全文获取类型
收费全文 | 10820篇 |
免费 | 2057篇 |
国内免费 | 2917篇 |
专业分类
测绘学 | 1165篇 |
大气科学 | 1831篇 |
地球物理 | 2594篇 |
地质学 | 5697篇 |
海洋学 | 1634篇 |
天文学 | 319篇 |
综合类 | 1029篇 |
自然地理 | 1525篇 |
出版年
2024年 | 80篇 |
2023年 | 260篇 |
2022年 | 571篇 |
2021年 | 697篇 |
2020年 | 508篇 |
2019年 | 638篇 |
2018年 | 610篇 |
2017年 | 638篇 |
2016年 | 712篇 |
2015年 | 624篇 |
2014年 | 715篇 |
2013年 | 749篇 |
2012年 | 763篇 |
2011年 | 780篇 |
2010年 | 854篇 |
2009年 | 702篇 |
2008年 | 699篇 |
2007年 | 646篇 |
2006年 | 527篇 |
2005年 | 410篇 |
2004年 | 344篇 |
2003年 | 294篇 |
2002年 | 295篇 |
2001年 | 299篇 |
2000年 | 253篇 |
1999年 | 341篇 |
1998年 | 243篇 |
1997年 | 266篇 |
1996年 | 185篇 |
1995年 | 199篇 |
1994年 | 163篇 |
1993年 | 165篇 |
1992年 | 133篇 |
1991年 | 89篇 |
1990年 | 52篇 |
1989年 | 59篇 |
1988年 | 62篇 |
1987年 | 35篇 |
1986年 | 31篇 |
1985年 | 18篇 |
1984年 | 15篇 |
1983年 | 11篇 |
1982年 | 13篇 |
1981年 | 12篇 |
1980年 | 16篇 |
1979年 | 5篇 |
1977年 | 1篇 |
1976年 | 2篇 |
1958年 | 5篇 |
1954年 | 4篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
991.
AMR Simulations of Magnetohydrodynamic Problems by the CESE Method in Curvilinear Coordinates 总被引:1,自引:0,他引:1
The objective of this paper is to present new extensions of the space – time conservation element and solution element (CESE)
method for simulations of magnetohydrodynamic (MHD) problems in general curvilinear coordinates by using an adaptive mesh
refinement (AMR) grid system. By transforming the governing MHD equations from the physical space (x,y,z) to the computational space (ξ,η,ζ) while retaining the form of conservation, the CESE method is established for MHD in the curvilinear coordinates. Utilizing
the parallel AMR package PARAMESH, we present the first implementation of applying the AMR CESE method for MHD (AMR-CESE-MHD)
in both Cartesian and curvilinear coordinates. To show the validity and capabilities of the AMR-CESE-MHD code, a suite of
numerical tests in two and three dimensions including ideal MHD and resistive MHD are carried out, with two of them in both
Cartesian and curvilinear coordinates. Numerical tests show that our results are highly consistent with those obtained previously
by other authors, and the results under both coordinate systems confirm each other very well. 相似文献
992.
The EGRET observations have confirmed and proposed the new isotropically distributed γ-ray background, but the known objects radiating γ-rays can not supply so much radiation. Meanwhile, EGRET also reveals a population of γ-ray sources with no radio counterparts which are isotropically distributed in the sky, indicating their possible cosmological origins. Wang et al.[13] proposed a new γ-ray radiation process driven by the radiation feedback of AGNs. The energy of the radiation peaks around 1 GeV—0.1 TeV with the typical luminosity of 1042—1043 ergs · s?1. This kind of radiation process in the radio quiet quasars make them the potential γ-ray radiation sources as well as the contributors to the γ-ray background. We consider two cases in which the seed photons in the inverse-Compton processes are from the accretion disks of quasars and cosmic microwave background (CMB), respectively. We find that the former contributes 78%—92% of the background radiation around 1 GeV, while the contribution from the latter is negligible. The radio quiet quasars are highly likely to become the objects which contribute the most energy to the γ-ray background around 1 GeV. 相似文献
993.
