全文获取类型
收费全文 | 13276篇 |
免费 | 2711篇 |
国内免费 | 3381篇 |
专业分类
测绘学 | 1792篇 |
大气科学 | 1737篇 |
地球物理 | 3372篇 |
地质学 | 7766篇 |
海洋学 | 2065篇 |
天文学 | 440篇 |
综合类 | 911篇 |
自然地理 | 1285篇 |
出版年
2024年 | 44篇 |
2023年 | 200篇 |
2022年 | 491篇 |
2021年 | 676篇 |
2020年 | 576篇 |
2019年 | 545篇 |
2018年 | 974篇 |
2017年 | 851篇 |
2016年 | 767篇 |
2015年 | 783篇 |
2014年 | 693篇 |
2013年 | 858篇 |
2012年 | 1425篇 |
2011年 | 1187篇 |
2010年 | 892篇 |
2009年 | 885篇 |
2008年 | 841篇 |
2007年 | 742篇 |
2006年 | 776篇 |
2005年 | 1402篇 |
2004年 | 1325篇 |
2003年 | 989篇 |
2002年 | 449篇 |
2001年 | 361篇 |
2000年 | 273篇 |
1999年 | 100篇 |
1998年 | 33篇 |
1997年 | 43篇 |
1996年 | 27篇 |
1995年 | 10篇 |
1994年 | 8篇 |
1993年 | 8篇 |
1992年 | 13篇 |
1991年 | 9篇 |
1990年 | 15篇 |
1989年 | 7篇 |
1988年 | 3篇 |
1987年 | 8篇 |
1986年 | 3篇 |
1985年 | 9篇 |
1984年 | 5篇 |
1983年 | 4篇 |
1981年 | 3篇 |
1980年 | 4篇 |
1976年 | 5篇 |
1975年 | 4篇 |
1965年 | 3篇 |
1963年 | 5篇 |
1954年 | 7篇 |
1948年 | 2篇 |
排序方式: 共有10000条查询结果,搜索用时 500 毫秒
81.
82.
以中华齿米虾(Neocaridina denticulata sinensis)基因组DNA为模板,根据胰蛋白酶基因保守序列设计简并引物,利用PCR技术获得一个基因。序列分析表明此基因与已报道的凡纳滨对虾(Litopenaeus vannamei)胰蛋白酶基因有较高的相似度,序列中包含一个内含子和两个不完整的外显子,编码182个氨基酸残基。该氨基酸序列与凡纳滨对虾胰蛋白酶氨基酸序列的相似度为83.5%;含有胰蛋白酶所特有的His、Asp和Ser组成的活性三联体、决定胰蛋白酶底物专一性的Asp、底物结合部位的G1y残基。综合分析认定该基因为胰蛋白酶基因片断。将其氨基酸序列与报道的其他动物胰蛋白酶氨基酸序列进行了系统进化分析。系统进化分析的结果与现有以表型特征为依据的虾分类结果是一致的。 相似文献
83.
Distribution pattern of pelagic amphipods and its affecting facors in the East China Sea 总被引:1,自引:1,他引:1
1 IntroductionAmphipoda, an order of marine pelagic shell-fish, belongs to class Crustacea, subclass Malacost-raca (Chen and Shi,2002). Species of this ordercan be found all over the world, especially in tropi-cal and subtropical oceans. As fish diets, th… 相似文献
84.
Two processes are generally explained as causes of temporal changes in the stoichiometric silicon/nitrogen (Si/N) ratios of
sinking particles and of nutrient consumption in the surface water during the spring diatom bloom: (1) physiological changes
of diatom under the stress of photosynthesis of diatom and (2) differences of regeneration between silicon and nitrogen. We
investigated which process plays an important role in these changes using a one-dimensional ecosystem model that explicitly
represents diatom and the other non-silicious phytoplankton. The model was applied to station A7 (41°30′ N, 145°30′ E) in
the western North Pacific, where diatom regularly blooms in spring. Model simulations show that the Si/N ratios of the flux
exported by the sinking particles at 100 m depth and of nutrient consumptions in the upper 100 m surface water have their
maxima at the end of the spring diatom bloom, the values and timings of which are significantly different from each other.
Analyses of the model results show that the differences of regeneration between silicon and nitrogen mainly cause the temporal
changes of the Si/N ratios. On the other hand, the physiological changes of diatoms under stress can hardly cause these temporal
changes, because the effect of the change in the diatom's uptake ratio of silicon to nitrogen is cancelled by that in its
sinking rate. 相似文献
85.
Several large deployments of neutrally buoyant floats took place within the Antarctic Intermediate (AAIW), North Atlantic Deep Water (NADW), and the Antarctic Bottom Water (AABW) of the South Atlantic in the 1990s and a number of hydrographic sections were occupied as well. Here we use the spatially and temporally averaged velocities measured by these floats, combined with the hydrographic section data and various estimates of regional current transports from moored current meter arrays, to determine the circulation of the three major subthermocline water masses in a zonal strip across the South Atlantic between the latitudes of 19°S and 30°S. We concentrate on this region because the historical literature suggests that it is where the Deep Western Boundary Current containing NADW bifurcates. In support of this notion, we find that a net of about 5 Sv. of the 15–20 Sv that crosses 19°S does continue zonally eastward at least as far as the Mid-Atlantic Ridge. Once across the ridge it takes a circuit to the north along the ridge flanks before returning to the south in the eastern half of the Angola Basin. The data suggest that the NADW then continues on into the Indian Ocean. This scheme is discussed in the context of distributions of dissolved oxygen, silicate and salinity. In spite of the many float-years of data that were collected in the region a surprising result is that their impact on the computed solutions is quite modest. Although the focus is on the NADW we also discuss the circulation for the AAIW and AABW layers. 相似文献
86.
With the development of high-resolution multibeam echosounder systems (MBES) for surveying shallow-water areas a new tool is available to monitor rapid changes in seabed morphology as, e.g., caused by the dumping of dredge spoil in coastal waters. In this study, four data sets of repeated bathymetric surveys with a MBES were processed and analyzed. The data were collected in a 1.94-km2 dumping site in the outer Weser Estuary (German Bight). Between June and December 1998, 2.6 million m3 of dredged sediment were deposited there. The bathymetric maps generated in the course of this study reveal features such as subaqueous dunes, scour holes, and mounds of dumped dredge spoil. The mean water depth decreased by about 1 m during the dumping period. Furthermore, difference grids showing changes in sediment volume allowed a calculation of the sediment budget for the monitored area. After a time period of only 5 months, 0.5 million m3 of the originally dumped 2.6 million m3 of dredge spoil had already been removed from the dumping site. 相似文献
87.
88.
In October and November of 1977 and September and October of 1978,a quantitative survey of benthic animals was conducted in the East China Sea Continental Shelf and its adjacent waters(26°00'-34°00'N,124°00'-129°00'E,water depth 39-1550m),where 307 stations were dredged and 1200 samples collected. 相似文献
89.
云南程海近500年来湖泊初始生产力的演化 总被引:14,自引:1,他引:14
程海为富营养化封闭湖泊,通过对程海CH01乳沉积物色素分析,定性恢复了近500a来程海湖泊初始生产力演化过程,结果表明,近500a来程海湖泊初始生产力总体上呈现由低到高的上升趋势,其中1700AD前后,1790AD前后是湖泊初始生产力出现变化的界限,另外,色素含量变化揭示研究时期内存在1750AD前后,1930AD前后二次明显暖波动。 相似文献
90.