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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：Springer Science and Business Media LLC  

To evaluate terahertz time-domain spectroscopy (THz-TDS) as a promising tool for discriminating pharmaceutical tablets, THz-TDS has been applied for discrimination between pharmaceutical tablets with sound-alike names. Two sets of medicine tablets with sound-alike names, that is, Amaryl and Almarl, Zyloric and Zantac, are examined in this study. Based on the difference in THz absorption spectra, we have succeeded in distinguishing between sound-alike medicine tablets clearly for each set. The results in this study suggest that THz-TDS is a useful tool that is indispensable for medical security maintenance, such as a non-destructive way to prevent mix-up of medicine. © 2013 Springer Science+Business Media New York.

DOI： 10.1007/s10762-013-9994-2

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その他リンク： http://link.springer.com/article/10.1007/s10762-013-9994-2/fulltext.html

担当区分：筆頭著者   記述言語：日本語  

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記述言語：日本語   出版者・発行元：岡山大学理学部地球科学教室  

Ordinary Kriging, OK, and Regression Kriging, RK, are the spatial statistical methods that are possible toestimate a horizontal distribution in a study area from discrete data. OK is the method which takes account ofonly spatial auto-correlation structure of the data, while RK is the method which takes account of an interrelationshipbetween spatial auto-correlation structure and some auxiliary variables to minimize the estimation error.Analytical processing for OK and RK methods was performed by the R-Language (R Core Team, 2012)and its some additional libraries. The auxiliary variables required to perform RK method were prepared by aGIS application, Quantum GIS (Quantum GIS Development Team, 2012). The 3-dimensional geographic representationof the estimation maps was performed by the Google Earth (Google, 2012).In this report, OK and RK methods were applied to one of the Earth scientific information, SPM (SupendedParticulate Matter). Then, these methods were considered by comparing two estimation maps, and finallyconsidered qualitatively by displaying these maps in the Google Earth.

DOI： 10.18926/ESR/49210

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担当区分：筆頭著者   記述言語：日本語  

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記述言語：日本語  

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：JAPAN SOC ANALYTICAL CHEMISTRY  

The absorption spectra of three kinds of medicines both before and after the expiration date: Amlodin OD (R) (5 mg), Basen OD (R) (0.2 mg) and Gaster D (R) (10 mg) have been measured by terahertz time domain spectroscopy (THz-TDS). All the medicines show some differences in the THz absorption spectra between medicines before and after the expiration dates. X-Ray powder diffraction (XRD) studies of all medicines suggest that the polymorph of the main effective compound is not changed before and after the expiration date. Therefore, the differences in the THz spectra between medicines before and after the expiration dates arise from aging variation of diluting agents and/or from modifications of intermolecular interaction between the effective compounds and diluting agents.

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記述言語：日本語   出版者・発行元：日本アイソトープ協会  

DOI： 10.3769/radioisotopes.60.461

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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記述言語：英語   掲載種別：研究論文（学術雑誌）  

