Microsoft PowerPoint - 鉱物学02.ppt
|
|
|
- ありかつ あいきょう
- 6 years ago
- Views:
Transcription
1 地球科学特別講義 A 2 宮脇律郎国立科学博物館地学研究部 前回のあらすじ 鉱物とは地質作用により自然にできた固体物質 岩石は数種 ( まれに一種 ) の鉱物の集合体 鉱物種は化学組成と結晶構造で定義される 約 4000 種の鉱物が知られている 毎年 50 種程度の新種が増えている 国際鉱物学連合の新鉱物 鉱物名委員会が新種の承認を判定する 鉱物 という物質は地球や宇宙のマクロの世界と分子や原子のミクロの世界を語る 博物館における研究活動 資料の採集 資料の受け入れ 資料の分析 評価 標本としての登録 標本の管理 ( 貸し出し 分与 ) 展示企画 ( 常設展 特別展 ) 教育普及活動 ( 講演会 野外観察会 ) 研究成果の報告と学会活動 Chemical composition: EDS 1
2 Chemical composition: WDS Crystallographic data: powder X-ray diffractometer Potassicleakeite, KNa 2 Mg 2 Fe 3+ 2 LiSi 8 O 22 (OH) 2, a new amphibole from the Tanohata Mine, Iwate Prefecture, Japan 2
3 Crystal structure: four-circle X-ray diffractometer The crystal structure of watatsumiite, KNa 2 LiMn 2 V 2 Si 8 O 24, a new mineral from the Tanohata mine, Iwate Prefecture, Japan NSM Mineral collections Foreign Total: Sakurai C.: 5500 Type: 4 Specimens from foreign countries Sakurai Collection Japanese Total: Sakurai C.: 7350 Type: 51 Kotoite and Suanite from Korea Specimens from Japan Sarabauite from Sarabau, Sarawak Malaysia Akimotoite from Tenham chondrite, South Gregory, Queensland, Australia New minerals described by NSM in these years Mineral Specimens 1998: Okayamalite, Ca 2 B 2 SiO : Tsugaruite, Pb 4 As 2 S : Itoigawaite, SrAl 2 Si 2 O 7 (OH) 2 H 2 O 2000: Kozoite-(Nd), Nd(CO 3 )(OH) 2000: Tamaite, (Ca,K,Ba,Na, ) 4 Mn 24 (Si,Al) 40 (O,OH) H 2 O 2001: Rengeite, Sr 4 ZrTi 4 Si 4 O : Pararsenolamprite, As 2002: Ominelite, (Fe,Mg)Al 3 BSiO : Matsubaraiite, Sr 4 Ti 5 Si 4 O : Potassicleakeite, KNa 2 Mg 2 Fe 3+ 2 LiSi 8 O 22 (OH) : Niigataite, CaSrAl 3 (Si 2 O 7 )(SiO 4 )O(OH) 2003: Kozoite-(La), La(CO 3 )(OH) 2003: Watatsumiite, KNa 2 LiMn 2 V 2 Si 8 O : Protoanthophyllite, (Mg,Fe) 7 Si 8 O 22 (OH) : Magnesiosadanagaite, (Na,K)Ca 2 (Mg 3 Al 2 )Si 5 Al 3 O 22 (OH) : Tokyoite, Ba 2 Mn 3+ (VO 4 ) 2 (OH) 2005: Aspidolite, NaMg 3 AlSi 3 O 10 (OH) 2 Iwashiroite-(Y), YTaO 4 Hingganite-(Ce), CeBeSiO 4 (OH) 3
4 Mineral Specimens Sakurai Collection Database 4
5 Kozoite-(Nd) Nd(CO 3 )(OH) Ancylite group Polymorph of hydroxylbastnäsite-(nd) Crystal system: Orthorhombic Space group: Pmcn Z: 4 Lattice constants: a = (1), b = (2), c = (2) Å 4 strongest diffraction lines [d(å), I/I0, hkl]: 4.29,100,110; 2.93,89,102; 2.33,78,131; 2.06,78,221 Optical properties: High birefringence, α = 1.698(2), γ = 1.780(5) Hardness: Not determined Density: 4.77 g/cm 3 (calc.) Cleavage: Not determined Habit: Euhedral showing rhombo-dipyramidal habit, and the dimension of crystal is approximately 10 µm or less Color Luster: Pale pinkish purple to white with a vitreous to powdery luster Mode of occurrence: Occurs in cavity and fissure of alkali olivine basalt exposed at Niikoba, Hizen-cho, Higashi Matsuura-gun, Saga Prefecture, Japan, in association with lanthanite-(nd) and kimuraite-(y). Name: After the late Prof. Kozo Nagashima ( ) Type specimen: National Science Museum, Tokyo #NSM M27940 Reference: Miyawaki, R. et al.. Am. Min., 85: (2000). 鉱物の化学組成 同形置換による固溶体の形成 5
![苦土橄欖石, forsterite [Mg 2 SiO 4 ] の結晶構造 Forsterite: St. John s Island, Red Sea, Egypt [Matsuyama Collection] Hazen, R. M.](/docs-images/80/80977151/images/6-0.jpg "(1976) Effects of temperature and pressure on the crystal structure of forsterite. Am. Mineral., 61, 1280-1293.")
6 苦土橄欖石, forsterite [Mg 2 SiO 4 ] の結晶構造 Forsterite: St. John s Island, Red Sea, Egypt [Matsuyama Collection] Hazen, R. M. (1976) Effects of temperature and pressure on the crystal structure of forsterite. Am. Mineral., 61, 苦土橄欖石, forsterite [Mg 2 SiO 4 ] の結晶構造 苦土橄欖石, forsterite [Mg 2 SiO 4 ] の結晶構造 鉄橄欖石, fayalite [Fe 2 SiO 4 ] の結晶構造 Smyth (1975) 鉱物の化学組成 同形置換による固溶体の形成 Mg 2 SiO 4 Fe 2+ 2SiO 4 ベガードの法則 Smyth, J. R. (1975) High temperature crystal chemistry of fayalite. Am. Mineral., 60,
![苦土橄欖石, forsterite [Mg 2 SiO 4 ] の結晶構造 苦土橄欖石, forsterite [Mg 2 SiO 4 ] の結晶構造 O b c Hazen, R. M.](/docs-images/80/80977151/images/7-0.jpg "(1976) Effects of temperature and pressure on the crystal structure of forsterite. Am. Mineral., 61, 1280-1293. Vegard 則固溶体の組成と格子定数の比例関係 鉱物の化学組成 Å 4.83 Å 10.50 4.82 10.45 4.")
