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The heat flow equation in cylindrical coordinates is solved numerically for any general distribution of thermal diffusivity. The temperature stabilization of a borehole is considered, and solutions for the case where thermal diffusivity is a function of radial distance from the borehole are obtained and compared to solutions for uniform diffusivity. The results are discussed in terms of thermal diffusivities that are different for the well contents and for the surrounding material. It is found that the approach to formation temperature is affected by differences between well contents and the surrounding region. 相似文献
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A numerical technique to compute the resistivity transform directly from the observed Wenner sounding data has been developed. In principle, the procedure is based on a decomposition method and consists of two steps: the first step determines a function that approximates the apparent resistivity data and the second step transforms this function into the corresponding kernel by an analytical operation. The proposed method is tested on some theoretical master curves. A high degree of precision is achieved with very little computer time. The applicability is shown on two field examples. 相似文献
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新疆是个多震区 ,破坏性地震常引起房屋的破坏和财产的损失。本文分析了房屋在震后产生地基失稳和不均匀沉降等破坏现象的原因 ,并提出了处理方法和补救措施 ,可供震区有类似图 1 车间柱网平面图Fig.1 Plan of the colonnade in the work- shop的现象房屋的补救处理参考使用。1 工程概况新疆喀什地区某车间建于 195 8年 ,柱网平面图如图 1所示。 1996— 1999年喀什地区连续发生多次 6级以上地震 ,致使 EA 列柱产生不均匀沉降 ,影响了车间的正常使用。测量表明 ,34、36、38、4 0、4 2号列柱中沉降量分别为 :13.1、12 .8、12 .2、11.9及… 相似文献
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Pedro A. BASILE Center for Hydroenvironmental Research National University of Rosario 《国际泥沙研究》2001,16(3)
1 INTRODUCTIONMany hydro-momhological mathematical models neglect the innuence of river bed maerialheterogeneity and its time and space changes during transport and related erosion/dePosition processes. Inthese models a rePresentative diameter of the river bed grain-size distribution (for examPle d5o) isspecified as initial data in each comPutational point of the modeled domain. Different d5o can be assignedto each ghd point but temPoral changes in bed material gradation cannot be simula… 相似文献
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不同地震烈度下边坡稳定性计算实例 总被引:3,自引:0,他引:3
按照工程场地地震安全性评价的有关规定,在充分研究场地工程地质,地震地质背景等工作的基础上,采用BISHOP法以某拟建工程场地在不同地震烈度下其边坡的稳定性进行了计算。 相似文献
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HANS-JÜRGEN LEHMANN 《Geophysical Prospecting》1971,19(1):133-155
In magnetic routine interpretation the comparison of two-dimensional model curves with measured magnetic anomalies is widely used for an approximate evaluation of the position and depth of magnetic models. Before starting an interpretation of a survey by means of two-dimensional models, it is very useful to have an idea of the shape of anomalies caused by extended but finite bodies, taking into account various strike directions: Three sets of anomalies of thin plates (horizontal length 19, downward length 9, width 1) dipping 30°, 60°, and 90° resp. for various strike directions and an inclination of 20° were computed. Some of these anomalies, e.g. those with nearly N-S strike direction look rather complicated, and at the first glance one would not expect that they are caused by such simple bodies. Several profiles crossing the computed anomalies perpendicularly were interpreted two-dimensionally. For less extended anomalies the depths determined for the top of the plates are 10-20% too small, the magnetization amounts to 50–75 % of the value of the finite bodies. The interpretation of the profiles covering more extended anomalies gave very accurately the same values for the position, depth and magnetization for the two-dimensional body as for the original three-dimensional model. Anomalies of vertical prisms with varying extensions in the y-direction were computed. Their differences in amplitude and in the distance maximum-minimum show that interpretation of short anomalies by two-dimensional methods yields depth errors of up to 20 percent. To see the possibilities of the separation of superimposed anomalies dike anomalies were added to the anomaly of a broad body in great depth and several attempts were made to interpret parts of the composite anomalies. The interpreted bodies lie too deep. In complicated cases the depth values can have large errors, but experienced interpreters should be able to keep the errors in the range of one third of the depth values. 相似文献
