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烃源岩—流体相互作用模拟实验研究 总被引:2,自引:0,他引:2
为了探讨烃源岩与孔隙流体之间相互作用过程和机理以及有机酸的生成及其影响因素,我们开展了烃源岩-流体相互作用模拟实验研究。实验结果表明:Ⅱ型干酪根形成有机酸的能力大于Ⅰ型干酪根,水的矿化度对有机酸的形成影响甚微,随着温度升高,流体中有机酸的含量也随之增大。pH值对有机酸形成的影响非常明显,中性和碱性条件更有利于生成有机酸。其中乙酸的形成有利于碳酸盐矿物的溶解,而草酸的形成不利于碳酸盐的溶解。温度对烃源岩的影响与烃源岩的矿物组成有很大的关系,对于富碳酸盐烃源岩,Ca、Mg、Na三元素在水中的溶解量,与温度呈反相关的关系,对于贫碳酸盐烃源岩,与反应温度之间则呈现出正相关的关系。而无论碳酸盐含量高低,Si在溶液中的含量都会随着温度的升高而增大。酸性溶液对烃源岩的溶解能力最强,无论原始反应溶液的酸碱性,反应结果都最终趋于弱碱性。流体的含盐量对烃源岩中Mg的溶解影响差异较大,低盐度的流体有利于Mg溶解。 相似文献
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为了探讨烃源岩与孔隙流体之间相互作用过程和机理以及有机酸的生成及其影响因素,我们开展了烃源岩-流体相互作用模拟实验研究。实验结果表明:Ⅱ型干酪根形成有机酸的能力大于Ⅰ型干酪根,水的矿化度对有机酸的形成影响甚微,随着温度升高,流体中有机酸的含量也随之增大。pH值对有机酸形成的影响非常明显,中性和碱性条件更有利于生成有机酸。其中乙酸的形成有利于碳酸盐矿物的溶解,而草酸的形成不利于碳酸盐的溶解。温度对烃源岩的影响与烃源岩的矿物组成有很大的关系,对于富碳酸盐烃源岩,Ca、Mg、Na三元素在水中的溶解量,与温度呈反相关的关系,对于贫碳酸盐烃源岩,与反应温度之间则呈现出正相关的关系。而无论碳酸盐含量高低,Si在溶液中的含量都会随着温度的升高而增大。酸性溶液对烃源岩的溶解能力最强,无论原始反应溶液的酸碱性,反应结果都最终趋于弱碱性。流体的含盐量对烃源岩中Mg的溶解影响差异较大,低盐度的流体有利于Mg溶解。 相似文献
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Ge Zhonghu Nanjing University Nanjing Jiangsu Fan Bingheng Feng Qiyan Wang Yonghong China University of Mining Technology Xuzhou Jiangsu Wang Xichuan 《《地质学报》英文版》1993,67(4):443-451
A model has been constructed to study water flow in a single clay crack, and a new concept of the critical rise rate of water level in the crack has been put forward. When the water level rises faster than this critical rate, the flow in a crack will increase, and vice versa. The flow in a crack is not in proportion to the water level. The maximium water flow in clay is 30-40 times smaller than that in a rock fissure under the same condition. In the process of water discharge, the flow in a crack will lessen gradually, and the crack will grow narrower by 3.0-4.0cm, with its depth reducing by over 50%. 相似文献
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Huang Lixing 《岩土力学》1985,6(2):89-97
The shock of stress waves causes deformation in intact medium, the form of new cracks and finally the failure in the material. The preexisting cracks not only help increase fracture efficiency but also absorb the energy of the stress wave to induce a decay of its propagation. Therefore the study of interaction of Stress waves with cracks will greatly contribute to the interpretation of blasting mechanism, the stress wave propagation and the dynamic behaviour of material. Our emphasis is laid on interaction of stress wave with cracks, and the influence of cracks on attenuation of the wave propagation. A view is made of the current state of model calculation and experimental technique carried out in this field. 相似文献
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Based on specific features of the geological structure and hydrogeological conditions of the Mezen Syneclise, the trend and quantitative estimates of compositional changes of groundwaters in Vendian sandy–clayey rocks in different hydrodynamic zones are given. 相似文献
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Wang Xiangqian Li Yingming Zhao Chengxing Wang Yi Huang Shunjie 《Geotechnical and Geological Engineering》2021,39(8):5931-5942
Geotechnical and Geological Engineering - In order to reveal the mechanism of surrounding rock deformation and instability of soft rock roadway in 12# working face of Puhe coal mine, and... 相似文献
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应力波与可滑移岩石界面间的相互作用研究 总被引:10,自引:1,他引:10
研究了应力波与用节理刚度系数描述的线性滑移岩石界面间的相互作用,给出了其透、反射波幅的一般表达式。通过应力波垂直人射界面时的具体分析,反映出岩石界面的节理刚度对应力波传播的重要影响,并揭示了岩石界面对应力波的高频滤波作用。 相似文献
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Zhang Dongjie Wang Jianduo Guo Shuai Cao Jianli 《Geotechnical and Geological Engineering》2022,40(11):5377-5395
Geotechnical and Geological Engineering - In the block caving mining, the significant rock mass deformation and surface subsidence will be formed with the continuous extraction of ore. However, the... 相似文献
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岩石裂纹扩展速度的研究与地震过程初探 总被引:1,自引:0,他引:1
本文试图通过对肥东大理岩的预制裂纹三点加载下的扩展速度的测量,模拟已有断裂再次经受应力变化时,断裂的扩展情况。试验结果给出了大理岩稳态扩展速度为1.1×10-5~2.8×10-4m/s,失稳后的扩展速度为5×101~1.2×103m/s。同时还给出了失稳后扩展速度的分布,并用断裂力学止裂观点对此作了解释。对裂纹扩展与地震孕震过程的关系也作了初步探讨。 相似文献
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对闽北570铀矿床,赣南6722铀矿床,赣东北银山多金属矿床的长英质隐爆角砾岩及其基底岩石,用pH=1.9,含ΣS=3.2×10-4,Σd=3.5×10-4,ΣF=3×10-5的水溶液,在90℃条件下进行水-岩作用实验,研究岩石中活动性U,Th,Pb,Zn等元素的地球化学行为。实验结果证实:岩石中铀、锌、铅具有较强的活化迁移能力;交代蚀变作用对铀活化和成矿富集有特殊重要意义;长英质隐爆角砾岩不是所研究矿床矿物质的主要来源;基底围岩对成矿有重要贡献。 相似文献
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S. Y. Wang S. W. Sloan M. L. Huang C. A. Tang 《Rock Mechanics and Rock Engineering》2011,44(2):179-198