7 苦土橄欖石, forsterite [Mg 2 SiO 4 ] の結晶構造 苦土橄欖石, forsterite [Mg 2 SiO 4 ] の結晶構造 O b c Hazen, R. M. (1976) Effects of temperature and pressure on the crystal structure of forsterite. Am. Mineral., 61, Vegard 則固溶体の組成と格子定数の比例関係 鉱物の化学組成 Å 4.83 Å Mg 0.6Fe 1.4SiO Mg 1.2 Fe 0.8 SiO Mg 2 SiO 4 a b Mg 2 SiO 4 Fe 2SiO 4 Mg 2SiO 4 Fe 2 SiO 4 Å Å c 294 V Mg 2 SiO 4 Fe 2 SiO 4 Mg 2SiO 4 Fe 2 SiO 4 同形置換による固溶体の形成 Mg 2 SiO 4 Fe 2+ 2SiO 4 端成分 Mg 1.98 Fe Si 0.99 O 4 実験式 (Mg,Fe 2+ ) 2 SiO 4 ( 簡略式 ) Mg 2 SiO 4 理想式 ベガードの法則 Data: Akimoto & Fujisawa (1968) J. Geophys. Res., 73, olivine forsterite fayalite Mg 2 SiO 4 MgFeSiO 4 Fe 2 SiO 4 50 % rule 橄欖 ( かんらん ) 石 : 苦鉄質から超苦鉄質火成岩の主要造岩鉱物 石灰岩または苦灰岩中のスカルン鉱物 低温含水変質で蛇紋石 滑石などに変化 橄欖岩 : 橄欖石 輝石を主成分鉱物とする超苦鉄質深成岩 マントル物質に最も近い岩石の一つ 7
![Mn 2 SiO 4 固溶体での種名決定 50% 則 化学組成が判らないと決まらない 1 つの鉱物種の化学組成には一定の幅がある tephroite forsterite fayalite Mg 2 SiO 4 Fe 2 SiO 4 同形化学組成は異なるが 結晶構造は同じ例 ) forsterite [Mg 2 SiO 4 ] と fayalite [Fe 2 SiO 4 ]](/docs-images/80/80977151/images/8-0.jpg "多形化学組成は同じだが 結晶構造は異なる例 ) diamond [C] と graphite [C] diamondはgraphiteの多形相 ( 変態 ) である 同形置換 同じ結晶構造を保ちながら原子が置き換わる Mg 2+ Fe 2+ 0.72 Å 0.")
8 Mn 2 SiO 4 固溶体での種名決定 50% 則 化学組成が判らないと決まらない 1 つの鉱物種の化学組成には一定の幅がある tephroite forsterite fayalite Mg 2 SiO 4 Fe 2 SiO 4 同形化学組成は異なるが 結晶構造は同じ例 ) forsterite [Mg 2 SiO 4 ] と fayalite [Fe 2 SiO 4 ] 多形化学組成は同じだが 結晶構造は異なる例 ) diamond [C] と graphite [C] diamondはgraphiteの多形相 ( 変態 ) である 同形置換 同じ結晶構造を保ちながら原子が置き換わる Mg 2+ Fe Å 0.78 Å (HS) 電荷とイオン半径の類似性 Kozoite-(Nd) Nd(CO 3 )(OH) Ancylite group Polymorph of hydroxylbastnäsite-(nd) Crystal system: Orthorhombic Space group: Pmcn Z: 4 Lattice constants: a = (1), b = (2), c = (2) Å 4 strongest diffraction lines [d(å), I/I0, hkl]: 4.29,100,110; 2.93,89,102; 2.33,78,131; 2.06,78,221 Optical properties: High birefringence, α = 1.698(2), γ = 1.780(5) Hardness: Not determined Density: 4.77 g/cm 3 (calc.) Cleavage: Not determined Habit: Euhedral showing rhombo-dipyramidal habit, and the dimension of crystal is approximately 10 µm or less Color Luster: Pale pinkish purple to white with a vitreous to powdery luster Mode of occurrence: Occurs in cavity and fissure of alkali olivine basalt exposed at Niikoba, Hizen-cho, Higashi Matsuura-gun, Saga Prefecture, Japan, in association with lanthanite-(nd) and kimuraite-(y). Name: After the late Prof. Kozo Nagashima ( ) Type specimen: National Science Museum, Tokyo #NSM M27940 Reference: Miyawaki, R. et al.. Am. Min., 85: (2000). つづく Kozoite-(Nd), NdCO 3 OH, a new mineral from Saga Prefecture 8
1. Precise Determination of BaAl2O4 Cell and Certification of the Formation of Iron Bearing Solid Solution. By Hiroshi UCHIKAWA and Koichi TSUKIYAMA (
1. Precise Determination of BaAl2O4 Cell and Certification of the Formation of Iron Bearing Solid Solution. By Hiroshi UCHIKAWA and Koichi TSUKIYAMA (Central Research Laboratory, Onoda Cement Co., Ltd.,
地質調査研究報告/Bulletin of the Geological Survey of Japan
Takayuki Uchino and Makoto Kawamura (2010) Glaucophane found from meta-basalt in the Nedamo Terrane, Northeast Japan, and its geologic significance. Bull. Geol. Surv. Japan, vol. 61 (11/12), p. 445-452,
SPring8菅野印刷.PDF
20021219Spring-8 Ah/kg Ah/dm 3 Li -3.01 540 3860 2090 Na -2.71 970 1160 1140 Al -1.66 2690 2980 8100 Zn -0.76 7140 820 5800 Fe -0.44 7850 960 7500 Cd -0.40 8650 480 4100 Pb -0.13 11340 260 2900 H 2 0
コロイド化学と界面化学
x 25 1 kg 1 kg = 1 l mmol dm -3 ----- 1000 mg CO 2 -------------------------------------250 mg Li + --------------------------------1 mg Sr 2+ -------------------- 10
