四川某水库大坝左坝肩边坡变形破坏机制及整治对策探讨   总被引：8，自引：0，他引：8  

王士天 《地质灾害与环境保护》1999,10(3):1-5

以现场考察和变形监测资料为依据,探讨一个下部有软弱基底,上部为硬脆性坡体的“二元结构”边坡的变形破坏问题,揭示这类边坡的变形总是以下部软弱岩体的不均匀压缩流变为先导,进而引起上部硬脆性坡体的拉裂与倾倒,最终通过渗入水的作用,使下部承载状况已进一步恶化了的软弱岩体,沿剪应力集中带发生剪切破坏而导致整个变形坡体的下滑。  相似文献   

The youngest lobe-dominated radio sources     

I. Owsianik  J. E. Conway  A. G. Polatidis   《New Astronomy Reviews》1999,43(8-10)

We present an analysis of multi-epoch global VLBI observations of the Compact Symmetric Objects: 2352+495 and 0710+439 at 5 GHz. Analysis of data spread over almost two decades shows strong evidence for an increase in separation of the outer components of both sources at a rate of 0.2h⁻¹c (for q=0.5 and H=100h km s⁻¹Mpc⁻¹). Dividing the overall sizes of the sources by their separation rates implies that these Compact Symmetric Objects have a kinematic age 10⁴ years. These results (and those for other CSOs) strongly argue that CSOs are indeed very young sources that probably evolve into much larger classical doubles.  相似文献   

大姚铜矿紫色砂岩的压拉变形特性试验研究     

谢强  余贤斌  张永兴  纳裕康 《岩土力学》2007,28(10):2155-2160

介绍了一种可对同一岩石试样分别进行单轴压缩和单轴拉伸实验的试验装置,该装置改变了因岩样不同而导致的压拉试验结果无法进行直接对比分析的现状,为岩石从受压转向受拉或从受拉转向受压的过渡特性的试验研究提供了可能。以云南大姚铜矿紫色砂岩为例,研究了其在压拉试验条件下的变形特性。结果表明：该种岩石从压缩到拉伸阶段弹模变化不大,但压缩泊松比与拉伸泊松比的变化较为复杂。试验同时证明该类岩石的压缩与拉伸并不是截然不同的两种过程,单轴压缩试验的卸载曲线与直接拉伸试验的加载曲线具有很好的连续性。  相似文献   

On the stability of compact supermassive objects     

L. Verozub  A. Kochetov 《Astronomische Nachrichten》2001,322(3):143-152

Proceeded from the gravitation equations proposed by one of authors it was argued in a previous paper that there can exist supermassive compact configurations of degenerated Fermi‐gas without events horizon. In the present paper we consider the stability of these objects by a method like the one used in the theory of stellar structure. It is shown that the configurations are stable.  相似文献   

Soil macroporosity and infiltration characteristics of a forest podzol     

J. M. Buttle  D. J. McDonald 《水文研究》2000,14(5):831-848

Spatial distribution of soil macroporosity was determined for a forest podzol from tension infiltrometer measurements at the soil surface. Surface‐derived macroporosity values were compared with point infiltration characteristics obtained from soil water content and soil water chemistry measurements during an experimental irrigation, and with parameters of a kinematic wave model applied to soil water content data. Macroporosity estimated by the tension infiltrometer ranged from 0·00087 to 0·0219% of soil volume, and infiltration at these two sites was dominated by propagation of a well‐defined wetting front through the soil profile and bypass flow via soil macropores, respectively. Infiltration at sites with intermediate macroporosities reflected a combination of these two processes, although results were inconclusive at one site owing to lateral flow at the base of the soil profile. There was no agreement between macroporosities estimated by the tension infiltrometer and the kinematic wave model. The maximum soil conductance parameter within the profile at a site, however, was related directly to the surface‐derived macroporosity. The partial agreement between surface‐derived macroporosity estimates and point infiltration characteristics shown here supports the use of tension infiltrometry as a rapid, non‐destructive method of assessing spatial variations in the relative contribution of macropore flow to the infiltration process. Copyright © 2000 John Wiley & Sons, Ltd.  相似文献   

Finch–Skea gravastar model in f(R,T) theory     

《New Astronomy》2022

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平台运动下深水钻井隔水管非线性动力响应研究   总被引：1，自引：0，他引：1  

王腾  张修占  朱为全 《海洋工程》2008,26(3)

建立深水钻井隔水管在波、流和平台运动的联合作用下的运动方程,模拟1 000 m深水钻井隔水管的非线性动力响应.分析在波、流作用下钻井液密度和顶部张力比等因素对隔水管振动频率的影响,研究平台的静偏移和动态运动对隔水管最大弯矩分布的影响.结果表明,平台运动对深水钻井隔水管的动力响应有较大影响,使隔水管上部最大弯矩峰值增加了1倍多.  相似文献   

液气共存的耗散粒子动力学模拟          下载免费PDF全文

王晓亮  陈硕 《海洋学报》2010,32(10):6778-6785

传统的耗散粒子动力学方法(DPD)由于采用了纯排斥的守恒力相互作用,从而不能适应液气共存或者带有自由面流体的模拟.这里研究了DPD方法中新近提出的一种短程排斥、长程吸引相互作用,探索了这种改进势能对于DPD方法模拟液气共存的能力.模拟了这种新势能所形成的液气过渡界面,计算了过渡界面区的应力分布,发现应力分布与多体DPD方法所得结果一致.进一步对表面张力进行了研究,验证了这种势能所形成的界面满足Laplace定律,而通过理论公式与Laplace定律分别所得到的表面张力也彼此相符.  相似文献