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   6809篇
  免费   882篇
  国内免费   675篇
测绘学   297篇
大气科学   912篇
地球物理   2297篇
地质学   3144篇
海洋学   538篇
天文学   405篇
综合类   370篇
自然地理   403篇
  2024年   10篇
  2023年   21篇
  2022年   72篇
  2021年   98篇
  2020年   83篇
  2019年   75篇
  2018年   499篇
  2017年   447篇
  2016年   340篇
  2015年   217篇
  2014年   208篇
  2013年   193篇
  2012年   725篇
  2011年   513篇
  2010年   209篇
  2009年   234篇
  2008年   197篇
  2007年   176篇
  2006年   180篇
  2005年   896篇
  2004年   924篇
  2003年   704篇
  2002年   237篇
  2001年   134篇
  2000年   124篇
  1999年   124篇
  1998年   85篇
  1997年   105篇
  1996年   75篇
  1995年   58篇
  1994年   57篇
  1993年   45篇
  1992年   64篇
  1991年   41篇
  1990年   32篇
  1989年   31篇
  1988年   27篇
  1987年   21篇
  1986年   14篇
  1985年   11篇
  1984年   9篇
  1983年   5篇
  1980年   4篇
  1976年   3篇
  1975年   4篇
  1965年   3篇
  1955年   2篇
  1954年   3篇
  1951年   2篇
  1948年   2篇
排序方式: 共有8366条查询结果,搜索用时 484 毫秒
41.
闽南近海常见鲨鳐类肝油的四种理化常数和角鲨烯含量   总被引:8,自引:0,他引:8  
刘晓春  丘书院 《台湾海峡》1997,16(4):468-472
本文分析测定了闽南近海常见鲨鳐类肝油的理化常数和角鲨烯含量。尖头斜齿鲨肝油的碘值特别高,说明其中脂肪酸的不饱和程度很高;非皂化物含量很低,约占肝油重的38×10-3(m/m);角鲨烯含量极微,在肝油中仅占84×10-5(m/m)。闽南近海常见鲨鳐类肝油的角鲨烯含量均很低,变化在(31~116)×10-5(m/m)之间。在相同的气相色谱条件下,小孔沙条鲨和狭纹虎鲨肝油中没有检测到角鲨烯。  相似文献   
42.
Scaling analysis of deposition from turbidity currents   总被引:3,自引:0,他引:3  
Many oil-bearing sedimentary deposits are formed by the settling of particles from turbidity currents. Modeling sedimentary processes that form these turbidites enables the calculation of properties such as extent, depth, porosity and permeability of hydrocarbon-bearing reservoirs. This paper estimates the extent and thickness of turbidites from the initial conditions of the turbidity flow. This is achieved by the application of scaling analysis of the partial differential equations that govern the dynamics of and deposition from turbidity currents. We apply the results of scaling analysis to five modern submarine fans. The predicted and actual values of the dimensions of the fan deposits match well. We then compare the derived results against tabulated sizes of ancient turbidites. The comparisons are good as long as we correctly identify the flow regimes in which the deposition took place. The good agreements observed in the two cases show that the estimates obtained using scaling analysis can provide useful first-guess values for the dimensions of the deposits.  相似文献   
43.
Two processes are generally explained as causes of temporal changes in the stoichiometric silicon/nitrogen (Si/N) ratios of sinking particles and of nutrient consumption in the surface water during the spring diatom bloom: (1) physiological changes of diatom under the stress of photosynthesis of diatom and (2) differences of regeneration between silicon and nitrogen. We investigated which process plays an important role in these changes using a one-dimensional ecosystem model that explicitly represents diatom and the other non-silicious phytoplankton. The model was applied to station A7 (41°30′ N, 145°30′ E) in the western North Pacific, where diatom regularly blooms in spring. Model simulations show that the Si/N ratios of the flux exported by the sinking particles at 100 m depth and of nutrient consumptions in the upper 100 m surface water have their maxima at the end of the spring diatom bloom, the values and timings of which are significantly different from each other. Analyses of the model results show that the differences of regeneration between silicon and nitrogen mainly cause the temporal changes of the Si/N ratios. On the other hand, the physiological changes of diatoms under stress can hardly cause these temporal changes, because the effect of the change in the diatom's uptake ratio of silicon to nitrogen is cancelled by that in its sinking rate.  相似文献   
44.
