全文获取类型
收费全文 | 179篇 |
免费 | 6篇 |
国内免费 | 2篇 |
专业分类
测绘学 | 13篇 |
大气科学 | 4篇 |
地球物理 | 55篇 |
地质学 | 69篇 |
海洋学 | 14篇 |
天文学 | 12篇 |
自然地理 | 20篇 |
出版年
2024年 | 1篇 |
2023年 | 2篇 |
2021年 | 8篇 |
2020年 | 5篇 |
2019年 | 6篇 |
2018年 | 4篇 |
2017年 | 7篇 |
2016年 | 10篇 |
2015年 | 5篇 |
2014年 | 9篇 |
2013年 | 8篇 |
2012年 | 7篇 |
2011年 | 12篇 |
2010年 | 8篇 |
2009年 | 14篇 |
2008年 | 11篇 |
2007年 | 4篇 |
2006年 | 6篇 |
2005年 | 6篇 |
2004年 | 7篇 |
2003年 | 8篇 |
2002年 | 5篇 |
2000年 | 5篇 |
1999年 | 2篇 |
1998年 | 3篇 |
1997年 | 3篇 |
1996年 | 2篇 |
1995年 | 5篇 |
1994年 | 2篇 |
1991年 | 1篇 |
1990年 | 1篇 |
1989年 | 2篇 |
1988年 | 1篇 |
1986年 | 1篇 |
1984年 | 1篇 |
1979年 | 1篇 |
1974年 | 2篇 |
1970年 | 1篇 |
1928年 | 1篇 |
排序方式: 共有187条查询结果,搜索用时 15 毫秒
91.
The Global Earthquake Vulnerability Estimation System (GEVES): an approach for earthquake risk assessment for insurance applications 总被引:4,自引:0,他引:4
Robin Spence Emily So Sarah Jenny Hervé Castella Michael Ewald Edmund Booth 《Bulletin of Earthquake Engineering》2008,6(3):463-483
For the insurance and reinsurance industries, earthquake loss estimation is crucial not only to adequately price its product
but also to manage the accumulation risk in the face of the ever-increasing exposure in highly seismic regions. Changes in
the built environment and a continuously evolving earthquake science make it a necessity for the industry to constantly refine
earthquake loss estimation models. In particular, it has been recognized for a long time that the vulnerability of buildings
to ground shaking is a key parameter in any earthquake risk model. Current methods tend either to rely on the limited historical
damage and loss data or on the numerical simulation of the response of individual buildings to the ground-shaking produced
by earthquakes. Although both methods have their advantages and pitfalls, we are proposing here a simple solution, using transparent
input data, that can be realistically used for the needs of the insurance and reinsurance industry, whether detailed information
about the insured structures is available or not. The resulting product is known as GEVES (Global Earthquake Vulnerability
Estimation System). It is primarily intended for evaluating the mean damage ratio (MDR) suffered by a portfolio of buildings
classified by use, under the action of a given earthquake scenario (i.e. an earthquake of given size at a given distance from
the portfolio of buildings). A key assumption was that macroseismic intensity rather than spectral displacement would be the
basis of loss estimation. The paper describes the model with emphasis on its structure and the justification for the assumptions
made. In addition to a new set of earthquake vulnerability functions, the paper also provides recommendations on some aspects
of the earthquake hazard, in particular about how to define macroseismic intensity at the site of interest, for a given earthquake
scenario. This paper also discusses validation of the GEVES model against calculated vulnerability approaches, and the treatment
of uncertainty within the model. 相似文献
92.
Bernard Bingen Jenny Andersson Ulf Soederlund Charlotte Moeller 《《幕》》2008,31(1):29-34
During the Mesoproterozoic, central Fennoscandia and Laurentia (Greenland) were characterized by a weakly extensional stress regime, as evident from episodic rapakivi granites, dolerite dykes, continental rift intrusives, sandstone basins and continental flood basalts. Along the southwestern active margin of Fennoscandia, the 1.64-1.52 Ga Gothian and 1.52-1.48 Ga Telemarkian accretionary events resulted in oceanwards continental growth. The 1.47-1.42 Ga Hallandian- Danopolonian event included high-grade metamorphism and granite magmatism in southern Fennoscandia. The pre-Sveconorwegian 1.34-1.14 Ga period is characterized by bimodal magmatism associated with sedimentation, possibly reflecting transcurrent tectonics. The Sveconorwegian orogeny involved polyphase imbrication of terranes between 1.14 and 0.97 Ga, as a result of a collision between Baltica and another major plate, followed by relaxation and post-collisional magmatism between 0. 96 and 0. 90 Ga. Recent geologic data support classical models restoring the Sveconorwegian belt directly to the east of the Grenville belt of Laurentia at 1.0 Ga. Fragments of Paleo-to Mesoproterozoic crust showing late Grenvillian-Sveconorwegian (1.00-0.92 Ga) magmatism and/or metamorphism are exposed in several tectonic levels in the Caledonides of Scandinavia, Svalbard and East Greenland, on both sides of the inferred Iapetus suture. Linking these fragments into a coherent late-Grenvillian tectonic model, however, require additional study. 相似文献
93.