Using a numerical modelling code, rock failure process analysis, 2D, the progressive failure process and associated acoustic
emission behaviour of serial and parallel rock samples were simulated. Both serial- and parallel sample models are presented
for investigating the mechanism of rock pillar failure. As expected, the numerical results show that not only the stiffness,
but also the uniaxial compressive strength of the rock plays an important role in pillar instability. For serial pillars,
the elastic rebound of a rock pillar with higher uniaxial compressive strength can lead to the sudden failure of an adjacent
rock pillar with lower uniaxial compressive strength. The failure zone forms and develops in the pillar with lower uniaxial
compressive strength; however, the failure zone does not pass across the interface of the two pillars. In comparison, when
two pillars have the same uniaxial compressive strengths but different elastic moduli, both serial pillars fail, and the failure
zone in the two pillars can interact, passing across the interface and entering the other pillar. For parallel pillars, damage
always develops in the pillar having the lower uniaxial compressive strength or lower elastic modulus. Furthermore, in accordance
with the Kaiser effect, the stress-induced damage in a rock pillar is irreversible, and only when the previous stress state
in the failed rock pillar is exceeded or the subsequent applied energy is larger than the energy released by the external
loading will further damage continue to occur. In addition, the homogeneity index of rock also can affect the failure modes
of parallel pillars, even though the uniaxial compressive strength and stiffness of each pillar are the same. 相似文献
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切削机理模型是研究岩石钻进切削过程中的切削力以及切削热的基础。在分析岩石切削机理模型的基础上,基于摩尔理论和裂纹扩展理论,分析中硬岩石切削状态,认为在中硬岩石切削过程中岩石存在着脆性切削和延展性切削2种方式,在此基础上得到新的中硬岩石切削机理模型。以砂岩、大理岩和花岗岩为钻进对象,开展微钻实验研究。结果表明:切削过程为岩石在刀具的扭矩和推进力作用下发生破坏,导致小岩屑、大切屑不断循环产生的过程,小大切屑形成主要源于岩石挤压变形和裂纹生成扩展。实验结果与岩石切削机理表现出较好的一致性。 相似文献
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金川软岩蠕变破坏机理电镜实验研究 总被引:1,自引:0,他引:1
为探讨金川矿岩石蠕变破坏机理,应用微观扫描电镜(SEM)对蠕变受力情况下岩石破坏断口微观形态进行了观察研究,并分析了其产生的微观破坏机制。结果表明:岩石蠕变断裂的微观机制主要是拉伸、剪切作用下岩石发生脆性断裂,从岩石断裂微观形态研究岩石蠕变断裂,可以更好的揭示岩石断口微观形貌特征、裂纹生核、扩展、及断裂方式与岩石蠕变演进过程的联系。 相似文献
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Effect of Surcharge on the Stability of Anchored Rock Slope with Water Filled Tension Crack under Seismic Loading Condition 总被引:1,自引:0,他引:1
S. K. Shukla S. Khandelwal V. N. Verma N. Sivakugan 《Geotechnical and Geological Engineering》2009,27(4):529-538
In this paper, an analytical expression is derived for the factor of safety of the rock slope incorporating most of the practically
occurring destabilizing forces as well as the external stabilizing force through an anchoring system. The slope stability
is analyzed as a two-dimensional problem, considering a slice of unit thickness through the slope and assuming negligible
resistance to sliding at the lateral boundaries of the sliding block. A detailed parametric study is presented to investigate
the effect of surcharge on the stability of the rock slope for practical ranges of governing parameters such as inclination
of the slope face, inclination of the failure plane, depth of tension crack, depth of water in tension crack, shear strength
parameters of the material at the failure plane, unit weight of rock, stabilizing force and its inclination, and seismic load.
For the range of parameters considered in the present study, it is found that the factor of safety of the rock slope decreases
with increase in surcharge; the rate of decrease being relatively higher for lower values of surcharge. It is also observed
that for a specific surcharge, the factor of safety depends significantly on all other parameters, except for unit weight
of rock and higher values of inclination of stabilizing force to the normal at the failure plane. For any combination of these
variables, the surcharge plays a vital role in the stability. A perfectly stable slope at relatively low surcharge can become
unsafe with the increase in surcharge. The deterioration in the stability can be quite rapid, depending on the combination
of the factors under consideration. The analysis and the general expression proposed herein can be used to carry out a quantitative
assessment of the stability of the rock slopes. 相似文献
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