検索結果 171 件
| 著者 | Yamamoto, Dai| Ghosh, Souvik| Ganesh, Balasubramanian| Krishnan, Triveni| Chawla-Sarkar, Mamta| Alam, Mohammed Mahbub| Aung, Tin Sabai| Kobayashi, Nobumichi| |
|---|---|
| 発行日 | 2010-07 |
| 出版物タイトル | Journal of General Virology |
| 巻 | 91巻 |
| 号 | 7号 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 中野 滿隆| |
|---|---|
| 発行日 | 1932-05-31 |
| 出版物タイトル | 岡山医学会雑誌 |
| 巻 | 44巻 |
| 号 | 5号 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 谷野 順造| |
|---|---|
| 発行日 | 1954-12-30 |
| 出版物タイトル | 岡山医学会雑誌 |
| 巻 | 66巻 |
| 号 | 12号 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 高木 良二| |
|---|---|
| 発行日 | 1955-04-30 |
| 出版物タイトル | 岡山医学会雑誌 |
| 巻 | 67巻 |
| 号 | 3-4号 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 河井 清| |
|---|---|
| 発行日 | 1957-01-31 |
| 出版物タイトル | 岡山医学会雑誌 |
| 巻 | 69巻 |
| 号 | 1号 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 三宅 健二| |
|---|---|
| 発行日 | 1959-09-30 |
| 出版物タイトル | 岡山医学会雑誌 |
| 巻 | 71巻 |
| 号 | 10-2号 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 池田 宏| |
|---|---|
| 発行日 | 1959-06-30 |
| 出版物タイトル | 岡山医学会雑誌 |
| 巻 | 71巻 |
| 号 | 7-1号 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 片山 靖夫| |
|---|---|
| 発行日 | 1989-06 |
| 出版物タイトル | 岡山医学会雑誌 |
| 巻 | 101巻 |
| 号 | 5-6号 |
| 資料タイプ | 学術雑誌論文 |
| JaLCDOI | 10.18926/40426 |
|---|---|
| タイトル（別表記） | CHEMICAL STUDIES ON THERMAL ALGAE (I) ON INORGANIC CONSTUENTS (1) |
| フルテキストURL | pitsr_012_011_014.pdf |
| 著者 | 梅本 春次| 御船 政明| |
| 抄録 | The thermal algae which grew in the thermal water of Misasa Hot Springs, namely Mastigocladus laminosus Cohn (1), Phormidium ambiguum Gomont (2), Oscillatoria Cortiana (Menegh.) Gomont (3) and the fresh water alga which grew in the River Misasa, namely Rhizocolonium hieroglyphicum (4) were collected. The spectrographic analysis and quantitative chemical analanalysis of the ashes of the algae gave the following results : 1. All four algae contained Cu, Zn, Al, Pb, Mn, Mo besides the phisiological elements. 2. Two algae, (1) and (2) which grew in thermal water rarely mixed with the river water, contained Ti and considerable amount of Ge. 3. The highest content of Si and highest value of ash per cent were those of (1), and their values were 27.22 % and 26.44 %. 4. The highest content of Fe and Mn were those of (2), and their values were 17.80 % and 3.27 %. 5. Great difference was not detected between the ratios of MgO/CaO of (1) and (2), and their values were 0.13 (1) and 0.14 (2). |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1953-09 |
| 巻 | 12巻 |
| 開始ページ | 11 |
| 終了ページ | 14 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002509303 |
| JaLCDOI | 10.18926/40421 |
|---|---|
| タイトル（別表記） | CHROMATOGRAPHIC ANALYSIS OF METALS BY ORGANIC REAGENTS (Ist Report) |
| フルテキストURL | pitsr_005_001_043.pdf |
| 著者 | 芦沢 峻| |
| 抄録 | The principle of this method is to combine the metals with organic reagents, then extract them with non-polar solvents, and determine them by making chromatograph with adequate adsorbents. Dithizone is used to determine Hg, Cd, Bi, Ag, Cu, Zn, Ni, Co, Tl, Pb, Pd and its isotopes, Pt group, Au, etc. Diphenylcarbazone is applicable to determine Hg, Cu, Zn, Ni, etc. Xanthate is useful to determine Mo, Cu, Ni, Co, etc. α-orβ- Nitrosoβ- orα-naphthol is used to determine Fe, Co, earth acids etc. Diethyldithiocarbamate is used to determine Mo, Cu, Ni, Co, Fe, etc. Oxine series are useful to determine Cu, Ni, Fe, V, rare earth etc. α-indolcarbonic acid is applied to determine Fe, Co, rare earth etc. Acethyl acetone is used to determine Th, Fe, etc. Some other organic reagents were used moreover. There are some elements of which necessary condition for quantitative determination is still not decided or the order of adsorption is indefmite. As adsorbents alkaline, neutral or acid alumina, diatom earth and aluminate, magnesium carbonate, calcium carbonate, urea formaline resin, heulandite, mordenite, desmine, chabazite etc· were used. With this method the author tryed severd determinations on rocks, minerals, mineral springs, organisms etc. The contento; of Cu, Zn, Ni and Co in