首页 | 官方网站   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   4331篇
  免费   981篇
  国内免费   1248篇
地球科学   6560篇
  2024年   5篇
  2023年   40篇
  2022年   99篇
  2021年   194篇
  2020年   222篇
  2019年   250篇
  2018年   220篇
  2017年   210篇
  2016年   243篇
  2015年   247篇
  2014年   278篇
  2013年   333篇
  2012年   287篇
  2011年   352篇
  2010年   281篇
  2009年   308篇
  2008年   312篇
  2007年   360篇
  2006年   332篇
  2005年   266篇
  2004年   244篇
  2003年   204篇
  2002年   175篇
  2001年   139篇
  2000年   142篇
  1999年   136篇
  1998年   95篇
  1997年   108篇
  1996年   92篇
  1995年   91篇
  1994年   71篇
  1993年   44篇
  1992年   44篇
  1991年   33篇
  1990年   16篇
  1989年   19篇
  1988年   19篇
  1987年   14篇
  1986年   11篇
  1985年   4篇
  1984年   3篇
  1983年   2篇
  1982年   3篇
  1981年   3篇
  1980年   1篇
  1979年   2篇
  1978年   1篇
  1977年   1篇
  1954年   4篇
排序方式: 共有6560条查询结果,搜索用时 15 毫秒
101.
滑带土动力学性质试验研究   总被引:1,自引:0,他引:1  
为了研究地震高烈度区老滑坡的复活变形原因,本文对滑坡滑带土的动力学特性进行了系列研究。本次试验采用扰动土样,制样基本物理指标按滑带土的现场测试指标确定,在不固结不排水条件下,运用MTS810Teststar程控液压伺服土动三轴仪对单个样品逐级放大动应力的分级试验方法进行。侧向压力 (围压 )分别采用 100kPa、20 0kPa、300kPa三级,通过施加轴向振动荷载 (力 )模拟地震作用,振动波形为正弦波,频率为 1Hz,振幅随试样性质确定。研究结果表明,滑带土在动荷载作用下的动力学性质与其静荷载作用下的力学性质有着较大的差异,主要表现在滑带土的动应力与动应变关系的非线性、滞后性及变形积累特点,动弹性模量与动强度的显著降低以及动阻尼比的显著增大特性。这揭示了动力作用下的滑坡复活原因之一,同时为滑坡稳定性评价和动力作用下的变形机制模拟分析提供了基础资料,也为分析滑带土动力本构模型提供了基本内容。  相似文献   
102.
挠曲线复位的微分方程解法求梁的位移   总被引:5,自引:0,他引:5  
梁位移求解的方法主要有两种:积分法和叠加法。积分法的困难是当多个荷载同时作用时,要按控制面分段列弯矩方程,这样,两次积分时带来的积分常数较多,导致依边界条件、连续条件定这些常数时要解多个联立方程,计算繁杂。梁位移求解的叠加法是借用典型荷载下梁已知积分结果来进行对应位置位移的叠加,具体是查转角方程、挠曲线方程表格。从表中知,梁任一位置处的位移方程大多是多次多项式,很难记忆,故离开表格便无法采用。本文找到了一种新的方法求梁的位移,通过设置比拟梁,使比拟梁的挠曲线复位于原梁,从而建立了相应的微分方程,求解此方程后便可得梁的位移,避开了分段多次积分或查表的弱点。  相似文献   
103.
郯庐断裂带的平移运动与成因   总被引:61,自引:4,他引:61  
在华北、华南板块碰撞期间,郯庐断裂带究竟是何种边界仍是没有解决的重大地学问题,许多学者对此提出了不同的构造解释模式。关于郯庐断裂的平移距离仍存在着较大的分歧与有待深入研究之处。在华北、华南板块拼合之后,郯庐断裂带发生了一次大规模的左行平移,其糜棱岩的^40Ar/^39Ar年龄为132~119Ma,指示为早白垩世的平移活动,平移活动中伴生了强烈的岩浆活动。这期左行平移标志着中国东部构造的重大转折,是滨太平洋构造对前期古特提斯构造的叠加,其动力学机制为太平洋区伊侨奈岐板块突然出现的高速斜向俯冲。  相似文献   
104.
长江河源区的河水主要元素与Sr同位素来源   总被引:20,自引:1,他引:20  
长江源区河水化学成分来自雨雪、蒸发盐岩、碳酸盐岩和硅酸盐岩。主要支流楚玛尔河、北麓河的主要阳离子为Na 、Ca2 和Mg2 ,占阳离子总量的97%以上.Ca Na,Mg Na,K Na的比值较低,87Sr 86Sr为0 709180±20~0 710280±11,河水成分以蒸发岩类溶解为主。发源于唐古拉山北坡的长江源头,及其支流主要阳离子为Ca2 ,Mg2 ,Na 占阳离子总量的97%以上,Ca Na,Mg Na,K Na的比值较楚玛尔河等河流高,87Sr 86Sr为0 708954±20~0 710455±18,表现为以碳酸盐岩和硅酸盐岩的溶解为主。计算表明,长江河源区河水中主要化学成分来自蒸发岩中Na 和Cl-,在河流水化学成分中占比例最大,长江河水中Cl-含量从河源区向下游明显逐渐减小,反应出河源区高寒干旱环境下河流蒸发岩的化学侵蚀作用较强的特征。  相似文献   
105.
医院住院部大楼抗震性能评价   总被引:1,自引:0,他引:1  
以某医院住院部大楼为例进行结构抗震性能评价,首先分析了场址的地震环境,开展了地震危险性分析工作,合成了不同地震危险水平下的地震动加速度时程。进而,通过对结构的模型简化,应用时程分析方法分析结构的抗震性能,得出了一些对其改造加固有意义的结论。  相似文献   
106.
