result 2732 件
Author | Takeuchi, Makoto| |
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Published Date | 1993-12-31 |
Publication Title | 岡山医学会雑誌 |
Volume | volume105 |
Issue | issue11-12 |
Content Type | Journal Article |
Author | Mizuta, Jun| |
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Published Date | 1993-12-31 |
Publication Title | 岡山医学会雑誌 |
Volume | volume105 |
Issue | issue11-12 |
Content Type | Journal Article |
Author | Mizukawa, Nobuyoshi| Tominaga, Susumu| Kimata, Yoshihiro| Onoda, Tomoo| Sugiyama, Narushi| Yamachika, Eiki| Yamada, Yousuke| Kimura, Takuji| Takeuchi, Tetsuo| Ueno, Takaaki| Takagi, Shin| |
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Published Date | 2008-12-01 |
Publication Title | 岡山医学会雑誌 |
Volume | volume120 |
Issue | issue3 |
Content Type | Journal Article |
Author | Suehisa, Hiroshi| Toyooka, Shinichi| Hotta, Katsuyuki| Uchida, Akiko| Soh, Junichi| Fujiwara, Yoshiro| Matsuo, Keitaro| Ouchida, Mamoru| Takata, Minoru| Kiura, Katsuyuki| Date, Hiroshi| |
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Published Date | 2008-12-01 |
Publication Title | 岡山医学会雑誌 |
Volume | volume120 |
Issue | issue3 |
Content Type | Journal Article |
Author | Izumi, Ken| |
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Published Date | 1994 |
Publication Title | 岡山医学会雑誌 |
Volume | volume106 |
Issue | issue3-4 |
Content Type | Journal Article |
JaLCDOI | 10.18926/ESR/13957 |
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FullText URL | ESR_1_27.pdf |
Author | Okano, Osamu| Nishiya, Nanayo| Kagami, Hiroo| |
Abstract | Rb-Sr isotopic study as well as petrologic investigations have been done on sixteen individul chondrule samples separated from the Allegan (H5) chondrite. The Rb-Sr chondrule isochron does not define a very precise age (4.42±0.17 Ga) and 87Sr/86Sr initial ratio (0.6997±0.0014) due to the very small variation in Rb/Sr ratio for the chondrules, whereas the model ages give a much more speciffic value (4.42±0.02 Ga). These ages may probably be indicative of the time of primary process (es) (e.g. chondrule formation) rather than secondary (metamorphic reheating) or tertiary (shock heating) processes in and/or on the H-chodrite parent body (or bodies). Chemical compositions of oliveines (Fa=17.5mol%, mean deviation (MD)=1.3%) and orthopyoxenes (Fs=15.4mol%, MD=3.2%) are moderately homogenized among the chondrules, while certains chemically uneguilibrated features are also distinctly preserved in this chondrite. Homogeneity of the mineral compositions, therefore, could not have been caused by thermal metamorphism but were probably inherited from processes prior to aggregation of the components. The overall implications of the chondrule isochron and model ages in relation to the petrological features and in comparison with Rb-Sr data of other chondrites of different chemical groups and petrologic types are discussed. |
Keywords | chondrule age Rb-Sr isochron Allegan H- chondrite meteorite metamorphism olivine pyroxene |
Publication Title | Okayama University Earth Science Report |
Published Date | 1994-09-20 |
Volume | volume1 |
Issue | issue1 |
Start Page | 27 |
End Page | 36 |
ISSN | 1340-7414 |
language | English |
Copyright Holders | 岡山大学地球科学研究報告編集委員会 |
File Version | publisher |
NAID | 120002310261 |
JaLCDOI | 10.18926/ESR/13936 |
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FullText URL | ESR_3_57.pdf |
Author | Okamoto Yasuhiko| Kawahara, Akira| |
Abstract | The syntheses of kaliophilite have been carried out from the starting materials of near kalsilite compotions (KAISiO4), of which the AI2O3/SiO2 ratio is greater than 1/2. The X-ray powder deffraction pattern fit well to those of previous investigators. The crystal structure of synthetic kaliophilite was proposed by using the model consisting of four different types of kalsilite structure. The positions and intensities of the X-ray powder pattern were able to be explained on the basis of these four domains, belonging to thr twinning by merohedory. As a result of the conditions of the syntheses, it may be supposed that the violation of the AI-O-AI avoidanice rule can possibly exist along the domain boundaries. |
Keywords | kaliophilite kalsilite synthese domain boundary |
Publication Title | Okayama University Earth Science Report |
Published Date | 1996-09-20 |
Volume | volume3 |
Issue | issue1 |
Start Page | 57 |
End Page | 64 |
ISSN | 1340-7414 |
language | English |
Copyright Holders | 岡山大学地球科学研究報告編集委員会 |
File Version | publisher |
NAID | 120002310557 |
Author | Yamate, Tomoo| |
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Published Date | 1993-02-27 |
Publication Title | 岡山医学会雑誌 |
Volume | volume105 |
Issue | issue1-2 |
Content Type | Journal Article |
JaLCDOI | 10.18926/ESR/13919 |
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FullText URL | ESR_4_41.pdf |
Author | Okamoto Yasuhiko| |
