全文获取类型
收费全文 | 24660篇 |
免费 | 187篇 |
国内免费 | 925篇 |
专业分类
测绘学 | 1422篇 |
大气科学 | 1989篇 |
地球物理 | 4594篇 |
地质学 | 11705篇 |
海洋学 | 1020篇 |
天文学 | 1650篇 |
综合类 | 2162篇 |
自然地理 | 1230篇 |
出版年
2024年 | 1篇 |
2023年 | 2篇 |
2022年 | 9篇 |
2021年 | 16篇 |
2020年 | 22篇 |
2019年 | 15篇 |
2018年 | 4774篇 |
2017年 | 4056篇 |
2016年 | 2598篇 |
2015年 | 246篇 |
2014年 | 105篇 |
2013年 | 55篇 |
2012年 | 1011篇 |
2011年 | 2750篇 |
2010年 | 2022篇 |
2009年 | 2319篇 |
2008年 | 1893篇 |
2007年 | 2361篇 |
2006年 | 54篇 |
2005年 | 197篇 |
2004年 | 404篇 |
2003年 | 410篇 |
2002年 | 251篇 |
2001年 | 49篇 |
2000年 | 52篇 |
1999年 | 14篇 |
1998年 | 21篇 |
1995年 | 1篇 |
1992年 | 1篇 |
1990年 | 1篇 |
1989年 | 1篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1982年 | 1篇 |
1981年 | 22篇 |
1980年 | 19篇 |
1979年 | 1篇 |
1977年 | 2篇 |
1976年 | 7篇 |
1975年 | 1篇 |
1974年 | 4篇 |
1972年 | 1篇 |
排序方式: 共有10000条查询结果,搜索用时 0 毫秒
991.
992.
YANGTaibao YUYongtao LIJijun ANCongrong LIUJinfeng ZHANGJunyan 《山地科学学报》2004,1(2):128-142
Paleomagnetic determinations on lithologieal profiles of two paralleled long drillin gcores covering the past 130 kyr B.P., GT40 and GT60,from the Yanchi Playa in the arid Northwestern China indicate that a series of pronounced paleomagnetic excursions have been documented. By correlating our results with published regional and worldwide reports 4 excursion events out of 10 apparent reversal signals (labeled from GT-1 to GT-10) were identified as excursion events coeval with the Mono Lake Event (28.4 kyr-25.8 kyr), Laschamp Event (43.3 kyr-40.5kyr), Gaotai Event (82.8 kyr-72.4 kyr) and the Blake Event (127.4 kyr-113.3 kyr), respectively. GT-9 correlates with the above-mentioned Gaotai Event,GT-7 and GT-6 correspond to two stages of the Laschamp Event and GT-5 to the Mono Lake Event. It is noteworthy that the so-called Gaotai Event has not been reported as a pronounced paleomagnetic excursion in the Northwestern China. Every magnetic excursion event corresponds to paleointensity minima, anteceding those established abrupt paleoclimatic change events, such as the Younger Drays and the Heinrich Events (H1-H6). Here, we tentatively propose that these geomagnetic excursions/reversals can be viewed as precursors to climate abruptness. During the transitional stages when the earth‘s magnetic field shifted between a temporal normal and a negative period, the earth‘s magnetic paleointensity fell correspondingly to a pair of minima. Although more precise chronology and more convincing rock magnetic parameter determinations are essentially required for further interpretation of their intricate coupling mechanism, these results may have revealed, to some extent, that the earth‘s incessantly changing magnetic field exerts an strong influence on the onset of saw-tooth shaped abrupt climate oscillations through certain feedback chains in arid Central Asia or even North Hemispheric high latitude regions. 相似文献
993.
Luis G. Rivera-Garcia Kristina M. Hill-Spanik Sean T. Berthrong Craig J. Plante 《Estuaries and Coasts》2018,41(3):772-783
Benthic microalgae are key contributors to near-shore food webs and sediment stabilization. Temporal variability in microalgal biomass and production throughout the tidal cycle has been well documented; however, due to limitations of traditional methods of analysis patterns of community composition and diversity over such time scales have not been revealed. To explore the latter and better understand how short-term changes throughout the tidal cycle may affect community functioning, we compared benthic diatom composition and diversity over tidal stage shifts. We employed two disparate molecular techniques (denaturing gel gradient electrophoresis with Sanger DNA sequencing of excised bands and high-throughput community metagenome sequencing) to characterize diatom assemblages in representative muddy and sandy intertidal sites in Charleston Harbor, SC, USA. In support of prior studies, we found higher diatom diversity in sandbar as compared to mudflat sediments. Spatial differences were stronger relative to tidal temporal differences, although diversity metrics generally were highest after prolonged tidal immersion as compared to low-tide emersion or just after immersion at flood tide. Composition of the diatom assemblage differed markedly between sites, with species in genera Halamphora, Amphora, and Navicula dominating the sandbar, whereas Cyclotella, Skeletonema, and Thalassiosira were the most prevalent genera on the mudflat. Diatom composition differed by tidal stage, with assemblages during low-tide exposure distinct from samples taken after immersion. Both sandbar and mudflat sediments exhibited increases in relative proportion of epipelic diatoms and decreases in planktonic taxa during low-tide exposure. Our findings of short-term changes in species composition and dominance could inform primary productivity models to better estimate understudied diatom contributions in heterogeneous and highly variable tidal systems. 相似文献
994.