应用本实验室建立的趋化模型对海水鱼类寄生虫刺激隐核虫(Cryptocaryon irritans)的趋化特性进行研究。结果显示, 刺激隐核虫幼虫在30min时趋化达到饱和, 在温度28℃时趋化率达到最高; 多种硬骨鱼的血清与粘液对刺激隐核虫的幼虫都有着强烈的吸引作用, 刺激隐核虫幼虫对碳水化合物、氨基酸等小分子物质没有趋化作用; 在组织匀浆液中, 刺激隐核虫幼虫对肌肉匀浆液有一定的趋化作用, 对肝、肠、胃的匀浆液都没有趋化作用; 感染后鱼类血清对刺激隐核虫的幼虫有着更加强烈的吸引作用(P<0.01); 18种中草药中的五倍子、大黄、槟榔、苦楝、虎杖、贯众等6种中药草对刺激隐核虫的幼虫有一定的驱虫作用。本文的研究结果有助于深化对刺激隐核虫致病性的认识并对“白点病”的防治有一定的参考价值。 相似文献
994.
995.
粘土防渗层是垃圾填埋设施中直接接触渗沥液的防渗层,防渗层有效地阻隔了垃圾渗沥液下渗,减少了渗沥液对环境的污染.以成都粘土为研究对象,采用高压固结试验研究粘土防渗层在不同浸润时间、不同pH渗沥液浸润下对粘土层固结参数的影响.结果表明:浸润时间和渗沥液pH对粘土固结参数的影响较大.随着浸润时间的增加,渗沥液pH值对土的压缩... 相似文献
996.
Zhang L Ye X Feng H Jing Y Ouyang T Yu X Liang R Gao C Chen W 《Marine pollution bulletin》2007,54(7):974-982
Concentrations of selected heavy metals (Cu, Pb, Zn, Cd, Cr, Ni and Fe) in surface sediments from nine sites in western Xiamen Bay and its vicinity were studied in order to understand current metal contamination due to urbanization and economic development in Xiamen, China. The sediment samples were collected in December 2004 and July 2005 respectively in order to examine temporal variations. In this study, we found that heavy metal concentrations in surface sediments sampled in the western Xiamen Bay and adjacent Maluan Bay and Yuandang Lagoon varied from 19 to 97mg kg(-1) for Cu, 45 to 60mg kg(-1) for Pb, 65 to 223mg kg(-1) for Zn, 0.11 to 1.01mg kg(-1) for Cd, 37 to 134mg kg(-1) for Cr, 25 to 65mg kg(-1) for Ni and 3.08 to 4.81% for Fe. Although all metal concentrations in sediments meets Chinese National Standard Criteria for Marine Sediment Quality, both metal enrichment factors (EF) and geoaccumulation index (I(geo)) show that Pb contamination exists in the entire study area and contamination of other metals are also present in some locations depending on the sources, of which sewage outlets and commercial ports are the main sources of contaminants to the area. This study shows that using the sediment quality standard criteria only to assess sediments cannot properly reflect sediment contamination. A multiple approaches should be applied for the sediment quality assessment. 相似文献
997.
Weihua Wu Shijin Xu Jiedong Yang Hongwei Yin Huayu Lu Kaijun Zhang 《Chemical Geology》2010,269(3-4):406-413
We systematically collected 40 modern clastic sediment samples from rivers in different tectonic units of the Tibetan Plateau and measured their Sr–Nd isotopic compositions. The isotopic characteristics provide insight into the controversial paleo-tectonic affinity of terranes of the Tibetan Plateau and the provenance of Songpan–Ganzi flysch complex. The Qilian Terrane and Himalaya Terrane have more negative εNd(0) values (from ? 14.3 to ? 11.8 and from ? 20.64 to ? 13.26, respectively) and high 87Sr/86Sr values (from 0.719674 to 0.738818 and from 0.721020 to 0.824959, respectively), reflecting old and mature continental crust origin of these two terranes. The southern Lhasa Terrane is more radiogenic in εNd(0) values (from ? 8.82 to ? 3.8) and low in 87Sr/86Sr values (from 0.711504 to 0.719489), implying the combined impact of the Neo-Tethys mantle and Himalaya old continental crust. Sr–Nd isotopic compositions of the Qilian Terrane are similar to those in the Yangtze Craton, indicating that the Qilian Terrane was probably separated from the Yangtze Craton. Sr–Nd isotopic characteristics of the Songpan–Ganzi Terrane are similar to the Yangtze Craton and are remarkably different to those in the North China Craton, eastern Kunlun–Qaidam and the central Qiangtang metamorphic belt, implying that the widely distributed flysch complex of the Songpan–Ganzi Terrane was sourced from the Yangtze Craton. 相似文献
998.