Table 1. Shape and smelting properties of chrome ores as delivered. Table 2. Chemical composition of chrome ores (%). Table 3. Chemical composition of
UDC 669.263.1: 669.046.462 The Reduction Process and Reducibility of Chromite with Carbon Hiroshi G. KATAYAMA and Akihiko TANAKA Synopsis: In the present work, various chrome ores and relatively pure chromites
00) îSìyçzï®äwÇÃäÓëb-1.pdf
(1) 16 Si 4+, Al 3+, Fe 3+, Fe 2+, Mg 2+, Ca 2+, Na +, K +. O 2-, OH -, F - nm m. - ) CaAl 2 Si 2 O 8 + 8H + Ca 2+ + 2Al 3+ + 2H 4 SiO 4 2Al 3+ + 2H 4 SiO 4 + H 2 O Al 2 Si 2 O 5 (OH) 4 + 6H + ph ph -
The Phase Behavior of Monooleoylglycerol-Water Systems Mivoshi Oil & Fat Co.. Ltd. Faculty of Science and Technology, Science University of Tokyo Inst
The Phase Behavior of Monooleoylglycerol-Water Systems Mivoshi Oil & Fat Co.. Ltd. Faculty of Science and Technology, Science University of Tokyo Institute of Colloid and Interface Science, Science University
PowerPoint Presentation
材料科学基礎 Ⅰ 材料科学の枠組み 元素の結晶構造 いろいろな金属間化合物, 合金の結晶 いろいろなセラミックスの結晶とイオン結晶 格子, 晶系, 点群 X 線と結晶 物質の性質と対称性 結晶の欠陥と組織 1 hcp (hexagonal close packed structure) 2 fcc (face centered cubic structure) 3 hcp の軸比 (c/a) について
Slide 1
3. 溶解 沈殿反応 天然水の化学組成 大陸地殻表層 (mg kg ) 河川水 (mg kg ) Al 77.4.5 Fe 3.9.4 Ca 9.4 3.4 Na 5.7 5. 8.6.3 Mg 3.5 3.4 Andrews et al. (3) An introduction to Environmental Chemistry 天然水の特徴 天然水の金属イオンは主に岩石の風化により生じる ただし
000..\..
Bull. Nagoya Univ. Museum No. 20, 79 91, 2004 Quantitative chemical analysis of rocks with X-ray fluorescence analyzer XRF-1800 NAKAZAKI Mineko TSUBOI Motohiro KANAGAWA Kazuyo KATO Takenori SUZUKI Kazuhiro
角閃石とは 標準的な角閃石の式は AB VI 2 C IV 5 T 8 O 22 X 2 式の A,B,C,T,X 成分は次の結晶学的サイトに対応する : A 上記の式当たり1サイト ; B 2つの M4 サイト ; C 2つの M1 サイト 2つの M2 サイト 1つの M3 サイトからなる計 5
角閃石とは 標準的な角閃石の式は AB VI 2 C IV 5 T 8 O 22 X 2 式の A,B,C,T,X 成分は次の結晶学的サイトに対応する : A 上記の式当たり1サイト ; B 2つの M4 サイト ; C 2つの M1 サイト 2つの M2 サイト 1つの M3 サイトからなる計 5つの八面体サイト ; T 4つの組の2セットからなる計 8つの四面体サイト ; X 2つのサイト これらのサイトを占めるのは
** Department of Materials Science and Engineering, University of California, Los Angeles, CA 90025, USA) Preparation of Magnetopulmbite Type Ferrite
** Department of Materials Science and Engineering, University of California, Los Angeles, CA 90025, USA) Preparation of Magnetopulmbite Type Ferrite Thin Films by Dip-Coating Method and Magnetic Properties
X線分析の進歩36 別刷
X X X-Ray Fluorescence Analysis on Environmental Standard Reference Materials with a Dry Battery X-Ray Generator Hideshi ISHII, Hiroya MIYAUCHI, Tadashi HIOKI and Jun KAWAI Copyright The Discussion Group
2 1 7 - TALK ABOUT 21 μ TALK ABOUT 21 Ag As Se 2. 2. 2. Ag As Se 1 2 3 4 5 6 7 8 9 1 1 2 3 4 5 6 7 8 9 1 1 2 3 4 5 6 7 8 9 1 Sb Ga Te 2. Sb 2. Ga 2. Te 1 2 3 4 5 6 7 8 9 1 1 2 3 4 5 6 7 8 9 1 1 2 3 4
01-表紙.ai
B 0 5 0-5 双極子核 I=1/ 2 四極子核 I 1 e Li Be B C N F Ne Na Mg 黒字はNMR 観測不可 Al Si P S Cl Ar K Ca Sc Ti V Cr MnFe Co Ni Cu ZnGaGe As Se Br Kr RbSr Y Zr NbMoTc RuRhPdAgCd In Sn SbTe I Xe Cs Ba La f Ta W Res Ir Pt
RAA-05(201604)MRA対応製品ver6
M R A 対 応 製 品 ISO/IEC 17025 ISO/IEC 17025は 試験所及び校正機関が特定の試験又は 校正を実施する能力があるものとして認定を 受けようとする場合の一般要求事項を規定した国際規格 国際相互承認 MRA Mutual Recognition Arrangement 相互承認協定 とは 試験 検査を実施する試験所 検査機関を認定する国際組織として ILAC 国際試験所認定協力機構
Fig. ph Si-O-Na H O Si- Na OH Si-O-Si OH Si-O Si-OH Si-O-Si Si-O Si-O Si-OH Si-OH Si-O-Si H O 6
NMR ESR NMR 5 Fig. ph Si-O-Na H O Si- Na OH Si-O-Si OH Si-O Si-OH Si-O-Si Si-O Si-O Si-OH Si-OH Si-O-Si H O 6 Fig. (a) Na O-B -Si Na O-B Si Fig. (b) Na O-CaO-SiO Na O-CaO-B -Si. Na O-. CaO-. Si -. Al O
元素分析
