検索結果 1446 件
著者 | 国塩 勝三| |
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発行日 | 1990-06 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 102巻 |
号 | 5-6号 |
資料タイプ | 学術雑誌論文 |
著者 | 馬場園 常子| |
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発行日 | 1990-06 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 102巻 |
号 | 5-6号 |
資料タイプ | 学術雑誌論文 |
著者 | 鈴木 茂樹| |
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発行日 | 1990-04 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 102巻 |
号 | 3-4号 |
資料タイプ | 学術雑誌論文 |
著者 | 河上 雄之介| |
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発行日 | 1990-04 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 102巻 |
号 | 3-4号 |
資料タイプ | 学術雑誌論文 |
著者 | 戸田 洋子| |
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発行日 | 1990-04 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 102巻 |
号 | 3-4号 |
資料タイプ | 学術雑誌論文 |
著者 | 清水 義央| |
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発行日 | 1990-04 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 102巻 |
号 | 3-4号 |
資料タイプ | 学術雑誌論文 |
JaLCDOI | 10.18926/40426 |
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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 |
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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 | 10.18926/40413 |
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タイトル(別表記) | STUDIES ON THE AGING OF MINERAL WATERS (II) CHANGES IN THE SILICATE CONTENT OF THERMAL WATERS OF MISASA AFTER FLOWING OUT |
フルテキストURL | pitsr_011_014_018.pdf |
著者 | 杉原 健| |
抄録 | The author determined the silicate content of the thermal water of Hisui-no-Yu, Misasa, Tottori Prefecture, Japan, at varying times after flowing out, and obtained the following results: 1) The change in the silicate content after flowing out is at first remarkable. 2) The velocity of the changes in the silicate content has a tendency to be faster in the sample that is kept in the vessel with a wide water surface than in the one that has a smaller surface. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1953-06 |
巻 | 11巻 |
開始ページ | 14 |
終了ページ | 18 |
ISSN | 0369-7142 |
関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40410 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002509298 |
JaLCDOI | 10.18926/40412 |
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タイトル(別表記) | STUDIES ON THE AGING OF MINERAL WATERS (I) CHANGES IN THE RADON CONTENT OF THERMAL WATERS OF MISASA AFTER FLOWING OUT |
フルテキストURL | pitsr_011_001_013.pdf |
著者 | 杉原 健| |
抄録 | The author determined the radon content of the thermal waters of Misasa, Tottori Prefecture Japan, at various times after flowing out, and obtained the following results: 1) The velocity of variation is expressed by a simple equation with respect to the radon content. At thermal temperaturee of 41.5-41.8°C and room temperature of 24.3-28.0°C, a following exrerimental equation was obtained, u:;ing a beaker with a inner diameter of about 17 cm and a height of 27 cm, log a = -0,0048t + 2.59 a: radon content in Mache unit. t : time in minute. 2) A close relation was observed between the room temperature and the rate of variation of radon, and also between the thermal temperature and the rate of variation of radon, that is, the rate of variaton of radon was proportional to the room temperature and the thermal temperature respectivly, as it is clearly seen from the distribution coefficient of radon. 3) There exists a c1ose relation between the velocity of variation of radon and the surface area being in contact with air, that is, the velocity was generally proportional to the square root of the surface area, or to the radius of the surface. 4) The velocity of variation of radon content was roughly inversely proportional to relative humidity of air. 5) Betweeen the range of sodium chloride concentrations from 0.1 to 40.1 g. per liter no difference was proved concerning the velocities of variation in radon content. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1953-06 |
巻 | 11巻 |
開始ページ | 1 |
終了ページ | 13 |
ISSN | 0369-7142 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002509297 |
JaLCDOI | 10.18926/40404 |
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タイトル(別表記) | CHEMICAL COMPOSITION OF SEKIGANE AND KAlKE HOT SPRINGS, TOTTORI PREFECTURE |
フルテキストURL | pitsr_010_010_012.pdf |
著者 | 御船 政明| |
抄録 | The waters of six springs of Sekigane and one spring of Kaike were analyzed by the author in 1951. All the springs of Sekigane belong to the simple radioactilTe thermals. And Kaike Hot Spring belongs to a calcium chloride containing saline spring, its water temperature being 73,5℃. The radon content of Sekigane Spring waters ranged from 57 to 137×10(-10) Curie units per liter. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1953-03 |
巻 | 10巻 |
開始ページ | 10 |
終了ページ | 12 |
ISSN | 0369-7142 |
関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40400 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002509292 |
JaLCDOI | 10.18926/40403 |
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タイトル(別表記) | CHEMICAL STUDIES ON THE SPRINGS IN SANYO DISTRICT (II) |
