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961.
Analytical simulation of the dynamic compressive strength of a granite using the sliding crack model
A sliding crack model is employed to simulate rock strength under dynamic compression. It is assumed that the growth and nucleation of a sliding crack array presented results in the shear fault failure and dominate the mechanical properties of rock material. The pseudo‐tractions method is used to calculate the stress intensity factor of the sliding crack array under compression. With the utilization of a dynamic crack growth criterion, the growth of the sliding crack array is studied and the simulated strengths of a granite under dynamic compression are correspondingly obtained. It is concluded that the simulated rock strengths increase with increasing strain rates at different confining pressures, and the rising rates have a trend to decrease with increasing confining pressures. It is also indicated that the simulated rock strengths increase with increment of confining pressure at different strain rates, and the rising rates are almost identical at different strain rates. The simulation results are validated by the experimental data for the granite. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
962.
梁侯美 《广东海洋大学学报》1990,(1)
本文介绍磁罗经自差实测五种方法,是为船长提供多种方法,因地制宜,利用船泊港具备条件,选择符合条件的方法,测定本船的磁罗经自差,确保船舶安全航行。 相似文献
963.
Different commonly used predictive equations for the reaeration rate coefficient (K2) have been evaluated using 231 data sets obtained from the literature and 576 data sets measured at different reaches of the River Kali in western Uttar Pradesh, India. The data sets include stream/channel velocity, bed slope, flow depth, cross‐sectional area and reaeration rate coefficient (K2), obtained from the literature and generated during the field survey of River Kali, and were used to test the applicability of the predictive equations. The K2 values computed from the predictive equations have been compared with the corresponding K2 values measured in streams/channels. The performance of the predictive equations has been evaluated using different error estimation, namely standard error (SE), normal mean error (NME), mean multiplicative error (MME) and coefficient of determination (r2). The results show that the reaeration rate equation developed by Parkhurst and Pomeroy yielded the best agreement, with the values of SE, NME, MME and r2 as 33·387, 4·62, 3·58 and 0·95, respectively, for literature data sets (case 1) and 37·567, 3·57, 2·6 and 0·95, respectively, for all the data sets (literature data sets and River Kali data sets) (case 2). Further, to minimize error estimates and improve correlation between measured and computed reaeration rate coefficients, supplementary predictive equations have been developed based on Froude number criteria and a least‐squares algorithm. The supplementary predictive equations have been verified using different error estimates and by comparing measured and computed reaeration rate coefficients for data sets not used in the development of the equations. Copyright © 2003 John Wiley & Sons, Ltd. 相似文献
964.
VLBI数据软件相关处理方法研究 总被引:1,自引:0,他引:1
VLBI技术是 2 0世纪 6 0年代后期发展起来射电干涉新技术 ,自 2 0世纪 70年代至今VLBI数据预处理主要采用硬件相关处理机。近年来随着通用计算机性能的大幅度提高 ,利用软件方法对VLBI数据进行相关处理逐渐成为可能。介绍了国内外VLBI软件相关处理机的研究进展情况和VLBI数据相关处理的基本数学模型。针对实际软件相关处理方法研究中数学模型应用和各类参数选取等情况作了详细介绍。根据现有数据处理精度和处理速度 ,进一步分析了提高软件相关处理速度的可能性。 相似文献
965.
A challenging computational problem arises when a discrete structure (e.g. foundation) interacts with an unbounded medium (e.g. deep soil deposit), particularly if general loading conditions and non‐linear material behaviour is assumed. In this paper, a novel method for dealing with such a problem is formulated by combining conventional three‐dimensional finite‐elements with the recently developed scaled boundary finite‐element method. The scaled boundary finite‐element method is a semi‐analytical technique based on finite‐elements that obtains a symmetric stiffness matrix with respect to degrees of freedom on a discretized boundary. The method is particularly well suited to modelling unbounded domains as analytical solutions are found in a radial co‐ordinate direction, but, unlike the boundary‐element method, no complex fundamental solution is required. A technique for coupling the stiffness matrix of bounded three‐dimensional finite‐element domain with the stiffness matrix of the unbounded scaled boundary finite‐element domain, which uses a Fourier series to model the variation of displacement in the circumferential direction of the cylindrical co‐ordinate system, is described. The accuracy and computational efficiency of the new formulation is demonstrated through the linear elastic analysis of rigid circular and square footings. Copyright © 2004 John Wiley & Sons, Ltd. 相似文献
966.
A comparison of mean number of scatterings and escape probabilities has been made in isotropic scattering and dipole scattering
by using the angle-averaged partial frequency redistribution functionR
I. We have solved the equations of radiative transfer and statistical equilibrium simultaneously in a spherically symmetric
expanding atmosphere. Two cases of atmospheric extension (i.e.)B/A=3 and 10 (whereB andA are the outer and inner radii of the atmosphere) have been treated.
We find that the partial frequency redistribution gives a larger mean number of scatterings compared to that given by complete
redistribution. Velocities tend to reduce the mean number of scatterings and in crease the mean escape probabilities. 相似文献
967.
高程精度低的问题,一直是航空摄影测量产品的弱点,因此也是生产设计中的技术要点,本文通过三个实例,对不同资料、不同比例尺成果要求,采用不同技术措施保证了成果高程精度的做法进行了总结. 相似文献
968.
969.
场地基本周期是表征场地动力特性最基本的指标,也是评价场地条件的重要依据。本文介绍了计算场地基本周期的四种方法——子层周期求和法(规范法)、子层周期贡献系数法、简化Rayleigh法以及逐层单自由度法。收集并筛选了国内605组钻孔深度达到工程基岩的剪切波速剖面资料,其中:Ⅰ类场地10个;Ⅱ类场地300个;Ⅲ类场地249个;Ⅳ类场地46个。以传递函数法结果为标准,对上述四种方法的计算结果进行对比检验,就不同方法的偏差进行了深入分析,给出了其统计结果,并剖析了各方法应用于实际工程场地的适宜性。主要结论:(1)我国规范所采用的子层周期求和法虽然在工程中方便使用,但计算结果普遍存在显著偏差,其偏差的平均值大于20%,最大偏差甚至接近50%。(2)简化Rayleigh法和逐层单自由度法相较于规范法计算精度均有大幅提高,二者偏差在5%以内的工况数占比分别达到80%和70%以上。(3)子层周期贡献系数法采用了加权累加的计算方式,继承了规范法便于操作的优点,并且计算精度为本文所选四种方法中最高,其最大偏差不超过10%,偏差在5%以内的工况数占比达到85%,建议在实际工程中推广应用。 相似文献
970.
在利用多波束测深系统进行高精度海底地形测量时,各传感器之间数据采集时间不同步的问题,即存在时延偏差,这将会直接影响多波束测深数据质量,为此提出了一种基于最小二乘原理的多波束测深时延偏差探测及校正方法,给出了时延偏差探测及校正计算模型,设计了时延偏差探测及校正流程,通过实例分析,验证了所提方法的适用性和有效性。 相似文献