: このマークが付してある著作物は 第三者が有する著作物ですので 同著作物の再使用 同著作物の二次的著作物の創作等については 著作権者より直接使用許諾を得る必要があります (PET) 1 18 1 18 H 2 13 14 15 16 17 He 1 2 Li Be B C N O F Ne 3 4 5 6 7 8 9 10 Na Mg 3 4 5 6 7 8 9 10 11 12 Al Si P
JAJP
Agilent 7500ce ORS ICP-MS Glenn Woods Agilent Technologies Ltd. 5500 Lakeside, Cheadle Royal Business Park Stockport UK Agilent 7500ce ICP-MS 5 7500ce (ORS) 1 ORS 7500ce ORS ICP-MS ( ) 7500 ICP-MS (27.12
<4D F736F F F696E74202D208DDE97BF955D89BF8A778AEE F8BF38AD48C512E B93C782DD8EE682E890EA97705D>
材料科学の枠組み 基礎編 材料評価学基礎 格子 晶系 空間群 ( 対称性 ) いろいろな結晶の構造 結晶と逆格子 ( 回折結晶学 ) X 線と結晶 応用編 電子顕微鏡 放射光 中性子線 1 格子 (Lattice) 3 次元の周期的な点の配列 点のまわりの環境が同一である, 空間の 点の無限の配列 c R n1a n2b n3c 格子定数 (Lattice parameters a or Lattice
ŁI’ÜTmŸ_Ł¶color
191997 217 227 Journal of the Geotherrmal Research Society of Japan Vol.19,No4.(1997) P.217~P.227 Timing of Fracture Development Deduced from Microthermometry of Fluid Inclusions in Minerals from the Hijiori
H1-H4
42 S H He Li H He Li Be B C N O F Ne Be B C N O F Ne H He Li Be B H H e L i Na Mg Al Si S Cl Ar Na Mg Al Si S Cl Ar C N O F Ne Na Be B C N O F Ne Na K Sc T i V C r K Sc Ti V Cr M n F e C o N i Mn Fe Mg
..8../8-9 ....
1 2 1933 GNP 3 1962 p OHASHI Toshihiro Abstracts AStudy on the Development of the Cultural Properties Policy in Korea from 1902 until 1962 OHASHI Toshihiro The investigation of cultural properties
untitled
NPO 2006( ) 11 14 ( ) (2006/12/3) 1 50% % - - (CO+H2) ( ) 6 44 1) --- 2) ( CO H2 ) 2 3 3 90 3 3 2 3 2004 ( ) 1 1 4 1 20% 5 ( ) ( ) 2 6 MAWERA ) MAWERA ( ) ( ) 7 6MW -- 175kW 8 ( ) 900 10 2 2 2 9 -- - 10
03J_sources.key
Radiation Detection & Measurement (1) (2) (3) (4)1 MeV ( ) 10 9 m 10 7 m 10 10 m < 10 18 m X 10 15 m 10 15 m ......... (isotope)...... (isotone)......... (isobar) 1 1 1 0 1 2 1 2 3 99.985% 0.015% ~0% E
渡辺(2309)_渡辺(2309)
[ 29 p. 241-247 (2011)] ** *** ** ** Development of a nickel-based filler metal containing a small amount of silicon by WATANABE Takehiko, WAKATSUKI Ken, YANAGISAWA Atsusi and SASAKI Tomohiro Authors tried
XFEL/SPring-8
DEVELOPMENT STATUS OF RF SYSTEM OF INJECTOR SECTION FOR XFEL/SPRING-8 Takao Asaka 1,A), Takahiro Inagaki B), Hiroyasu Ego A), Toshiaki Kobayashi A), Kazuaki Togawa B), Shinsuke Suzuki A), Yuji Otake B),
1) K. J. Laidler, "Reaction Kinetics", Vol. II, Pergamon Press, New York (1963) Chap. 1 ; P. G. Ashmore, "Catalysis and Inhibition of Chemical Reactio
1) K. J. Laidler, "Reaction Kinetics", Vol. II, Pergamon Press, New York (1963) Chap. 1 ; P. G. Ashmore, "Catalysis and Inhibition of Chemical Reactions", Butterworths, London (1963) Chap. 7, p. 185. 2)
untitled
254nm UV TiO 2 20nm :Sr 5 Ta 4 O 15 3 4 KEY-1 KEY-2 (Ti,Nb,Ta) 5 KEY-1 KEY-2 6 7 NiO/ Sr 2 Ta 2 O 7 mmol h -1 g -1 20 15 10 5 H 2 O 2 H 2 O 2 0 0 2 4 6 8 10 12 NiO/Sr 2 Ta 2 O 7 The synthesis of photocatalysts
2008/02/18 08:40-10:10, 12:50-14:20 14:30-16:00, 16:10-17:40,
008/0/18 08:40-10:10, 1:50-14:0 14:30-16:00, 16:10-17:40, 1pt A 1911 Leiden Heike Kammelingh-Onnes H.Kammelingh Onnes 1907 He 1 4. K H H c T c T H c Hg:40 mt, Pb:80 mt, Sn:30 mt 100 mt I c H c H c H
museum data no74
74 Museum Data No.74 (2008.12) 1 2 Museum Data No.74 (2008.12) Museum Data No.74 (2008.12) 3 4 Museum Data No.74 (2008.12) Museum Data No.74 (2008.12) 5 6 Museum Data No.74 (2008.12) Museum Data No.74
特-7.indd
Mechanical Properties and Weldability of Turbine Impeller Materials for High Temperature Exhaust Gas Turbocharger 1 000 1 050 246 IN100 The increase in environmental awareness in recent years has led to
Evaluation of Anisotropy and Preferred Orientation of Carbon and Graphite Materials Yoshihiro Hishiyama Fig.1 Diffraction condition in Fourier space.