DOI： 10.2465/jmps.061130

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記述言語：英語   掲載種別：研究論文（学術雑誌）  

DOI： 10.2113/gscanmin.45.2.307

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出版者・発行元：一般社団法人 日本鉱物科学会  

岡山県高梁市備中町布賀の布賀鉱山からborcarite Cuが置換体を見出したので，その産状および鉱物学的性質について報告する．BorcariteのCu置換体は結晶質石灰岩を切るpentahydroborite，nifontoviteのレンズ中に3 mm以下の粒状結晶をなして産出した．この結晶の外側は無色でborcarite，内側はエメラルドグリーンを呈しborcariteのCu置換体である．本鉱物は無から淡緑色のborcarite中に細脈をなしていることもある．共存鉱物はborcarite，nifontovite，calcite，bultfonteiniteである．肉眼的にはエメラルドグリーン_から_無色透明でガラス光沢を示す．鏡下では無色透明で，多色性はみられない．二方向に完全な劈開が認められる．密度は2.96(2) g cm-3(meas)，2.96 g cm-3(calc)．ビッカース硬度は376 (290-464) kg mm-2(25 g荷重)，モース硬度は4.5．光学的には二軸性負，屈折率α＝1.618，β＝1.658，γ＝1.672，2VX(calc)＝60°．WDSおよびTGAによって得られた分析値は，CaO 38.26，CuO 11.51，MgO 0.59，ZnO 0.09，B2O3 24.27，CO2 15.33，H2O 9.28，total 99.33 wt%で，O＝18とした実験式はCa3.965(Cu0.841Mg0.085Zn0.006)？0.932 B4.040O5.941(OH)5.987(CO3)2.024．単結晶を用いて四軸自動回折計で測定した結果は，単斜晶系，ラウエ群C2/m．粉末X線回折値から計算した格子定数は，a＝17.794(2)，b＝8.381(1)，c＝4.4494(7)Å，β＝102.42(2)°．IRでは3540，3260 cm-1にO-H，1410，870，290 cm-1に炭酸基，1450，390 cm-1にホウ酸基による吸収がそれぞれ認められた．TG-DTAでは484 °CにH2Oの放出による重量減少を伴う吸熱ピーク，682 °CにCO2の放出による重量減少を伴う吸熱ピークがそれぞれ認められた．これらの結晶学的データ，赤外吸収スペクトルおよびTG-DTAはborcariteと類似している．

DOI： 10.14824/kobutsu.2005.0.118.0

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：JAPAN ASSOC MINERALOGICAL SCIENCES  

Inyoite was found as fissure fillings in calcium borate minerals, which occur as an irregularly shaped body in the crystalline limestone near the gehlenite-spurrite skarns at the Fuka mine, Okayama Prefecture, Japan. Inyoite occurs as aggregates of tabular crystals up to 1 mm wide, and rarely as euhedral crystals up to 0.5 mm wide in fissures of calcium borate minerals such as nifontovite, pentahydroborite, sibirskite and parasibirskite. The fissure fillings are composed only of inyoite. This is the first finding of inyoite in Japan. The type of occurrence is also different from those in many other localities in the world. Electron microprobe and CHNS / O analyses gave the empirical formula Ca1.99B5.96O5.92(OH)(10).8.08H(2)O on the basis of O = 24. The unit cell parameters are a = 10.616(2), b = 12.068(1), c = 8.404(1) angstrom and beta = 114.01(1)degrees. The mineral is optically biaxial negative with refractive indices alpha = 1.492, beta = 1.506 and gamma = 1.517, giving a calculated 2V = 82 degrees. The Vickers microhardness is 91 kg mm(-2) (10 g load) and the Mohs hardness number is 2.5. The measured density is 1.875 g cm(-3). It is likely that the inyoite at the Fuka mine was formed by a reaction of ground water with calcium borate minerals at a temperature of around 20 degrees C.

DOI： 10.2465/jmps.99.67

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：JAPAN ASSOC MINERALOGICAL SCIENCES  

Ramsbeckite was found as a vein forming mineral in altered shale at the Hirao mine, Minoo, Osaka, Japan. It occurred as aggregates of euhedral granular crystals up to 0.5 mm across, in association with sphalerite, chalcopyrite, smithsonite, aurichalcite, amorphous manganese dioxide, schulenbergite, brochantite, serpierite, limonite and an unidentified mineral. It was emerald green to blue-green in color with a vitreous luster in hand specimen. An EPMA and CHNS/O analyzer gave the empirical formula (Cu(9.380)Zn(5.54)2Ni(0.034)Co(0.027)Fe(0.020) Mn-0.013)(Sigma 15.016)[(SO4)(3.871)(CO3)(0.166)](Sigma 4.037)(OH)(21.958)center dot 6.06H(2)O on the basis of O = 44. The unit cell parameters were a = 16.106 (3), b = 15.568 (2), c = 7.109 (1), angstrom, beta = 90.23 (1)degrees, and Z = 2. The mineral was optically biaxial negative with refractive indices alpha = 1.676, beta = 1.704 and gamma = 1.707, and 2V(X)(calc) = 37.8 degrees. The Vickers micro-hardness was 162 (144-182) kg/mm(2) ( 10 g load), and the Mohs hardness was 3.5. The measured density was 3.36 g/cm(3). It is likely that ramsbeckite at the Hirao mine crystallized from Cu and Zn-bearing fluids.

