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21.
HEYaoqi WANGYongjin KONGXinggong CHENGHai 《科学通报(英文版)》2005,50(10):1003-1008
Based on MC-ICP-MS U-series dating andstable O-isotope analysis results, a 4-5 years resolution monsoon record over the past 1000 years has been established for two stalagmites from Dongge Cave, Guizhou. The high resolution oxygen isotope record serves as a proxy for variations in rainfall of Asian southwest monsoon over the Yunnan-Guizhou Plateau. A close relation of the δ18O record with the A^14C record from tree rings largely reflects impact of centennial-scale solar activity on the monsoon climate changes. The conspicuous decrease in the δ18O value at AD 1720 indicates an abrupt increase in monsoon rainfall, suggesting that an atmospheric-oceanic couple over the tropical Indian Ocean plays an important role in rapid increase of the Northern Hemisphere temperature over the last century. 相似文献
22.
考洲洋表层沉积物的重金属含量及其污染分析 总被引:3,自引:0,他引:3
用原子吸收光谱法测定了南海东北部考洲洋表层沉积物中重金属的含量,各测站镉和铅含量超标率分别达到91.7%和50%,铜、锌含量未见超标,镍含量较低,比较和回归分析表明,考洲洋表层沉积物重金属含量在广东沿海居中等水平,并表现出同源相关关系,元素相关图显示,考洲洋表层沉积物尚未受人为来源镉和铅的影响。 相似文献
23.
Indicators of δ13C and δ18O of gas hydrate-associated sediments 总被引:1,自引:0,他引:1
The analyses of δ13C and δ18O of gas hydrate-associated sediments from two cores on Hydrate Ridge in Cascadia convergent margin offshore Oregon, eastern North Pacific show the values of d 13C from -29.81‰ to -48.28‰ (PDB) and d 18O from 2.56‰ to 4.28‰ (PDB), which could be plotted into a group called typical carbonate minerals influenced by the methane in cold venting. Moreover, the values of d 13C and d 18O show a consistent trend in both cores from top to bottom with increasing of d 13C and decreasing of d 18O. This trend could be explained as an effect caused by the anaerobic oxidation of methane (AOM) in depth and the oxygen fraction during the formation of gas hydrate in depth together. These characteristics of d 13C and d 18O indicate that the gas hydrate-associated sediments are significantly different from the normal marine carbonates, and they are deeply influenced by the formation and evolution of gas hydrate. So, the distinct characteristics of d 13C and d 18O of gas hydrate-associated sediments could be undoubtedly believed as one of parameters to determine the presence of gas hydrates in other unknown marine sediment cores. 相似文献
24.
Persistent organic pollutants PCNs and PBDEs in sediments from coastal waters of Qingdao,Shandong Peninsula 总被引:4,自引:0,他引:4
YANGYongliang PANJing LIYue YINXiaocai SHILei 《科学通报(英文版)》2004,49(1):98-106
Thirty-one congeners of polychlorinated naphthalenes (PCNs) and 21 congeners of polybrominated diphenylethers(PBDEs)in surface sediments at 5 stations and one mussel sample from Qingdao coastal waters were analyzed. The maximum contents occur at the station near the Haibo River mouth. The total PCNs contents are in the range of 212-1209 pg/g dw, dominated by tri-Cl CN. The total PBDEs contents are in the range of 117-5510 pg/g dw,dominated by tri- to hexa-BrBDEs. The local sources of PCNs are likely from combustion processes such as incinerations and coal burnings. The sources of PBDEs are molecular diffusion from the materials containing them. Except for the area near the river mouth where is affected by the sewage sludges, an important source of PCNs and PBDEs in this area is believed to be the atmospheric deposition. Mussels enrich PCNs and PBDEs relative to the sediments. The total TEQs of PCNs in mussels are lower than the total TEQs of PCBs. 相似文献
25.
WANG Weiming LIU Jinling & ZHOU Xiaodan . Nanjing Institute of Geology Palaeontology Chinese Academy of Sciences Nanjing China . Nanjing Geological Museum Nanjing China Correspondence should be addressed to Wang Weiming 《科学通报(英文版)》2003,48(18):2005-2009
Many related papers have been published since the first report on the discovery of Nanjing hominid crania by Mu et al.[1]. Mu et al.[1], Xu et al.[2—4], the Tangshan Ar-chaeological Team[5] and Dong[6] have successively stud-ied the Nanjing Homo erectus?symbiotic faunas. Mu et al. and Xu et al. considered that the nature of the fauna in the Tangshan area belongs to the Oriental Realm,and this region was usually occupied by Ailuropoda-Tapirus fauna in the Pleistocene. However, the typica… 相似文献
26.
东岛牛塘为目前在西沙群岛少见的淡水型湖泊,其中保存完好的粪土沉积物记录了距今1 300年来东岛生态环境演化历史.对DY4粪土沉积柱的研究结果表明,在1 400 AD前,东岛海鸟数量较多,牛塘湖岸周围植被生长较为繁盛,而在1 400~1 850 AD期间,东岛海鸟数量和植被生长都处于低谷.通过综合对比研究区、中国乃至北半球降雨量、温度变化记录,发现1 400 AD前岛屿生物量较高的时期对应于暖干的中世纪温暖期,而低生物量时期与凉湿的小冰期一致,证明南海热带孤立岛屿生态系统对区域乃至全球气候环境变化响应非常灵敏. 相似文献
27.