Evaluation of Anisotropy and Preferred Orientation of Carbon and Graphite Materials Yoshihiro Hishiyama Fig.1 Diffraction condition in Fourier space. Corresponding Author, E-mail: yhishiya@eng.musashi-tech.ac.jp
Fig.1 A location map for the continental ultradeep scientific drilling operations.
Application of a Synthetic Smectite to the Ultradeep Scientific Drilling Operations Makoto KOGA Nitchitsu Co., Ltd. Resources Development Devision, Powder Technological Laboratory 351-1 Kamitano, Arakawa-mura,
9) H. SCHMCLZRIED: Z. Elektrochem. 66 (l%1) p ) W. D. KINGERY et al.: J. Am. Chem. Soc., 42 (1959), p ) F. HUND: Z. Phys. Chem., 199 (195
9) H. SCHMCLZRIED: Z. Elektrochem. 66 (l%1) p. 572 10) W. D. KINGERY et al.: J. Am. Chem. Soc., 42 (1959), p.394 11) F. HUND: Z. Phys. Chem., 199 (1952), p. 142 12) J. F. ELLIOTT and M. GLEISER: " Thermochemistry
The Japanese economy in FY2015 suffered from sluggish growth in individual consumption, while the foreign exchange market remained unstable with high volatility. Even in such an economic environment, MSF
X線分析の進歩45
Advances in X-Ray Chemical Analysis, Japan, 45 (2014) ISSN 0911-7806 NaCl Color Center in NaCl Takuya TSUJI, Hiroyuki IWASAKI and Jun KAWAI NaCl Color Center in NaCl Takuya TSUJI, Hiroyuki IWASAKI and
Microsoft PowerPoint - 図材料科学基礎Ⅰ14_基礎編１.pptx
材料科学基礎 Ⅰ 材料科学の枠組み 基礎編 元素の結晶構造 いろいろな金属間化合物, 合金の結晶 いろいろなセラミックスの結晶とイオン結晶 格子, 晶系, 点群 X 線と結晶 応用編 電子顕微鏡 放射光 中性子線 結晶の格子定数 結晶の欠陥と組織 1 hcp (hexagonal close packed structure) ABAB.. : hcp 2 hcp (hexagonal close
*...X Z-.....F.{..
No. 35 (2000) pp.115-124 The Late Quaternary stratigraphy in the western margin of Yodobashi- dai, northern part of Setagaya-ku, Tokyo Jiro KOMORI, Kunihiko ENDO, Fumihiko HASEGAWA, and Sei TAMURA (Received
CH 2 CH CH 2 CH CH 2 CH CH 2 CH 2 COONa CH 2 N CH 2 COONa O Co 2+ O CO CH 2 CH N 2 CH 2 CO 9 Change in Ionic Form of IDA resin with h ph CH 2 NH + COO
CH 2 CH CH 2 CH CH 2 CH CH 2 CH 2 COONa CH 2 N CH 2 COONa O Co 2+ O CO CH 2 CH N 2 CH 2 CO 9 Change in Ionic Form of IDA resin with h ph CH 2 NH + COOH COOH COOH COO - CH 2 NH + + CH 2 NH COO - COO - COO
スライド 1
Matsuura Laboratory SiC SiC 13 2004 10 21 22 H-SiC ( C-SiC HOY Matsuura Laboratory n E C E D ( E F E T Matsuura Laboratory Matsuura Laboratory DLTS Osaka Electro-Communication University Unoped n 3C-SiC
SEISMIC HAZARD ESTIMATION BASED ON ACTIVE FAULT DATA AND HISTORICAL EARTHQUAKE DATA By Hiroyuki KAMEDA and Toshihiko OKUMURA A method is presented for using historical earthquake data and active fault
ｽﾗｲﾄﾞ ﾀｲﾄﾙなし
1 2 3 4 27,500 5 6 2000 7 8 9 10 11 12 < 13 SPECIFICATION CHARACTERISTICS UNIT Regular Gasoline Premium Gasoline METHOD A Type C Type A Type C Type ABNT ASTM Color - (1) (2) (1) (2) Appearance - (4) (4)
00) î âûë¨ìx.pdf
....... .... = 1) 2) Ca + CO CaCO 3) 温泉水からの鉱物生成 指宿温泉での鉄鉱物の生成 霧島丸尾温泉でのシリカ鉱物の生成 湧水からの鉱物生成 Dissolution of anorthite Ca 2 2 O 8 + 8H + Ca 2+ + 2 3+ + 2H 4 O 4 Reaction of Ca ions Ca 2+ + CO 2 + H 2 O CaCO
Fig. 1 Sampling positions from the ingot. Table 2 Chemical compositions of base metal (%) Fig. 2 (unit: mm) Shape and size of fatigue test specimen. T
Friction welding of ADC 12 aluminum alloy diecastings Kazuyoshi KATO* and Hiroshi TOKISUE* Both squeeze and gravity castings of ADC 12 aluminum alloy were friction-welded, using a brake type welding machine.
