首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   792篇
  免费   122篇
  国内免费   117篇
测绘学   69篇
大气科学   93篇
地球物理   269篇
地质学   200篇
海洋学   277篇
天文学   50篇
综合类   36篇
自然地理   37篇
  2024年   4篇
  2023年   1篇
  2022年   5篇
  2021年   7篇
  2020年   16篇
  2019年   15篇
  2018年   12篇
  2017年   29篇
  2016年   30篇
  2015年   19篇
  2014年   37篇
  2013年   57篇
  2012年   41篇
  2011年   44篇
  2010年   55篇
  2009年   62篇
  2008年   60篇
  2007年   69篇
  2006年   48篇
  2005年   38篇
  2004年   37篇
  2003年   48篇
  2002年   30篇
  2001年   26篇
  2000年   32篇
  1999年   28篇
  1998年   28篇
  1997年   18篇
  1996年   11篇
  1995年   14篇
  1994年   23篇
  1993年   18篇
  1992年   12篇
  1991年   7篇
  1990年   9篇
  1989年   13篇
  1988年   7篇
  1987年   9篇
  1986年   2篇
  1985年   3篇
  1984年   1篇
  1983年   1篇
  1980年   1篇
  1978年   2篇
  1973年   2篇
排序方式: 共有1031条查询结果,搜索用时 46 毫秒
981.
把重力时序系统视为慢时变系统,根据线性系统分析的理论方法,用差分方程描述该系统的等价参数模型, 通过判断参数序列的稳定性来探索前兆异常。对河西流动重力观测网1994—2009年3个测点的观测数据的计算分析验证了该方法的有效性,但失稳与地震前兆的关系还需进一步研究。  相似文献   
982.
徐明江  魏德敏  何春保 《岩土力学》2011,32(4):1113-1118
考虑土颗粒、孔隙流体的压缩性及各相物质间的黏性、惯性耦合作用,采用理论上更加严谨的饱和度本构关系式,建立了非饱和土的动力控制方程。该组方程与饱和土的经典Biot波动方程完全兼容,因此,具有更广泛的适用性。通过引入一组状态向量,在圆柱坐标系下将非饱和土满足的波动方程转化为状态方程组,利用Hankel变换,求解状态方程组,得到了传递矩阵。结合边界条件及层间接触连续条件,求解了层状非饱和地基的稳态动力响应问题。数值算例表明:土层对地表动位移的影响主要集中在临界深度范围内;软硬土层的相对次序对地表动位移幅值有显著影响;饱和度增大会引起土的物理参数发生相应的改变,尤其是动剪切模量通常降幅较大,而动剪切模量是决定位移幅值的关键因素,最终的结果是导致地表动位移幅值明显增大。  相似文献   
983.
王小岗 《岩土力学》2008,29(3):685-690
基于提出的横观各向同性饱和多孔介质Biot波动方程的一般解,研究了饱和半空间地基在竖向点源简谐激振荷载作用下地表振动的衰减特征,分析了激振频率以及横观各向同性饱和土介质的各向异性参数和孔隙渗透系数对地表振动特征的影响。计算结果表明,低频和高频激振时,地表位移衰减特性存在明显差异;在饱和土的各向异性参数中,纵向和水平方向动态渗透系数比值和刚度系数比值对地表位移衰减影响最大,这也说明采用各向同性饱和介质的动力学模型不能准确地描述具有明显各向异性特性的饱和土地基的动力特性。  相似文献   
984.
碳酸盐岩储层多角度弹性阻抗流体识别方法   总被引:8,自引:5,他引:3       下载免费PDF全文
碳酸盐岩储层的AVO响应要比碎屑岩储层响应微弱,因此,弹性阻抗(EI)即使在确定了最佳入射角的情况下,要判断碳酸盐岩储层中的流体性质,依然十分困难.本文提出了一种多角度扩展弹性阻抗(MEEI)反演进行碳酸盐岩储层流体识别方法.利用已有钻井的测井数据,通过计算目的层段的MEEI,建立相应的含流体模式,进而建立了碳酸盐岩储层流体检测中的有效气水判据.通过不同入射角下EEI随入射角变化的不同趋势,可以有效识别储层中含气或含水情况,判别储层好坏.本文方法的有效性在四川盆地某地区实际资料应用中取得了良好的流体检测效果.  相似文献   
985.
Based on arbitrarily wide-angle wave equations,a reverse-time propagation scheme is developed by substituting the partial derivatives of depth and time with central differences. The partial derivative of horizontal direction is replaced with high order difference. The imaging condition is computed by solving the eikonal equations. On the basis of above techniques,a prestack reverse-time depth migration algorithm is developed. The processing exam-ples of synthetic data show that the method can remove unwanted internal reflections and decrease the migration noise. The method also has the advantage of fidelity and is applicable of dip angle reflector imaging.  相似文献   
986.