rocks were 0.007, 0.008, 0.002 and 0.004% respectively. Cobalt content proved to be more than that of nickel. The mercury content of rocks was proved to be 10 times more to Clarke number, bismuth and cadmium content as same as or less than Clarke number. Silver in plants, soil and mineral waters, platinum in serpentine; mercury, cadmium, bismuth etc in mineral waters, trace heavy metals in organism, etc were determined. Radium B and Thorium B in hot spring waters were used as tracer. As organic solvents methyl-, ethyl-, butyl-, amy1-, octyl alcohol, dioxan, benzol, toluene, xylol, petroleum ether, ether, ethylacetate, chloloform, carbon tetrachloride, carbon disulfide etc were applied. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1951-08 |
| 巻 | 5巻 |
| 開始ページ | 1 |
| 終了ページ | 43 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/15296 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002509302 |
| JaLCDOI | 10.18926/40384 |
|---|---|
| タイトル（別表記） | CHEMICAL STUDTES ON THE RIVER WATERS IN THE INFECTED LOCALITIES WITH KATAYAMA-DISEASE (II) |
| フルテキストURL | 009_043_048.pdf |
| 著者 | 杉原 健| 明石 務| 横井 信| |
| 抄録 | In the previous report, one of the authors, T. Sugihara, discussed the results of chemical analysis of waters in the infected localites with Katayama-disease in the whole neighbourllood of Kannabe-cho, Fukayasu-distriict, Hiroshima-Prefecture. In this report, the authors discussed the results obtained in Yamanashi prefecture, and in the area drained by Chikugo River, and found the following facts: 1) The amount of KMnO(4) consumed and the copper content were high as in the previous report. 2) The calcium content was 7.3~22.2 mg/ℓ in the river waters of this report, but it was 18.7~38.2 mg/ℓ in the waters in the places of the previous paper. And in the previous report the author pointed out that the calcium content was fairly higher in the waters in the infected localities with Katayama disease than in the non-infected localities. But as the calcium content was relatively lower this time than in the previous investigation, more research is intended to reach definite conclusion. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1953-01 |
| 巻 | 9巻 |
| 開始ページ | 43 |
| 終了ページ | 48 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40388 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532516 |
| JaLCDOI | 10.18926/40319 |
|---|---|
| タイトル（別表記） | REPORT OF THE CHEMICAL ANALYSIS OF MISASA HOT SPRINGS, TOTTORI PREFECTURE |
| フルテキストURL | 016_001_018.pdf |
| 著者 | 大島 良雄| 御船 政明| 山田 尚春| 上山 昭子| |
| 抄録 | The water samples of 55 springs of Misasa were analysed in the years 1950～1951. The temperatures of the waters ranged from 44° to 85° C. Radon content ranged from 34.1 to 2360×10(-10) curies per liter. pH 6.2～7.5. Evaporation residue: 534～1940 mg/kg. K(+) :10.4～47.3mg/kg. Na(+) : 140.4～574mg/kg. Ca(2+) : 7.56～49.06mg/kg. Mg(2+) : 0.11～15.3mg/kg.. Fe(2+) : 0.10～0.67mg/kg. Cl(-) : 138～854mg/kg. SO(4)(2-) : 29.2～187mg/kg. HCO(3)(-) : 74.8～370mg/kg. HBO(2)(-) : 1.80～19.6mg/kg. S(2)O(3)(2-) : o.62～3.69mg/kg. Radon sources seem to exist at shallow places under the ground and the radon in the thermal wacer is supposed to have been derive partly from the ground water which also contains considerable amount of radon. A close linear correlation (r=0.751) was proved between the sulfate and the chloride ion contents. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1956-01 |
| 巻 | 16巻 |
| 開始ページ | 1 |
| 終了ページ | 18 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40318 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532473 |
| JaLCDOI | 10.18926/40265 |
|---|---|
| タイトル（別表記） | Studies on Paper-Analysis in the Field of Balneology (I) Studies on Iron in Serum by Means of Parper-Electrophoresis and Paper-Chromatography |
| フルテキストURL | 022_037_054.pdf |
| 著者 | 石橋 丸応| |