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本文提出了一类用于地震预测的统计模型,该模型包括地震活动的趋势部分、周期成分及随机波动部分,并据该模型对小华北地区的地震趋势进行了估计。 相似文献
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三维粘弹性LDDA方法及其在地学中的初步应用 总被引:1,自引:0,他引:1
在二维弹性LDDA方法的基础上提出了三维粘弹性LDDA方法,并开发了相应的计算机软件.通过两个三维块体的摩擦滑动数值实验,证明了这个方法的理论和程序是正确和可靠的.用该程序研究了印度板块碰撞引起的东亚地区的现今速度场和沿主要断裂带的相对位移速率.初步结果表明,碰撞边界附近的速度最大,向内部衰减很快.青藏高原向北东方向运动,华北平原向东运动,东南亚向东南运动.在祁连山西南和东北速率变化的衰减梯度分别为0.05和0.007mm/a/km,衰减是非线性的,运动方向由北东转向近东西方向,变化很大.穿过龙门山断裂的速度衰减基本是线性的,其值为0.01 mm/a/km,运动方向为南东.印度板块碰撞对于东经115以东和北纬45以北的区域影响很小.由计算得到的速度场与GPS观测结果基本一致.计算得到的班公湖——怒江——澜沧江断裂带在近1Ma以来的相对滑动速率平均约0.5mm/a;金沙江断裂带相对滑动速率最大,为0.8 mm/a;郯庐断裂带基本不动.理论和计算表明,三维粘弹性LDDA方法可以用于研究具有断层的地球动力学问题. 相似文献
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本文通过地震史料考证,野外地质调查,钻孔土层力学性质分析,场地震害考察等资料的研究,认为琼州历史地震在滨海地带第四纪软弱土层中诱发了砂土液化、软土流滑、造成地基失效、场地不均匀沉陷的情况,是导致震区内特殊地段“陆地沉陷”的主要原因 相似文献
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Formulae are developed to determine the three-dimensional response of twin lined tunnels buried in an infinite medium subjected to seismic loadings using the method of successive reflection. The convergence of the method has been demonstrated both analytically and numerically. The dynamic interaction of the twin tunnels subjected to seismic waves is investigated numerically. It is found that the three-dimensional response of twin tunnels may differ significantly from the two-dimensional response, and that through-soil interaction between the tunnels may also be significant. 相似文献
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D. W. POWELL 《Geophysical Prospecting》1967,15(2):208-220
The symmetry shown, by the function describing the magnetic anomaly due to a dyke or vertical fault step leads to a method by which an observed profile may be adjusted to conform with that symmetry. By making these adjustments a minimum the ideal dyke or fault profile closest to the observations is constructed. In three of four possible situations this is interpreted by simple geometry. Parallelpiped models may be transformed into two dykes for symmetry analysis. Depth limited models are not so amenable, even in special cases. 相似文献
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Applications of hydrological models to northern wetland-dominated regions have been limited in the past to a few case studies on small basins employing ‘lumped’ models. Only recently have there been attempts to apply the grouped response unit (GRU) distributed modelling approach using terrain classifications to these same basins. This study summarizes recent efforts in applying such a model. For the purposes of implementing the GRU approach, terrain types that are hydrologically significant and characteristic to the wetland-dominated regime were successfully discriminated using a principal component analysis and a hybrid unsupervised/supervised classification technique on Landsat–Thematic Mapper imagery. The terrain classifications were then used as input into a distributed hydrological model for calibration and validation using recorded spring runoff events. Preliminary model applications and results are described. Calibration to a historic spring runoff event yielded an r2 value of 0.86. Model validation, however, yielded much poorer results. The problems of model applicability to this region and limitations of sparse data networks are highlighted. The need for more field research in this type of hydrological regime, and associated improvements to the model parameter set are also identified. 相似文献