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991.
基于2015—2016年湖北省环境监测数据和气象资料,分析了3种地形下空气质量指数(AQI)特征及其与气象因子的关系。结果表明:湖北省年空气质量指数时空分布特征为山区低平原高,冬季高夏季低,日高峰值襄阳出现在中午,武汉和宜昌出现在23:00—24:00;与空气质量指数关系较显著的气象因子包括相对湿度、变温、变压、风、降水等,其中降水对污染物的沉降作用跟空气质量等级有关,污染程度越重,需要清洁空气的雨量越大,轻度以上污染时,需要中雨及以上降水才会产生有效清洁,当降水为微量(1mm以下)时,AQI反而会增长;受不同地形影响,不同城市污染天气输入路径不同,襄阳为北风、武汉西北风、宜昌多弱东风扰动,且襄阳大风速出现的频数较高,而宜昌以小风为主。 相似文献
992.
Song Jingjing Xia Xiangao Zhang Xiaoling Che Huizheng Li Xiaojing 《Theoretical and Applied Climatology》2018,131(3-4):1019-1041
Theoretical and Applied Climatology - A weekly cycle of surface particulate matter (PM) characterized by smaller values during weekends and larger values during weekdays was reported in eastern... 相似文献
993.
994.
Mingjie Shen Shouyun Hu Uli. Blaha Haitao Yan Wolfgang. R?sler Ewin. Appel Viktor. Hoffmann 《Frontiers of Earth Science》2008,2(4):400-407
An expressway-side soil profile 22 cm long was sampled from the grassland of the expressway linking Beijing and the Capital
International Airport. Magnetic measurements, geochemical and multivariate statistic analyses were performed on the soil samples.
The results reveal that the soil profile can be divided into two parts with significant difference in magnetic proxies and
heavy metal concentration. The uppermost soil horizon (0–8 cm) represents the pollution-rich layer with higher concentration
of ferrimagnetic phases and metallic elements. The values of xare very high with an average of 141.60 × 10−8 m3·kg−1 in the layer. We explain that the anthropogenic dust input from traffic is the predominant cause for strong signals of magnetic
phases and heavy metals. Below the profile depth of 8 cm, there is minor pollution in the soil with lower concentration of
magnetic minerals and heavy metals compared to the natural background values. χ remains quite stable and relatively low with
an average of 49.44 × 10−8 m3·kg−1. S-ratio also generally decreases with depth, and it changes from 0.93 in the 0–8 cm layer to 0.87 below the depth of 8 cm.
It indicates that the soil samples are overwhelmingly predominated by ferrimagnetic minerals in the upper part soil, while
the contribution of imperfect antiferromagnetic components is stronger in the lower part. Rock magnetic experiments show MD
magnetite as the main magnetic carrier both in the upper and lower parts. Themagnetic grain size in the upper part is, however,
a bit coarser than that in the lower part. Cluster analysis shows a positive correlation between magnetic properties (χ, ARM,
SIRM) and heavy metal pollutants of Pb, Zn, Cu. Fuzzy C-means cluster analysis can clearly help divide the soil profile into
two different layers and distinguish their characteristics. It can be concluded that these magnetic concentration-related
parameters can be used as proxies for pollution investigation in a fast, sensitive, low-cost and highly efficient approach
to screening heavy metal pollution.
__________
Translated from Quaternary Sciences, 2007, 27(6): 1113-1120 [译自:第四纪研究] 相似文献
995.
David T. Johnston James Farquhar Yanan Shen Andrew L. Masterson 《Geochimica et cosmochimica acta》2008,72(17):4278-4290
Previous geochemical and biomarker studies of the late Paleo-Mesoproterozoic propose a stratified world, with strongly reducing (possibly sulfidic) deep-ocean conditions overlain by an oxygenated surface-ocean and atmosphere. To investigate such a scenario, we look to the structure of the biogeochemical sulfur cycle. We present sulfur (32S, 33S, 34S, and 36S in sulfides) isotope data from the McArthur Basin (Barney Creek, Reward, Velkerri, and McMinn formations) that allows for a direct evaluation of the surface biosphere. We are interested in investigating the types of information that can be gained by including 33S and 36S. When the 34S/32S fractionations are small, the inclusion of 33S and 36S provides little additional information, but does provide ancillary evidence for relative isotopic homogeneity (with the internal consistency of 33S/32S and 36S/32S). When the 34S/32S fractionations are large, direct information about the fractionation mechanisms can be obtained, with the potential to distinguish the biological from abiological processes. For example, the reconstruction of the Roper Group suggests that seawater sulfate concentrations were high enough to buffer against spatial heterogeneities. Overall, our findings agree with previously proposed redox structure of the Proterozoic ocean, highlight contributions from the oxidative sulfur cycle, and outline a new tool for interpreting the state of the surface sulfur cycle. 相似文献
996.
