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排序方式: 共有61条查询结果,搜索用时 15 毫秒
31.
自1949 年新中国建立以后,在中国各地相继发现中新世早期以来的远古人类化石,使之有可能逐渐阐明亚洲人类的演化过程,笔者根据各化石的特征考察它们的系统,根据各时期的古环境及古气候情况推断它们的演化途径,把在欧洲出现的古类人猿 Alsaticopithecus 当成发现种,非洲系人类在非洲及欧洲或亚洲中部完成了演化。同时,把在缅甸出现的古类人猿 Amphipithecus 或 Pondaungia 当成发源种,亚洲系人类在亚洲东南部完成了演化。在此期间,在非洲及欧洲或亚洲中部的巴基斯坦出现的西瓦古猿及腊玛 相似文献
32.
Coronal holes (CHs) are regions of open magnetic field lines in the solar corona and the source of the fast solar wind. Understanding the evolution of coronal holes is critical for solar magnetism as well as for accurate space weather forecasts. We study the extreme ultraviolet (EUV) synoptic maps at three wavelengths (195 Å/193 Å, 171 Å and 304 Å) measured by the Solar and Heliospheric Observatory/Extreme Ultraviolet Imaging Telescope (SOHO/EIT) and the Solar Dynamics Observatory/Atmospheric Imaging Assembly (SDO/AIA) instruments. The two datasets are first homogenized by scaling the SDO/AIA data to the SOHO/EIT level by means of histogram equalization. We then develop a novel automated method to identify CHs from these homogenized maps by determining the intensity threshold of CH regions separately for each synoptic map. This is done by identifying the best location and size of an image segment, which optimally contains portions of coronal holes and the surrounding quiet Sun allowing us to detect the momentary intensity threshold. Our method is thus able to adjust itself to the changing scale size of coronal holes and to temporally varying intensities. To make full use of the information in the three wavelengths we construct a composite CH distribution, which is more robust than distributions based on one wavelength. Using the composite CH dataset we discuss the temporal evolution of CHs during the Solar Cycles 23 and 24. 相似文献
33.
Miki S Ikeda K Oba Y Satone H Honda M Shimasaki Y Onikura N Arakawa O Oshima Y 《Marine pollution bulletin》2011,62(11):2533-2536
We investigated levels of the pollutant tributyltin (TBT) in blood of pufferfishes (six species), Japanese sea perch, red sea bream, Japanese common goby, Japanese flounder, rockfish, conger eel, and sea mullet collected off the coast of northern Kyushu, Japan. We found considerable levels of TBT (1.4-190 ng/mL) accumulated in the blood of these fish. Blood TBT concentrations were 1.3-22.5 times liver concentrations and 4.9-78 times muscle concentrations, except in conger eel and mullet. We detected TBT (16-111 ng/mL-blood) in the plasma of the fine-patterned puffer (Takifugupoecilonotus) year-round, without any apparent seasonal trend. These results suggest that fish inhabiting coastal areas of Kyushu, Japan, continue to be contaminated with TBT. 相似文献
34.
Isobe T Oshihoi T Hamada H Nakayama K Yamada TK Tajima Y Amano M Tanabe S 《Marine pollution bulletin》2011,63(5-12):564-571
Contamination status of brominated flame retardants (BFRs) and persistent organic pollutants (POPs) in blubber of finless porpoises (Neophocaena phocaenoides) stranded along the coasts of Seto Inland Sea and Omura Bay in Japan were investigated. Levels of PCBs, DDTs and CHLs were significantly higher than those of HCHs, HCB, PBDEs and HBCDs. Concentrations of PBDEs and HBCDs, as well as organochlorine compounds in males increased with body length (p<0.05). Among 14 PBDE congeners analyzed, BDE-47 was the predominant, which is similar to those generally reported in biota. PBDEs, HBCDs and PCBs showed no obvious temporal trend in concentrations during the study period, suggesting continuous environmental release of these chemicals. On the other hand, levels of DDT, CHLs and HCHs have decreased. Concentrations of PCBs in liver trematode infected individuals were significantly higher than those in not infected individuals, implying there could be a relationship between contaminant levels and parasitic infection. 相似文献
35.
Shigeto Hirai Yohei Kojima Hiroaki Ohfuji Norimasa Nishiyama Tetsuo Irifune Stephan Klemme Geoffrey Bromiley J. Paul Attfield 《Physics and Chemistry of Minerals》2011,38(8):631-637
Raman spectroscopy and heat capacity measurements have been used to study the post-perovskite phase of CaIr0.5Pt0.5O3, recovered from synthesis at a pressure of 15 GPa. Laser heating CaIr0.5Pt0.5O3 to 1,900 K at 60 GPa produces a new perovskite phase which is not recoverable and reverts to the post-perovskite polymorph
between 20 and 9 GPa on decompression. This implies that Pt-rich CaIr1−xPtxO3 perovskites including the end member CaPtO3 cannot easily be recovered to ambient pressure from high P–T synthesis. We estimate an increase in the thermodynamic Grüneisen
parameter across the post-perovskite to perovskite transition of 34%, of similar magnitude to those for (Mg,Fe)SiO3 and MgGeO3, suggesting that CaIr0.5Pt0.5O3 is a promising analogue for experimental studies of the competition in energetics between perovskite and post-perovskite
phases of magnesium silicates in Earth’s lowermost mantle. Low-temperature heat capacity measurements show that CaIrO3 has a significant Sommerfeld coefficient of 11.7 mJ/mol K2 and an entropy change of only 1.1% of Rln2 at the 108 K Curie transition, consistent with the near-itinerant electron magnetism. Heat capacity results for post-perovskite
CaIr0.5Rh0.5O3 are also reported. 相似文献
36.
