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41.
C.C. Fong Y.F. Shi W.K. Yu F. Wei J.P. van de Merwe Alice K.Y. Chan R. Ye Doris W.T. Au Rudolf S.S. Wu M.S. Yang 《Marine pollution bulletin》2014
A recent study demonstrated that 2,2′,4,4′-tetrabromodiphenyl ether (BDE-47) may have an adverse effect on the reproduction in marine medaka (Oryzias melastigma), but the molecular mechanisms remain largely unknown. In this study, we investigated the protein expression profiles of male and female gonads of O. melastigma exposed to dietary BDE-47 at two dosages (0.65 and 1.30 μg/g/day, respectively) for 21 days. Extracted proteins were labeled with iTRAQ and analyzed on a MALDI TOF/TOF analyzer, as results, 133 and 144 unique proteins were identified in testis and ovary, respective, and they exerted dose- and sex-dependent expression patterns. In testis, among the 42 differentially expressed proteins; down-regulation of histone variants and parvalbumins implicated BDE-47 may disrupt the spermatogenesis and induce sterility in fishes. In ovary, 38 proteins were differentially expressed; the elevation of vitellogenins and apolipoprotein A–I expression indicated BDE-47 acts as an estrogen-mimicking compound and led to reproductive impairment in O. melastigma. 相似文献
42.
基于GPD分布的黑河流域极端降水频率特征分析 总被引:2,自引:0,他引:2
采用广义帕雷托分布(GPD)对黑河流域极端降水的频率特征进行了分析。采用百分位数法、Hill图法、年交叉率法选取了极端降水阈值,借助L矩法对GPD分布的参数进行了估计;采用Mann-Kendall和Pettitt方法对超阈值日极端降水序列的平稳性进行了检验。结果表明:① 采用百分位数法和Hill图法得到的日极端降水阈值差别很大,在综合考虑以上两种方法的基础上,结合年交叉率法,最终确定了流域各站点日极端降水的阈值;② 根据Mann-Kendall和Pettitt方法,超阈值日极端降水序列基本满足平稳性假定;通过Kolmogorov-Smirnov检验以及理论频率曲线和经验频率曲线的拟合程度可以看出,GPD分布能够很好地拟合研究区极端降水的分布特征;③ 通过分析理论累积频率达到90%以上的极端降水可以发现,黑河流域20世纪60年代发生极端降水的次数最多,其次是90年代以后,70年代、80年代发生极端降水次数较少;在过去51年间,下游发生极端降水的次数最多,其次是中游和上游。 相似文献
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Fluid inclusions and clusters of water molecules at nanometer-to submicron-scale in size have been investigated using transmission electron microscopy (TEM) and Fourier transform infrared spectroscopy (FTIR) in jadeite, quartz and symplectite aegirine–augite, albite, taramite and magnetite corona minerals from ultrahigh-pressure (UHP) jadeite–quartzite at Shuanghe, the Dabie Mountains, China. Fluid inclusions from 0.003 μm to 0.78 μm in size occur in jadeite and quartz crystals, and a small number of fluid inclusions from 0.001 μm to 0.25 μm have also been detected in symplectite-forming minerals. Most of the fluid inclusions have round or negative crystal morphology and contain aqueous fluids, but some contain CO2-rich fluids. They are usually connected to dislocations undetectable at an optical scale. The dislocations represent favorable paths for fluid leakage, accounting for non-decrepitation of most fluid inclusions when external pressure decreased at later stages, although there was partial decrepitation of some fluid inclusions unconnected to defect microstructures resulting from internal overpressure. Non-decrepitation and partial decrepitation of fluid inclusions resulted in changes of original composition and/or density. It is clear that identification of hidden re-equilibration features has significant implications for the petrological interpretation of post-peak metamorphic processes. Micro-FTIR results show that all jadeite and quartz samples contain structural water occurring as hydroxyl ions (OH−) and free water (H2O) in the form of clusters of water molecules. The H2O transformed from OH− during exhumation and could have triggered and enhanced early retrograde metamorphism of the host rocks and facilitated plastic deformation of jadeite and quartz grains by dislocation movement, and thus the H2O released during decompression might represent early-stage retrograde metamorphic fluid. The nominally anhydrous mineral (NAM) jadeite is able to transport aqueous fluids in concentrations of at least several hundred ppm water along a subduction zone to mantle depths in the form of clusters of water molecules and hydroxyl ions within crystals. 相似文献
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真实地震情况下人群疏散特征与模拟演练的差异是应急疏散的统计物理研究中的一个关键问题.本文通过互联网收集和分析了2008年5月12日汶川MS8.0地震中一些记录到地震时人群疏散的监控录像.这些监控录像不仅为真实地震情况下人员疏散行为的研究提供了目前仍十分稀缺的实例.而且可用于约束紧急情况下人群疏散的统计物理模型.对条件相似的真实地震情况下和模拟演练情况下的疏散人数一疏散时间进行研究,发现出口处的疏散人数和疏散时间呈显著的非线性关系,这与通过模拟演练所得出的线性关系具有明显的差异. 相似文献
47.