Incubation studies were carried out using 5 freshly collected sediments from shallow aquifers of the Hetao Basin, Inner Mongolia. The aquifer sediments covering a range of redox conditions, as indicated by their deep grey to yellow color were mixed with degassed artificial As solution or degassed deionized water at a ratio of solid to water of about 1:10 (wt./wt.). Suspensions which were either amended with glucose or autoclaved, were incubated in parallel with unamended suspensions. Five microcosm cultures of unamended sediments gradually release the equivalent of 0.03–0.30 μg/g As to the dissolved phase. The addition of glucose as a potential electron donor results in a marked stimulation in the mobilization of As (0.71–3.81 μg/g) in the amended incubations for all sediments. The quantity of As released accounts for 60–70% of As bound to Fe/Mn oxides in the original sediments. The microbially mediated mobilization of As with the organic nutrient as an electron donor is strongly associated with the As bound to Fe/Mn oxides, as well as the exchangeable As. During the incubations amended with glucose, 2–4% of the sediment Fe is released. The results suggest that the introduction of labile dissolved organic C into the yellowish sediment aquifers with As-free groundwater would reduce a significant proportion of the Fe(III) oxyhydroxides mediated by anaerobic bacteria respiration and increase groundwater As concentrations. 相似文献
997.
Combined effects of heavy metal and polycyclic aromatic hydrocarbon on soil microorganism communities 总被引:2,自引:0,他引:2
Soil contaminated sites contain a variety of pollutants, especially heavy metals and polycyclic aromatic hydrocarbons (PAHs).
Interactions between heavy metals have been relatively well studied, but little is known about interactions between heavy
metals and PAHs. The combined effect of heavy metals and PAHs on soil microorganism was studied in laboratory conditions and
evaluated by random denaturing gradient gel electrophoresis. We extracted DNA directly from contaminated soils and then amplified
the V3 sequences of the 16S rDNA. The results showed that with different culture time, the gene diversity of the single and
combined contaminated soil differed as well. After 15 days of culture, the microorganisms were stimulated and accommodated.
After 45 days of cultivation, the quantities of the soil microorganisms were affected. It is concluded that some of the microorganisms
utilize phenanthrene as important carbon resources. Microorganisms directly isolated from soil could reflect the diversity
of soil microorganism and population distribution conditions. 相似文献
998.
Application of allochthonous organic carbon and phosphorus forms in the interpretation of past environmental conditions 总被引:2,自引:0,他引:2
Changwei Lü Jiang He Huimin Sun Hongxi Xue Ying Liang Saruli Bai Ying Sun Lili Shen Qingyun Fan 《Environmental Geology》2008,55(6):1279-1289
Organic matter in sediments, for instance, carbon, nitrogen and phosphorus, can be used to reconstruct the paleoecological
and pollution history of lakes and their catchment basins. In this paper, the contents of allochthonous organic carbon (allochthonous
OC) and autochthonous organic carbon (autochthonous OC) in sediment cores taken from Wuliangsuhai Lake and Daihai Lake in
northern China are quantified by using a binary model, and phosphorus forms in the sediment cores from the two lakes are extracted
by sequential extraction techniques. The results indicate that the palaeoenvironment and paleoclimate of Daihai Lake and
its catchment basin in the recent 250 years can be well reconstructed based on the content of allochthonous OC. The climate
was relatively humid and warm in the period of 1865–2005, while relatively dry and cold in the period of 1765–1865. The sedimentary
information of allochthonous OC in the 22–42-cm portion of the sediment cores in Daihai Lake corresponds to the final cold
fluctuation of the Little Ice Age that occurred since the Middle Holocene. The difference of phosphorus forms in the sediment
cores between the two lakes indicates that phosphorus input to the lakes and the correlation between phosphorus forms and
distribution and the changes of environment are influenced by the eutrophication mechanisms and environmental conditions of
the two lakes. 相似文献
999.
在ICT技术推动下,地图学的发展迎来空前的挑战,本文针对当前地图学的发展面临的问题和转变,深入分析传统地图学的限制——物理空间的传统约束,面向现代地图的形式松散化,从现实与虚拟、外表与内里、纸质与电子等8个方面论述现代地图学信息空间的数字自由,并针对数字时代和大数据的发展机遇和需求,拓展地图学框架,同化新兴元素,推动地图学复兴。 相似文献
1000.
A GPS positioning algorithm is studied and applied to locate a spinning vehicle on which a single-patch antenna is mounted. Because the antenna is directional and the received signal is periodically discontinuous, the bits and frames cannot be synchronized to assemble the transmission time of the satellite signals. The characteristics of the signals received by a single-patch antenna are described. The means by which the tracking loop works with these discontinuous signals are analyzed and simulated. Aiming at spinning projectiles, the positioning algorithm forming differencing with respect to a reference satellite is applied to locate the spinning vehicle by using code phases obtained in the tracking of the discontinuous signals. Experiments were carried out, and the results showed that the positioning algorithm works properly on the spinning vehicle. The results revealed that the positioning error of the algorithm applied to a spinning vehicle is close to that of the conventional positioning method applied to a non-spinning vehicle. 相似文献