検索結果 2449 件
| JaLCDOI | 10.18926/21340 |
|---|---|
| タイトル（別表記） | Electrcardiographic Changes in Rheumatoid Arthritis: Part 2. Frequency of Electrocardiographic Changes in Rheumatoid Arthritis and Other Diseases |
| フルテキストURL | pitsr_031_031_039.pdf |
| 著者 | 北山 稔| |
| 抄録 | As reported in Part 1 of this paper, the author observed a variety of electrocardiographic aberrations in 27 patients with rheumatoid arthritis. This report will compare the frequency of electrocardiographic aberrations in 45 such cases with the frequencies shown by other groups, namely : a group of 122 patients with normal blood pressure and noncardiac diseases, a group of 121 patients with hypertension, and a group of 14 patients with mitral valve diseases. The results are as follows : 1) The electrocardiographic patterns reported in Part 1 occurred more frequently in both the group of rheumatoid arthritis patients and the groups of hypertension and mitral valve disease patients than in the group with normal blood pressure and noncardiac diseases. 2) On the basis of the electrocardiographic findings, it may be assumed that many of the patients with rheumatoid arthritis suffered from pathological heart conditions, such as heart diseases or cardiac involvement, not accessible to clinical observation. 3) Patients with unequivocal cardiac involvement constituted 21 (46.6%) of the rheumatoid arthritis patients, 65 (53.7%) of the hypertension patients, 9 (64.3%) of the mitral valve didease patients, and 21 (17.2%) of the normal blood pressure and noncardiac disease patients. 4) Patients with suspected cardiac involvement, as defined in Part 1 of this paper constituted 4 (8.9%) of the rheumatoid arthritis patients, 10 (8.3%) of the hypertension patients, 1 (7.1%) of the mitral valve disease patients and 2 (1.6%) of the normal blood pressure and noncardiac disease patients. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1963-01-25 |
| 巻 | 31巻 |
| 開始ページ | 31 |
| 終了ページ | 39 |
| ISSN | 0369-7142 |
| 関連URL | http://eprints.lib.okayama-u.ac.jp/21336 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311038 |
| JaLCDOI | 10.18926/21334 |
|---|---|
| タイトル（別表記） | The Geochemistry of Rocks from Asama Volcano, Japan. New Approaches in the Quantitative Interpretation of the Chemical Composition of Volcanic Rocks |
| フルテキストURL | pitsr_032_001_085.pdf |
| 著者 | 松井 義人| |
| 抄録 | In dealing with the geochemistry of volcanic rocks, it appears imperative, first, to refine the procedure of rock analysis with respect to both major and minor components, and second, to improve present methods of interpreting analytical data on common rock suites such as basalts, andesites and dacites. In regard to the first problem, the rapid method of silicate analysis as described by Shapiro and Brannock (1956) and by Riley (1958) deserves special attention. With such a method it is possible to estimate the accuracy and precision of data with far greater ease than is possible with a classical one, yet without any loss of quality. For the determination of some components, however, it is felt that the procedures recommended previously lack precision and/or simplicity. In Part I of this paper, new methods are suggested for these components. The sum of Mg, Ca and Mn is titrated with EDTA in the presence of Al, Fe and other metals, using thymolphthalein complexone as indicator at pH 10-10.5. The sum of Al and Fe is determined by the back-titration of excess EDTA with the standard Cu solution. PAN is used as indicator at pH about 4, and tartrate is added as the masking agent of Ti. Na and K are determined by flame photometry using very dilute solutions (1-5ppm Na or K), without the separation of other metals and without the use of the internal standard. Sr is included in the scheme of analysis, and is determined by flame photometry according to the standard addition technique. These procedures are tested for their accuracy using the standard samples G-1 and W-1 (Tables 3, 5, 9, 12 and 15). Procedures for other components are also described in the text in full detail. The system of