*1 *2 *1 JIS A X TEM 950 TEM JIS Development and Research of the Equipment for Conversion to Harmless Substances and Recycle of Asbe
*1 *2 *1 JIS A 14812008X TEM 950 TEM 1 2 3 4 JIS Development and Research of the Equipment for Conversion to Harmless Substances and Recycle of Asbestos with Superheated Steam Part 3 An evaluation with
36 th IChO : - 3 ( ) , G O O D L U C K final 1
36 th ICh - - 5 - - : - 3 ( ) - 169 - -, - - - - - - - G D L U C K final 1 1 1.01 2 e 4.00 3 Li 6.94 4 Be 9.01 5 B 10.81 6 C 12.01 7 N 14.01 8 16.00 9 F 19.00 10 Ne 20.18 11 Na 22.99 12 Mg 24.31 Periodic
基礎地学I.ppt
I torutake@mail.sci.hokudai.ac.jp http://geotec.sci.hokudai.ac.jp/geotec/ I 800 2940 7/26 8/9 2/3 9 15 10% 6/1 20% 70% 15% 30% 40% 15% R=6400 km θ (S) θ/360 o =S/2πR (1) GPS (Global Positioning System)
THE WEATHERING OF QUARTZ-DIORITE IN SENMAYA DISTRICȚ IWATE PREFECTURE, JAPAN The weathering process of quartz-diorite mass in Senmaya district, Iwate Prefecture, was studied from chemical and mineralogical
C 3 C-1 Cu 2 (OH) 3 Cl A, B A, A, A, B, B Cu 2 (OH) 3 Cl clinoatacamite S=1/2 Heisenberg Cu 2+ T N 1 =18K T N 2 =6.5K SR T N 2 T N 1 T N 1 0T 1T 2T 3T
C 3 C-1 Cu 2 (OH) 3 Cl A, B A, A, A, B, B Cu 2 (OH) 3 Cl clinoatacamite S=1/2 Heisenberg Cu 2+ T N 1 =18K T N 2 =6.5K SR T N 2 T N 1 T N 1 0T 1T 2T 3T 4T 5T 6T C (J/K mol) 20 18 16 14 12 10 8 6 0 0 5 10
磁気測定によるオーステンパ ダクタイル鋳鉄の残留オーステナイト定量
33 Non-destructive Measurement of Retained Austenite Content in Austempered Ductile Iron Yoshio Kato, Sen-ichi Yamada, Takayuki Kato, Takeshi Uno Austempered Ductile Iron (ADI) 100kg/mm 2 10 ADI 10 X ADI
(Shigen to Sozai) Vol.116 p (2000) 石炭灰フライアッシュからのゼオライトのアルカリ水熱合成と生成物の陽イオン交換特性 * 1 1 村山憲弘山川洋亮 2 3 小川和男芝田隼次 Alkali Hydrothermal Synthesis of Zeol
石炭灰フライアッシュからのゼオライトのアルカリ水 Title 熱合成と生成物の陽イオン交換特性 Author(s) 村山, 憲弘, 山川, 洋亮, 小川, 和男, 芝田, 隼次 Citation 資源と素材 : 資源 素材学会誌, 116(4): 279-284 Issue Date 2000 URL http://hdl.handle.net/10112/5454 資源 素材学会 (http://www.jstage.jst.go.
JAMSTEC Rep. Res. Dev., Volume 12, March 2011, 27 _ 35 1,2* Pb 210 Pb 214 Pb MCA 210 Pb MCA MCA 210 Pb 214 Pb * 2
JAMSTEC Rep. Res. Dev., Volume 12, March 2011, 27 _ 35 1,2* 1 1 1 1 210 Pb 210 Pb 214 Pb MCA 210 Pb MCA MCA 210 Pb 214 Pb 2010 10 4 2010 12 10 1 2 * 237-0061 2-15 046-867-9794 ogurik@jamstec.go.jp 27 210
SpecimenOTKozGo indd
TM The Kozuka Gothic TM typeface family is composed of six weights that cover various uses ranging from body text composition to headline compositions. This typeface family is now available in OpenType
untitled
1 2 3 4 5 130mm 32mm UV-irradiation UV-cationic cure UV-cationic cure UV-cationic cure Thermal cationic Reaction heat cure Thermal cationic Cation Reaction heat cure Cation (a) UV-curing of
温泉の化学 １
H O 1,003 516 149 124 2,237 1974 90 110 1km 2,400 ( 100 Mg 200 (98 ) 43,665 mg 38,695 mg 19,000 mg 2000 2000 Na-Ca-Cl 806 1970 1989 10 1991 4 ph 1 981 10,000 1993... (^^; (SO_4^{2-}) " " 1973-1987 1970
地質調査研究報告/Bulletin of the Geological Survey of Japan
Makoto Saito and Kazuhiro Miyazaki (2006) Jadeite-bearing metagabbro in serpentinite melange of the Kurosegawa Belt in Izumi Town, Yatsushiro City, Kumamoto Prefecture, central Kyushu. Bull. Geol. Surv.
製紙用填料及び顔料の熱分解挙動.PDF
Thermogravimetric analysis of pigments and fillers for papermaking Toshiharu Enomae Graduate School of Agricultural and Life Sciences Contact e-mail address: enomae@psl.fp.a.u-tokyo.ac.jp A2 350 450 A2
Continuous Cooling Transformation Diagrams for Welding of Mn-Si Type 2H Steels. Harujiro Sekiguchi and Michio Inagaki Synopsis: The authors performed
Continuous Cooling Transformation Diagrams for Welding of Mn-Si Type 2H Steels. Harujiro Sekiguchi and Michio Inagaki Synopsis: The authors performed a series of researches on continuous cooling transformation
1 1 H Li Be Na M g B A l C S i N P O S F He N Cl A e K Ca S c T i V C Mn Fe Co Ni Cu Zn Ga Ge As Se B K Rb S Y Z Nb Mo Tc Ru Rh Pd Ag Cd In Sn Sb T e
No. 1 1 1 H Li Be Na M g B A l C S i N P O S F He N Cl A e K Ca S c T i V C Mn Fe Co Ni Cu Zn Ga Ge As Se B K Rb S Y Z Nb Mo Tc Ru Rh Pd Ag Cd In Sn Sb T e I X e Cs Ba F Ra Hf Ta W Re Os I Rf Db Sg Bh
Title 多重構造音響連成場の振動解析制御 Author(s) 菅野, 秀 Citation Issue Date 2012-03-25 URL http://hdl.handle.net/10748/5587 DOI Rights Type Thesis or Dissertation Textversion publisher http://www.tmu.ac.jp/ 首都大学東京機関リポジトリ
結晶粒と強度の関係
SPring-8 金属材料評価研究会 218 年 1 月 22 日 @AP 品川 転載不可 アルミニウムにおける 置換型固溶元素が引張変形中の 転位密度変化に及ぼす影響 兵庫県立大学材料 放射光工学専攻〇足立大樹 背景 放射光を用いた In-situ XRD 測定により 変形中の転位密度変化を高時間分解能で測定可能となっており 結晶粒径による転位増殖挙動の変化について明らかにしてきた * * H.
