全文获取类型
收费全文 | 1529篇 |
免费 | 267篇 |
国内免费 | 415篇 |
专业分类
测绘学 | 149篇 |
大气科学 | 312篇 |
地球物理 | 418篇 |
地质学 | 771篇 |
海洋学 | 204篇 |
天文学 | 150篇 |
综合类 | 87篇 |
自然地理 | 120篇 |
出版年
2024年 | 9篇 |
2023年 | 39篇 |
2022年 | 64篇 |
2021年 | 58篇 |
2020年 | 59篇 |
2019年 | 65篇 |
2018年 | 51篇 |
2017年 | 60篇 |
2016年 | 86篇 |
2015年 | 71篇 |
2014年 | 71篇 |
2013年 | 86篇 |
2012年 | 86篇 |
2011年 | 104篇 |
2010年 | 93篇 |
2009年 | 124篇 |
2008年 | 123篇 |
2007年 | 118篇 |
2006年 | 100篇 |
2005年 | 98篇 |
2004年 | 102篇 |
2003年 | 69篇 |
2002年 | 66篇 |
2001年 | 67篇 |
2000年 | 74篇 |
1999年 | 68篇 |
1998年 | 51篇 |
1997年 | 27篇 |
1996年 | 15篇 |
1995年 | 15篇 |
1994年 | 23篇 |
1993年 | 19篇 |
1992年 | 23篇 |
1991年 | 2篇 |
1990年 | 7篇 |
1989年 | 1篇 |
1988年 | 3篇 |
1986年 | 5篇 |
1985年 | 2篇 |
1984年 | 2篇 |
1983年 | 2篇 |
1982年 | 1篇 |
1980年 | 1篇 |
1978年 | 1篇 |
排序方式: 共有2211条查询结果,搜索用时 15 毫秒
11.
I. M. Dwairi 《Environmental Geology》1998,34(4):293-296
̳4;The renewable and controlled-release fertilization system investigated here uses NH4
+-exchanged phillipsite tuff, from Jordan, to help in the dissolution of phosphate rock. Accordingly, controlled and renewable
soluble nitrogen, phosphate and Ca are released as nutrients for plants. NH4
+ phillipsite can sequester Ca ions released by the dissolution of phosphate rock, therefore, leading to further phosphate
rock dissolution. In this study the results show that the amount of phosphate released is more than that released by phosphate
rock alone. This method offers an alternative to the use of highly soluble fertilizers and may avoid environmental problems
associated with their extensive use in agriculture.
Received: 22 May 1997 · Accepted: 12 August 1997 相似文献
12.
13.
西安地铁四号线沿线地裂缝的灾害分析与对策研究 总被引:1,自引:0,他引:1
西安地裂缝是一种地区性的地质灾害现象。目前西安共发育有14条地裂缝。地铁四号线将穿越13条,给隧道施工造成了诸多考验。文章选取西安市地铁四号线沿线的地裂缝灾害作为研究对象。探讨了地裂缝对隧道工程的影响因素和致灾特点、以及相关的评估理论方法。最后针对地裂缝灾害特征以及工程特点提出若干防治措施,对于科学研究地裂缝的灾害特点、合理防治地裂缝的灾害发生具有一定的指导意义。 相似文献
14.
15.
Breakdown of hydrous ringwoodite to pyroxene and spinelloid at high P and T and oxidizing conditions
To get deeper insight into the phase relations in the end-member system Fe2SiO4 and in the system (Fe, Mg)2SiO4 experiments were performed in a multi-anvil apparatus at 7 and 13 GPa and 1,000–1,200°C as a function of oxygen fugacity.
The oxygen fugacity was varied using the solid oxygen buffer systems Fe/FeO, quartz–fayalite–magnetite, MtW and Ni/NiO. The
run products were characterized by electron microprobe, Raman- and FTIR-spectroscopy, X-ray powder diffraction and transmission
electron microscopy. At fO2 corresponding to Ni/NiO Fe-ringwoodite transforms to ferrosilite and spinelloid according to the reaction: 9 Fe2SiO4 + O2 = 6 FeSiO3 + 5 Fe2.40Si0.60O4. Refinement of site occupancies in combination with stoichiometric Fe3+ calculations show that 32% of the total Fe is incorporated as Fe3+ according to 474k70n/269_2008_281_Article_IEq1.gif" alt="$$ \left ( {{\text{Fe}}_{1.60}^{2 + } {\text{Fe}}_{0.40}^{3 + } } \right)^{\text{VI}} \left ( {{\text{Si}}_{0.60} {\text{Fe}}_{0.40}^{3 + } } \right)^{\text{IV}} {\text{O}}_{4} . $$" align="middle" border="0"> From the Rietveld refinement we identified spl as spinelloid III (isostructural with wadsleyite) and/or spinelloid V. As
we used water in excess in the experiments the run products were also analyzed for structural water incorporation. Adding
Mg to the system increases the stability field of ringwoodite to higher oxygen fugacity and the spinel structure seems to
accept higher Fe3+ but also water concentrations that may be linked. At oxygen fugacity corresponding to MtW conditions similar phase relations
in respect to the breakdown reaction in the Fe-end-member system were observed but with a strong fractionation of Fe into
spl and Mg into coexisting cpx. Thus, through this strong fractionation it is possible to stabilize very Fe-rich wadsleyite
with considerable Fe3+ concentrations even at an intermediate Fe–Mg bulk composition: assuming constant K
D independent on composition and a bulk composition of x
Fe = 0.44 this fractionation would stabilize spl with x
Fe = 0.72. Thus, spl could be a potential Fe3+ bearing phase at P–T conditions of the transition zone but because of the oxidizing conditions and the Fe-rich bulk composition
needed one would expect it more in subduction zone environments than in the transition zone in senso stricto.