DOI： 10.2465/jmps.99.19

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：ACADEMIC PRESS INC ELSEVIER SCIENCE  

Dielectric measurements were carried out on suspensions of montmorillonite clay exchanged with three different counterions: sodium, ammonium, and tetramethylammonium (TMA). Only two dielectric absorption peaks could be identified for the clay sample with the TMA counterion, whereas three peaks were found for the two inorganic counterions. The dielectric process observed at around 10 GHz is due to the orientation of bulk water molecules, judging from the relaxation time and relaxation strength. The relaxation strength of the process occurring at around 10 MHz was compared with the coefficient of adiabatic compressibility obtained from ultrasound velocity measurements. The increase in the relaxation strength with decreasing compressibility indicates that the process at around 10 MHz is caused by the orientation of bound water molecules on the clay samples. The relaxation strength of the process occurring at around 10 MHz for the TMA sample was remarkably small. Furthermore, the network structure of the bound water molecules can be characterized by a property peculiar to the TMA sample, taking into account the value of its Cole-Cole parameter. Results for the relaxation strength of the process occurring at around 100 kHz were compared with those for electrophoretic mobility. This comparison revealed that discrimination between bound ions and ions in the diffuse double layer is important, and both the relaxation and electrophoretic results could be satisfactorily explained by surface polarization of the clay. (C) 2003 Elsevier Inc. All rights reserved.

DOI： 10.1016/S0021-9797(03)00688-X

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出版者・発行元：一般社団法人 日本鉱物科学会  

一般式Zn₄(SO₄)(OH)₆・mH₂Oで示される亜鉛の塩基性硫酸塩は，合成物ではm=0, 0.5, 3, 4, 5の５種が報告されている(Jacob and Riquier, 1969; Bear et al., 1986, 1987)。天然ではm=4で，CuがZnの一部を置換したnamuwite(e.g. Bevins et al., 1982; Groat, 1996)のみが報告されている。今回，大阪府箕面市温泉町の平尾旧坑から，これまでに天然では報告のない合成Zn₄(SO₄)(OH)₆・5H₂Oとほぼ一致する性質をもつnamuwite類似の含水塩基性硫酸亜鉛鉱物を見出したので，その産状および鉱物学的性質について報告する。<BR>
箕面産含水塩基性硫酸亜鉛鉱物は湿った旧坑内の坑壁表面，またはchlorite化した母岩の裂罅に，sphaleriteなどの分解による二次生成物として，最大2mmの六角薄板状結晶をなして産出した。坑壁の表面には薄板状結晶が鍾乳状に集合したものがみられた。共存鉱物はhydrozincite，smithsonite，namuwiteである。肉眼的には淡青ないし無色，透明ないし半透明で真珠光沢を示す。鏡下では無色ないし淡青色透明で，一方向に完全な劈開がみられる。主なX線粉末回折値[dÅ(I)(hkl)]は，10.93(100)(001)，2.723(26)(3-10)，1.576(24)(1-50)，3.642(20)(003)，2.560(16)(-311)，4.16(14)(1-20)，5.47(12)(002)，3.236(12)(-122)，3.409(10)(1-13)，3.285(10)(013)，2.673(10)(121)，3.409(10)(1-13)，3.285(10)(013)，2.673(10)(121)で，Bear et al.(1987)に基づいて三斜晶系として求めた格子定数は，a=8.36(3)，b=8.35(3)，c=11.02(1)，α=94.1(3)，β=83.0(2)，γ=120.0(3)°である。KBr錠剤法によるIRスペクトルは，3400cm^-1付近および1620cm^-1付近に水，1120cm^-1付近に[SO₄]による吸収を示した。EPMAによる化学分析の平均値は，ZnO 51.34，CuO 7.25，FeO 0.13，MnO 0.12，NiO 0.12，CoO 0.02，SO₃ 15.84，H₂O 25.18 (差)，total 100 wt%で，O=15としたときの実験式は(Zn_3.481Cu_0.503Fe_0.010Mn_0.009Ni_0.009Co_0.001)_Σ4.010(SO₄)_1.092(OH)_5.843・4.79H₂Oである。Zn/(Zn+Cu) は0.82-0.93を示した。

