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压实作用

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In this paper,Laterite soil adjacent to some stake of the highway in Chenzhou, Hunan section from Xiamen to Chengdu was used to investigate the deformation characteristics and protection methods of the Laterite soil subgrade under the influence of environment factors.Properties like water-holding capacity,capillary rise, coupled heat-moisture transfer and wetting deformation of samples under different compactness were studied through a series of laboratory tests.In addition,by using meteorological data of two consecutive years in Chenzhou,coupled process of moisture transfer and subgrade deformation was stimulated under the impacts of groundwater and the atmosphere.Specific work done in this paper is as follows:(1) Samples under different compactness were subjected to a series of conventional laboratory tests,such as permeability,consolidation,contraction,shear test and etc.

论文以厦门至成都高速公路湖南郴州段的红粘土为研究对象,以环境因素作用下红粘土路基的变形特征与防护方法为研究目的,通过室内试验研究了不同压实度红粘土的持水性能、毛细上升、湿热耦合迁移及湿化变形等特征,借助郴州地区连续两年的气象数据,模拟在地下水和大气的共同作用下路基内部红粘土水分迁移与路基变形的耦合过程,主要研究内容及结论如下:(1)针对不同压实度的红粘土,系统开展了其渗透、固结、收缩、剪切等试验研究。

The principle and effect of impact compaction, and its application in rockfill subgrade is introduced in this paper.

并对冲击压实的作用原理,压实功效以及冲击压实在填石路基中的应用作了介绍。

Through the methods of polarizing microscope and cathodoluminescence, the diagenesis of Late Carboniferous phylloid algal reefs in southern Guizhou is studied, which indicates diagenesis are mainly of bio-binding and baffling actions, micritization, cementation, compaction-pressure solution, fracture, recrystallization and dissolution in type.

东北大学资源与土木工程学院,沈阳110004通过偏光显微镜研究和阴极发光技术,对黔南晚石炭世叶状藻礁灰岩的成岩作用做了详细研究,认为礁灰岩主要成岩作用类型有:生物黏结障积作用、泥晶化作用、胶结作用、压实压溶作用、破裂作用、重结晶作用和溶解作用等。

From the middle to the south in the research area, the compaction, the pressure dissolves the function and the structure disruption intensity enlarges gradually, the silicon nature agglutinates the content to increase gradually, and the corrosion function intensity reduces gradually. The diagenesis stage is carried on according to the division standards of secondary enlargement degree, pellet contact type as well as porosity type, the authigenic mineral characteristic, agglutinates, the diagenesis of Xujiahe formation is thoughted degree to be intense, which already entered the late diagenesis stage A sub-stage.

从研究区中部向南部,压实、压溶作用和构造破裂作用的强度逐渐加大,硅质胶结物含量逐渐增多,溶蚀作用强度逐渐降低;并根据成岩作用类型、自生矿物特征、胶结物的次生加大程度、颗粒接触类型以及孔隙类型等划分标准,对须家河组进行了成岩作用阶段划分,认为研究区须家河组成岩作用程度强烈,已经进入晚成岩作用阶段A亚期。

Tropism properties of particles are used to describe stability and distributing properties of particles to depicting compactness, evaluating parameters of coarse particle in principal axis direction, asphalt mastics film thickness and particle area are used to e-valuate the compacting characteristics.

针对旋转压实法,利用不同压实功作用成型试件模拟压实过程,采用数字图像处理技术,研究沥青混合料的压实成型特性,提出了以集料颗粒的取向特性描述沥青混合料的稳定性,以集料颗粒的分布特性来反映混合料的密实程度,定义了集料颗粒主轴方向、沥青砂胶膜厚及颗粒面积比等参数来进行评价。

The results showed that tillage had stronger compaction effect on Red soil. By analyzing retention properties, water content was higher in the same suction for Red soil. Field capacity and wilting coefficient were higher for Red soil than those for Lou soil, but effective moisture and saturated hydraulic conductivity were lower for Red soil. For Red soil, Lateral infiltration ability was stronger, infiltration rate was greater than one number degree for Lou soil and preferential flow occurred easily.

结果表明:耕作片红壤有较强的压实作用;从持水特征分析,同一吸力下红壤的含水量较高,田间持水量和凋萎系数也高于塿土,而有效水含量略低于塿土,饱和导水率却低于塿土1个数量级;从入渗特征分析,红壤的侧渗能力很强,入渗率比塿土高1个数量级,容易发生大孔隙流。

As the years pass and layer on layer of rock fragments pile up, they are squeezed or compacted by the weight of the materials on top of them. Then sediments may be cemented together, forming the sedimentary rocks.

随着时间的流逝,岩石和矿物碎屑一层层地堆积起来,上覆岩屑物质的重量对下伏岩屑产生压实作用,然后沉积物被胶结在一起,最终形成沉积岩。

As the years pass and layer on layer of rock fragments pile up, they are squeeze d or compacted by the weight of the materials on top of them. Then sediments may be cemented together, forming the sedimentary rocks.

随着时间的流逝,岩石和矿物碎屑一层层地堆积起来,上覆岩屑物质的重量对下伏岩屑产生压实作用,然后沉积物被胶结在一起,最终形成沉积岩。

As the years pass and layer on layer of rock fragments pile up, they are squeezed or compacted by the weight of the materials on top of them. Then sediment s may be cemented together, forming the sediment ary rocks.

随着时间的流逝,岩石和矿物碎屑一层层地堆积起来,上覆岩屑物质的重量对下伏岩屑产生压实作用,然后沉积物被胶结在一起,最终形成沉积岩。

The parameters of anisotropy of isothermal remanent magnetism are directly related to the shape of magnetic carrier minerals in rocks. They reflect the deformation and dislocation of carriers under compaction.

与非滞后剩磁各向异性的参数一样,等温剩磁各向异性的参数直接与岩石中的携磁矿物颗粒形状有关,它直接反映了岩石形成与压实作用下携磁矿物的变形和变位。

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