ゼリーこんにゃくの分析
39 Analysis of Jelly Konjac Hiromichi HAYANO, Tsutomu KUMAZAWA Central Customs Laboratory, Ministry of Finance 531, Iwase, Matsudo shi, Chiba Ken, 271 Japan Some properties of so called jelly Konjac have
and surrounding areas used for pasture. The habitat is sometimes affected by strong winds containing sea salt water particularly during typhoons. A population of Glycine koidzumii (I-19) was found at Hirakubozaki.
VESTA講習-v001-gaku.PDF
2008/4/18 ver0.1 T. Nishida VESTA ( ) CrystalMaker VESTA VESTA http://www.geocities.jp/kmo_mma/ 2008 4 Ver1.4 Windows, Mac, Linux Windows ZIP ZIP VESTA.exe ZIP VESTA K. Momma and F. Izumi, Commission on
Netsu Sokutei 32 (3) Phase Relations of Minerals and Structure of the Earth's Interior Masaki Akaogi (Received April 2, 2005; Accepted May 11,
Netsu Sokutei 32 (3) 141-147 Phase Relations of Minerals and Structure of the Earth's Interior Masaki Akaogi (Received April 2, 2005; Accepted May 11, 2005) In high-pressure high-temperature conditions
ｎｓｇ０２－１３／ｋｙ０４５０５９３０１６０００３３２１０
φ φ φ φ κ κ α α μ μ α α μ χ et al Neurosci. Res. Trpv J Physiol μ μ α α α β in vivo β β β β β β β β in vitro β γ μ δ μδ δ δ α θ α θ α In Biomechanics at Micro- and Nanoscale Levels, Volume I W W v W
Report of Special Research from the National Institute for Environmental Studies, Japan NATIONAL INSTITUTE FOR ENVIRONMENTAL STUDIES
Report of Special Research from the National Institute for Environmental Studies, Japan NATIONAL INSTITUTE FOR ENVIRONMENTAL STUDIES ) V O Cvolatile organic compounds V O C V O C 1940 10 1 1 N Ox V
The Eevaluation One Bottle Type Silane Coupling Agents Masahiro Aida, Hideo Kanaya, Taira Kobayashi, Keiji Utsugizaki, Yoshizumi Murata, Tohru Hayakaw
The Eevaluation One Bottle Type Silane Coupling Agents Masahiro Aida, Hideo Kanaya, Taira Kobayashi, Keiji Utsugizaki, Yoshizumi Murata, Tohru Hayakawa* and Kozo Horie* Abstract: Here is investigated the
2_R_新技術説明会（佐々木）
% U: 6.58%, Np, Am:.5%, Pu:.% 5.8% Cs 6.5% Sr %.9%Mo 8.74% Tc.9% TODA C 8 H 7 C 8 H 7 N CH C CH N CH O C C 8 H 7 O N MIDOA C 8 H 7 DOODA NTA + HN(C 8 H 7 ) + H O DCC + SOCl + HN(C 8 H 7 ) + Cl TODA (TODA)
<32322D8EA D89CD8D8797B294C E8A968388DF814589C193A1899B E5290EC8F438EA12D966B8A4393B98F5C8F9F926E95FB82CC8BC7926E F5
No.432008pp.287 302 Climatological Characteristics of Local Wind in the Tokachi District, Hokkaido, JAPAN Takashige KAWAI, Mai NAKAJYO, Hisashi KATO and Shuji YAMAKAWA Received September 30, 2007 Climatological
【実績報告書】後藤.doc
Edy M.ArsadiReseach Center for Geotechnology-LIPI vol.24,no2(2007)35-42. 23 (2007) 23 (2007) 115 (2007) (Ni,NH4) 5 (2007) 19 (2007) Tb3+ 19 (2007) Yoshiaki GotoToshio OgiwaraTaiji MatsumotoMasato Yoshida,Zeolitization
資源と素材
(Shigen to Sozai) Vol.116 p. 285 290 (2000) 共存硫酸塩を含む強酸性 MnSO 4 溶液中のオゾン酸化によって生成した沈殿の X 線回折および放電特性 * 西村忠久 1 梅津良昭 2 X-ray Diffraction and Discharge Behavior of Precipitates Produced by Ozone Oxidation in
宇宙理論研究室ガイダンス
60 S.L.Glashow Glashow : Interaction Warner Books 4 4 1978 12 CMB 10-40 -40 CMB / The universe in a nutshell A H He C, O Ne, Mg Si Fe Sphere(0.1 cylinder (0. slab (0. Cylinder hole (0. Spherical hole
Trip Trip Trip
- - - - 1999 Leonid MAC Multi-Instrument Aircraft Campaign November 8-23, 1999 1998-2002 (2001 ) Predictions, Observational Plans and Results for Leonid 1998-2002. Photo Gallery taken by Photographic Camera
01津行篤士ほか.indd
Biosphere Sci. 55 1-6 (2016) 耳石 Sr:Ca 比によって推定した利根川産大型ヤマメの回遊履歴 1) 2) 3) 1) * 1) 739 8528 1-4-4 2) 375-0011 3) 371-0036 13 要旨 8 Sr:Ca 3 5 4 243km キーワード : Sr:Ca 緒 言 Oncorhynchus masou masou 1980 2014 4 2014
Microsoft Word - ganseki-2
岩石学 -2 2010.4.20 [2] 造岩鉱物 A. 鉱物の結晶構造による分類 1. 晶系 :crystal system 単位格子の対称性に基づく 軸率 軸角で単位格子の対称性を分類 立方晶系 cubic 軸率 :1:1:1, 軸角 =90 正方晶系 tetragonal a:a:c, 軸角 =90 六方晶系 hexagonal a:a:a:c, 軸角 =120 90 三方晶系 trigonal
202
201 Presenteeism 202 203 204 Table 1. Name Elements of Work Productivity Targeted Populations Measurement items of Presenteeism (Number of Items) Reliability Validity α α 205 α ä 206 Table 2. Factors of
