而TDS值、电导率及盐度均有所降低;羟基纤维素主要通过胶结颗粒和填充孔隙的方式来增强预崩解炭质泥岩的力学性能。展开更多
岩石作为地球表面的主要组成部分,可分为火成岩、沉积岩和变质岩,这种分类反映了岩石的成因和基本特性,对工程实践具有重要意义。岩石的矿物成分和结构决定了其物理和力学特性,直接影响工程的设计、施工和长期稳定性。常见岩石类型如花...岩石作为地球表面的主要组成部分,可分为火成岩、沉积岩和变质岩,这种分类反映了岩石的成因和基本特性,对工程实践具有重要意义。岩石的矿物成分和结构决定了其物理和力学特性,直接影响工程的设计、施工和长期稳定性。常见岩石类型如花岗岩、玄武岩、砂岩、石灰岩、大理岩和片麻岩等在工程中具有广泛应用,这些岩石因其独特的形成过程和组成,表现出不同的强度、耐久性、透水性和加工性等特性,在建筑、道路、桥梁、隧道等工程领域发挥重要作用。As the main component of the earth’s surface, rocks can be divided into igneous rocks, sedimentary rocks and metamorphic rocks. This classification reflects the origin and basic characteristics of rocks, and is of great significance to engineering practice. The mineral composition and structure of a rock determine its physical and mechanical properties, which directly affect the design, construction and long-term stability of the project. Common rock types such as granite, basalt, sandstone, limestone, marble and gneiss are widely used in engineering. These rocks show different characteristics of strength, durability, permeability and workability due to their unique formation process and composition, and play an important role in construction, roads, Bridges, tunnels and other engineering fields.展开更多
文摘为探究羟基纤维素对预崩解炭质泥岩工程特性的改良效果,开展了无侧限抗压强度、干湿循环以及理化特性的试验,以分析掺量、养护时间、干湿循环次数对预崩解炭质泥岩力学和理化特性的影响,并结合扫描电子显微镜(scanning electron microscope,SEM)技术揭示了羟基纤维素改良预崩解炭质泥岩的微观机制。结果表明:在养护时间相同的情况下,改良后的预崩解炭质泥岩的无侧限抗压强度随羟基纤维素掺量的增加呈现出先增大后减小的趋势,且当掺量为4%时,其无侧限抗压强度达到最大值;当羟基纤维素的掺量保持不变时,随着养护时间的增加,改良后的预崩解炭质泥岩的无侧限抗压强度也随之增加,并在养护14 d后趋于稳定;在干湿循环作用下,经羟基纤维素改良后的预崩解炭质泥岩的无侧限抗压强度变化符合指数函数规律;改良后的预崩解炭质泥岩的pH基本保持不变,而TDS值、电导率及盐度均有所降低;羟基纤维素主要通过胶结颗粒和填充孔隙的方式来增强预崩解炭质泥岩的力学性能。
文摘岩石作为地球表面的主要组成部分,可分为火成岩、沉积岩和变质岩,这种分类反映了岩石的成因和基本特性,对工程实践具有重要意义。岩石的矿物成分和结构决定了其物理和力学特性,直接影响工程的设计、施工和长期稳定性。常见岩石类型如花岗岩、玄武岩、砂岩、石灰岩、大理岩和片麻岩等在工程中具有广泛应用,这些岩石因其独特的形成过程和组成,表现出不同的强度、耐久性、透水性和加工性等特性,在建筑、道路、桥梁、隧道等工程领域发挥重要作用。As the main component of the earth’s surface, rocks can be divided into igneous rocks, sedimentary rocks and metamorphic rocks. This classification reflects the origin and basic characteristics of rocks, and is of great significance to engineering practice. The mineral composition and structure of a rock determine its physical and mechanical properties, which directly affect the design, construction and long-term stability of the project. Common rock types such as granite, basalt, sandstone, limestone, marble and gneiss are widely used in engineering. These rocks show different characteristics of strength, durability, permeability and workability due to their unique formation process and composition, and play an important role in construction, roads, Bridges, tunnels and other engineering fields.