全文获取类型
收费全文 | 5986篇 |
免费 | 147篇 |
国内免费 | 62篇 |
专业分类
测绘学 | 123篇 |
大气科学 | 503篇 |
地球物理 | 1376篇 |
地质学 | 1986篇 |
海洋学 | 592篇 |
天文学 | 957篇 |
综合类 | 14篇 |
自然地理 | 644篇 |
出版年
2021年 | 47篇 |
2020年 | 65篇 |
2019年 | 73篇 |
2018年 | 111篇 |
2017年 | 116篇 |
2016年 | 132篇 |
2015年 | 103篇 |
2014年 | 129篇 |
2013年 | 316篇 |
2012年 | 177篇 |
2011年 | 260篇 |
2010年 | 238篇 |
2009年 | 236篇 |
2008年 | 241篇 |
2007年 | 209篇 |
2006年 | 228篇 |
2005年 | 182篇 |
2004年 | 184篇 |
2003年 | 171篇 |
2002年 | 165篇 |
2001年 | 117篇 |
2000年 | 108篇 |
1999年 | 103篇 |
1998年 | 95篇 |
1997年 | 86篇 |
1996年 | 88篇 |
1995年 | 92篇 |
1994年 | 86篇 |
1993年 | 76篇 |
1992年 | 87篇 |
1991年 | 70篇 |
1990年 | 99篇 |
1989年 | 85篇 |
1988年 | 75篇 |
1987年 | 100篇 |
1986年 | 75篇 |
1985年 | 96篇 |
1984年 | 131篇 |
1983年 | 108篇 |
1982年 | 97篇 |
1981年 | 100篇 |
1980年 | 88篇 |
1979年 | 100篇 |
1978年 | 71篇 |
1977年 | 86篇 |
1976年 | 71篇 |
1975年 | 70篇 |
1974年 | 55篇 |
1973年 | 61篇 |
1972年 | 35篇 |
排序方式: 共有6195条查询结果,搜索用时 15 毫秒
991.
992.
Harris E. Mason Robert S. Maxwell Susan A. Carroll 《Geochimica et cosmochimica acta》2011,75(20):6080-6093
We present the results of a series of experiments designed to probe the interactions between Al and the amorphous silica surface as a function of thermodynamic driving forces. The results from 27Al single pulse magic angle spinning (SP/MAS) and 27Al{1H} rotational echo double resonance (REDOR) allow us to identify the reaction products and constrain their structure. In all cases, despite low Al and Si concentrations we observe the formation of metastable aluminosilicates. Results from low temperature experiments indicate that despite thermodynamic driving forces for the formation of gibbsite we observe the precipitation of separate octahedrally coordinated Al (Al[6]) and tetrahedrally coordinated Al (Al[4]) silicate phases. At higher temperatures the Al[4] silicate phase dominates the speciation. Structural models derived from the NMR data are also proposed, and the results are discussed as they relate to previous work on Al/Si cycling. 相似文献
993.
994.
Geomorphic river design strives for natural resilience by encouraging geomorphic form complexity and morphological processes linked to greater habitat diversity. Increasing availability of high-resolution topographic data and spatial feature mapping methods provide advantages for morphological analysis and river restoration planning. We propose and evaluate an approach to quantifying topographic variability of geomorphic form and pixel-level surface roughness resulting from channel planform geometry differences using spatially continuous variety computation applied to component metrics including flow direction, aspect and planform curvature. We define this as the geomorphic form variation (GFV) approach and found it scalable, repeatable and a multi-stage analytical metric for quantifying physical aspects of river-bed topographic variability. GFV may complement process-based morphological feature mapping applications, hydraulic assessment indices and spatial habitat heterogeneity metrics commonly used for ecological quality evaluation and river restoration. The GFV was tested on controlled synthetic channels derived from River Builder software and quasi-controlled sinuous planform flume experiment channels. Component variety metrics respond independently to specific geometric surface changes and are sensitive to multi-scaled morphology change, including coarser-grained sediment distributions of pixel-level surface roughness. GFV showed systematic patterns of change related to the effects of channel geometry, vertical bed feature (pool-bar) frequency and amplitude, and bar size, shape and orientation. Hotspot analysis found that bar margins were major components of topographic complexity, whereas grain-scale variety class maps further supported the multi-stage analytical capability and scalability of the GFV approach. The GFV can provide an overall variety value that may support river restoration decision-making and planning, particularly when geomorphic complexity enhancement is a design objective. Analysing metric variety values with statistically significant hotspot cluster maps and complementary process-based software and mapping applications allows variety correspondence to systematic feature changes to be assessed, providing an analytical approach for river morphology change comparison, channel design and geomorphic process restoration. 相似文献
995.
Total mercury content has been determined in three tissues of the intertidal mussel Mytilus californianus collected at locations along the southern California coast and at island control stations. The apparent influence of certain harbours and municipal wastewater outfalls was reflected by the relatively higher levels of mercury in all tissues of mussels from these areas. In general, the concentrations reported here are lower than those in mussels on west European coasts. 相似文献
996.