High force‐to‐volume extrusion damping devices can offer significant energy dissipation directly in structural connections and significantly reduce seismic response. Realistic force levels up to 400 kN have been obtained experimentally validating this overall concept. This paper develops spectral‐based design equations for their application. Response spectra analysis for multiple, probabilistically scaled earthquake suites are used to delineate the response reductions due to added extrusion damping. Representative statistics and damping reduction factors are utilized to characterize the modified response in a form suitable for current performance‐based design methods. Multiple equation regression analysis is used to characterize reduction factors in the constant acceleration, constant velocity, and constant displacement regions of the response spectra. With peak device forces of 10% of structural weight, peak damping reduction factors in the constant displacement region of the spectra are approximately 6.5 ×, 4.0 ×, and 2.8 × for the low, medium, and high suites, respectively. At T = 1 s, these values are approximately 3.6 ×, 1.8 ×, and 1.4 ×, respectively. The maximum systematic bias introduced by using empirical equations to approximate damping reduction factors in design analyses is within the range of +10 to ?20%. The seismic demand spectrum approach is shown to be conservative across a majority of the spectrum, except for large added damping between T = 0.8 and 3.5 s, where it slightly underestimates the demand up to a maximum of approximately 10%. Overall, the analysis shows that these devices have significant potential to reduce seismic response and damage at validated prototype device force levels. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献   
987.
This article presents a method to estimate flow variables for an open channel network governed by the linearized Saint-Venant equations and subject to periodic forcing. The discharge at the upstream end of the system and the stage at the downstream end of the system are defined as the model inputs; the flow properties at selected internal locations, as well as the other external boundary conditions, are defined as the outputs. Both inputs and outputs are affected by noise and we use the model to improve the data quality. A spatially dependent transfer matrix in the frequency domain is constructed to relate the model input and output using modal decomposition. A data reconciliation technique is used to incorporate the error in the measured data and results in a set of reconciliated external boundary conditions; subsequently, the flow properties at any location in the system can be accurately estimated from the input measurements. The applicability and effectiveness of the method is demonstrated with a case study of the river flow subject to tidal forcing in the Sacramento-San Joaquin Delta, in California. We used existing USGS sensors in place in the Delta as measurement points, and deployed our own sensors at selected locations to produce data used for the validation. The proposed method gives an accurate estimation of the flow properties at intermediate locations within the channel network.  相似文献   
988.
In this paper we present a reliable algorithm, the homotopy perturbation method, to construct numerical solutions of the space–time fractional advection–dispersion equation in the form of a rapidly convergent series with easily computable components. Fractional advection–dispersion equations are used in groundwater hydrology to model the transport of passive tracers carried by fluid flow in a porous medium. The fractional derivatives are described in the Caputo sense. Some examples are given. Numerical results show that the homotopy perturbation method is easy to implement and accurate when applied to space–time fractional advection–dispersion equations.  相似文献   
989.
This paper presents a well-balanced numerical scheme for simulating frictional shallow flows over complex domains involving wetting and drying. The proposed scheme solves, in a finite volume Godunov-type framework, a set of pre-balanced shallow water equations derived by considering pressure balancing. Non-negative reconstruction of Riemann states and compatible discretization of slope source term produce stable and well-balanced solutions to shallow flow hydrodynamics over complex topography. The friction source term is discretized using a splitting implicit scheme. Limiting value of the friction force is derived to ensure stability. This new numerical scheme is validated against four theoretical benchmark tests and then applied to reproduce a laboratory dam break over a domain with irregular bed profile.  相似文献   
990.
渗透压力作用下加锚裂隙岩体围岩稳定性研究   总被引:1,自引:0,他引:1  
王刚  李术才  王明斌 《岩土力学》2009,30(9):2843-2849
岩体中裂隙水的存在加剧了岩体结构围岩损伤;锚杆作为岩体工程的重要支护手段,被广泛应用于岩体加固工程中。结合无损伤材料的柔度张量的概念,用裂隙附加柔度张量来表示裂隙对岩体的损伤影响;引入渗透压力附加柔度张量的概念来定义渗透压力对裂隙岩体强度的损伤影响;利用附加刚度来反映锚杆对裂隙岩体的加固作用,附加刚度求逆即得柔度张量。对渗透压力作用下锚固裂隙岩体渗流场与损伤场相互作用及耦合机制进行了深入研究;基于能量互易定理,自洽理论等,分别在压剪和拉剪应力状态下推导了渗透压力作用下加锚裂隙岩体等效损伤模型,建立了相应的计算方法,应用半解耦方法对理论模型进行了有限元程序化。在有限元程序中,将渗透体积力化为等效节点力,参与各单元间应力调整且表现为岩体变形过程中刚度的降低;锚杆锚固力等效为单元节点力,并体现为岩体整体变形刚度的提高。结合工程实际,着重讨论渗透压力作用对隧道围岩稳定性的影响。分析表明,渗透压力对岩体围岩变形破坏及稳定性的影响是不可忽略的。  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号