Significance of an amorphous SiO2 phase in a pseudomorph after coesite enclosed in garnet from ultrahigh‐pressure eclogite,Su–Lu Belt,eastern China 下载免费PDF全文
Tomoki Taguchi Akira Miyake Masaki Enami Yohei Igami 《Journal of Metamorphic Geology》2018,36(7):843-854
Here, we report the first discovery of an amorphous SiO2 phase (APSI phase) in a pseudomorph after coesite included in garnet from an ultrahigh‐pressure (UHP) eclogite from the Su–Lu metamorphic belt, eastern China. Using transmission electron microscopy, Raman spectroscopy and selected area electron diffraction, we show that the internal structure of the pseudomorph consists of an APSI phase with nano/submicrocrystalline particles of quartz and a polycrystalline K‐bearing fibrous sheet‐silicate phase (KFSS phase). The APSI phase‐bearing aggregates included in the garnet might have formed by reactions involving a supercritical fluid during exhumation by the following processes: (1) the development of radial cracks within the host garnet by the phase transition of coesite to quartz; (2) the decomposition of a part of the pseudomorph following infiltration of supercritical fluid; (3) the precipitation of the KFSS phase from the fluid phase during subsequent exhumation and cooling, which was likely promoted by a change in the metamorphic fluid from supercritical and/or subcritical to aqueous fluid; and (4) the rapid precipitation of the APSI phase under a metastable (non‐equilibrium) state, such as quenching, during a later stage of the exhumation. Whether the APSI phase generally formed during exhumation and survived widely throughout the Su‐Lu terrane is unknown. However, the presence of the APSI phase in a UHP eclogite provides new insight into the geodynamic phenomena occurring at continental collision zones. 相似文献
37.
Lewis C. Roberts Jr. Doyle T. Hall John V. Lambert John L. Africano Keith T. Knox Jacob K. Barros Kris M. Hamada Dennis Liang Paul F. Sydney Paul W. Kervin 《Icarus》2007,192(2):469-474
In August 2002, the near-Earth Asteroid 2002 NY40, made its closest approach to the Earth. This provided an opportunity to study a near-Earth asteroid with a variety of instruments. Several of the telescopes at the Maui Space Surveillance System were trained at the asteroid and collected adaptive optics images, photometry and spectroscopy. Analysis of the imagery reveals the asteroid is triangular shaped with significant self-shadowing. The photometry reveals a 20-h period and the spectroscopy shows that the asteroid is a Q-type. 相似文献
38.
Osamu Abe Atsushi Watanabe V. V. S. S. Sarma Yohei Matsui Hiroya Yamano Naohiro Yoshida Toshiro Saino 《Journal of Oceanography》2010,66(3):363-372
We estimated gas exchange rates in Kabira Reef at Ishigaki Island, southwest Japan, using a mass balance calculation with
dual “biological” tracers: dissolved inorganic carbon (DIC) and dissolved oxygen (DO). The nighttime results allowed us to
obtain reasonable gas transfer velocity k
w values, all of which exceeded those obtained in wind-dominant studies. The difference is likely due to the contribution of
turbulence generated by the interaction between the current and bottom topography. The k
w obtained during high tides is consistent with that reported by Raymond and Cole (2001), whereas k
w during low tides is significantly higher, which seems to be caused by enhanced friction with the bottom of the reef and/or
bubble-induced gas transfer by wave breaking at the reef crest. 相似文献
39.
The frequency characteristics of near-surface sediments obtained from small scale S-wave refraction measurements conducted at two sites in the Garf Hussein area, contiguous to the High Dam Lake, South of Aswan, have shown drastic changes in the frequency-selective amplification of horizontal ground motion within a relatively short surface distance. This effect is attributed mainly to such factors as the variation in layer thickness and the presence or absence of soft alluvial deposits.These results indicate that movements initiated deep in the earth's crust may not be faithfully reflected on the ground surface. As geodetic work principally involves monitoring relative horizontal and vertical displacements on the earth's surface with time, geodesists are advised to take the spectral response of the ground into consideration. 相似文献
40.
Morihisa Hamada Didier Laporte Nicolas Cluzel Kenneth T. Koga Tatsuhiko Kawamoto 《Bulletin of Volcanology》2010,72(6):735-746
Decompression experiments of a crystal-free rhyolitic liquid with ≈ 6.6 wt. % H2O were carried out at a pressure range from 250 MPa to 30–75 MPa in order to characterize effects of magma ascent rate and
temperature on bubble nucleation kinetics, especially on the bubble number density (BND, the number of bubbles produced per
unit volume of liquid). A first series of experiments at 800°C and fast decompression rates (10–90 MPa/s) produced huge BNDs
(≈ 2 × 1014 m−3 at 10 MPa/s ; ≈ 2 × 1015 m−3 at 90 MPa/s), comparable to those in natural silicic pumices from Plinian eruptions (1015–1016 m−3). A second series of experiments at 700°C and 1 MPa/s produced BNDs (≈ 9×1012 m−3) close to those observed at 800°C and 1 MPa/s (≈ 6 × 1012 m−3), showing that temperature has an insignificant effect on BNDs at a given decompression rate. Our study strengthens the theory
that the BNDs are good markers of the decompression rate of magmas in volcanic conduits, irrespective of temperature. Huge
number densities of small bubbles in natural silicic pumices from Plinian eruptions imply that a major nucleation event occurs
just below the fragmentation level, at which the decompression rate of ascending magmas is a maximum (≥ 1 MPa/s). 相似文献