analytical procedures recommended is shown in Table 16. To investigate the problem of the interpretation of compositional variation, typical rocks from Asama volcano and the surrounding area were selected, namely, andesites and dacites of calc-alkaline type. Twenty-one samples, described in Tables 18 and 19, are analyzed according to the above procedures. Results are shown in Table 20. Variation diagrams are presented in Figs. 3 to 5. Since it may be questioned whether the "trend" seen in the diagrams implies a genetic relationship, a least squares approximation technique has been introduced in order to determine whether the composition of the main components of a rock (F) can be expressed by the linear combination of a selected set of compositions of a magma and the phenocrysts crystallized from it : F(o)=F(1)x(1)+F(2)x(2)+······+F(m)x(m) ······(1) where F(1), F(2), ... denote the compositions of a magma and minerals, and F(o) is the calculated composition of F. These calculations lead to the conclusion that there are at least two series of rocks in Asama (Tables 25 to 30 and Fig. 9), distinguished from each other mainly by their K(2)O content. Those rocks showing features of assimilation (Aramaki, 1963) all belong to the K(2)O-rich series. Contents of minor components such as TiO(2), MnO, P(2)O(5) and SrO are analyzed by the linear regression technique in two ways, for example : TiO(2)(o)=C(1)x(1)+C(2)x(2)+ ······(2) and TiO(2)(o)=aMgO+bFe(o) +cK(2)O ······(3) These methods are found useful in discriminating rocks of different ongm and in distinguishing the characteristic behavior of each component. Results of calculations (Tables 31 to 34) support the conclusion reached by calculations based on the contents of major components. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1963-10-25 |
| 巻 | 32巻 |
| 開始ページ | 1 |
| 終了ページ | 85 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310984 |
| JaLCDOI | 10.18926/21325 |
|---|---|
| フルテキストURL | pitsr_034_063_094.pdf |
| 著者 | 奥野 孝晴| |
| 抄録 | The Kamioka mine, Gifu prefecture, working the largest lead and zinc deposit in Japan, lies in the eastern corner of the Hida gneiss complex. The skarn minerals in this mining district are genetically divided into the following three groups. Skarn A : Recrystallized skarn, formed by a regional metamorphism of impure limestone beds. The creation of skarn A is same in age to the formation of the Hida metamorphic complex. Skarn B : Zoned skarn along the contact between limestone and Inishi syenitic rock, having a same origination to Shimonomoto granite. The formation of skarn B is closely related to the intrusion of Shimonomoto granite. Skarn C : Pyrometasomatic skarn, formed by pyrometasomatic replacement of limestone probably after the deposition of the Mesozoic Tetori formation. The ore deposits of the Kamioka mine are composed of the pyrometasomatic skarn (skarn C) called "Mokuji" and the hydrothermal deposits called "Shiroji". Skarn A and skarn B have no genetical relation to the ore deposits. But skarn A acts the valuable role for the stratigrahical classification of ore deposits and limestone beds. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1964-10-25 |
| 巻 | 34巻 |
| 開始ページ | 63 |
| 終了ページ | 94 |
| ISSN | 0369-7142 |
| 言語 | 英語 |
| 論文のバージョン | publisher |
| NAID | 120002310950 |
| JaLCDOI | 10.18926/21324 |
|---|---|
| タイトル（別表記） | Determination of Dissolved Gases in the Ground Water at Mt. Daisen |
| フルテキストURL | pitsr_034_053_062.pdf |
| 著者 | 渡辺 晃二| 奥野 孝晴| |
| 抄録 | 鳥取県大山火山の西北麓の地下水中に潜存するガス成分比は Ar : 0.34～0.40 (cc/l) 1.48～1.64 (%) O(2) : 6.69～9.08 (cc/l) 27.92～35.30 (%) N(2) : 15.16～17.23 (cc/l) 63.22～67.92 (%) の範囲内で定量できる.また,飽和度は次の如くである. O(2) : 87.8～113.9 (%) N(2) : 110.5～123.2 (%) この結果を地表水と比較して,O(2)の飽和度は小さいが,量的な差異はあまりみられず,地表水と地下水の中間的な性質を示している.地質構造,地形が溶存ガス成分比に及ぼす影響は,地下水の流通経路が長距離とみなされる場合に若干のO(2)の消費が認められ,短距離で湧出したと思われるものにはO(2)の飽和度が大きい傾向がある.また,水理地質的にみて,地質と湧出量には密接な関連を見出せるが,ガス成分には影響を与へてはいない. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1964-10-25 |
| 巻 | 34巻 |
| 開始ページ | 53 |
| 終了ページ | 62 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310987 |