フルテキストURL | 010_003_009.pdf |
著者 | 杉原 健| |
抄録 | The author determined the radon contents of spring waters in the eastern part of Hiroshima Prefecture. In this district granite is distributed, and radon was found in most of the spring waters, although their content was variable. The results are as follows: 1) The highest radon content was 172 Mache (626×10(-10) Curie/ℓ) of Harada Spring. Such a high mdon content is rare in the spring waters of Sanyo District. 2) Kanae Spring showed 73.2 Mache (266.4×10(-10) Curie/ℓ) and the well waters near by it showed also comparatively high radon content. 3) The radon contents of the springs of Niwakayama, Immyoseki and No.1 of Hongo, and Takasu water were 44.6 (162.3), 23.2 (84.5), 7.5 (27.3) and 14.7 (53.5) Mache (×10(-10) Curie/ℓ) respectively. 4) The radon contents of rain, river and sea waters could not be determined by the I. M. fontactoscopeon account of its low values. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1953-03 |
巻 | 10巻 |
開始ページ | 3 |
終了ページ | 9 |
ISSN | 0369-7142 |
関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40400 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 40017532421 |
JaLCDOI | 10.18926/40402 |
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タイトル(別表記) | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (VII) POSSIBILITY OF CHEMICAL PROSPECTING OF MINERAL SPRINGS |
フルテキストURL | pitsr_010_001_002.pdf |
著者 | 梅本 春次| |
抄録 | The results of the previous reports I-VI were synthetically discussed, and the possibility of the chemical prospecting of mineral springs was concluded. That is, by determining the chloride and sulfate content and water temperature of well waters and the amounts of chloride and sulfate fixed to the soil, the existence of mineral springs will be prospected. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1953-03 |
巻 | 10巻 |
開始ページ | 1 |
終了ページ | 2 |
ISSN | 0369-7142 |
関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40400 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002509291 |
JaLCDOI | 10.18926/40384 |
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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 | 10.18926/40382 |
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タイトル(別表記) | ON THE DISTRIBUTION OF THE NITRATE CONTENT IN THE MISASA HOT SPRINGS, TOTTORI PREFECTURE |
フルテキストURL | 009_032_036.pdf |
著者 | 杉原 健| |
抄録 | The author determined the nitrate content in Misasa Hot-Springs, sampled from August to October, 1952, In all the well-waters, the amounts of nitrate were higher than 1mg/l, and the highest nitrate content was 9.6mg/l in the well-water in front of Mr. Aoki, s house. In the hot-springs, the author found 10 springs containing more than 1 mg/l of nitrate, and the highest nitrate content was 9.0 mg/l in the Hakuro-Yu, but the lotvest content was about 0 mg/l in the Iwasaki Hot-Springs. In Ishiyu and "Yamadaku-KyodoYu" during the stay of irrigation water in rice-fields from the rain season to September, the amounts of flow incrensed, but the content of radon and chloride decreased. On the other hand, in Hisui-no-yu, the chloride content decreased and the radon content increased with the amount of flow. Moreover, the amounts of nitrate were considerably high in the Ishiyu and Yamndaku-KyodoYu Hot Springs, but fairly low in the Hisui-no-Yu. So the author expects that some relation may be found between the variation of the radon content and the amounts of nitrate. The water samples, which nitrate contents were high, showed a tendency to have a high phosfate content generally. |
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 | 32 |
終了ページ | 36 |
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 | 40017532514 |
JaLCDOI | 10.18926/40381 |
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タイトル(別表記) | STUDY ON RADON CONTENT OF WATERS AND EARTH TEMPERATURES IN FUKUDOME KITADANI VILLAGE, TOTTORI PREFECTURE, JAPAN |
フルテキストURL | 009_028_031.pdf |
著者 | 杉原 健| 御船 政明| |
抄録 | In Fukudome, Kitadani Village, Tottori Prefecture, the radon content of well waters and waters in rice-field and earth temperatures were determined. The radon content of waters in "A" district was higher than that in its neighbourhood, and earth temperatures of "A'" district were higher than those in its neighbourhood. Furthermore, "A" district coincides nearly with "A'" district. These results seem to be dne to the effects of the spring which issues in A (or N) district and supplies a water of high salinity. |
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 | 28 |
終了ページ | 31 |
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 | 40017532513 |
JaLCDOI | 10.18926/40380 |
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タイトル(別表記) | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (VI) DISTRICT NEAR THE SPRING IN KITADANI VILLAGE, TOTTORI PREFECTURE, JAPAN |
フルテキストURL | 009_024_027.pdf |
著者 | 梅本 春次| |