| 抄録 | 1. The author showed by means of paper-electrophoresis using o-nitrosoresorcinmonomethylether (hereafter N. R. M. E.), a colourdeveloping reagent, that iron in serum combines with β-fraction of serum protein. 2. The author proposed a new method for the determination of serum iron by means of paper-chromatography. Procedure is as follows. In a centriguged tube, 0.5 ml. of clear serum is taken, acidified with 0.15 ml. of 20% HNO(3), and allowed to stand for 20 minutes. After addition of 0.2 ml. of saturated solution of CH(3)COONa and 1 ml. of acetic acid-sodium acetate buffer solution (pH: 3.8), the mixture is kept for at least 10 min. and filtered through Toyo-filter-paper No.5 A. The clear filtrate is taken in a stoppered test tube (the inside diameter: 1.2 cm.; height: 15 cm.). To this filtrate are added 0.2 ml. of 20% Hydroxylamine hydrochloride and 0.25 ml. of saturated aqueous solution of N. R. M. E. After being allowed to stand for at least 20 min., the mixture is shaken with 5 ml. of carbon tebrachloride. Then the excess of N. R. M. E. is removed. The supernatant aqueous solution (0.2 ml.) is used for a determination sample. The sample is placed on the paper (Toyo,filter-paper No.51 or 50) in a thin line at a distance of 10 cm. from the edge, and the spots are developed with 90 % ethylalcohol. After development for 4-6 hours, a green-coloured linear spot appsars at a distance of 12-16 cm. from the origin-point. Spot intensity at 670 mμ is measured with Natsume's densitometer, and from this, concentration of Fe can be estimat.ed on the standard graph (Fig. 5). 3, Effects of radioactive thermal spring bathing and internal use of vitriol water upon serum iron levels were studied with the result.s as follows. The above-mentioned author's method of determining the iron level in a small amount of serum is very convenient in investigating iron metabolism in the field of balneotherapy. The author examined changes of iron levels in serum after radioactive thermal bathing as well as after internal use of acid vitriol water. a) The iron levels in serum were maasurecl by the author's method before and 5, 30 and 60 minutes after the radioactive thermal bath (Rn-content: 10-30 Mache, 42-3°C., for 10 min,). The iron levels in the serum of healthy subjects showed no significant change after the thermal bathing. b) Yanahara Mineral Water (an acid vitriol water, pH; 2.2) contains 0.045 gm. of Cl(-), 12.35 gm. of SO(4)(--), 2.5 gm. of Fe(++)+Fe(+++), 0.0938 gm. of Al(+++) and 0.0001 gm. of Cobalt in one liter. i) Thirty ml. of Yanahara, water diluted with plain water to 200 ml. (Fe(++) content: ca. 75 mg.) and administered to health fasting subjects orally. As a control matter, 0.65 gm. of Glukon-F powder (Fe(++) content.: ca. 75 mg.) was then given. Blood samples were taken from the cubital vein before and 1, 3 and 6 hours after the intake of the dtriol water. Iron contents of the serum samples were measured by the author's paper chromatographic method. The results were shown in the table and the figure. The iron contents of the serum after the intake of the mineral water were higher than in the case of the control. ii) Two ml. of Yanahara vitriol water was administered to rabbits with the aid of a stomach tube, and serum iron levels wera determined before and 1, 3, 4 and 6 hours after the administration. An amount of 0.05 gm. of Glukon-F powder was dissolved in 5 ml. of plain water, and this solution was given to rabbits as a control. After the internal use of vitriol water, iron levels in serum rose and remained unexpactedly high for about 1-4 hours, in a manner that did not. correspond to the amount of iron in the given mineral water. So that it was suspected that the iron originally contained in the living subjects had been mobilized by the intake of vitriol water. Iron levels in serum after administration of a solution of Glukon-F powder were lower than in the case of the mineral water. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1958-07 |
| 巻 | 22巻 |
| 開始ページ | 37 |
| 終了ページ | 54 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40263 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532359 |
| JaLCDOI | 10.18926/40252 |
|---|---|
