検索結果 47817 件
| JaLCDOI | 10.18926/21224 |
|---|---|
| タイトル（別表記） | Semi-automatic processing of EPMA data |
| フルテキストURL | pitsr_044_007_020.pdf |
| 著者 | 川嵜 智佑| |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1975-03-25 |
| 巻 | 44巻 |
| 開始ページ | 7 |
| 終了ページ | 20 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310998 |
| JaLCDOI | 10.18926/21223 |
|---|---|
| タイトル（別表記） | Applications of critical point drying for scanning electron microscopic study of clay minerals |
| フルテキストURL | pitsr_044_001_006.pdf |
| 著者 | 野一色 泰晴| 田崎 和江| |
| 抄録 | The scanning electron microscopic studies of the clay minerals have usually been made on air-dried samples. The air-drying method is, however, not always preferable for H(2)O rich clay minerals such as imogolite because of their strong contraction in the dehydration process. The present writers examined the critical point drying for H(2)O rich clay mineral (imogolite) and proved that this drying method is excellent in preservation of natural surface of the minerals than that of air-drying. Imogolite which examined was separated from Kurayoshi pumice beds. The samples were treated first with OsO(4) solution and then were dehydrated progressively with ethanol. After completing above treatments, the imogolites which sealed in vessel were dried successively at critical point of CO(2). The samples were mounted onto brass stubs and coated first with carbon and then with Au-Pd alloy. The Japan Electron Optics Laboratory Co. scanning electron microscope Model JSM-50A which was installed in the Division of Rehabilitation Medicine in the present Institute was used at the operating conditions: accelerating voltage 25kV, magnifications ranging from 3000 to 40000. The scanning electron micrographs of the air-dried imogolite are shown in plate I, and cry tical point dried ones are in plate II and III. The former shows twig-like shape which indicated the effect of contractility, whereas the latter exhibits softly curled and entangled threads. The diameter of these threads ranges from 280A to 560A. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1975-03-25 |
| 巻 | 44巻 |
| 開始ページ | 1 |
| 終了ページ | 6 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311009 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1975-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 44巻 |
| 資料タイプ | その他 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1975-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 44巻 |
| 資料タイプ | その他 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1976-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 45巻 |
| 資料タイプ | その他 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1976-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 45巻 |
| 資料タイプ | その他 |
| 著者 | 本間 弘次| 酒井 均| |
|---|---|
| 発行日 | 1976-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 45巻 |
| 資料タイプ | データ・データベース |
| 著者 | 井上 妙子| 森永 寛| |
|---|---|
| 発行日 | 1976-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 45巻 |
| 資料タイプ | データ・データベース |
| JaLCDOI | 10.18926/21216 |
|---|---|
| タイトル（別表記） | Genetic relationship between the Hiroshima and Ryoke granites as indicated by some geochemical evidence |
| フルテキストURL | pitsr_045_033_046.pdf |
| 著者 | 本間 弘次| |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1976-03-25 |
| 巻 | 45巻 |
| 開始ページ | 33 |
| 終了ページ | 46 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310988 |
| JaLCDOI | 10.18926/21215 |
|---|---|
| タイトル（別表記） | Studies on lithium in the field of balneology : Effects of lithium salts on analgesic activity of aminopyrine |
| フルテキストURL | pitsr_045_025_031.pdf |
| 著者 | 古野 勝志| 御船 政明| |
| 抄録 | The authors studied the effect of pretreatment with internal use of lithium salts on analgesic activity of aminopyrine by hot-plate test in mice. The male mice at 4 weeks of age weighting 17-19 g were divided into 7 groups. Earch group being composed of 9-10 mice was given oraBy 0.1 ml of LiCI-solution per 10 g of body weight for 35 days, LiCl was dissolved in 0.9% saline solution, in such concentrations that each group received 0 mg, 50 mg, 100mg, 200 mg and 400mg of LiCl for each kg of body weight of mouse, respectively, Control group received only 0.9% saline solution. On the 1st, 3rd, 7th, 14th, 21st, 28th and 35th days of this experiment, 0.1 ml of 1% solution of aminopyrine per 109 of body weight was injected intraperitoneaJly and then tested 30 minutes later. In the hot-plate test, a mouse is placed on a hot plate being adjusted with the thermostat at 55°±1℃, and the response is licking or lifting the hind feet or an outright attempt to escape from the plate, The increase in response time is used to quantify the analgesic effect of aminopyrine, The results were as follows : 1. The response time in groups receiving 0-50 mg of LiCl per kg of body weight had decreased on the 14 th day, but it tended to return to the initial level after the 21st day of experiment. 