<362D985F95B62D97E996D88F47986190E690B62D936390A391A5975990E690B62E706466>
No.50 pp.101 111, 2014 Komazawa Journal of Geography Origin and Geochemistry of a Flowing Confined Groundwater at the Northern Foot of Mt. Iwate, Northeast Japan SUZUKI Hidekazu and TASE Norio Ca-HCO 3
chap1_MDpotentials.ppt
simplest Morse : simplest (1 Well-chosen functional form is more useful than elaborate fitting strategies!! Phys. Rev. 34, 57 (1929 ( 2 E ij = D e 1" exp("#(r ij " r e 2 r ij = r i " r j r ij =r e E ij
42 3 u = (37) MeV/c 2 (3.4) [1] u amu m p m n [1] m H [2] m p = (4) MeV/c 2 = (13) u m n = (4) MeV/c 2 =
![42 3 u = (37) MeV/c 2 (3.4) [1] u amu m p m n [1] m H [2] m p = (4) MeV/c 2 = (13) u m n = (4) MeV/c 2 =](/thumbs/73/68712188.jpg "42 3 u = (37) MeV/c 2 (3.4) [1] u amu m p m n [1] m H [2] m p = (4) MeV/c 2 = (13) u m n = (4) MeV/c 2 =")
3 3.1 3.1.1 kg m s J = kg m 2 s 2 MeV MeV [1] 1MeV=1 6 ev = 1.62 176 462 (63) 1 13 J (3.1) [1] 1MeV/c 2 =1.782 661 731 (7) 1 3 kg (3.2) c =1 MeV (atomic mass unit) 12 C u = 1 12 M(12 C) (3.3) 41 42 3 u
Introduction Jones & Palme (2000), Jones & Hood (990), Mueller et al. (988) ρ~3.34g/cm 3, MI~0.39 (<400km) Nakamura et al. (982), Kuskov & Kronrod (99
Introduction Jones & Palme (2000), Jones & Hood (990), Mueller et al. (988) ρ~3.34g/cm 3, MI~0.39 (
"Moir6 Patterns on Video Pictures Taken by Solid State Image Sensors" by Okio Yoshida and Akito Iwamoto (Toshiba Research and Development Center, Tosh
"Moir6 Patterns on Video Pictures Taken by Solid State Image Sensors" by Okio Yoshida and Akito Iwamoto (Toshiba Research and Development Center, Toshiba Corporation, Kawasaki) Reproduced resolution chart
The Effect of the Circumferential Temperature Change on the Change in the Strain Energy of Carbon Steel during the Rotatory Bending Fatigue Test by Ch
The Effect of the Circumferential Temperature Change on the Change in the Strain Energy of Carbon Steel during the Rotatory Bending Fatigue Test by Chikara MINAMISAWA, Nozomu AOKI (Department of Mechanical
宇宙環境利用蛋白質結晶生成応用利用実証プロジェクトのご案内
16 8 23 1. 14 17 ISS JEM (JAXA) 2. JAXA 14 6 1 4 1 02/02/2003 29/08/2003 29/01/2004 11/08/2004 Baikonur Kazakhstan Progress 03/05/2003 28/10/2003 29/04/2004 19/10/2004 Kazakhstan Soyuz 13 weeks 9 weeks
untitled
COLAK Mehmed 11000 305 305 180 10000 9000 8000 160 140 120 7000 100 6000 1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 80 GH IGF-1 GH GH 5 4 3 2 1 0 2 3 4 5
神奈川県西部山北南高感度地震観測井の掘削および孔内検層，Borehole Drilling and Physical Properties of the Yamakita-minami Seismic Observatory in Western Ka
*1 *2 *3 *4 *5 *5 *6 *6 *2 *7 *5 *4 *5 *5 *6 *6 Borehole Drilling and Physical Properties of the Yamakita-minami Seismic Observatory in Western Kanagawa Prefecture, Central Honshu, Japan Hiroki HAYASHI
FC741E2_091201
T101-1587-04 1 2 2 0 0 9 2 0 0 8 0 9 0 1 0 5 0 9 1 4 0 5 1 0 5 5 1 2 3 4 4 5 6 7 8 9 1 2 3 0 3 3 0 2 1 1 5 0 1 3 3 3 0 2 0 3 0 3 4 0 9 1 1 0 9 0 9 1 1 5
untitled
but ( Intro Experimental Results&Discussion or kinetics Prof. Juan Manuel Garcia Ruiz Gypsum (36 feet ~ 11 m) CaSO 4 2H 2 O Cueva de los Cristales (Cave of Crystals) http://news.nationalgeographic.com/news/2007/04/photogalleries/giant-crystals-cave/
18 2 20 W/C W/C W/C 4-4-1 0.05 1.0 1000 1. 1 1.1 1 1.2 3 2. 4 2.1 4 (1) 4 (2) 4 2.2 5 (1) 5 (2) 5 2.3 7 3. 8 3.1 8 3.2 ( ) 11 3.3 11 (1) 12 (2) 12 4. 14 4.1 14 4.2 14 (1) 15 (2) 16 (3) 17 4.3 17 5. 19
<4D F736F F F696E74202D2091E63589F1926E8B85955C917782CC8D5C90AC82C AC2E707074>
第 5 回 地球表層 ( 地殻 ) の構成と組成 地球の平均密度は 5.52g/cm 3 である 地球表層の地殻をつくる花崗岩の密度は 2.67g/cm 3 玄武岩の密度は 2.80g/cm 3 であり ともに地球の平均密度の半分ほどしかない 石 砂粒の平均密度は 3.0g/cm 3 以下である この事実は 地球内部が地球表層の岩石よりずっと重い物質でできていることを示唆している 地震波の解析から
E-2 A, B, C A, A, B, A, C m-cresol (NEAT) Rh S m-cresol m-cresol m-cresol x x x ,Rh N N N N H H n Polyaniline emeraldine base E-3 II
E 7, 8, 9 E-1 A, B B A, A, A,, [Novoselov, et al., Science 306, 666, (2004)].,,,.,,,.,. (t a, t b, t c ), [PRB.74, 033413, (2006)],.,, t b /t a t c /t a 0.5., [Ni, etal., ACS, Nano2, 2301, (2008)],, [Zhou