DOI： 10.14824/kobutsu.2003.0.134.0

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：TAYLOR & FRANCIS LTD  

Phase relationships for FeS polymorph have been studied at the pressure of 16-20 GPa and temperature of 300-1350 K by in situ X-ray observation using a large volume high-pressure apparatus and a synchrotron radiation. Contrary to Fei's prediction [1], we found the stability field of NiAs-type phase of FeS extending at least to 18 GPa. Results of in situ X-ray observation correspond with the NiAs-hexagonal phase boundary determined by Kusaba et al. [2,3], Assuming the straight NiAs-hexagonal phase boundary, we estimate that the NiAs-hexagonal-liquid triple junction is located at 39.5 GPa and 2300 K.

DOI： 10.1080/08957950290006866

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出版者・発行元：一般社団法人 日本鉱物科学会  

DOI： 10.14824/kobutsu.2002.0.42.0

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出版者・発行元：一般社団法人 日本鉱物科学会  

DOI： 10.14824/kobutsu.2002.0.32.0

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担当区分：筆頭著者   記述言語：英語  

The crystal structure of scapolite from the Liitzow-Holm Bay region, East Antarctica with cell formular (Na_<1.97>Ca_<1.48>K_<0.46>Mg_<0.03>) _<3.94> (Al_<4.15>Si_<7.85>Fe_<0.01>) _<12.01>O_<24.00> (Cl_<0.65>(CO_3) _<0.42>) _<1.07>, Me_<39>, was determined in tetragonal, P4_2/n, a=12.122(2); c=7.585(2) A by the single crystal X-ray diffraction method. The structure is the same as that of meionite but with some difference in atomic coordinates and Al percentage in the tetrahedon. The CO_3 groups were mainly disordered on the xy plane and off-centred from the Anion site. The cation site was 8-coordinate rather than 6-coordinate.

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：Tohoku University  

Baghdadite was found in a spurrite zone in skarns at Fuka, Okayama Prefecture, Japan. It occurs as anhedral grains up to 0,5 mm in length and prismatic crystals up to 0.6×0.4×0.2 mm, in association with gehlenite, spurrite, tilleyite, peroéskite, grandite garnet and éesuéianite. The empirical formula of the mineral is (Ca3.03Na0.01)∑3.04(Zr 0.83Ti0.15)∑0.98(Si1.99Al 0.01Fe0.01)∑2.01O9 on the basis of O=9, which is consistent with the ideal formula Ca3ZrSi2O9. The unit cell parameters are a= 10.429(2), b= 10.170(2), c=7.365(1)A and β = 91.01(1)°. The mineral is optically biaxial negatiée with refractiée indices a= 1.735, β= 1.747, and γ= 1.755, and calculated 2 V = 1W. The Vickers microhardness is 803 kg mm2 (25 g load) and the density is 3.36 g cm3. It is likely that baghdadite at Fuka was formed by a reaction of pre-existing rankinite and/ or kilchoanite, and ZrO2 eéoléed from an intrusiée igneous liquid at a high temperature.

DOI： 10.2465/jmps.96.43

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：Tohoku University  

Kinoite was found in a dump at the Fuka mine, Okayama Prefecture, Japan. It occurs as aggregates of flaky crystals, and rarely as subhedral platy crystals up to 1 mm wide in a vein cutting into crystalline limestone. Associated minerals are stringhamite, calcite and an unidentified mineral. The empirical formula of the mineral is (Ca2.00Mga0.02)∑2.02(Cu 1.92Fe0.04Co0.04)∑2.00Si 2.98O10 · 2.25H2O on the basis of O=10 (anhydrous). The unit cell parameters are a=6.989 (1), b=12.904 (2), c=5.659 (1) Å, and β=96.15 (2)°. The mineral is optically biaxial negative with refractive indices α= 1.642 (2), β= 1.662 (2), and γ= 1.675 (2). The Vickers microhardness is 536 kg mm-2 (50 g load) and the density is 3.14 g cm-3. It is likely that kinoite at the Fuka mine was formed as a primary mineral by a reaction of Cu- and Si-bearing fluids with limestone.

