全文获取类型
收费全文 | 557篇 |
免费 | 95篇 |
国内免费 | 209篇 |
专业分类
测绘学 | 202篇 |
大气科学 | 63篇 |
地球物理 | 65篇 |
地质学 | 304篇 |
海洋学 | 134篇 |
天文学 | 3篇 |
综合类 | 60篇 |
自然地理 | 30篇 |
出版年
2024年 | 4篇 |
2023年 | 11篇 |
2022年 | 42篇 |
2021年 | 30篇 |
2020年 | 20篇 |
2019年 | 31篇 |
2018年 | 36篇 |
2017年 | 36篇 |
2016年 | 22篇 |
2015年 | 32篇 |
2014年 | 36篇 |
2013年 | 32篇 |
2012年 | 55篇 |
2011年 | 71篇 |
2010年 | 71篇 |
2009年 | 49篇 |
2008年 | 58篇 |
2007年 | 52篇 |
2006年 | 42篇 |
2005年 | 18篇 |
2004年 | 25篇 |
2003年 | 14篇 |
2002年 | 9篇 |
2001年 | 16篇 |
2000年 | 19篇 |
1999年 | 9篇 |
1998年 | 3篇 |
1997年 | 5篇 |
1996年 | 2篇 |
1995年 | 1篇 |
1994年 | 1篇 |
1992年 | 4篇 |
1991年 | 2篇 |
1989年 | 1篇 |
1986年 | 1篇 |
1957年 | 1篇 |
排序方式: 共有861条查询结果,搜索用时 46 毫秒
21.
Mariculture has rapidly grown worldwide, which might greatly influence the biogeochemical cycle of organic carbon in coastal seas. In this study, several geochemical parameters, including grain size composition, sedimentary total organic carbon(TOC), total nitrogen(TN), stable carbon(δ13 C) and nitrogen(δ15 N) isotopic compositions, were analyzed for surface sediments collected from different mariculture zones of Sanggou Bay and in different seasons. We investigated the composition and distribution of organic matter in surface sediments and further evaluated the contribution of mariculture activities to TOC sources. The TOC and TN contents(mass percentage) in the bay were in the range of 0.14% to 1.45% and 0.03% to 0.20%, respectively. The spatial distribution indicated that sedimentary TOC and TN contents in shellfish monoculture and shellfish-kelp polyculture zones were higher than in other mariculture zones, which might be related to grain size composition and mariculture organisms. Seasonal variations of TOC contents were observed in different mariculture zones. The TOC/TN atomic ratio(C/N), δ13 C and δ15 N were in the ranges of 5.97 to 10.97,-21.76‰ to-13.14‰ and 2.13‰ to 8.08‰, respectively, implying that sedimentary organic matter in Sanggou Bay was the mixture of marine phytoplankton, terrestrial and maricultural sources. A simple mixing model based on δ13 C was applied and the results indicated that the relative contributions of organic carbon sources in Sanggou Bay followed the order kelp(36.6%) ? marine phytoplankton(28.7%) ? shellfish bio-deposition(23.8%) ? terrestrial input(10.9%). Surface sediments in Sanggou Bay were dominated by mariculture-derived organic carbon, which on average accounted for 60.4% of TOC. 相似文献
22.
Floodplains are important and distinctive ecosystems around the world, and the recruitment of ichthyoplankton from river to floodplain lakes is crucial to maintain this unique ecosystem. However,this process has not been well documented. In this study, ichthyoplankton were sampled to investigate the details of ichthyoplankton recruitment from the Changjiang(Yangtze) River to the Dongting Lake via a floodway channel, the Songzi River, from May to July in 2013 and 2014. During the study period, 41 species of eggs and larvae were sampled. Among the samples, 16 were river-lake migratory species(RL), representing23.5% of the species in the Dongting Lake. In 2013, an estimated 130 million eggs and 3 180 million larvae drifted through the sampling section, and in 2014, an estimated 1 060 million eggs and 1 040 million larvae drifted through the sampling section. The amount of eggs and larvae of RL reached 3 210 million in 2013 and 1 850 million in 2014, respectively. These results demonstrated the importance of ichthyoplankton recruitment from the river to the lake, as species diversity will decrease sharply without this recruitment.Canonical correspondence analysis(CCA) showed that water temperature and water flow are the two most important factors influencing the spawning activities of fish. To maintain the high fish diversity in the Changjiang floodplain, we suggest to irrigate the channel to increase water discharge and increase the transport of ichthyoplankton from the Changjiang mainstream into the Dongting Lake. 相似文献
23.