GUO LanLan FENG ZaoDong LI XinQing LIU LianYou WANG LiXia 《科学通报(英文版)》2007,52(7):959-966
A 5.3 m lake core was drilled in Baahar Nuur Lake in the Ordos Plateau, and measurements of meangrain size, organic δ 13C (δ 13Corg), organic carbon content (TOC), C/N, carbonate content, carbonate δ 13C(δ 13Ccar) and δ 18O (δ 18Ocar) were conducted for retrieving the Holocene chronosequence of climaticchanges based on 15 AMS 14C dates. The record documented four major stages of climate change inthe Ordos Plateau: (IV) a cold and dry condition before ~7.65 14C ka BP; (III) a warm and humid stagebetween ~7.65 and ~5.40 ka BP; (II) a generally drier and cooler climate since ~5.40 ka BP with twohumid events occurring from ~4.70 to ~4.60 ka BP and from ~4.20 to ~3.70 ka BP, and (I) a dry climatecharacterized by complete desiccation of the lake after 3.70 ka BP. Stage III can be further divided intothree sub-stages: (IIIa) a warm and humid episode from ~7.65 to ~6.70 ka BP, (IIIb) a warm and relativelydry episode from ~6.70 to ~6.20 ka BP, and (IIIc) the magthermal and maghumid episode of the Holo-cene from ~6.20 to ~5.40 ka BP. 相似文献
28.
Clay minerals in surface sediments of the Pearl River drainage basin and their contribution to the South China Sea 总被引:5,自引:0,他引:5
LIU ZhiFei Christophe COLIN HUANG Wei CHEN Zhong Alain TRENTESAUX CHEN JianFang 《科学通报(英文版)》2007,52(8):1101-1111
Clay minerals have played a significant role in the study of the East Asian monsoon evolution in the South China Sea by being able to track oceanic current variations and to reveal contemporaneous paleoclimaUc changes prevailing in continental source areas. As one of the most important rivers inputting terrigenous matters to the northern South China Sea, the Pearl River was not previously paid attention to from the viewpoint of clay mineralogy. This paper presents a detailed study on clay minerals in surface sediments collected from the Pearl River drainage basin (including all three main channels, various branches, and the Lingdingyang in the estuary) by using the X-ray diffraction (XRD) method. The results indicate that the clay mineral assemblage consists dominantly of kaolinite (35%-65%), lesser abundance of chlorite (20%-35%) and illite (12%-42%), and very scare smectite occurrences (generally 〈5%). Their respective distribution does not present any obvious difference throughout the Pearl River drainage basin. However, downstream the Pearl River to the northern South China Sea, the clay mineral assemblage varies significantly: kaolinite decreases gradually, smecUte and illite increase gradually. Additionally, illite chemistry index steps down and illite crystallinity steps up. These variations indicate the contribution of major kaolinite, lesser illite and chlorite, and very scarce smecUte to the northern South China Sea from the Pearl River drainage basin. The maximum contribution of clay minerals from the Pearl River is 72% to the northern margin and only 15% to the northern slope of the South China Sea. In both glacials and interglacials, kaolinite indicates that the ability of mechanical erosion occurred in the Pearl River drainage basin. 相似文献
29.
阐述了一些国内外对船舶压载水沉积物的处理方法及其资源化利用现状.考虑到压载水沉积物的特殊理化性质,提出了两种可用于压载水沉积物无害化处理的可行性方案,并针对处理后沉积物的性质提出了资源化利用方案. 相似文献
30.
《科学通报(英文版)》2008,(19)
The n-alkanes are extracted from NMLC-1 core that was drilled in the Nam Co, central Tibet. They are measured by using Gas Chromatography and Mass Spectrometry (GC/MS) for componential and quantitative analyses. According to the constructed depth-age model, the component and concentration of n-alkanes, together with total organic carbon (TOC), total nitrogen (TN) and carbonate are used to elu- cidate palaeoenvironmental changes of Nam Co during the past 8.4 ka. The results indicate that Holo- cene environment performs three stages in the lake area. In the stage of 8.4―6.7 kaB.P., it was warmer while precipitation slightly increased. This stage was ended by an obvious cold/dry event. During 6.7― 5.8 kaB.P., temperature increased rapidly and reached its maximum values at about 6.0 kaB.P. The environments were warm/wet optimum for the blooming of terrestrial plants and submerged aquatic plants. After that, temperature decreased continuously and showed the lowest values at about 3.0 kaB.P. From 2.9 kaB.P. to the present, temperature rose again but alternated with cold and warm. The lake area tended to be dry after 1.4 kaB.P. During 600―400 aB.P., the environmental feature was the reflection of "Little Ice Age". 相似文献