| JaLCDOI | 10.18926/21321 |
|---|---|
| タイトル（別表記） | Fluorescent X-ray Spectrometric Determination of Uranium,Zirconium, Yttrium and Strontium in Solution |
| フルテキストURL | pitsr_034_011_020.pdf |
| 著者 | 奥野 孝晴| |
| 抄録 | ウラン鉱床の成因およびウラン鉱物の生成状況を解明するためには,ウラン含有量と同時に,ジルコニウム,イットリウム,ストロンチウムなどの含有量の多少を知ることが,人形峠周辺の鉱床の研究過程において重要となった.これら諸元素の定量をかなりの精度で微量の場合にまで迅速に行なうため,溶液法による蛍光X線分析法を検討した.試料は細粉としたのち,王水などの強酸で分解し,残りはロ過除去してのち,濃縮して一定容となし,その一部をあらたに試作した液体試料保持台(内容積1.8ml,液層の厚さ2.5mm)に入れて測定を行なう.タングステン管球を用い,45KV,22mAの条件で,理学電機製の装置(結晶はLiF)を用い,固定計数法によって各螢光X線(ULα,ZrKα,SrKα,YKα)の強度を計測する.各元素の標準溶液について,最適の角度,バックダウランド値,強度と濃度の関係を検討し,比較的低濃度(20μg/ml前後)まで,検量線の直線性によって,精度よく定量し得ること を知った.さらにこれら諸元素の混合溶液についても検討し,ZrKα に対するウランおよびストロンチウムの影響,さらに共存元素として含有量の多い鉄の影響をしらべ,蛍光X線法により定量した鉄の存在量による諸元素の測定値に対する補正を検討した.以上の諸検討にもとずいて,本法の迅速性を活用し,実際の各種試料について諸元素の定量を行ない,興味ある結果を得られることを知った. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1964-10-25 |
| 巻 | 34巻 |
| 開始ページ | 11 |
| 終了ページ | 20 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311018 |
| JaLCDOI | 10.18926/21316 |
|---|---|
| タイトル（別表記） | The role and problems of balneotherapy in current medicine from the viewpoint of the modern medicine. Appendix: A compilation of the literatures on balneo- and hydrotherapy in european languages published in the last decade. |
| フルテキストURL | pitsr_035_101_203.pdf |
| 著者 | 北山 稔| |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1965-10-25 |
| 巻 | 35巻 |
| 開始ページ | 101 |
| 終了ページ | 203 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311020 |
| JaLCDOI | 10.18926/21312 |
|---|---|
| タイトル（別表記） | U-234 : U-238 in Nature |
| フルテキストURL | pitsr_035_057_066.pdf |
| 著者 | 梅本 春次| |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1965-10-25 |
| 巻 | 35巻 |
| 開始ページ | 57 |
| 終了ページ | 66 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310977 |
| JaLCDOI | 10.18926/21310 |
|---|---|
| タイトル（別表記） | Varieties and regularities in the abundance patterns of the rareearth elements |
| フルテキストURL | pitsr_035_015_050.pdf |
| 著者 | 松井 義人| |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1965-10-25 |
| 巻 | 35巻 |
| 開始ページ | 15 |
| 終了ページ | 50 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311003 |
| 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 |
| JaLCDOI | 10.18926/21182 |
|---|---|
| タイトル（別表記） | Prevalence of periCardial effusion in patients with rheumatoid arthritis -An echocardiographic study- |
| フルテキストURL | pitsr_048_049_054.pdf |
| 著者 | 石井 廣文| 道明 道弘| 田中 淳太郎| 高杉 潔| |
| 抄録 | In order to determine the incidence of pericardial effusion in rheumatoid arthritis (RA), echocardiographic studies were performed on patients with classical or definite RA as determined by ARA criteria, none of whom showed any clinical cardiac symptoms at the time of examination. Of 50 RA patients studied so far, fifteen (30%) showed evidence of posterior pericardial effusion, as recorded on the strip charts. Additionally, in one full-blown case of rheumatoid vasculitis, massive accumulation of pericardial fluid was demonstrable. Compared to those without pericardial effusion, patients shown to have pericardial fluid tended to have decreased RBC, Hct, Hgb, serum protein concentration and increased ESR. The statistical difference between the two groups was significant (P<0.005). The most conspicuous difference between the two, however, was noted in the degree of hypoalbuminemia that is more profound in the effusion positive group (P<0.005). The possible cause of fluid retention in the pericardial cavity in RA was briefly discussed. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1979-03-25 |
| 巻 | 48巻 |
| 開始ページ | 49 |
| 終了ページ | 54 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310937 |
| JaLCDOI | 10.18926/21160 |
|---|---|
| タイトル（別表記） | The determination of uric acid using modified Patel's method |
| フルテキストURL | pitsr_050_025_031.pdf |
| 著者 | 西村 佳子| 青木 宏子| 御舩 政明| |