The toxicity of a number of new anti-fouling paints, claimed to function by physical means and not by leakage of toxic substances, have been tested on two common organisms in the Baltic Sea, i.e., the red macro alga Ceramium tenuicorne and the copepod Nitocra spinipes. In order to compare the toxicity between the paints a ranking system was developed based on the EC50- and LC50-values. The results showed a wide span in toxicity with the most toxic paints ranked 160 times more toxic than the ones ranked least toxic.
Also, TBT, irgarol and diuron, which have been used as active ingredients in traditional anti-fouling paints, were used to evaluate the sensitivity of the two test organisms. The results showed that the test organisms were equally sensitive to the substances as similar organisms in earlier studies.
In conclusion, the ranking system presented in this study permits ranking and comparison of total toxicity of complex mixtures. 相似文献
94.
Prepared by the MSR Campaign Science Group A. D. Czaja M.-P. Zorzano the rest of the MCSG team with Chairs G. Kminek M. A. Meyer Members D. W. Beaty E. Sefton-Nash B. L. Carrier F. Thiessen T. Haltigin A. Bouvier N. Dauphas K. L. French L. J. Hallis R. L. Harris E. Hauber L. E. Rodriguez S. P. Schwenzer A. Steele K. T. Tait M. T. Thorpe T. Usui J. Vanhomwegen M. A. Velbel S. Edwin K. A. Farley D. P. Glavin A. D. Harrington L. E. Hays A. Hutzler M. Wadhwa 《Meteoritics & planetary science》2023,58(6):885-896
The Mars 2020/Mars Sample Return (MSR) Sample Depot Science Community Workshop was held on September 28 and 30, 2022, to assess the Scientifically-Return Worthy (SRW) value of the full collection of samples acquired by the rover Perseverance at Jezero Crater, and of a proposed subset of samples to be left as a First Depot at a location within Jezero Crater called Three Forks. The primary outcome of the workshop was that the community is in consensus on the following statement: The proposed set of ten sample tubes that includes seven rock samples, one regolith sample, one atmospheric sample, and one witness tube constitutes a SRW collection that: (1) represents the diversity of the explored region around the landing site, (2) covers partially or fully, in a balanced way, all of the International MSR Objectives and Samples Team scientific objectives that are applicable to Jezero Crater, and (3) the analyses of samples in this First Depot on Earth would be of fundamental importance, providing a substantial improvement in our understanding of Mars. At the conclusion of the meeting, there was overall community support for forming the First Depot as described at the workshop and placing it at the Three Forks site. The community also recognized that the diversity of the Rover Cache (the sample collection that remains on the rover after placing the First Depot) will significantly improve with the samples that are planned to be obtained in the future by the Perseverance rover and that the Rover Cache is the primary target for MSR to return to Earth. 相似文献
95.
Bojan Šavrič Bernhard Jenny 《International journal of geographical information science》2014,28(12):2373-2389
The recently introduced adaptive composite map projection technique changes the projection to the geographic area shown on a map. It is meant as a replacement for the commonly used web Mercator projection, which grossly distorts areas when representing the entire world. The original equal-area version of the adaptive composite map projection technique uses the Lambert azimuthal projection for regional maps and three alternative projections for world maps. Adaptive composite map projections can include a variety of other equal-area projections when the transformation between the Lambert azimuthal and the world projections uses Wagner’s method. To select the most suitable pseudocylindrical projection, the distortion characteristics of a pseudocylindrical projection family are analyzed, and a user study among experts in the area of map projections is carried out. Based on the results of the distortion analysis and the user study, a new pseudocylindrical projection is recommended for extending adaptive composite map projections. The new projection is equal-area throughout the transformation to the Lambert azimuthal projection and has better distortion characteristics then small-scale projections currently included in the adaptive composite map projection technique. 相似文献
96.
Hedman JE Rüdel H Gercken J Bergek S Strand J Quack M Appelberg M Förlin L Tuvikene A Bignert A 《Marine pollution bulletin》2011,62(10):2015-2029
The implementation of the EU Marine Strategy Framework Directive necessitates the development of common criteria and methodological standards for marine environmental monitoring and assessment across Europe. Eelpout (Zoarces viviparus) is proposed as a key indicator organism in the Baltic and North Sea regions. This benthic fish species is widely used in ecotoxicological studies and as a bioindicator of local pollution due to its stationary behavior. Eelpout is included in the environmental monitoring program of several Baltic States, covering both chemical and biological effects measurements, and samples have been archived in environmental specimen banks for >15 years. A method for evaluating the frequency of larval aberrations has been suggested as a standardized assessment tool. The large scientific knowledge-base and considerable experience of long-term chemical and biological effects monitoring and specimen banking, make eelpout a suitable species for the assessment of Good Environmental Status in the Baltic and North Seas. 相似文献
97.