DOI： 10.2465/jmps.96.29

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：Tohoku University  

Uralborite, CaB2O2(OH)4, was found in a vein consisting of borate minerals that cut into crystalline limestone at Fuka, Okayama Prefecture, Japan. It occurs as aggregates of fibrous crystals up to 0.2 mm long and as euhedral crystals up to 7 mm long and 3 mm wide, in association with sibirskite, borcarite, fluorite and calcite. Electron microprobe analyses and ICP gave the empirical formula Ca1.006B2.019O2.069(OH)3.931 on the basis of O=6. X-ray powder diffraction were indexed on the monoclinic cell, a=6.923(1), b=12.326(1), c=9.831(1)Å, β=97.09(1)°, determined by a single crystal method. The mineral was optically biaxial positive with refractive indices α=1.605(2), β=1.611(2), γ=1.618(2). The Vickers microhardness was 372 kg mm-2 and the Moh's scale of hardness was 4.5. The density was 2.58(2) g cm-1. It is likely that uralborite at Fuka was formed as a secondary mineral by a late-hydrothermal alteration of sibirskite.

DOI： 10.2465/jmps.95.43

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担当区分：筆頭著者   記述言語：日本語   出版者・発行元：岡山大学理学部地球科学教室  

Native gold was found at Mikawa mine, Niigata Prefecture, Japan. The mineral was associated with quartz in a druse within quartz-vein in propyrite. The crystals were formed in filiform, reticulated and dendritic shapes with about 1 mm length with 0.1 mm width and 0.05 mm thickness. Very malleable and ductile, opaque and yellow with metallic luster. Qualitative and semi-quantiative analyses were performed by the wavelength dispersive EPMA. Quantitatively, the crystals contained Au, Ag and Hg. Semi-quantitative analyses were executed with ZAF correction algorithm. The results showed that these specimens had a average chemical composition Au0.77 Ag0.11Hg0.12. This specimen was archived at our site with a collection number ESO-M01001.

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記述言語：英語   出版者・発行元：Japan Association of Mineralogical Sciences  

Hexahydroborite was found in a vein consisting of borate minerals which developed along the boundary between crystalline limestone and skarns at Fuka, Okayama Prefecture, Japan. Hexahydroborite occurred as aggregates of pyramidal crystals up to 2mm wide on the cavity wall, in association with olshanskyite and calcite. Wet analyses and ICP-MS gave the empirical formula Ca_1.001B_2.102O_4.154·5.846H₂O on the basis of O=10, which was consistent with the ideal formula Ca[B(OH)₄]₂·2H₂O. The reflections of X-ray powder data for hexahydroborite from Fuka were indexed on the monoclinic cell, a=16.011(2), b=6.688(1), c=7.954(2)Å, β=103.81(1)°, determined by single crystal method. The mineral was optically biaxial positive with refractive indices α=1.502(2), β=1.505(2), γ=1.509(2) and had a Mohs hardness of 2.5 and a density of 1.84gcm⁻³. It is likely that hexahydroborite at Fuka was formed by a reaction of ground water with sibirskite and/or parasibirskite at a low temperature around 25°C.

DOI： 10.2465/minerj.21.9

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記述言語：フランス語   掲載種別：研究論文（学術雑誌）   出版者・発行元：Blackwell Munksgaard  

Tetrasodium heptacobalt hexaphosphate, a new monophosphate prepared by hydrothermal methods, comprises CoO6 and CoO4 coordination polyhedra connected to each other by corner and edge sharing to form zigzag layers parallel to the ab plane. These layers are interconnected by Co-O polyhedra and P-O tetrahedra via corner sharing to form a three-dimensional network. The Na+ ions are located in the tunnels running parallel to the a axis. This compound is isostructural with Na4Ni7(PO4)6. © 1998 International Union of Crystallography all rights reserved.

