全文获取类型
收费全文 | 34801篇 |
免费 | 757篇 |
国内免费 | 246篇 |
专业分类
测绘学 | 909篇 |
大气科学 | 2619篇 |
地球物理 | 7796篇 |
地质学 | 12650篇 |
海洋学 | 2750篇 |
天文学 | 7056篇 |
综合类 | 95篇 |
自然地理 | 1929篇 |
出版年
2021年 | 372篇 |
2020年 | 405篇 |
2019年 | 376篇 |
2018年 | 955篇 |
2017年 | 942篇 |
2016年 | 1163篇 |
2015年 | 708篇 |
2014年 | 1059篇 |
2013年 | 1894篇 |
2012年 | 1217篇 |
2011年 | 1457篇 |
2010年 | 1290篇 |
2009年 | 1595篇 |
2008年 | 1359篇 |
2007年 | 1299篇 |
2006年 | 1289篇 |
2005年 | 960篇 |
2004年 | 939篇 |
2003年 | 879篇 |
2002年 | 851篇 |
2001年 | 792篇 |
2000年 | 787篇 |
1999年 | 601篇 |
1998年 | 598篇 |
1997年 | 673篇 |
1996年 | 510篇 |
1995年 | 538篇 |
1994年 | 545篇 |
1993年 | 427篇 |
1992年 | 429篇 |
1991年 | 397篇 |
1990年 | 423篇 |
1989年 | 387篇 |
1988年 | 380篇 |
1987年 | 401篇 |
1986年 | 368篇 |
1985年 | 468篇 |
1984年 | 450篇 |
1983年 | 487篇 |
1982年 | 465篇 |
1981年 | 406篇 |
1980年 | 442篇 |
1979年 | 362篇 |
1978年 | 350篇 |
1977年 | 334篇 |
1976年 | 294篇 |
1975年 | 306篇 |
1974年 | 300篇 |
1973年 | 300篇 |
1971年 | 215篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
991.
The flow of organic matter along the main navigation channel of Ria Formosa, Portugal, was assessed using determinations of suspended particulate matter (SPM), particulate organic matter (POM), and chlorophyll a (chla) concentrations in conjunction with stable isotope values of primary producers, particulate matter, and two filter feeders. SPM in the lagoon is dominated by inorganic particles comprising 80% of total weight with organic matter averaging about 20%. The algal component of the POM averaged about 5% with the remainder comprised of detritus. The δ13C values of primary producers ranged from ?9.1‰ in the intertidal seagrassZostera noltii to ?30.7‰ in the red seaweedBostrychia scorpioides revealing underlying differences in the mechanisms of carbon uptake. The δ13C value ofB. scorpioides, which develops entangled on the salt marsh speciesSpartina maritima, suggests that its main source of inorganic carbon is atmospheric CO2. The δ13C values of the high marsh macrophyteSarcocornia perennis significantly increased with distance from the ocean while δ13C values ofZ. noltii decreased, probably because higher decomposition of organic matter at inner stations lowers the δ13CO2 value in the water. The δ15N values of Ulvales, seagrasses, and marsh plants significantly increased from outer stations to inner stations. This increase may be due either to recycling of nitrogen (N) within the marsh (with loss of light N2 or NH4) or to inputs of isotopically heavy N from sewage. The δ15N values of particulate matter showed an opposite trend, which indicates higher microbial degradation of organic matter at the inner lagoon. The data demonstrate that the seston in the lagoon is a mixture of detritus from lagoon primary producers with a minor contribution of microalgae. The filter feeders are most likely assimilating a mixture of phytoplankton and microphytobenthos. Digestion of lagoon seston is selective. The δ15N values of both muscle and digestive gland of filter feeders showed the opposite gradient of particulate matter indicating that the depleted δ15N of SPM at inner stations was not assimilated or even ingested. Stable isotopes values did not differ between the filter-feeders—the musselMytilus galloprovincialis collected on buoys and the clamTapes decussatus collected in the sediment—suggesting a considerable mixture of benthic-pelagic organic matter throughout the water column. Assessment of the changes in isotopic decomposition of detritus as it decays is required to refine our understanding of organic matter transfers in detrital food webs. 相似文献
992.
993.
994.
995.
K. Nageswara Rao G. Murali Krishna D. Ramprasad Naik B. Hema Malini 《Journal of the Indian Society of Remote Sensing》2003,31(2):71-80
Interpretation of IRS LISS II and LISS III imagery has revealed the various landforms as well as land use/land cover features in a part of the Godavari delta coastal belt. A comparative analysis of geomorphological vs. land use/land cover maps suggested that the landforms exert a certain degree of control over human land use activities even in this monotonously plain area. Further, an analysis of the sequential imagery pertaining to 1992 and 2001 aimed at detecting the land use/land cover change has indicated that the aquaculture has phenomenally increased by 9,293.5 ha during the 9-year period. At the same time, the cropland which occupied about 29,104 ha in 1992 has been reduced to 19,153.9 ha by 2001 mainly due to the encroachment of aquaculture. Village level data on temporal variation in land use/land cover extracted through GIS analysis revealed that in 14 out of the total 39 villages in the area, the conversion of cropland into aquaculture ponds was more than 30% with the highest conversion rate of 89.8% in Gondi village. These fourteen villages, which are designated as ‘aquaculture hotspots’ are grouped into 4 priority classes based on the intensity of conversion. 相似文献
996.