Several large deployments of neutrally buoyant floats took place within the Antarctic Intermediate (AAIW), North Atlantic Deep Water (NADW), and the Antarctic Bottom Water (AABW) of the South Atlantic in the 1990s and a number of hydrographic sections were occupied as well. Here we use the spatially and temporally averaged velocities measured by these floats, combined with the hydrographic section data and various estimates of regional current transports from moored current meter arrays, to determine the circulation of the three major subthermocline water masses in a zonal strip across the South Atlantic between the latitudes of 19°S and 30°S. We concentrate on this region because the historical literature suggests that it is where the Deep Western Boundary Current containing NADW bifurcates. In support of this notion, we find that a net of about 5 Sv. of the 15–20 Sv that crosses 19°S does continue zonally eastward at least as far as the Mid-Atlantic Ridge. Once across the ridge it takes a circuit to the north along the ridge flanks before returning to the south in the eastern half of the Angola Basin. The data suggest that the NADW then continues on into the Indian Ocean. This scheme is discussed in the context of distributions of dissolved oxygen, silicate and salinity. In spite of the many float-years of data that were collected in the region a surprising result is that their impact on the computed solutions is quite modest. Although the focus is on the NADW we also discuss the circulation for the AAIW and AABW layers.  相似文献   
45.
With the development of high-resolution multibeam echosounder systems (MBES) for surveying shallow-water areas a new tool is available to monitor rapid changes in seabed morphology as, e.g., caused by the dumping of dredge spoil in coastal waters. In this study, four data sets of repeated bathymetric surveys with a MBES were processed and analyzed. The data were collected in a 1.94-km2 dumping site in the outer Weser Estuary (German Bight). Between June and December 1998, 2.6 million m3 of dredged sediment were deposited there. The bathymetric maps generated in the course of this study reveal features such as subaqueous dunes, scour holes, and mounds of dumped dredge spoil. The mean water depth decreased by about 1 m during the dumping period. Furthermore, difference grids showing changes in sediment volume allowed a calculation of the sediment budget for the monitored area. After a time period of only 5 months, 0.5 million m3 of the originally dumped 2.6 million m3 of dredge spoil had already been removed from the dumping site.  相似文献   
46.
Frequency-selective attenuation of sound propagaion and reverberation in shallow waterTXFrequency-selectiveattenuationofsoundp...  相似文献   
47.
贻贝棘尾虫形态及二分裂期间形态发生的扫描电镜观察   总被引:1,自引:0,他引:1  
于1986年在哈尔滨郊外水池采集贝棘尾虫标本,利用扫描电镜观察其形态及二分裂期间形态发生,在扫找镜样品制备中,采KMnO4代替常用的OsO4研究表明,(1)口原基发生的位置在第一横棘毛的左前角,这下贪食棘尾虫相同,但不同于鬃棘尾虫。参与后仔虫额,腹,横棘毛原基发生的老腹棘毛只有一个,这与前人在其他贻贝棘尾虫株系上的观察结果不同,这些表明,口原基起源的位置和参与形成额、腹,横棘毛原基的老腹棘毛的数目  相似文献   
48.
台湾海峡金色小沙丁鱼幼鱼索饵群体研究   总被引:2,自引:1,他引:2  
杨圣云  丘书院 《台湾海峡》1992,11(3):244-250
本文研究了台湾海峡南部和北部的金色小沙丁鱼当年生幼鱼计数性状和量度性状特征差异,并结合其生物学特性、产卵场、洄游及海区环境特征进行综合分析。结果表明,台湾海峡南部和北部的索饵幼鱼仍属于同一地方种群:闽南-台湾浅滩语地方种群。根据其索饵洄游特点,可分为台湾海峡南部和北部两个索饵群体.  相似文献   
49.
In order to estimate primary production from ocean color satellite data using the Vertical Generalized Production Model (VGPM; Behrenfeld and Falkowski, 1997), we propose a two-phytoplankton community model. This model is based on the two assumptions that changes in chlorophyll concentration result from changes of large-sized phytoplankton abundance, and chlorophyll specific productivity of phytoplankton tends to be inversely proportional to phytoplankton size. Based on the analysis of primary production data, P opt B , which was one parameter in the VGPM, was modeled as a function of sea surface temperature and sea surface chlorophyll concentration. The two-phytoplankton community model incorporated into the VGPM gave good estimates in a relatively high productive area. Size-fractionated primary production was estimated by the two-phytoplankton community model, and P opt B of small-sized phytoplankton was 4.5 times that of large-sized phytoplankton. This result fell into the ranges observed during field studies.  相似文献   
50.
In this paper, the irregular wave force on a cylindrical pier group is calculated by the method of spectrum analysis, and the coefficients of the group effect of piers in the pier group are given here. The calculated results, using P-M and Bretshneider's. (B's) spectra, are obtained for the cases of 2 piers, 3 piers and 4 piers. To compare these results with those obtained for regular waves, we can come to some significant conclusions. Under the action of the irregular wave, when the distance between the piers in the pier group increases, the coefficient of the group effect decreases and tends rapidly to the case of a single pier. In general, when the ratio of the distance between the piers to the diameter of the pier is greater than 4, the group effect can be neglected.  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