全文获取类型
收费全文 | 112篇 |
免费 | 2篇 |
国内免费 | 1篇 |
专业分类
大气科学 | 2篇 |
地球物理 | 21篇 |
地质学 | 53篇 |
海洋学 | 11篇 |
天文学 | 26篇 |
自然地理 | 2篇 |
出版年
2019年 | 1篇 |
2018年 | 2篇 |
2017年 | 3篇 |
2016年 | 2篇 |
2015年 | 2篇 |
2014年 | 9篇 |
2013年 | 5篇 |
2012年 | 1篇 |
2011年 | 7篇 |
2010年 | 9篇 |
2009年 | 8篇 |
2008年 | 3篇 |
2007年 | 6篇 |
2006年 | 2篇 |
2005年 | 5篇 |
2004年 | 4篇 |
2003年 | 2篇 |
2002年 | 2篇 |
2001年 | 3篇 |
2000年 | 8篇 |
1999年 | 5篇 |
1998年 | 3篇 |
1997年 | 3篇 |
1995年 | 3篇 |
1989年 | 2篇 |
1984年 | 3篇 |
1983年 | 3篇 |
1982年 | 1篇 |
1981年 | 2篇 |
1976年 | 1篇 |
1975年 | 2篇 |
1972年 | 1篇 |
1970年 | 1篇 |
1963年 | 1篇 |
排序方式: 共有115条查询结果,搜索用时 15 毫秒
111.
Takeshi Sakai Eiji Ohtani Hidenori Terasaki Masaaki Miyahara Masahiko Nishijima Naohisa Hirao Yasuo Ohishi Nagayoshi Sata 《Physics and Chemistry of Minerals》2010,37(7):487-496
Fe–Mg partitioning between post-perovskite and ferropericlase has been studied using a laser-heated diamond anvil cell at
pressures up to 154 GPa and 2,010 K which corresponds to the conditions in the lowermost mantle. The composition of the phases
in the recovered samples was determined using analytical transmission electron microscopy. Our results reveal that the Fe–Mg
partition coefficient between post-perovskite and ferropericlase (K
DPPv/Fp) increases with decreasing bulk iron content. The compositional dependence of K
DPPv/Fp on the bulk iron content explains the inconsistency in previous studies, and the effect of the bulk iron content is the most
dominant factor compared to other factors, such as temperature and aluminum content. Iron prefers ferropericlase compared
to post-perovskite over a wide compositional range, whereas the iron content of post-perovskite (X
FePPv, the mole fraction) does not exceed a value of 0.10. The iron-rich ferropericlase phase may have significant influence on
the physical properties, such as the seismic velocity and electrical conductivity at the core–mantle boundary region. 相似文献
112.
The density of liquid Fe–S was measured at 4 GPa and 1,923 K using a sink/float method with a composite density marker. The
density marker consisted of a Pt rod core and an Al2O3 tube surrounding. The uncertainty in the density of the composite marker is much smaller than that of the composite sphere,
which had been used in previous density measurements. The density of liquid Fe–S decreases nonlinearly with increasing sulfur
content at 4 GPa and 1,923 K. This tendency is consistent with the results measured at ambient pressure. The molar volume
of FeS calculated from the measured density gradually increases with sulfur content. The excess molar volume from ideal mixing
of Fe and S at 4 GPa was negative value. The new method proposed here is applicable to the density measurement of other Fe
alloys at high pressure. The tendency of the molar volume and the excess molar volume with sulfur content at ambient pressure
is consistent with these at high pressure at least up to 4 GPa. The excess molar volume at high pressure is essential for
estimating the amount of light elements in the outer core. 相似文献
113.
Eiji Ohtani Naohisa Hirao Tadashi Kondo Masayoshi Ito Takumi Kikegawa 《Physics and Chemistry of Minerals》2005,32(1):77-82
We observed a direct reaction of metallic iron with water to form iron hydride and iron oxide, 3Fe + H2O–>2FeHx + FeO, at pressures from 6 GPa to 84 GPa and temperatures above 1,000 K in diamond anvil cell (DAC). Iron hydride is dhcpFeHx or -FeHx, and iron oxide has the rhombohedral or B1 structure at pressures at least up to 37 GPa. The formation of an assembly composed of dhcpFeHx and FeO with the B8 structure was observed at 84 GPa. In primordial Earth, water formed by dehydration of the low temperature primitive materials reacts with metallic iron in the high temperature component to form iron hydride FeHx and iron oxide FeO. The former would be incorporated in the iron forming the core. Thus hydrogen could be an important element of the Earths core. This reaction would be essential for transport of hydrogen into the core in the accretion stage of the Earth. 相似文献
114.
The existence of escape and nonescape orbits arbitrarily close to the homothetic equilateral triplecollision orbit is considered analytically in the threebody problem with zero initial velocities and equal masses. It is proved that escape orbits in the initial condition space are distributed around three kinds of isosceles orbits. It is also proved that nonescape orbits are distributed in between the escape orbits where different particles escape. In order to show this, it is proved that the homotheticequilateral orbit is isolated from other triplecollision orbits as far as the collision at the first triple encounter is concerned. Moreover, the escape criterion is formulated in the planarisosceles problem and translated into the words of regularizing variables. The result obtained by us explains the orbital structure numerically. 相似文献
115.
Effect of winter meteorological conditions on the formation of the cold bottom water in the eastern Bering Sea shelf 总被引:2,自引:0,他引:2
The cold bottom water, formed in the previous winter on the eastern Bering Sea shelf, remains throughout the summer. in order to examine the mechanism for the formation of the cold bottom water, we used minimum water temperature in the cold bottom water observed over the eastern Bering Sea shelf for 30 years. The interannual variation in the minimum water temperature of the cold bottom water was closely related to that of mean air temperature during cooling period at St. Paul Island. The air temperature in previous winter primarily affects the cold bottom water. We estimated decrement of the water temperature due to ice melting with simple box model. It was found with the box model that decreasing of the water temperature and lowering of the salinity depend on ice melting. To investigate the cause of interannual variation in air temperature in winter, we applied EOF analysis to the 500 hPa height. The Pacific/North American pattern (PNA) was related to mean air temperature at St. Paul Island in cooling season and the cold bottom water temperature. These results suggest the connection between ENSO events and warming or cooling in the Bering Sea shelf in winter. 相似文献