Zhaosheng Qian Hui Feng Wenjing Yang Yingjie Wang 《Geochimica et cosmochimica acta》2010,74(4):1230-1032
In this paper, the structure of the Al30O8(OH)56(H2O)2618+(Al30) polyoxocation in aqueous solution is investigated, including an exploration of its water-exchange reaction using a supramolecular model. Thirty-one solvent water molecules were explicitly included in the supramolecular model to approximate the influence of the solvent. The calculated results indicated that both the gas-phase and the supramolecular models could correctly reproduce the structure of the Al30 polyoxocation, but the supramolecular model described the structure more accurately. Using the supramolecular model, we calculated the 27Al NMR chemical shifts of various aluminum atoms using HF and GIAO methods, and they compared well to the chemical shifts determined experimentally. The water-exchange reaction of the Al30 polyoxocation could not be simulated with the gas phase model because of a proton-transfer reaction that is induced by the highly positive charge of the Al30 polyoxocation. However, the inclusion of an explicit second solvation sphere lowered the acidity of the coordinated water molecules and allowed simulation of the water exchange reaction. 相似文献
999.
T.S. Peretyazhko J.M. Zachara D.W. Kennedy J.K. Fredrickson B.W. Arey J.P. McKinley C.M. Wang A.C. Dohnalkova Y. Xia 《Geochimica et cosmochimica acta》2010,74(13):3751-60
The reductive biotransformation of 6-line ferrihydrite located within porous silica (intragrain ferrihydrite) by Shewanella oneidensis MR-1 was investigated and compared to the behavior of 6-line ferrihydrite in suspension (free ferrihydrite). The effect of buffer type (PIPES and NaHCO3), phosphate (P), and an electron shuttle (AQDS) on the extent of reduction and formation of Fe(II) secondary phases was investigated under anoxic conditions. Electron microscopy and micro X-ray diffraction were applied to evaluate the morphology and mineralogy of the biogenic precipitates and to study the distribution of microorganisms on the surface of porous silica after bioreduction. Kinetic reduction experiments with free and intragrain ferrihydrite revealed contrasting behavior with respect to the buffer and presence of P. The overall amount of intragrain ferrihydrite reduction was less than that of free ferrihydrite [at 5 mmol L−1 Fe(III)T]. Reductive mineralization was not observed in the intragrain ferrihydrite incubations without P, and all biogenic Fe(II) concentrated in the aqueous phase. Irrespective of buffer and AQDS addition, rosettes of Fe(II) phosphate of approximate 20-30 μm size were observed on porous silica when P was present. The rosettes grew not only on the silica surface but also within it, forming a coherent spherical structure. These precipitates were well colonized by microorganisms and contained extracellular materials at the end of incubation. Microbial extracellular polymeric substances may have adsorbed Fe(II) promoting Fe(II) phosphate nucleation with subsequent crystal growth proceeding in different directions from a common center. 相似文献
1000.
西太平洋深海沉积物古菌多样性垂直分布 总被引:3,自引:2,他引:1
以提取并纯化的西太平洋深海沉积物DNA为模板,利用古菌PCR特异性引物扩增出样品中古菌的16S rDNA片段,构建其克隆文库,建立阳性克隆子RFLP(Restriction Fragment Length Polymor-phism)酶切图谱。据酶切图谱对所获得的120个克隆进行测序,并与数据库中的序列进行比对,从而进行古菌的多样性和系统发育分析。结果表明,沉积物中扩增的16S rDNA古菌序列分别来自泉古生菌(Crenarchaeota)和广古生菌(Euryarchaeota),以Marine Benthic Group B(11.8%)、Marine Benthic Group D(13.6%)、Marine Crenarchaeotic Group(68.69%)为主。少量序列为South African Gold Mine Euryarchaeotic Group(1.07%)、Deep-Sea Hydrothermal Vent Euryarchaeotic Group(1.61%)、UIIB(1.25%)、VALIII(1.79%)、Marine Benthic Group E(0.18%)。以上结果表明西太平洋深海沉积物中有丰富多样的古菌群落。 相似文献