MATHEMATICAL MODELS FOR LIQUID-SOLID TWO-PHASE FLOW 总被引:2,自引:0,他引:2
Weiming Wu Sam S.Y. Wang National Center for Computational Hydroscience Engineering The University of Mississippi MS U.S.A. 《国际泥沙研究》2000,(3)
I INTRODUCTIONTurbulence models for single-phase fluid flows have been developed and widely applied in mechanical,aeronautical, environmental and hydraulic engineering, and other fields. The closure techniques for theReynolds-averaged Navier-Stokes equations for various levels of models including the simple turbulencemodel, one-equation turbulence model, k-s turbulence model and turbulence stress/flux model have beenverified to be physically reasonable and have acceptable accuracy in app… 相似文献
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DU Wala JIANG Li LIU Huijuan YU Shan ZHANG Hongyan ZHANG Qiaofeng ZHAO Jianjun 《中国地理科学(英文版)》2020,(4):572-587
Grassland fires results in carbon emissions, which directly affects the carbon cycle of ecosystems and the carbon balance. The grassland area of Inner Mongolia accounts for 22% of the total grassland area in China, and many fires occur in the area every year. However, there are few models for estimation of carbon emissions from grassland fires. Accurate estimation of direct carbon emissions from grassland fires is critical to quantifying the contribution of grassland fires to the regional balance of atmospheric carbon. In this study, the regression equations for aboveground biomass(AGB) of grassland in growing season and MODIS NDVI(Normalized Difference Vegetation Index) were established through field experiments, then AGB during Nov.–Apr. were retrieved based on that in Oct. and decline rate, finally surface fuel load was obtained for whole year. Based on controlled combustion experiments of different grassland types in Inner Mongolia, the carbon emission rate of grassland fires for each grassland type were determined, then carbon emission was estimated using proposed method and carbon emission rate. Results revealed that annual average surface fuel load of grasslands in Inner Mongolia during 2000–2016 was approximately 1.1978 × 10~(12) kg. The total area of grassland which was burned in the Inner Mongolia region over the 17-year period was 5298.75 km2, with the annual average area of 311.69 km~2. The spatial distribution of grassland surface fuel loads is characterized by decreasing from northeast to southwest in Inner Mongolia. The total carbon emissions from grassland fires amounted to 2.24 × 10~7 kg with an annual average of 1.32 × 10~6 for the study area. The areas with most carbon emissions were mainly concentrated in Old Barag Banner and New Barag Right Banner and on the right side of the Oroqin Autonomous Banner. The spatial characteristics of carbon emission depend on the location of grassland fire, mainly in the northeast of Inner Mongolia include Hulunbuir City, Hinggan League, Xilin Gol League and Ulanqab City. The area and spatial location of grassland fires can directly affect the total amount and spatial distribution of carbon emissions. This study provides a reference for estimating carbon emissions from steppe fires. The model and framework for estimation of carbon emissions from grassland fires established can provide a reference value for estimation of carbon emissions from grassland fires in other regions. 相似文献