Biofloc technology has been applied successfully in the intensive aquaculture of several fish and shrimp species.The growth of heterotrophic microorganisms can be stimulated through adding extra carbon,which reduces the nitrogen level in the water and provides microbial protein to the animals.However,most of the studies and practical applications have been conducted in freshwater and marine environment.This paper focused on brine shrimp Artemia that lives in high salinity environment together with other halophilic or halotolerant microorganisms.The effect of carbon supplementation on Artemia growth,water quality,and microbial diversity of bioflocs was studied in the closed culture condition without any water exchange.The salinity of the culture medium was 100.A 24-d culture trial was conducted through supplementing sucrose at carbon/nitrogen(C/N)ratio of 5,15,and 30(Su5,Sul5,and Su30),respectively.The culture without adding sucrose was used as a control.Artemia was fed formulated feed at a feeding ration of 60% recommended feeding level.The results showed that sucrose supplementation at higher C/N ratio(15 and 30)significantly improved the Artemia survival,growth and water quality(P0.05).Addition of sucrose at C/N ratio of 15 and 30 significantly increased biofloc volume(BFV)(P0.05).The Illumina MiSeq sequencing analysis showed that supplementing carbon at C/N ratio of 15 had a better total bacterial diversity and richness,and shaped the microbial composition at genera level.This study should provide information for studying the mechanism of biofloc technology and its application in high salinity culture conditions. 相似文献
25.
由于不同的水深探测手段及海深反演方法适用于不同深度的海域,且全球海域水深分布不均,因此在探测及反演海深之前,需对目标海域的水深分布有一定认识。本文采用ETOPO1模型对全球及部分海域进行统计分析,结果表明,全球及大西洋、印度洋、太平洋区域的水深大多处于3 000—10 000 m,其中3 000—5 000 m水深海域占比较大,因此,在这些海域主要采用重力数据结合船测数据进行反演,同时应注意避开海岸带、岛屿较多、海脊存在的区域;对于水深小于1 000 m的海域,可以根据外部环境,采用多波束船测、水深遥感、机载激光测深等方式进行探测。通过分析及统计全球和重点海域的水深可以为海深探测及海底地形反演方法的选取提供参考。 相似文献
26.
综述了我国海域无脊椎动物的分类学和系统演化研究的历史和概况,以及我国分类系统学工作者在海洋无脊椎动物分类学、区系与动物地理学、系统发育与分子系统学领域的主要工作,重点介绍了中国科学院海洋研究所的海洋无脊椎动物分类学工作。涉及类群包括原生动物、海绵动物、刺胞动物、线虫、多毛类环节动物、星虫、螠虫、软体动物、节肢动物、苔藓动物、毛颚动物、棘皮动物、半索动物等主要的无脊椎动物门类。涉及海域以我国管辖海域,特别是中国近海为主,也涉及了西太平洋、西南印度洋等深海环境的无脊椎动物类群的分类学报道。本文总结过去,展望未来,对于在我国在海洋无脊椎动物分类与系统演化研究领域成就基础上,发现薄弱环节,研讨今后本学科的发展方向,填补研究空白,赶超本领域国际前沿,都有重要借鉴意义。 相似文献
27.
Formation of saddle dolomites in Upper Cambrian carbonates, western Tarim Basin (northwest China): Implications for fault-related fluid flow 总被引:1,自引:0,他引:1
Juntao Zhang Wenxuan Hu Yixiong Qian Xiaolin Wang Jian Cao Jingquan Zhu Qing Li Xiaomin Xie 《Marine and Petroleum Geology》2009,26(8):1428-1440
The saddle dolomites occur more intensely in cores closely to fault than that in cores far away from the fault in Upper Cambrian carbonate of western Tarim basin, suggesting that formation of the saddle dolomites is likely related to fault-controlled fluid flow. They partially fill in fractures and vugs of replacement dolomite. The saddle dolomites exhibit complex internal textures, commonly consisting of core and cortex. In comparison with the matrix dolomites, the saddle dolomites show lower Sr-content and 87Sr/86Sr ratios, higher Fe- and Mn-content, and more negative δ18O values. Combined with high Th (100–130 °C) of primary fluid inclusions, it is suggested that the saddle dolomites precipitated from hydrothermal fluid derived from the deep evaporite-bearing Middle Cambrian strata, and the magnesium source may be due to dissolution of host dolomite during hydrothermal fluid migration. Fault activity resulted in petrographic and geochemical difference of the core and cortex of the saddle dolomites. The cores precipitated from the formation water mixed by deep brines at the early stage of fault activity, and the cortexes precipitated from the deep fluid with higher temperatures through the Middle Cambrian later. In summary, the formation of the saddle dolomites implies a hydrothermal fluid event related to fault activity, which also resulted in high porosity in Upper Cambrian carbonate in western Tarim Basin. 相似文献
28.
本文描述了于1959年采自中国黄海和东海锥头虫科刺尖锥虫属一新种——中国刺尖锥虫Leodamas sinensis sp.nov.。本文详细描述了该物种的形态特征及与近似种的区别,并编制了刺尖锥虫属Leodamas Kinberg,1866物种检索表。 相似文献
29.
牟平-乳山成矿带是山东省重要的金成矿带,姜格庄金矿位于牟平-乳山成矿带东北部,米山断裂西侧。姜格庄金矿矿床成因为中低温岩浆热液金矿床,控矿构造以近SN向断裂构造为主。矿区内地表出露矿化蚀变带5个,圈定矿体5个,矿体多呈脉状、透镜状,成矿严格受矿断裂控制,产状与蚀变带一致,围岩为邱家单元片麻状黑云二长花岗岩,蚀变主要为硅化、钾化、褐铁矿化等。矿石矿物主要有黄铁矿、褐铁矿及黄铜矿,金矿物主要为自然金等。通过对矿体地质特征和分布规律研究,认为该区域断裂构造内具有较好的找矿潜力。 相似文献
30.