| タイトル（別表記） | Studies on Paper-analysis in the Field of Balneology. (II) 1. A New Method for the Determination of Cobalt in Blood. 2. Effects of Radioactive Thermal Bathing and Internal Use of Vitriol Water upon Cobalt Levels in Blood. |
| フルテキストURL | 024_029_053.pdf |
| 著者 | 石橋 丸応| |
| 抄録 | 1. A new method for the determination of cobalt in blood. The author proposed a new method for the determination of cobalt in blood by means of paper-chromatography. The procedure is follows. In a Kjeldahl colben, 5 m!. of blood is taken, and turned into wet ash with 3 ml. of HNO(3), 0.5 ml. of H(2)SO(4) and 1.5 ml. of HClO(4) and the ash aqueus solution is then neutralized with ammonium hydroxid, the neutralization being indicated by the development of color of 0.1% of p-nitrophenol (one drop) added to the solution. After addition of 2 ml. of 40% ammonium citrate, 0.5 ml. of 20% Na(2)S(2)O(3), 3～5 drops of H(2)O(2) and 1 ml. of o-nitrosoresorcine monomethyl ether (hereafter N.R.M.E.), the mixture is left for at least 15 minutes and the aqueus solution is taken in a stoppered test tube (inside diameter: 1.3 cm., hight: 16.5 cm.). The mixture is shaken with 2 ml. of carbon tetrachloride. Carbon tetrachloride is shaken with 5 ml. of 20% Na(2)CO(3) solution. Then the excess of N.R.M.E. is removed and carbon tetrachloride is concentrated on water bath to 0.3～0.5 ml. and all CCl(4) is used for a determination sample. The sample is placed on the paper (Toyo-filter paper No. 50 or 51A) in a thin line at a distance of 3 cm. from the edge, and the spot is developed with a mixture of 20 ml. of CCl(4) and 1 ml. of 90% ethylalcohoI. After development for 30～40 min., an orange-colored linear spot appears at a distance of 9～10 em. from the origin point. Spot intensity is measured at 460 mμ with Natsume's densitometer and quantitative estimation is made comparing with the standard graph. 2. Effects of radioactive thermal spring bathing and internal use of vitriol water upon cobalt levels in blood. As the author's method above-mentioned is able to determine the cobalt level in a small amount of blood, it is very convenient in investigating cobalt metabolism in the field of balneology. The author examined the changes of cobalt levels in blood after radioactive thermal bathing as well as after internal use of acid vitriol water. a. By the author's method cobalt in normal human blood was 0.4～3.6γ/100ml. in man (average: 1.6±0.4γ/100ml.) and 0.2～2.2γ/100ml. in woman (average: 0.7±0.3γ/100ml.). b. The cobalt levels in blood were measured by the author's method before and 5, 30, 60 minutes after the radioactive thermal single bathing, and before and 1, 2, 3, 4 weeks after a series of radioactive thermal baths (Rn-content: 10～30 Mache, 42～3°C., for 10 minutes). The cobalt levels in the blood of healthy subjects showed no significant change after the thermal single bathing, but those of patients with rheumatoid arthritis showed a slight increase on 3rd or 7th day and a fall on 2nd week of a series of radioactive thermal baths and then tended to return to the initial levels during the 3rd and 4th weeks of spa treatment. c. Thirty ml. of Yanahara mineral water (an acid vitriol water, pH: 2.2) was diluted with plain water to 200 ml. (Co(++)content: ca.3γ) and administered to healthy fasting subjects orally. Blood samples were taken from the cubital vein before and 1, 3, 6 hours after the intake of the vitriol water. The cobalt levels in the blood showed an increase of 14% of the initial levels at 1 and 3 hours and a decrease of 22% at 6 hours after the drinking of Yanahara mineral water. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1959-01 |
| 巻 | 24巻 |
| 開始ページ | 29 |
| 終了ページ | 53 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40250 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532366 |
| JaLCDOI | 10.18926/40246 |
|---|---|
| タイトル（別表記） | Studies on the Chemical Composition and Levels of Ground Water at Misasa Hot Springs |
| フルテキストURL | 025_013_024.pdf |
| 著者 | 坂上 正信| |