相似文献
M. Koch-MüllerEmail: |
16.
C_4植物的出现与全球环境变化 总被引:17,自引:0,他引:17
C4 光合作用途径 (C4 植物 )的出现和随后的扩展 ,是发生在新生代晚期的重大事件。这一事件是晚新生代全球环境演化的产物。C4 植物在某些生态系统中占据主导地位 ,又通过食物链 ,影响了动物 ,特别是食草动物的演化。以C4 植物为主的干草原环境甚至与人类的起源有着某种成因上的联系。C4 植物的出现对中新世以来全球环境变化和现代环境格局形成过程具有特殊的意义。文中就C4 植物出现和扩展的时间、C4 植物的分布和生态特征、C4 植物出现的环境背景、构造运动 ,特别是印度和欧亚板块碰撞以及由青藏高原强烈隆升引发的侵蚀作用和大气组分变化及其与C4 植物出现的联系等问题作了较为系统的综述。文章还介绍了中国北方现代草本植物的δ13 C值的最新研究结果 ,并就草本植物δ13 C值与环境参数之间可能的关系进行了初步讨论。 相似文献
17.
The Laverton region, located in the eastern Yilgarn Craton (EYC) Western Australia, is second only to the Kalgoorlie region for gold endowment. The integration of high-density, potential-field data, regional- and camp-scale seismic reflection data, regional- and mine-scale structural analysis, and geochronologically-constrained stratigraphy, provided new insights into the 4D architecture and tectonic evolution of Laverton region. 相似文献
18.
D.?LenazEmail author H.?Skogby F.?Princivalle U.?H?lenius 《Physics and Chemistry of Minerals》2004,31(9):633-642
The influence on the structure of Fe2+ 48th/xxlarge8594.gif" alt="rarr" align="BASELINE" BORDER="0"> Mg substitution was studied in synthetic single crystals belonging to the MgCr2O4–FeCr2O4 series produced by flux growth at 900–1200 °C in controlled atmosphere. Samples were analyzed by single-crystal X-ray diffraction, electron microprobe analyses, optical absorption-, infrared- and Mössbauer spectroscopy. The Mössbauer data show that iron occurs almost exclusively as IVFe2+. Only minor Fe3+ (<0.005 apfu) was observed in samples with very low total Fe. Optical absorption spectra show that chromium with few exceptions is present as a trivalent cation at the octahedral site. Additional absorption bands attributable to Cr2+ and Cr3+ at the tetrahedral site are evident in spectra of end-member magnesiochromite and solid-solution crystals with low ferrous contents. Structural parameters a0, u and T–O increase with chromite content, while the M–O bond distance remains nearly constant, with an average value equal to 1.995(1) Å corresponding to the Cr3+ octahedral bond distance. The ideal trend between cell parameter, T–O bond length and Fe2+ content (apfu) is described by the following linear relations: a0=8.3325(5) + 0.0443(8)Fe2+ (Å) and T–O=1.9645(6) + 0.033(1)Fe2+ (Å) Consequently, Fe2+ and Mg tetrahedral bond lengths are equal to 1.998(1) Å and 1.965(1) Å, respectively. 相似文献
19.
Considering the M48;ller, Weinberg and Qadir-Sharif's definitions in general relativity, we find the momentum 4-vector of the closed universe based on the Bianchi-type metrics. The momentum 4-vector (due to matter plus fields) is found to be zero. This result supports the viewpoints of Albrow and Tryon and extends the previous works by Cooperstock–Israelit, Rosen, Johri et al., Banerjee–Sen and Vargas who investigated the problem of the energy in Friedmann–Robertson–Walker universe and Salt?-Havare who studied the problem of the energy-momentum of the viscous Kasner-type space-times. 相似文献
20.