2. The response time in groups receiving 100-400 mg of LiCl per kg of body weight had also decreased on the 14 th day, and the degree of the decrease in response time was greater than that of the former and then remained faily constant at this level to the end of the observation period. These results would indicate that LiCl inhibits the analgesic activity of aminopyrine. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1976-03-25 |
| 巻 | 45巻 |
| 開始ページ | 25 |
| 終了ページ | 31 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311002 |
| JaLCDOI | 10.18926/21214 |
|---|---|
| タイトル（別表記） | 斜長石から生成したギブサイトの走査電顕観察―大山および三瓶山降下地積物中の粘土鉱物,その8― |
| フルテキストURL | pitsr_045_011_024.pdf |
| 著者 | 田崎 和江| |
| 抄録 | 大山降下堆積物中の斜長石のギブサイト化過程を,偏光顕微鏡,X線,示差熱分析,走査型電顕,EPMAを用いて調べた. 斜長石は風化によって,カオリナイト,イライト,ハロイサイト,ギブサイト等を生成することが知られているが,今回,ギブサイト化した斜長石についてのみ検討をおこなった. EPMA分析によれば,一個の斜長石の表面に,Al, Si, Na, Caの多く存在する新鮮な斜長石の部分と,Na, Caをほとんど含まず,多量のAlと,ごく少量のSiを含んでいるギブサイトの部分とが分布し,その境界は, 明瞭であることがわかった（図版2）.それぞれの部分の分析値は第1表のとおりである. 走査型電顕による斜長石の微細形態観察から,下記のことが明らかになった. ①新鮮な斜長石の表面は,平滑かまたは離溶ラメラがみとめられる（図版3-1）. ②風化過程の初期に,水を合んだ非晶質の薄層が,斜長石の表層に生成する.この非晶質薄層の生成にさき立って,斜長石の表面の一部に, ロート状のくぼみが形成される場合がある（図版3-2,3）. ③この非晶質薄層に亀裂が生じる（図版4）.一方, ロート状のくぼみの上にも非晶質の薄層ができ,亀裂が生じる（図版8-1,2）. ④さらに風化が進むと,ラメラ, 亀裂およびロート状のくぼみを部分的に残しながら,-･部には,ギブサイトの結晶が生成する（図版5）. ⑤ギブサイトの結晶は,横1～3μm, 縦2～15μm, 厚さ0.5μm前後の平板状の形態,または,直径15-25μm,厚さ0.5～1μm の円盤上の形態をもつ（図版6）. ⑥ギブサイトの結晶は,平板状のものが数段重なり,集合体をなす場合もあり（図版7-1）,これは,ブラジルのミナス鉱山産のギブサイトの集合状態（図版7-2）とよく似ている. すなわち,斜長石の表面に,風化により,水を含んだ非晶質の薄層ができ,次に,その薄層に亀裂が生じ,イモゴライトの生成をともないながら,直接ギブサイトが結晶すると考えられる. 地名 Okachi 大河内 Hongu 本宮 Kurayoshi 倉吉 Daisen-Cho 大山町 Shuki 秋喜 Hiruzenbara 蒜山原 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1976-03-25 |
| 巻 | 45巻 |
| 開始ページ | 11 |
| 終了ページ | 24 |
| ISSN | 0369-7142 |
| 言語 | 英語 |
| 論文のバージョン | publisher |
| NAID | 120002311010 |
| JaLCDOI | 10.18926/21213 |
|---|---|
| タイトル（別表記） | The effect of radioactive thermal bathing upon catecholamines of the whole brain of male mice |
| フルテキストURL | pitsr_045_007_010.pdf |
| 著者 | 伊東 恵子| |
| 抄録 | The author studied the changes of catecholamine levels of the whole brain of male mice weighing 15-20g before and after a single bathing for 20 minutes, 37±1℃ in temperature, in the radioactive hot spring in Misasa (Rn content : 74.83×10(-10)C/l), and compared the results obtained with those of the plain hot water bathing. The catecholamines (dopamine and noradrenaline) were measured by gaschromatographic method using electrone capture detector. It may be summarized as follows : 1. No significant change of dopamine and noradrenaline levels of the whole brain of mice was recognized before and after the plain hot water bathing used as a control. 2. Noradrenaline levels of the whole brain of mice had increased following the radioactive hot spring bath, and remained at same levels for 30 minutes after bathing. Dopamine levels had no change immediately after bathing, but had lowered at 30 minutes from the time of the bath. 3. Causes of these results are under investigation. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1976-03-25 |
| 巻 | 45巻 |
| 開始ページ | 7 |
| 終了ページ | 10 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310996 |
| JaLCDOI | 10.18926/21212 |
|---|---|
| タイトル（別表記） | Micromorphology of dendritic titanaugite |
| フルテキストURL | pitsr_045_001_006.pdf |
| 著者 | 田崎 耕市| |
| 抄録 | Dendritic titanaugite in ultrabasic picrite basalt from the Mineoka tectonic belt, Boso peninsula shows two contrastive morphology such as ; 1) ferny type and 2) skeletal type. Scanning electron microscopic observation reveals that there are three types of morphology as follows; 1) the cluster of needle crystals (Plate I-2, 3), 2) the pile of rail or fence like crystals (Plate II), 3) the stepped crystals (Plate III). The needle crystals have the cross section of distorted ellipsoid with 2 to 5μm in long diameter. The skeletal type morphology is ascribed to the cross section of the pile of rail or fence like crystals. The ferny type morphology comprises the clusters of needle and rail or fence like crystals. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1976-03-25 |
| 巻 | 45巻 |
| 開始ページ | 1 |
| 終了ページ | 6 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310955 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1976-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 45巻 |
