検索結果 19474 件
| JaLCDOI | 10.18926/21341 |
|---|---|
| タイトル（別表記） | Causes and Prevention of Intestinal Adhesions Part 1. Surve of the Literature |
| フルテキストURL | pitsr_031_040_053.pdf |
| 著者 | 大谷 満| |
| 抄録 | 1) Seven types of irritation causing intestinal adhesions are recognized in the literature : namely, a) mechanical injury; b) chemical injury; c) thermal injury; d) bacterial infection; e) foreign body; f) blood; and g) exsiccation. Certain minor differences of opinion exist among investigators, according to the experimental methods and the experimental animals used, and blood is not universally accepted as a cause of adhesions. The author believes, however, that the above list includes all of the etiological factors so far recognized in the literature. 2) The mechanism of intestinal adhesions is similar to that of wound healing. The problem of fibre synthesis is still unsolved, despite many advances in electlon microscopy, histochemistory and X-ray analysis. In recent years it has been accepted that fibres are synthesized in extra-cellular space from cytoplasmic materials derived from either mesenchymal cells or fibroblasts, and from polysaccharides in ground substances, althoughth eexact kind of polysaccharides which plays an important role in this process is still unknown. 3) Many papers are recognized with the prevention and treament of adhesions. These may be devided into six groups according to the method suggested: a) limitation of the original peritoneal injury; b) prevention of the coagulation of the exudate; c) avoidance of prolonged contact between the injured surfaces; d) removal of the fibrin after its formation; e) stopping or slowing down of the proliferation of fibroblasts; f) prevention of further obstruction by means of controlling the area of damaged intestine in stepladder fashion, the so-called the plication method. 1. It is the common practice of surgeons to limit the original peritoneal lllJury by laparotomy. Experimental studies have demonstrated that peritonealization of an area denuded of serosa often results in more extensive adhesions. 2. To prevent coagulation of the exudate, Lehman and Boys and other investigators used heparin and dicumarol. The role of heparin in the prevention of adhesions may be summarized as follow: there is a short time interval separating the production of the exudate and its subsequent coagulation with the deposition of fibrin on injured serosal surfaces. Anticoagulants of various types should be effective in preventing this fibrin formation if it is assumed that the coagulation mechanism of both exudate and blood is the same. Though the use of heparin and dicumarol has demonstrated a preventive effect on adhesion formation in experimental animals, many surgeons believe that the risk of hemorrhage from heparin and dicumarol outweighs their possible benefit in the prevention of adhesions. 3. To prevent prolonged contact between injured surfaces, amnion, omental and mesothelial graft, and so on, have been used without success. The stimulation of peristalsis by means of prostigmin and early feeding, however, appears to be effective in the prevention of adhesions, although its use in clinical cases has not been reported. 4. The experimental data indicates that streptokinase alone has no preventive effect on the formation of adhesions, because fibrinolysis is facilitated only by the existence of activated human plasmin. Concernig the use of hyaluronidase, this is an enzyme with the property of hydrolyzing hyaluronic acid, one of the polysaccharides that constitutes the intercellular ground substances. Experimental studies on the use of this material indicate, in summary, that topically administered hyaluronidase reduces the number of adhesions and particularly their density. The reason why hyaluronidase is effective in the prevention of adhesions is still unknown. 5. The use of corticoids and ACTH, according to all available experimental data, appears to delay the formation of adhesions and to prevent talc-induced adhesions, possibly by increasing the absorption of talc. In administrating corticoids, however, their tendency to delay wound healing, to perforate the intestinal wall, and to induce hemorrhage must be taken into account. 6. Experimental study and clinical USe of the plication method demonstrate that in patients with severe recurrent adhesions, or in those for whom the afore-mentio ned methods have been ineffective, this procedure is probably the most effective therapy available. |
| 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 | 40 |
| 終了ページ | 53 |
| 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 | 120002310946 |
| 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 | 10.18926/21338 |
|---|---|
| タイトル（別表記） | The Effect of Laparotomy (Appendectomy) on Portal Circulaton Time |
| フルテキストURL | 031_005_009.pdf |
| 著者 | 仲原 泰博| |