本假设对于确定的相关系数及子台间距存在一个相干波长,将不同频率、震中距的相关性变化的原因归纳为视波长的变化.对近事件而言,几乎不存在相关系数十分理想的子台间距的区间范围.对非理想相关的台阵,应用S.Mykkeltveit等介绍的增益公式来预测台阵的增益,其效果与实际情况吻合的较好.论述了区域台阵与侦察远处事件的台阵有诸多不同之处.  相似文献   
107.
Introduction The rock medium shows mainly elastic character under low-temperature, low-pressure and external force for short duration, yet it shows rheologic property under high-temperature, high-pressure and long-time external force. It is reasonable that the rapid earthquake generating process lasted for tens seconds is analyzed by the elastic theory. As for the earthquake generating process for hundreds or thousand years, nevertheless, the rheologic property of rock must be taken into accou…  相似文献   
108.
In continent Lg is usually one of the predominant phases recorded by short-period or broad-band seismometers. A ray-theoretical approach shows that Lg wave is the superposition of higher-mode surface waves propagating in the continental crust[1—4]. The g…  相似文献   
109.
From April 1997 to June 1998 Nemurella pictetii populations were regularly sampled in two springstreams at 220 and 850 m a.s.l., respectively, in Hesse (Germany), at approximately 51°N. Random samples of larvae were taken at three week intervals during the vegetation period, and once a month during winter. Sex, instar, body length, head capsule width and wing pad length of all larvae were recorded. Temperatures were recorded every hour, temporal patterns of temperature agreed closely between sites. Mean winter lows were 3.9 °C at both sites, the mean summer high was 11.9 °C at the lower site, as opposed to 9.6 °C at the mountain site.At both sites, adult emergence started in May. At the mountain site, recruitment started in late July and continued into autumn. There was cohort splitting in the young generation. Some individuals grew rapidly until October–November, but last instar larvae first appeared in March the next year. 1600 degree-days above 0 °C were accumulated during complete development. At the lower site, recruitment began in early July, and cohort splitting also occurred. Fast growing summer recruits emerged as adults in late August, having accumulated only 700 degree-days (above 0 °C). Their offspring hatched in November-December and emerged the next spring, having accumulated also only 700 degree-days. However, only part of the population was bivoltine. Many of the summer recruits grew more slowly and accumulated close to 1900 degree days until they emerged the next spring, together with the offspring of their own fast-growing siblings. Dependence of growth rate on temperature could not be estimated and appears to vary with daylength. For example, 3–6 °C support growth and development provided daylength exceeds 10 hrs of light, or is rising.At both sites and in all cohorts individuals emerging earliest were larger than later emerging ones. The size decline is significantly correlated with number of days after the winter solstice. For the first time it is shown that the decline does not occur shortly before adult emergence but actually takes place several instars before the last. Size differences are then carried on, and amplified, during subsequent molts, until adulthood. The literature presently relates seasonal size declines of insects to high or rising temperatures experienced by larvae approaching adulthood. Our data show that, at least in Nemurella, this explanation fails. On average, females were distinctly larger than males. Differences in mean last instar size were noticed also between sites and years. They remain presently unexplained. The mean sex ratio in both populations was close to 1:1.  相似文献   
110.
The five MTMD models, with natural frequencies being uniformly distributed around their mean frequency, have been recently presented by the first author. They are shown to have the near‐zero optimum average damping ratio (more precisely, for a given mass ratio there is an upper limit on the total number, beyond which the near‐zero optimum average damping ratio occurs). In this paper, the eight new MTMD models (i.e. the UM‐MTMD1~UM‐MTMD3, US‐MTMD1~US‐MTMD3, UD‐MTMD1 and UD‐MTMD2), with the system parameters (mass, stiffness and damping coefficient) being, respectively, uniformly distributed around their average values, have been, for the first time here, proposed to seek for the MTMD models without the near‐zero optimum average damping ratio. The structure is represented by the mode‐generalized system corresponding to the specific vibration mode that needs to be controlled. Through minimization of the minimum values of the maximum dynamic magnification factors (DMF) of the structure with the eight MTMD models (i.e. through the implementation of Min.Min.Max.DMF), the optimum parameters and values of Min.Min.Max.DMF for these eight MTMD models are investigated to evaluate and compare their control performance. The optimum parameters include the optimum mass spacing, stiffness spacing, damping coefficient spacing, frequency spacing, average damping ratio and tuning frequency ratio. The six MTMD models without the near‐zero optimum average damping ratio (i.e. the UM‐MTMD1~UM‐MTMD3, US‐MTMD1, US‐MTMD2 and UD‐MTMD2) are found through extensive numerical analyses. Likewise, the optimum UM‐MTMD3 offers the higher effectiveness and robustness and requires the smaller damping with respect to the rest of the MTMD models in reducing the responses of structures subjected to earthquakes. Additionally, it is interesting to note, by comparing the optimum UM‐MTMD3 with the optimum MTMD‐1 recently investigated by the first author, that the effectiveness and robustness for the optimum UM‐MTMD3 is almost identical to that for the optimum MTMD‐1 (without inclusion of the optimum MTMD‐1 with the near‐zero optimum average damping ratio). Recognizing these performance benefits, it is preferable to employ the optimum UM‐MTMD3 or the optimum MTMD‐1 without the near‐zero optimum average damping ratio, when installing the MTMD for the suppression of undesirable oscillations of structures under earthquakes. Copyright © 2003 John Wiley & Sons, Ltd.  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-23

京公网安备 11010802026262号