抄録 | In Fukudome, Kitadani Village, the chloride, sulfate and phosfate content and water temperatures of well waters and the amounts of chloride and sulhte fixed to the soil were determined with the samples collected from various parts near the spring which contains much inorganic salts. The chloride, sulfate and phosfate content of the well water samples collected from the district which surrounds the spring, were higher than those from its neighhonrhood, but for the water temperatures of the well water samples, no difference was recognized. As the existence of other sources which would supply the chloride, sulthte and phosfate to the well water is not expected, the difference in the chloride, sulfate and phosfate content of well waters between the samples collected from the A district and its neighbourhood, seems to be due to the effects of the spring which contains much inorganic salts or its sources. |
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 | 24 |
終了ページ | 27 |
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 | 40017532512 |
JaLCDOI | 10.18926/40379 |
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タイトル(別表記) | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (V) HAMAMURA AND KACHIMI HOT-SPRINGS, TOTTORI PREFECTURE, JAPAN |
フルテキストURL | 009_020_023.pdf |
著者 | 梅本 春次| |
抄録 | In Hamamura and Kachimi Hot-Springs, the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from vmions parts of the mineral spring districts. The chloride and sulfate content and warter temperatures of well waters were higher in the samples collected from the thermal spring districts than in the samples collected from its neighbourhood, but for the amounts of chloride and sulfate fixed to the soil, no difference was recognized. As the existence of other sources whlch would supply the chloride, sulfate and heat to the well waters is not expected, the difference in the chloride and sulfate content and water temperatures of well waters, between the samples collected from the thermal spring districts and its neighbourhood, seems to he due to the effects of the thermal springs. |
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 | 20 |
終了ページ | 23 |
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 | 40017532512 |
JaLCDOI | 10.18926/40378 |
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タイトル(別表記) | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (IV) TAMATSUKURI HOT-SPRINGS, SHIMANE PREFECTURE, JAPAN |
フルテキストURL | 009_016_019.pdf |
著者 | 梅本 春次| |
抄録 | In Tamatsukuri Hot-Springs, the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from various parts of the mineral spring districts. For the values which were determined with samples collected from the thermal spring districts and its neighbourhood, no difference was recognized. This result is quite different from the results given in the previous reports of the present author. But this fact may be explaned as the effects of the sea warter, and the further study is being continued. |
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 | 16 |
終了ページ | 19 |
ISSN | 0369-7142 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 40017532512 |
JaLCDOI | 10.18926/40377 |
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タイトル(別表記) | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (III) SIIGAKU AND YUGAKAI HOT-SPRINGS, SHIMANE PREFECTURE, JAPAN |
フルテキストURL | 009_010_015.pdf |
著者 | 梅本 春次| |
抄録 | 1) In Shigaku Hot-Springs, the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from various parts of the thermal spring district and its neighbourhood. The amounts of chloride and sulfate fixed to the soil were greater in the samples from the thermal spring district than in those from its neighbourhood. As the existence of other sources which would supply the chloride and foulfate to the soil is not expected, the difference in the amounts of chloride and sulfate, between the samples from the thermal spring district and it; neighbourhood, seems to be due to the effects. of thermal springs. 2) In Yugakai Hot-Springs the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from various parts of the mineral spring district. The water temperatures of well water samples from the district which has the mineral springs with higher temperatures, were higher than those from the district which has the mineral springs with lower temperatures, but for the chloride and sulfate content of the well water samples and the amounts of chloride and sulfate fixed to the soil, no difference was detected. As the existence of other sources which would supply the heat to the water is not expected, the difference in the water temperatures, between the samples from the district which has the mineral springs with higher temperatures and the district which has the mineral springs with lower temperatures, seems to be due to the effects of the mineral springs. On the other hand, for the chloride and sulfate content of well water samples and the amounts of chloride and sulfate fixed to the soil, no difference is recognized. |
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 | 10 |
終了ページ | 15 |
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 | 40017532512 |