| 抄録 | The water levels of the thermal springs and the ground water levels were measured and the contour of the water table was obtained. The contour was disturbed at two regions in which many springs issue. The thermal and ground waters were sampled all over the springs district, and the water temperatures were measured when they were sampled. The chloride, bicarbonate, sulfate, calcium and magnesium content was also determined. In addition, the analytical methods for the determination of arsenic, phosphorus and acid-soluble iron were improved. Also the concentration of these elements was determined. Based on the results of the observations and chemical analysis, the relations between the water temperatures and content of chemical constituent and the chloride content were checked respectively. Positive correlations were found in the relations between water temperature～Cl(-), HCO(3)(-)～Cl(-), SO(4)(2-)～Cl(-), Ca(2+)～Cl(-), and As～Cl(-). Furthermore, the regional differences were detectable in the ratios of water temperature to chloride content and of bicarbonate to chloride content, nevertheless the correlation as a whole were valid. The diversity and regional differences of the chemical composition of the waters were explained as due to the differences in the mixing proportion of the magmatic thermal water and the varying kinds of ground water at the deep site in the ground and at the site near the ground surfaces. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1959-05 |
| 巻 | 25巻 |
| 開始ページ | 13 |
| 終了ページ | 24 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40244 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| JaLCDOI | 10.18926/40236 |
|---|---|
| タイトル（別表記） | Geochemical Studies on the Area of Hot Springs in Hamamura and Shikano District Comparison of Characteristics of Hot Springs in the Central part of Tottori Prefecture, Japan |
| フルテキストURL | 027_025_044.pdf |
| 著者 | 阪上 正信| 御船 政明| |
| 抄録 | The thermal and ground waters were sampled in the hot springs district of Hamamura-Katsumi and Shikano and in their neighborhoods. The water temperatures were measured when they were sampled. Among the major chemical constituents, the chloride, sulfate, bicarbonate (methyl-orange alkalinity), calcium and magnesium content was determined. Furthermore, as the minor constituents, the arsenic and phosphorus content was also determined. The uranium, radium and radon content was determined in some samples of hot springs. Based on the results of chemical analysis, the relations between the chloride content and the content of other chemical constituents were cheked respectively. Positive correlations were found in the relations between water temperature-Cl(-), SO(4)(2-)-Cl(-), Ca(2+)-Cl(-) and As-Cl(-), although the ratios of each content showed the different characteristic in Hamamura-Katsumi compared with that in Shikano. In the samples of Hamamura-Katsumi where the thermal waters were pumped out from the sedimentary beds of volcanic rocks, the sulfate and calcium content was relatively richer compared with the content of these ions in the samples of Shikano where granitic rocks underlay as the basement in the fairly shallow depth from the cground surface. These characteristics were also noticed when the chemical compositions of other hot springs in the central part of Tottori prefecture were examined. In the neighborhood of the hot springs district mentioned-above, distinctive indications of hot spring were found at Kinashi which was placed between Hamamura and Shikano, comprehensively examining the content of chemical constituents in the ground water samples in this region. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1961-01 |
| 巻 | 27巻 |
| 開始ページ | 25 |
| 終了ページ | 44 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532371 |
| JaLCDOI | 10.18926/40197 |
|---|---|
| タイトル（別表記） | Minor elements of the Nanbu Kotai of Nakatsugo Deposits, Ningyo Toge Uranium Mine |
| フルテキストURL | pitsr_036_023_030.pdf |
| 著者 | 渡辺 晃二| |