| 抄録 | N 13-b method for determination of uric acid by AutoAnalyzer- I was proposed from Technicon Corporation, but the sensitivity of this method was insufficient. According to the modification by Patel, good sensitivity was obtained for determining of uric acid, but insufficient separation between peaks was accompanied. To get good separation, Patel's method was reexamined by the authors, and the results were as follows. Sufficient separation was obtained by modifing the flow diagram of Patel's method. The mean recovery rates of uric acid added to serum and urine were 103.6% and 102.5%, and coefficients of variation were 1.27% and 1.05% respectively. The correlation between this modified Patel's method and the U.A. test Wako method was recognized (serum : n=95, r=0.97, urine : n=35, r =0.99). According to our modified method, uric acid concentration in serum of 68 subjects, were 5.8±0.9mg/100ml in 29 males and 4.4±0.8mg/100ml in 39 females. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1980-03-25 |
| 巻 | 50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 | 120002310944 |
| JaLCDOI | 10.18926/21135 |
|---|---|
| タイトル（別表記） | Studies on Rat Peritoneal Mast Cells 2. Effect of BSA on Ca(2+) Uptake of Mast Cells |
| フルテキストURL | pitsr_052_029_032.pdf |
| 著者 | 谷崎 勝朗| 田中 淳太郎| 駒越 春樹| 森永 寛| 岸本 卓巳| 木村 郁郎| Townley Robert G.| |
| 抄録 | To examine the effect of BSA on the cell surface of mast cells, the (45)Ca influx was observed in mast cells from actively sensitized rats and also in cells passively sensitized with IgE-containing serum before or after purification by BSA. The mast cells from actively sensitized rats showed a marked increase in the (45)Ca uptake with stimulation by ovalbumin. The value of (45)Ca uptake by the cells was 1495 ± 104 cpm / 10(5) cells. The uptake of (45)Ca by mast cells passively sensitized before or after separation through BSA was also increased in response to ovalbumin, although the degree of 45Ca uptake by the latter showed marked variation. These results may suggest that BSA affects mast cell surface when the cells are sensitized after separation by BSA. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1982-03-25 |
| 巻 | 52巻 |
| 開始ページ | 29 |
| 終了ページ | 32 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311041 |
| JaLCDOI | 10.18926/21132 |
|---|---|
| タイトル（別表記） | Effect of Hot-Air Room Treatment on Peripheral Leucocytes in Guinea Pigs 1. Effect of Single 30 Min. Hot-Air Room Treatment on Leucocytes Count |
| フルテキストURL | pitsr_052_001_011.pdf |
| 著者 | 小田 康広| 西村 佳子| 駒越 春樹| 谷崎 勝朗| |
| 抄録 | Effect of hot-air room treatment on peripheral leucocytes was examined in guinea pigs by observing the numerical changes after the treatment. The results were as follows. 1. Number of totalleucocytes was decreased immediately after hot-air room treatment with a room temperature of 43℃, humidity of 75-87% and rapidly increased from 30 to 120 min after the treatment. Numerical changes of neutrophils showed a same tendency as that of total leucocytes. 2. Lymphocyte count was not changed or slightly decreased after the hot-air room treatment. 3. Number of basophils was decreased 30 min after the treatment and then increased, differing from that of eosinophils which showed a decreased tendency 120 min after the treatment. 4. Numbers of monocytes and Kurloff cells were slightly increased after the treatment. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1982-03-25 |
| 巻 | 52巻 |
| 開始ページ | 1 |
| 終了ページ | 11 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311011 |
| 著者 | 山田 淳三| |
|---|---|
| 発行日 | 1987-07 |
| 出版物タイトル | 岡山実験動物研究会報 |
| 巻 | 5巻 |
| 資料タイプ | その他 |
| 著者 | 石井 猛| 寺澤 孝男| 樋口 久直| |
|---|---|
| 発行日 | 1991-06 |
| 出版物タイトル | 岡山実験動物研究会報 |
| 巻 | 8巻 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 石井 猛| 寺本 光徳| |
|---|---|
| 発行日 | 1992-06 |
| 出版物タイトル | 岡山実験動物研究会報 |
| 巻 | 9巻 |
| 資料タイプ | 学術雑誌論文 |
| 著者 | 伊永 隆史| 加瀬野 悟| |
|---|---|
| 発行日 | 1990 |
| 出版物タイトル | 環境制御 |
| 巻 | 12巻 |
| 資料タイプ | 紀要論文 |
| 著者 | 岡山大学環境管理センター| |
|---|---|
| 発行日 | 1991-12 |
| 出版物タイトル | 環境制御 |
| 巻 | 13巻 |
| 資料タイプ | その他 |
| 著者 | 加瀬野 悟| 篠田 純男| 高橋 照男| |
|---|---|
| 発行日 | 1994-12-25 |
| 出版物タイトル | 環境制御 |
| 巻 | 16巻 |
| 資料タイプ | 紀要論文 |
| 著者 | 岡山大学環境管理センター| |
|---|---|
| 発行日 | 2003-08 |
| 出版物タイトル | 環境制御 |
| 巻 | 25巻 |
| 資料タイプ | その他 |