Brooke E. Marston Bernhard Jenny 《International journal of geographical information science》2013,27(7):1144-1165
Relief shading is the most common type of cartographic relief representation for print and digital maps. Manual relief shading results in informative and visually pleasing representations of terrain, but it is time consuming and expensive to produce. Current analytical relief shading can be created quickly, but the resulting maps are not as aesthetically appealing and do not show landscape features in an explicit manner. This article introduces an automated digital method that produces shaded relief with locally adjusted illumination directions to simulate the techniques and cartographic principles of manual relief shading. Ridgelines and valley lines are derived from a digital terrain model, vectorized, and used in a diffusion curve algorithm. A graph analysis generalizes the lines before using them for diffusion curve shading. The direction of illumination is adjusted based on the spatial orientation of ridgelines and valley lines. The diffusion curve shading is combined with standard analytical relief shading to create a final diffusion relief shading image. Similar to manual relief shading, major landforms and the structure of the terrain are more clearly shown in the diffusion relief shading. The presented method best highlights major landforms in terrain characterized by sharp, clearly defined ridges and valleys. 相似文献
98.
Barbara Wohlfarth Francesco Muschitiello Sarah L. Greenwood August Andersson Malin Kylander Rienk H. Smittenberg Margret Steinthorsdottir Jenny Watson Nicola J. Whitehouse 《Boreas: An International Journal of Quaternary Research》2017,46(2):143-161
The Last Termination (19 000–11 000 a BP) with its rapid and distinct climate shifts provides a perfect laboratory to study the nature and regional impact of climate variability. The sedimentary succession from the ancient lake at Hässeldala Port in southern Sweden with its distinct Lateglacial/early Holocene stratigraphy (>14.1–9.5 cal. ka BP) is one of the few chronologically well‐constrained, multi‐proxy sites in Europe that capture a variety of local and regional climatic and environmental signals. Here we present Hässeldala's multi‐proxy records (lithology, geochemistry, pollen, diatoms, chironomids, biomarkers, hydrogen isotopes) in a refined age model and place the observed changes in lake status, catchment vegetation, summer temperatures and hydroclimate in a wider regional context. Reconstructed mean July temperatures increased between c. 14.1 and c. 13.1 cal. ka BP and subsequently declined. This latter cooling coincided with drier hydroclimatic conditions that were probably associated with a freshening of the Nordic Seas and started a few hundred years before the onset of Greenland Stadial 1 (c. 12.9 cal. ka BP). Our proxies suggest a further shift towards colder and drier conditions as late as c. 12.7 cal. ka BP, which was followed by the establishment of a stadial climate regime (c. 12.5–11.8 cal. ka BP). The onset of warmer and wetter conditions preceded the Holocene warming over Greenland by c. 200 years. Hässeldala's proxies thus highlight the complexity of environmental and hydrological responses across abrupt climate transitions in northern Europe. 相似文献
99.
It is argued in this commentary that, in order to understand better the physical mechanisms that generate boundary shear stress over water‐worked gravel beds, flow velocity data should be re‐evaluated by spatial averaging the Reynolds equations to produce time‐ and space‐averaged (double‐averaged) momentum equations. A series of laboratory experiments were conducted in which the flow velocities were measured using a PIV system over two water‐worked gravel deposits. Combined with detailed data on the bed surface topography and vertical porosity, the physical components of shear stress were obtained. This enabled the various momentum transfer mechanisms present above, within and at the interface of a porous, fluvial deposit, to be quantified. This included the examination of the relevant contributions of temporal and spatial fluctuations in velocity and surface drag to the overall momentum transfer. It is demonstrated that double‐averaging represents a logical framework for assessing the fluid forces responsible for sediment entrainment and for investigating intragravel flow and sediment–water interface exchange mechanisms within the roughness layer in water‐worked gravel deposits. By considering the physical components of shear stress and their relative sizes it was possible to provide a physically based explanation for existing observations of enhanced mobility of gravel–sand mixtures and the transfer of solutes into porous, gravel deposits. This analysis reveals the importance of obtaining co‐located, high quality spatial data on the flow field and bed surface topography in order to gain a physical understanding of the mechanisms which generate boundary shear stress. Copyright © 2010 John Wiley & Sons, Ltd. 相似文献
100.
Sediment transport mechanics 总被引:3,自引:3,他引:0
The Editor of Acta Geophysica and the Guest Editors wish to dedicate this Topical Issue on Sediment Transport Mechanics to the memory of Stephen Coleman, who died recently. During his career, Stephen had made an outstanding scientific contribution to the topic of Sediment Transport. The level of his contribution is demonstrated in the paper by Aberle, Coleman, and Nikora included in this issue, on which he started working before becoming aware of the illness that led to his untimely death. For scholars and colleagues Stephen remains an example of intellectual honesty and scientific insight. 相似文献