| 資料タイプ | その他 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1976-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 45巻 |
| 資料タイプ | その他 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1976-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 45巻 |
| 資料タイプ | その他 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1977-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 46巻 |
| 資料タイプ | その他 |
| 著者 | 岡山大学温泉研究所| |
|---|---|
| 発行日 | 1977-03-25 |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 巻 | 46巻 |
| 資料タイプ | その他 |
| JaLCDOI | 10.18926/21206 |
|---|---|
| タイトル（別表記） | Study of metabolism of uric acid. (1) Observation of uric acid values |
| フルテキストURL | 046_061_070.pdf |
| 著者 | 青木 宏子| |
| 抄録 | Uric acid was measured in serum and urine of the ambulant and hospitalized patients with various disorders including gout. in Misasa-Branch Hospital of Okayama University Medical School from January 1975 to December 1976. Serum and urine samples were obtained from 283 males and 260 females, and from 2 males respectively. The results are as follws; (1) Uric acid in males was 1.4 mg/100mf higher than in females. (2) Uric acid in males decreased with ages, showing two peaks between 15 and19 , and between 35 and 44 years old. (3) Uric acid in females showed low levels between third and fifth decades and increased thereafter with ages. (4) There were many fatty subjects among the patients with gout. (5) An increase in total daily excretion of urinary uric acid was observed concomitantly with increased daily urine volume. (6) Periodical fluctuations of uric acid in serum and other clinical findings were show in several cases of gout, who had been controlled in MisasaBranch Hospital for several years. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1977-03-25 |
| 巻 | 46巻 |
| 開始ページ | 61 |
| 終了ページ | 70 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311005 |
| JaLCDOI | 10.18926/21205 |
|---|---|
| タイトル（別表記） | Hydrogen and oxygen isotopic ratios of thermal and mineral springs in Arima area |
| フルテキストURL | pitsr_043_015_028.pdf |
| 著者 | 松葉谷 治| 酒井 均| 鶴巻 道二| |
| 抄録 | Saline waters of thermal and mineral springs in Arima area, at Takarazuka, and in Ishibotoke area of Kawachinagano City indicate wide ranges of δD and δ(18)O values (Table 1). Excellent linearity exists between the δD and δ(18)O values (Fig. 1) and between the δ(18)O value and the chloride concentration (Fig. 2). These facts as well as the chemical evidence of the previous investigators strongly support the view that Arima springs are admixtures of a single deep brine and local ground water (TSURUMAKI, 1964). The deep brine may have the δ(18)O value of +8.0～+8.5‰, the δD value of -25～-30‰, and the chloride concentration of 1.20～1.25 eq/l, which were estimated from the water of the maximum salinity so far reported. Because the thermal and mineral springs in Arima area closely associate with the upper Cretaceous granitic rocks, and the estimated δ(18)O value of the deep brine is similar to a value of water in isotopic equilibrium with those granitic rocks at 500～600℃, the deep brine of Arima might have been the magmatic water of those granitic rocks. The mineral springs at Takarazuka and in Ishibotoke area also show the similar linearity among Cl(-), δ(18)O and δD to those in Arima area. Therefore it is assumed that the mineral springs at Takarazuka may be of the same origin as that in Arima area, and the mineral springs in Ishibotoke area might have been the fluid associated with Ryoke metamorphic rocks. Alternatively, the deep brine in Arima area may be isotopically and chemically similar to the saline formation waters in Illinois basin (GRAF et al., 1966). The high δD values and salinities of those formation waters were attributed to the isotopic and chemical fractionation during the passage of water through sediments. The deep brine in Arima area may be genetically similar to those saline formation waters. If such a saline water could have formed in Osaka basin, it is not surprising to find out the similar brines at Arima and Ishibotoke which are the northwestern and southeastern rims of the basin, respectively. At the present, it cannot be answered which of these two models is more probable. Further studies on other saline springs fluid inclusions of Cretaceous granitic rocks may be useful in order to solve this problem. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1974-03-25 |
| 巻 | 43巻 |
| 開始ページ | 15 |
| 終了ページ | 28 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310971 |