High-resolution simulations of global climate, part 2: effects of increased greenhouse cases 总被引:6,自引:0,他引:6
We report results from the highest-resolution simulations of global warming yet performed with an atmospheric general circulation model. We compare the climatic response to increased greenhouse gases of the National Center for Atmospheric Research (NCAR) climate model, CCM3, at T42 and T170 resolutions (horizontal grid spacing of 300 and 75 km respectively). All simulations use prescribed sea surface temperatures (SST). Simulations of the climate of 2100 ad use SSTs based on those from NCAR coupled model, Climate System Model (CSM). We find that the global climate sensitivity and large-scale patterns of climate change are similar at T42 and T170. However, there are important regional scale differences that arise due to better representation of topography and other factors at high resolution. Caution should be exercised in interpreting specific features in our results both because we have performed climate simulations using a single atmospheric general circulation model and because we used with prescribed sea surface temperatures rather than interactive ocean and sea-ice models. 相似文献
997.
The Multi frequency Scanning Microwave Radiometer (MSMR) onboard Oceasat-1 was used to develop a retrieval method fornear-surface specific humidity by means of multivariate regressiontechnique. The MSMR measures the microwaveradiances in 8 channels at the frequencies of 6.6, 10.7, 18 and 21 GHzfor both vertical and horizontal polarizations. Regression coefficients were derived using the ship reports of the Comprehensive Ocean-Atmosphere Data Set (COADS) for the months of July, October and December, in 1999. Daily near-surface specific humidity data from COADS in 2° × 2° latitude/longitude bins and collocated brightness temperature data from MSMR were used to derive the coefficients. The derived coefficients werevalidated with humidity given in COADS.A linear relationship is established to determine the near-surface specifichumidity from MSMR brightness temperature (Tb) with an rms error of 1.2 g kg-1 for individual situations and an rms errorof 0.84 g kg-1 for monthly time scales over global oceans.The retrieval algorithm is validonly for the open sea regions. 相似文献
998.
A. Gelencsér A. Hoffer G. Kiss E. Tombácz R. Kurdi L. Bencze 《Journal of Atmospheric Chemistry》2003,45(1):25-33
Current climate models seem to underestimate the flux of solar energy absorbed by the global troposphere. All of these models are constrained with the assumption that cloud droplets consist of pure water. Here we demonstrate in a simple laboratory experiment that aromatic hydroxy-acids which are found in continental fine aerosol can react with hydroxyl radicals under typical conditions prevalent in cloud water influenced by biomass burning. The reactions yield colored organic species which do absorb solar radiation. We also suggest that the products of such reactions may be humic-like substances whose presence in continental aerosol has been confirmed but their source mechanisms are still much sought after. We also attempt to give a first order estimate of the enhancement of water absorption at a visible wavelength under atmospheric conditions. 相似文献
999.
M. Krämer Ri. Müller H. Bovensmann J. Burrows J. Brinkmann E. P. Röth J.-U. Grooß Ro. Müller Th. Woyke R. Ruhnke G. Günther J. Hendricks E. Lippert K. S. Carslaw Th. Peter A. Zieger Ch. Brühl B. Steil R. Lehmann D. S. McKenna 《Journal of Atmospheric Chemistry》2003,45(1):51-77
Several stratospheric chemistry modules from box, 2-D or 3-D models, have been intercompared. The intercomparison was focused on the ozone loss and associated reactive species under the conditions found in the cold, wintertime Arctic and Antarctic vortices. Comparisons of both gas phase and heterogeneous chemistry modules show excellent agreement between the models under constrained conditions for photolysis and the microphysics of polar stratospheric clouds. While the mean integral ozone loss ranges from 4–80% for different 30–50 days long air parcel trajectories, the mean scatter of model results around these values is only about ±1.5%. In a case study, where the models employed their standard photolysis and microphysical schemes, the variation around the mean percentage ozone loss increases to about ±7%. This increased scatter of model results is mainly due to the different treatment of the PSC microphysics and heterogeneous chemistry in the models, whereby the most unrealistic assumptions about PSC processes consequently lead to the least representative ozone chemistry. Furthermore, for this case study the model results for the ozone mixing ratios at different altitudes were compared with a measured ozone profile to investigate the extent to which models reproduce the stratospheric ozone losses. It was found that mainly in the height range of strong ozone depletion all models underestimate the ozone loss by about a factor of two. This finding corroborates earlier studies and implies a general deficiency in our understanding of the stratospheric ozone loss chemistry rather than a specific problem related to a particular model simulation. 相似文献
1000.
B. Kasietczuk 《Journal of Geodesy》1997,71(3):131-136
This paper presents an extension of the geodetic network adjustment model. The proposed extension makes possible the estimation
of the 3-rd and 4-th central moments for the vector of measurement errors in the process of network adjustment by the least-squares
method with application of orthogonal matrices. It allows to estimate the asymmetry and kurtosis of the measurement errors
distribution.
Received 13 April 1993; Accepted 8 July 1996 相似文献