The cable shovel is widely used in surface mining. High operating and ownership costs necessitate efficient use of the cable
shovel. Operator practices have long been suspected to contribute towards the inefficient use of the shovel. Crowd arm and
hoist rope speeds are key measures of operator practices. The objective of this work is to find the crowd arm and hoist rope
speeds for optimal shovel performance for given initial conditions and material properties. Shovel kinematics and dynamic modeling, using shovel
geometry and the simultaneous constraint method, respectively, have been employed to build models of the excavation process.
Dynamic models of the shovel payload and the material cutting resistance have also been developed using geometric simulation
and passive soil pressures techniques, respectively. These models are solved numerically by combining Runge–Kutta and Gaussian
elimination algorithms to compute the work done and the resistive forces during shovel excavation. The algorithms have been
combined into a shovel simulator. The simulator has been used to simulate the P&H 2100BL shovel. The simulation results indicate
that input energy and digging time increase with increasing crowd arm and decreasing hoist rope speeds. The input energy per
unit loading rate is proposed as an appropriate measure of shovel performance. High energy per unit loading rate occurs for
high crowd speeds and low hoist rope speeds. For the simulated conditions and crowd arm and hoist rope speeds ranging from
0.25 to 0.5 ms−1 and 0.5 to 0.7 ms−1, respectively, the optimal crowd arm and hoist rope speeds were found to be 0.25 ms−1 and 0.7 ms−1, respectively, and the objective function value was 0.21 KJs/kg. This work establishes, theoretically, the fact that operator
practices have an effect on shovel performance and is useful in establishing optimum practices. The results are the initial
steps towards full automation of the excavation process. 相似文献
995.
The Precambrian basement of Egypt is part of the Red Sea Mountains and represents the north-western part of the Arabian–Nubian Shield (ANS). Five volcanic sections are exposed in the Egyptian basement complex, namely El Kharaza, Monqul, Abu Had, Mellaha and Abu Marwa. They are located in the north Eastern Desert (ED) of Egypt and were selected for petrological and geochemical studies as they represent the Dokhan volcanics. The volcanics divide into two main pulses, and each pulse was frequently accompanied by deposition of immature molasse type sediments, which represent a thick sequence of the Hammamat group in the north ED. Compositionally, the rocks form a continuum from basaltic andesite, andesite, dacite (lower succession) to rhyodacite and rhyolite (upper succession), with no apparent compositional gaps. These high-K calc-alkaline rocks have strong affinities to subduction-related rocks with enriched LILEs (Rb, Ba, K, Th, Ce) relative to high field strength elements (Nb, Zr, P, Ti) and negative Nb anomalies relative to NMORB. The lower succession displays geochemical characteristics of adakitic rocks with SiO2 >53 wt%, Al2O3 >15 wt%, MgO >2.5 wt%, Mg# >49, Sr >650 ppm, Y <17 ppm, Yb <2 ppm, Ni >25 ppm, Cr >50 ppm and Sr/Y >42.4. They also have low Nb, Rb and Zr compared to the coexisting calc-alkaline rhyodacites and rhyolites. The highly fractionated rhyolitic rocks have strong negative Eu anomalies and possess the geochemical characteristics of A-type suites. Trace element geochemical signatures indicate a magma source consistent with post-collisional suites that retain destructive plate signatures associated with subduction zones. The adakitic rocks in the northern ANS are generated through partial melting of delaminated mafic lower crust interacting with overlying mantle-derived magma. The Dokhan volcanics were likely generated by a combination of processes, including partial melting, crystal fractionation and assimilation. 相似文献
996.
