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981.
982.
针对活动断层震间InSAR形变场提取中存在SAR观测数据不足、轨道误差难以合理去除的问题,该文进行了利用单幅InSAR图像提取震间形变场的模拟研究:考虑到InSAR图像中轨道误差和震间形变场的空间分布特征,利用一次多项式模型和深部滑动模型模拟了100组叠加的InSAR形变场;然后采用直接恢复震间形变场、先分离轨道误差再恢复震间形变场、一步法分离轨道误差与恢复震间形变场3种方法对模拟的震间形变场进行了恢复实验。结果表明,基于单幅InSAR图像,利用一步法能够较为准确地恢复震间形变场。 相似文献
983.
一种相机标定参数的柱面全景影像拼接方法 总被引:1,自引:0,他引:1
针对全景影像拼接方法存在批量快速拼接困难、匹配精度低、匹配成功率不高等问题,该文提出一种多拼柱面全景相机影像的严密拼接方法。首先对全景相机进行标定,获取每台相机的内参数和单相机之间的相对外方位元素;再根据摄影距离以及摄影中心、像点与物点三点共线的原则,求出每张影像中像点对应的物方点的坐标;最后根据虚拟摄影中心、物点和虚拟像点三点共线的原则,得出像点在柱面上对应的虚拟像点坐标,经过角度归算和影像间的融合处理,获取柱面全景影像。实验表明,多拼全景相机影像拼接方法达到了严密、快速的拼接效果,可方便实现全景影像和单相机影像之间的坐标变换,为后续全景影像的浏览、量测、真彩激光点云的生成和实景测量等应用提供了一种影像拼接方法。 相似文献
984.
针对冰箱企业中存在多个抽样室的情况 ,本文提出了 1种基于网络的多服务器抽样测试系统的设计方案 ,并给出了实现方法。该系统为企业类似测试系统的应用提供了 1种方案 相似文献
985.
986.
Mao Fangguan Lu Shunchang Luo Ruiren
Senior Engineer Naval Medical Research Institute P. L. A. of China Shanghai Senior Engineer Navigation Guarantee 《中国海洋工程》1995,(4)
The Diver Gas Recovery Installation (DGRI) was evaluated at 80 msw saturation - 100 msw excursion diving on HeO2 in the Naval Medical Research Institute (NMRI) of China in April, 1995. The diving depth, lockout time, breathing gas flow rate and consumption, inspired oxygen partial pressure (PO2) and carbon dioxide partial pressure (PCO2) were monitored. The results indicated that PO2 was controlled to fluctuate from 64.3 to 84.0 kPa and PCO2 went up from 0.01 kPa up to O.I kPa during 4 hours excursion diving; recovery of breathing gas reached 95%; three divers felt well and breathed comfortably during simulating heavy work. The test showed that it met desired performance goals. The DGRI is a kind of important equipment for long duration deep dive. It enables the gases exhaled by the divers to be re-cycled, and therefore it has great social, military and economic significance for diving operation and submarine rescue. 相似文献
987.
Tips and tricks in designing management procedures 总被引:2,自引:2,他引:2
Rademeyer Rebecca A.; Plaganyi Eva E.; Butterworth Doug S. 《ICES Journal of Marine Science》2007,64(4):618-625
988.
989.
Jeffrey?W.?BookEmail author Pavel?Pistek Henry?Perkins Keith?R.?Thompson William?J.?Teague Gregg?A.?Jacobs Moon-Sik?Suk Kyung-Il?Chang Jae-Chul?Lee Byung?Ho?Choi 《Journal of Oceanography》2004,60(6):977-993
During 1999–2000, 13 bottom mounted acoustic Doppler current profilers (ADCPs) and 12 wave/tide gauges were deployed along two lines across the Korea/Tsushima Strait, providing long-term measurements of currents and bottom pressure. Tidally analyzed velocity and pressure data from the moorings are used in conjunction with other moored ADCPs, coastal tide gauge measurements, and altimeter measurements in a linear barotropic data assimilation model. The model fits the vertically averaged data to the linear shallow water equations in a least-squares sense by only adjusting the incoming gravity waves along the boundaries. Model predictions are made for the O1, P1, K1, μ2, N2, M2, S2, and K2 tides. An extensive analysis of the accuracy of the M2 surface-height predictions suggests that for broad regions near the mooring lines and in the Jeju Strait the amplitude prediction errors are less than 0.5 cm. Elsewhere, the analysis suggests that errors range from 1 to 4 cm with the exception of small regions where the tides are not well determined by the dataset. The errors in the model predictions are primarily caused by bias error in the model’s physics, numerics, and/or parameterization as opposed to random errors in the observational data. In the model predictions, the highest ranges in sea level height occur for tidal constituents M2, S2, K1, O1, and N2, with the highest magnitudes of tidal velocities occurring for M2, K1, S2, and O1. The tides exhibit a complex structure in which diurnal constituents have higher currents relative to their sea level height ranges than semi-diurnal constituents. 相似文献
990.
For microearthquake surveys conducted with small networks in regions where the seismic velocity structure has large vertical gradients, the formal errors accompanying hypocentral solutions obtained by a generalized inverse method may be misleading since they do not incorporate the effects of nonlinearity in travel times. An alternative method for estimating uncertainties involves calculating travel time residuals over a regular grid and using the F statistic to contour confidence volumes. We present a statistical expression for the latter confidence limits that is applicable when an independent estimate of arrival time errors is available from observations accumulated for a number of earthquakes. Synthetic experiments comparing the results of the grid search and generalized inverse methods show that in cases where solutions are obtained either without S wave information or for epicenters which lie well outside the network, the effects of nonlinearity on the shape of the confidence regions may be significant. However, for the well-observed events both methods yield comparable confidence volumes in good agreement with the distribution of hypocenters obtained from repeated locations incorporating random errors. The generalized inverse method has the advantage that it requires fewer calculations, so the examination of systematic errors in hypocentral parameters produced by uncertainties in the seismic velocity structure can be studied in a more computationally efficient manner. Except in the cases of poorly resolved earthquakes, the effects of nonlinearity on uncertainties in hypocentral parameters can be observed by the application of the F statistic to the variation of the generalized inverse travel time residuals with focal depth. 相似文献