DOI： 10.1107/S010827019701189X

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記述言語：フランス語   掲載種別：研究論文（学術雑誌）  

DOI： 10.1107/S0108270197006689

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担当区分：筆頭著者   記述言語：日本語   出版者・発行元：岡山大学理学部地球科学教室  

A used 8 bit microcomputer is applied for an instrument of controlling the heating temperatures of hydrothermal reactor furnaces. The temperatures were changed into appropriate values of voltage by thermocouples and additional devices. The interface board, programmable peripheral interface LSI and some IC's for addres decording are assembled into a complte unti. The device is useful for the inexpensive way of the construction of the accurate temperature control system.

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記述言語：英語   掲載種別：研究論文（学術雑誌）   出版者・発行元：MUNKSGAARD INT PUBL LTD  

The structure belongs to the monophosphate group and contains one type of PO4 tetrahedra connected to one type of MgO6 octahedra by corner sharing. These PO4-MgO6 groups are connected along the two shorter a and b axes to form two-dimensional zigzag sheets. Two sheets are connected along the longer c axis by two types of Na-O polyhedra. Pairs of PO4 tetrahedra in the sheets are connected by H atoms situated at the centres of symmetry, forming short hydrogen bonds.

DOI： 10.1107/S0108270195006901

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担当区分：筆頭著者   記述言語：日本語   掲載種別：研究論文（大学，研究機関等紀要）  

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担当区分：筆頭著者   記述言語：英語   掲載種別：研究論文（学術雑誌）  

DOI： 10.1107/S0108270193014337

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記述言語：英語   出版者・発行元：Japan Association of Mineralogical Sciences  

The syntheses of zinc hydroxyl monophosphate Zn₂(OH)PO₄ were carried out under hydrothermal conditions of 573 K and 200 kg/cm². The crystal data are: orthorhombic, P2₁2₁2, a=8.099(1), =8.325(1) and c=5.966(1) Å. The structure was solved by three dimensional Patterson syntheses and refined by least squares methods to give a final residual index of R=0.042. There are four units of Zn₂(OH)PO₄ in a unit cell and three kinds of zinc atoms with different coordinations, where the first zinc atom is six-coordinated by four oxygen atoms and two hydroxyl groups, the second one is octahedrally coordinated by six oxygen atoms and the third one is five-coordinated by four oxygen atoms and one hydroxyl group forming distorted pyramids. The framework consists of infinite straight chains of Zn–O octahedra along c-axis, connected together by isolated PO₄ tetrahedra and distorted Zn–O pyramids. This compound is a polymorph of tarbuttite.

DOI： 10.2465/minerj.17.132

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担当区分：筆頭著者   記述言語：フランス語   掲載種別：研究論文（学術雑誌）  

DOI： 10.1107/S0108270193012004

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

J-GLOBAL

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担当区分：筆頭著者  

DOI： 10.2465/minerj.16.371

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   掲載種別：記事・総説・解説・論説等（商業誌、新聞、ウェブメディア）  

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担当区分：筆頭著者   記述言語：日本語   出版者・発行元：化学同人  

CiNii Article

CiNii Books

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その他リンク： http://ousar.lib.okayama-u.ac.jp/52208

担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者   記述言語：日本語  

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担当区分：筆頭著者  

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担当区分：筆頭著者   記述言語：日本語  

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記述言語：日本語   会議種別：口頭発表（一般）  

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記述言語：日本語   会議種別：口頭発表（一般）  

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会議種別：口頭発表（一般）  

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会議種別：口頭発表（一般）  

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記述言語：日本語   会議種別：口頭発表（招待・特別）  

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記述言語：日本語   会議種別：口頭発表（招待・特別）  

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記述言語：日本語  

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会議種別：口頭発表（招待・特別）  

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記述言語：日本語  

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記述言語：日本語   会議種別：口頭発表（招待・特別）  

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記述言語：日本語  

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記述言語：英語  

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記述言語：日本語  

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記述言語：日本語  

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