| 抄録 | The Nakatsugo Deposits are the main deposits of the Ningyo Toge Mine which is located in the northern part of Okayama Prefecture. Nakatsugo Deposits consists of the two main ore body, namely, Nanbu Kotai (southern ore body) and Hon Kotai (main ore body). Nanbu Kotai is occupied mostly by the unoxidized zone and high grade ores containing ningyoite (n% U) are widely found in the basal conglomerates. Minor elements in the common rocks such as basal granites, conglomerates, sandstones, dikes, and shales as well as the uraniferous ores were determined quantatively by fluorescent X-ray spectrometric analysis (for U, Zr, Y, Sr, As, and Fe) and spectrophotometric analysis (for Ni and Co). As the results of this study, it is found that the uraniferous ores are characterised by extremely high contents of Zr, Y, Sr, and As, which show positive and linear correlation with the U contents. It is confirmed that As is concentrated in pyrite which is usually associated with the uraniferous ores. Elements such as Ni and Co are slightly concentrated both in the uraniferous ores and andesite dikes. This fact may suggest some genetic relationship among them. However, it does not seem to be plausible to draw any definite conclusion on the origin of the uranium deposits from these relationships. As to the minor element distribution in common rocks, no systematic variation was found except for the rock samples closely associated with the ore deposits. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1966-10-25 |
| 巻 | 36巻 |
| 開始ページ | 23 |
| 終了ページ | 30 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002400933 |
| 著者 | Muncharoen, Sasithorn| Sitanurak, Jirayu| Tiyapongpattana, Warawut| Choengchan, Nathawut| Ratanawimarnwong, Nuanlaor| Motomizu, Shoji| Wilairat, Prapin| Nacapricha, Duangjai| |
|---|---|
| 発行日 | 2008-05-17 |
| 出版物タイトル | Microchimica Acta |
| 巻 | 164巻 |
| 号 | 1号 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | Kikuchi, Kazuhiro| Ekwall, Hans| Tienthai, Paisan| Kawai, Yasuhiro| Noguchi, Junko| Kaneko, Hiroyuki| Rpdriguez-Martinez, Heriberto| |
|---|---|
| 発行日 | 2002-07-25 |
| 出版物タイトル | Zygote |
| 巻 | 10巻 |
| 号 | 4号 |
| 資料タイプ | 学術雑誌論文 |
| JaLCDOI | 10.18926/AMO/32819 |
|---|---|
| フルテキストURL | fulltext.pdf |
| 著者 | Okamoto, Osamu| Yamamoto, Yuji| Inagaki, Sachiyo| Yoshitome, Kei| ishikawa, Takaki| Imabayashi, Kiyomi| Miyaishi, Satoru| Ishizu, Hideo| |
| 抄録 | Allele and genotype frequencies for 15 short tandem repeat (STR) polymorphisms--D3S1358, TH01, D21S11, D18S51, Penta E, D5S818, D13S317, D7S820, D16S539, CSF1PO, Penta D, vWA, D8S1179, TPOX and FGA--in a Japanese population were estimated. No deviations of the observed allele frequency from Hardy-Weinberg equilibrium expectations were found for any of the systems studied. Between 2 new pentanucleotide STR loci, Penta E and Penta D, for which there is only limited data regarding the allelic distribution in Japanese, the Penta E locus was found to be highly polymorphic and exhibited a tri- or tetra-modal distribution pattern having allelic peaks with 5, 11, 15 and 20 repeats. The distribution was significantly different from that of the other ethnic groups. Statistical parameters of forensic importance, the power of discrimination (PD), observed and expected heterozygosity values (H), polymorphism information content (PIC), power of discrimination (PD), matching probability (pM), power of exclusion (PE), and typical paternity index (PI), were calculated for the loci. These parameters indicated the usefulness of the loci in forensic personal identification and paternity testing among Japanese. The systems Penta E, FGA, D18S51 and D8S1179 were the most informative. This method was successfully applied to forensic personal identification and paternity testing among Japanese, thereby confirming its efficacy for forensic practice. |
| キーワード | population data DNA typing short tandem repests personal identification paternity testing |
| Amo Type | Article |
| 出版物タイトル | Acta Medica Okayama |
| 発行日 | 2003-04 |
| 巻 | 57巻 |
| 号 | 2号 |
| 出版者 | Okayama University Medical School |
| 開始ページ | 59 |
| 終了ページ | 71 |
| ISSN | 0386-300X |
| NCID | AA00508441 |
| 資料タイプ | 学術雑誌論文 |
| 言語 | 英語 |
| 論文のバージョン | publisher |
| 査読 | 有り |
| PubMed ID | 12866745 |
| Web of Science KeyUT | 000182520400003 |