Seasonal variations of stable isotope in precipitation and moisture transport at Yushu,eastern Tibetan Plateau 总被引:3,自引:0,他引:3
LiDe Tian LingLong Ma WuSheng Yu ZhongFang Liu ChangLiang Yin ZhongPing Zhao Wei Tang Yu Wang 《中国科学D辑(英文版)》2008,51(8):1121-1128
Precipitation δ 18O at Yushu, eastern Tibetan Plateau, shows strong fluctuation and lack of clear seasonality. The seasonal pattern of precipitation stable isotope at Yushu is apparently different from either that of the southwest monsoon region to the south or that of the inland region to the north. This different seasonal pattern probably reflects the shift of different moisture sources. In this paper, we present the spatial comparison of the seasonal patterns of precipitation δ 18O, and calculate the moisture transport flux by using the NCAR/NCEP reanalysis data. This allows us to discuss the relation between moisture transport flux and precipitation δ 18O. This study shows that both the southwest monsoon from south and inland air mass transport from north affected the seasonal precipitation δ 18O at Yushu, eastern Tibetan Plateau. Southwest monsoon brings the main part of the moisture, but southwest transport flux is weaker than in the southern part of the Tibetan Plateau. However, contribution of the inland moisture from north or local evaporation moisture is enhanced. The combined effect is the strong fluctuation of summer precipitation δ 18O at Yushu and comparatively poor seasonality. 相似文献
997.
The ocean drift current consists of a (local) pure drift current generated by the interaction of wind and waves at the sea surface, to which the surface geostrophic current is added vectorially. We present (a) a similarity solution for the wave boundary layer (which has been validated through the prediction of the 10-m drag law), from which the component of pure drift current along the direction of the wind (and hence the speed factor) can be evaluated from the 10-m wind speed and the peak wave period, and (b) a similarity solution for the Ekman layers of the two fluids, which shows that under steady-state neutral conditions the pure drift current lies along the direction of the geostrophic wind, and has a magnitude 0.034 that of the geostrophic wind speed. The co-existence of these two similarity solutions indicates that the frictional properties of the coupled air-sea system are easily evaluated functions of the 10-m wind speed and the peak wave period, and also leads to a simple expression for the angle of deflection of the pure drift current to the 10 m wind. The analysis provides a dynamical model for global ocean drift on monthly and annual time scales for which the steady-state neutral model is a good approximation. In particular, the theoretical results appear to be able to successfully predict the mean surface drift measured by HF Radar, which at present is the best technique for studying the near surface velocity profile. 相似文献
998.
Wind erosion causes serious problems and considerable threat in most regions of the world. Vegetation on the ground has an important role in controlling wind erosion by covering soil surface and absorbing wind momentum. A set of wind tunnel experiments was performed to quantitatively examine the effect of canopy structure on wind movement. Artificial plastic vegetations with different porosity and canopy shape were introduced as the model canopy. Normalized roughness length (Z 0/H) and shear velocity ratio (R) were analyzed as a function of roughness density (λ). Experiments showed that Z 0/H increases and R decreases as λ reaches a maximum value, λ max, while the values of Z 0/H and R showed little change with λ value beyond as λ max. 相似文献
999.
Ioannis A. Daglis Georgios Balasis Natalia Ganushkina Fiori-Anastasia Metallinou Minna Palmroth Risto Pirjola Ioanna Tsagouri 《Acta Geophysica》2009,57(1):141-157
Comprehensive understanding of the dynamics of the coupled solar wind-magnetosphere-ionosphere system is of utmost interest,
both from the perspective of solar system astrophysics and geophysics research and from the perspective of space applications.
The physical processes involved in the dynamical evolution of this complex coupled system are pertinent not only for the Sun-Earth
connection, but also for major phenomena in other astrophysical systems. Furthermore, the conditions in geospace collectively
termed space weather affect the ever increasing technological assets of mankind in space and therefore need to be understood,
quantified and efficiently forecasted. The present collaborative paper communicates recent advances in geospace dynamic coupling
research through modeling, simulations and data analysis and discusses future directions. 相似文献
1000.
Matjaz Dolsek 《Bulletin of Earthquake Engineering》2010,8(6):1309-1329
A computing environment for the seismic performance assessment of reinforced concrete frames has been developed in Matlab
in combination with OpenSees. It includes several functions which provide calculations of the moment-rotation relationship
of plastic hinges in columns and beams, rapid determination of simplified nonlinear structural models, the post-processing
of the results of analyses and structural performance assessment with different methods. The user can add new functions to
the PBEE toolbox in order to support additional procedures for the seismic performance assessment of RC frames, or can just
change the rules for determining the moment-rotation relationship of plastic hinges in columns and beams, which are the main
source of uncertainty in simplified nonlinear models. In the paper, the capabilities of the computing environment (PBEE toolbox)
are first explained by focusing on the procedures for determining the moment-rotation relationship of plastic hinges. Different
examples are then presented, starting with a comparison between the calculated response of a four-storey RC frame building
and the response obtained in a pseudo-dynamic experiment. The calculated response was determined with the two different structural
models which are later on used for the demonstration of the seismic performance assessment of the same structure by the N2
method. Lastly, seismic performance assessment of an eight-storey frame is performed by using incremental dynamic analysis
with consideration of the modelling uncertainties. 相似文献