Abstract | Kalsilite, a polymorph of KAISiO4 is an end member of nepheline-kalsilite series and the mineral was syn-thesized by hydorhermal methods. The synthetic kalsilite is hexagonal, P63, with a=5.151(5), c=8.690(8) A. The structure was refined by full-matrix least-squares methods to a R-value 0.084, using 373 observed reflections. The obtained structure agrees well with those of the natural and the alkali-exchanged specimens reported in the previous literatures. The oxygen atoms are disordered at two mirror-equivalent sites, constructing the domain structure. The average domain structure shows P63mc symmetry and the strctural relation between the two P63 structure corresponds to the twinning by merohedry. The domain structure was considered to be caused accompanied with the high-low inversion of the kalslite structure. Heating experiments of kalsilite reveal that the X-ray powder pattern changes at 865℃, and that cell dimensions vary discontinuously at this temperature. It was confirmed that kalsilite underwent a displacive transition like those observed in quartz or tridymite. The high-form is refered as 'high-kalsilite', and a possible simulate model is proposed. The structure of the high-kalsilite at 950℃ was refined byfull-matrix least-squares methods to a R-value 0.095, using 115 observed reflections. The high-kalsilite is also hexagonal, P63mc or P63/mmc, with a=5.288(1), c=8.628(5) A at 950℃. The structure almost prefectly coincides with that of the simulated model. Based on the interatomic distances, the distribution of silicon and aluminum atoms is found to be or-dered and the space group is determined to be P63mc. Kaliophilite and the related orthorhombic from, polymorphs of KAISiO4, were synthesized by dry method. The synthetic kaliophilite (kaliophilite-H2) is hexagonal with a=5.17(1), c=8.49(3) A, and the orthorhombic KAISiO4 (kaliophilite-O1) is orthormbic with a=9.01(1), b=15.60(2), c=8.53(4) A. Detailed examina-tion of the obtained powder patterns together with that of simulated model indicates that the kaliophilite-H2 has a disorderd structure of four types of the low-kalsilite. The structure was refined by the X-ray powder pattern-fitting method (Rietvelt method) to a R-value 0.121. |
Keywords | kalsilite kaliophilite faldspathoid systheses crystal structre |
Publication Title | Okayama University Earth Science Report |
Published Date | 1997-09-20 |
Volume | volume4 |
Issue | issue1 |
Start Page | 41 |
End Page | 72 |
ISSN | 1340-7414 |
language | English |
Copyright Holders | 岡山大学地球科学研究報告編集委員会 |
File Version | publisher |
NAID | 120002310427 |
JaLCDOI | 10.18926/ESR/13891 |
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Title Alternative | Automated observation of sea surface eddy flux on a cruising ship |
FullText URL | ESR_7_1.pdf |
Author | Takahashi, Satoshi| Tsukamoto, Osamu| Ishida, Hiroshi| Yoneyama, Kunio| |
Abstract | Sea surface eddy fluxes were evaluated with the eddy correlation method including ship motion correction for the wind vector components. Previous ship motion correction algorithm was revised as a simple scheme setting a motion sensor at the same place with the sonic anemometer. This revised eddy flux system was mounted as a routine continuous measurement system on the R/V 'Mirai' of Japan Marine Science and Technology Center. The first cruise was conducted at the tropical weatern Pacific in June 2000. Continuous sea surface fluxes were obtained and the data quality was checked with some parameters. This system is planned to be developed as a automated data processing system including ship motion correction and real-time flux evaluation system. These eddy fluxes can be integrated with the bulk fluxes and radiation fluxes to understand sea surface heat balance over the global ocean. |
Keywords | Sea surface fliux Automated observation Eddy correlation method |
Publication Title | Okayama University Earth Science Report |
Published Date | 2000-09-20 |
Volume | volume7 |
Issue | issue1 |
Start Page | 1 |
End Page | 14 |
ISSN | 1340-7414 |
language | Japanese |
Copyright Holders | 岡山大学地球科学研究報告編集委員会 |
File Version | publisher |
NAID | 120002310644 |
Author | Kimura, Yasuhiro| |
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Published Date | 1994-12 |
Publication Title | 岡山医学会雑誌 |
Volume | volume106 |
Issue | issue11-12 |
Content Type | Journal Article |
Author | Miyashita, Katuhiro| |
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Published Date | 1993-08 |
Publication Title | 岡山医学会雑誌 |
Volume | volume105 |
Issue | issue7-8 |
Content Type | Journal Article |
Author | Miyashita, Katuhiro| |
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Published Date | 1993-08 |
Publication Title | 岡山医学会雑誌 |
Volume | volume105 |
Issue | issue7-8 |
Content Type | Journal Article |
Author | Ishioka, Kazunari| |
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Published Date | 1994-12 |
Publication Title | 岡山医学会雑誌 |
Volume | volume106 |
Issue | issue11-12 |
Content Type | Journal Article |
Author | Hidaka, Hidekuni| |
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Published Date | 1994-10 |
Publication Title | 岡山医学会雑誌 |
Volume | volume106 |
Issue | issue9-10 |
Content Type | Journal Article |
Author | Furusho, Yoshiaki| Makita, Nobuaki| Ono, Masato| Ishiyama, Takashi| Takahashi, Motoyuki| Motomizu, Shoji| |
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Published Date | 2008-01-29 |
Publication Title | 分析化学 |
Volume | volume56 |
Issue | issue12 |
Content Type | Journal Article |
Author | Sei, Tetsurou| |
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Published Date | 1994-02 |
Publication Title | 岡山医学会雑誌 |
Volume | volume106 |
Issue | issue1-2 |
Content Type | Journal Article |
Author | Sakurai, Masaru| |
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Published Date | 1994-10 |
Publication Title | 岡山医学会雑誌 |
Volume | volume106 |
Issue | issue9-10 |
Content Type | Journal Article |
Author | Uchida, Shinji| |
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Published Date | 1993-08 |
Publication Title | 岡山医学会雑誌 |
Volume | volume105 |
Issue | issue7-8 |
Content Type | Journal Article |
Author | Kimura, Kazuhi| |
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Published Date | 1994-10 |
Publication Title | 岡山医学会雑誌 |
Volume | volume106 |
Issue | issue9-10 |
Content Type | Journal Article |