Robert R. Hoffman 《国际地球制图》2013,28(2):3-13
In a previous article (Hoffman & Conway, 1989), we reviewed some of the available psychological research that pertains to remote sensing. We focused on two major problem areas: Research on the knowledge of expert interpreters of remotely‐sensed imagery, and research on the use of color in graphic displays. Here, we pursue one of the broad implications of the research ‐ that the field of remote sensing can benefit by incorporating research methods and ideas from experimental psychology. From the experimental psychology viewpoint, “remote sensing”; is actually a misnomer when used to denote a field or area of scientific inquiry. Remote perceiving, as a total process, depends not only on the technology of remote sensing, but also depends critically on the ability of humans to interpret remote sensing displays. This perspective is contrasted with traditional approaches to remote sensing. The discussion involves some ideas about the theoretical and methodological foundations of remote sensing as a unified science. 相似文献
997.
998.
Kanchan Maiti Claudia R. Benitez-Nelson Yoshimi Rii Robert Bidigare 《Deep Sea Research Part II: Topical Studies in Oceanography》2008,55(10-13):1445
Mesoscale eddies may enhance primary production (PP) in the open ocean by bringing nutrient-rich deep waters into the euphotic zone, potentially leading to increased transport of particles to depth. This hypothesis remains controversial, however, due to a paucity of direct particle export measurements. In this study, we investigated particle dynamics using 234Th–238U disequilibria within a mesoscale cold-core eddy, Cyclone Opal, which formed in the lee of the Hawaiian Islands. 234Th samples were collected along two transects across Cyclone Opal as well as during a time-series within the eddy core during a decaying diatom bloom. Particulate carbon (PC), particulate nitrogen (PN) and biogenic silica (bSiO2) fluxes at 150 m varied spatially and temporally within the eddy and strongly depended on the 234Th model formulation used (e.g., steady state versus non-steady state, inclusion of upwelling, etc.). Particle fluxes estimated from a steady state model assuming an upwelling rate of 2 m day−1 yielded the best fit to sediment-trap data. These 234Th-derived particle fluxes ranged from 332±14 to 1719±53 μmol C m−2 day−1, 27±3 to 114±12 μmol N m−2 day−1, and 33±20 to 309±73 μmol Si m−2 day−1. Although PP rates within Cyclone Opal were elevated by a factor of 2–3, PC and PN fluxes were the same, within error, inside and outside of Cyclone Opal. The ratio of PC export to PP remained surprisingly low at <0.03 and similar to those measured in surrounding waters. In contrast, bSiO2 fluxes within the eddy core were three times higher. Detailed analyses of 234Th depth profiles consistently showed excess 234Th at 100–175 m, associated with the remineralization and possible accumulation of suspended and dissolved organic matter from the surface. We suggest that strong microzooplankton grazing facilitated particulate organic matter recycling and resulted in the export of empty diatom frustules. Thus, while eddies may increase PP, they do not necessarily increase PC and PN export to deep waters. This may be a general characteristic of wind-driven cyclonic eddies of the North Pacific Subtropical Gyre and suggests that eddies may preferentially act as a silica pump, thereby playing an important role in promoting silicic-acid limitation in the region. 相似文献
999.
Summary Litton Divisions presently produce both high accuracy GPS surveyors and low—cost GPS navigation sets. Aero Service'sMACROMETER
R Interferometric Surveyors, have become the standard against which GPS surveying equipment is measured. Litton Aero Products
has developed a highly digitized, low costL
1,C/A code GPS card set. The integration of these technologies had led to the development of a low-cost, high-precision, GPS survey
system which can be configured with or without a codelessL
2 capability.
TheMINI-MAC surveying system is the first member of the new generation of GPS survey systems resulting from this joint development. The
system design is described in this paper, and initial survey test results using a prototypeMINI-MAC surveying system are presented. 相似文献
1000.
Richard A. Beck Douglas W. Burbank William J. Sercombe Asrar M. Khan Robert D. Lawrence 《Geodinamica Acta》2013,26(2-3):114-144
AbstractCollision of the Kohistan island arc with Asia at ~100 Ma resulted in N-S compression within the Neo-Tethys at a spreading center north of the Indo-Pakistani craton. Subsequent India-Asia convergence converted the Neo-Tethyan spreading center into a short-lived subduction zone. The hanging wall of the subduction zone became the Waziristan, Khost and Jalalabad igneous complexes. During the Santonian- Campanian (late Cretaceous), thrusting of the NW IndoPakistani craton beneath Albian oceanic crust and a Cenomanian volcano-sedimentary complex, generated an ophiolite-radiolarite belt. Ophiolite obduction resulted in tectonic loading and flexural subsidence of the NW Indian margin and sub-CCD deposition of shelf-derived olistostromes and turbidites in the foredeep. Campanian-Maastriehtian calci- clastic and siliciclastic sediment gravity flows derived from both margins filled the foredeep as a huge allochthon of Triassic-Jurassic rise and slope strata was thrust ahead of the ophiolites onto the Indo-Pakistani craton. Shallow to intermediate marine strata covered the foredeep during the late Maastrichtian. As ophiolite obduction neared completion during the Maastrichtian, the majority of India-Asia convergence was accommodated along the southern margin of Asia. During the Paleocene, India was thrust beneath a second allochthon that included open marine middle Maastrichtian colored mélange which represents the Asian Makran-Indus-Tsangpo accretionary prism. Latérites that formed on the eroded ophiolites and structurally higher colored mélange during the Paleocene wei’e unconformably overlapped by upper Paleocene and Middle Eocene shallow marine limestone and shale that delineate distinct episodes of Paleocene collisional and Early Eocene post-collisional deformation. 相似文献