| 抄録 | Following Ueda-Yasuda's Procedure, the author observed changes on the portal blood circulation time, the body temperature, the blood pressue and the pulse rate of 16 patients (A group, five patients with caecum mobile or appendicitis chronica : B group, six patients with appendicitis acuta non-perforativa : C group, five patients with appendicitis acuta perforativa = appendicular peritonitis). Measurements were taken four or five times: before operation, immediately after operation, on the first, third, and fifth, postoperative day. Portal blood circulation time before operation was significantly prolonged in C and B group as compared with A group. Portal blood circulation time immediately after operation was prolonged in each group as compared with that taken before operation. Postoperative duration of prolonged portal blood circulation time was longer in C group more than in A and B group. Postoperative courses of all 16 patients were good and without postoperative complications. |
| 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 | 5 |
| 終了ページ | 9 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532386 |
| JaLCDOI | 10.18926/21337 |
|---|---|
| タイトル（別表記） | The Effect of a Single Cold Bath in 27℃ Water on Portal Circulation Time |
| フルテキストURL | 031_001_004.pdf |
| 著者 | 仲原 泰博| |
| 抄録 | Following Ueda-Yasuda's procedure, the author observed changes on the portal blood circulation time, the blood pressure and the pulse rate of five normal men following a cold bath in water. Measurements were taken three times 30 minutes before the bath, immediately after the bath and 30 minutes after the bath (the bath was either 5 or 10 minutes in duration, and ranged in temperature from 26°to 28℃). Portal blood circulation time immediately after a 10 minute cold bath was found to be probably shortened as compared with that taken before the cold bath. The changes in blood pressure and pulse rate observed after the cold bathing were similar to those reported by other authors. |
| 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 | 1 |
| 終了ページ | 4 |
| 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 | 40017532387 |
| 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 | 10.18926/21330 |
|---|---|
| タイトル（別表記） | The Effect of A Single Bath in Radioactive Hot Spring Water on Variability in Electrocardiograms of Patients with Internal Diseases (1) Repeat Variability in Electrocardiograms of the 100 Patients without Bathing |
| フルテキストURL | pitsr_033_029_038.pdf |
| 著者 | 北山 稔| 河田 義郎| |
| 抄録 | The authors studied time-to-time variability of 100 patients with internal diseases in 100 ECG's over a period of 15 minutes. The variavirity were observed on eleven electrocardiographic items which were measured in 12 leads (I～III, (a)V(R)～(a)V(F), V(1～6)). The electrocardiograms were recorded by same technician, who carefully recorded in confomity to the description on the variability due to techinical and biologocal sources in Simonson's writing and were measured by one of the authors. Frequency distribution of differences between each two electrocardiograms of the same patients are shown in Figures (from 1 to 11) and 5% rejection limits of these differences, which were calculated in use of the stochastics, were as follows : P duration (sec. ) : + 0.022 >X(0)> - 0.021 P-Q duration (sec.) : + 0.029 >X(0)> - 0.024 QRS duration (sec.) : + 0.018 > X(0)> - 0.013 R-R interval (sec.) : + 0.168 >X(0)> - 0.141 QT Ratio (%) + 10.01 >X(0)> - 7.89 QT(c) : + 0.032 >X(0)> - 0.022 P/PR segment : + 0.914 >X(0)> - 0.832 QT/TQ + 0.192 >X(0)> - 0.190 T/R V(5) : + 0.116 >X(0)> - 0.090 AQRS (front. plane) : + 13. 29°>X(0)> - 13.83° AT (front. Plane) : + 14.88°>X(0)> - 16.94° |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1964-03-25 |
| 巻 | 33巻 |
| 開始ページ | 29 |
| 終了ページ | 38 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311006 |
| 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 | 10.18926/21323 |
|---|---|
| タイトル（別表記） | Mineral Composition of Boring Core at Tottori Hot Spring |
| フルテキストURL | pitsr_034_041_052.pdf |
| 著者 | 渡辺 晃二| |
| 抄録 | 鳥取温泉の深度300mに及ぶ試錐のボーリング･コアを検討した結果,主成分鉱物として,石英,長石類(斜長石,加里長石,)と二次的生成鉱物としてモンモリロナイト,カオリナイト,イライト,緑泥石,黄鉄鉱などを認めた.このうち,イライトは堆積岩中に普遍的に存在し,更に緑泥石も全般的にしかも第三紀層で多量に認められている.モンモリロナイトは方解石と共に温泉による生成が考へられ,また,カオリナイトは表土層にのみ認める事ができる.一方,加里長石,黄鉄鉱,緑泥石の産出状態,及びコアが示す粒度,酸化状態からして第四紀層の堆積環境が推定され,25mを境として下部は数回の陸化を含む浅い堆積層であるのに対し,上部は比較的深い.背後供給地から離れた海成層を示唆する. |
| 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 | 41 |
| 終了ページ | 52 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310959 |
| JaLCDOI | 10.18926/21322 |
|---|---|
| タイトル（別表記） | Bed Rock and Wall Rock Alteration of the Uranium Deposits at the Togo Mine, Tottori Prefecture (1) Katamo and Asabatake Deposits |
| フルテキストURL | pitsr_034_021_040.pdf |
| 著者 | 渡辺 晃二| |
| 抄録 | 東郷鉱山,方面･麻畑ウラン鉱床の基盤岩および母岩は粘土化が著しく,その特徴として次のことが挙げられる. (a)粘土鉱物の種類,存在量は,鉱床の酸化帯･非酸化帯にはゞ規制されている.(b)粘土化の程度は原岩の種類により異なり,同一種数の岩石では酸化帯における変質が特に顕著である.(c)粘土量とウラン含有量との間には明確な相関は見出せないが,モンモリロナイトの量についてのみ観察すると,おおよそ負の相関がみられる.また,粘土化の主体をなすモンモリロナイトは,結晶度が良好で熱水変質が示唆きれる.化学分析の結果,SiO(2)の量が少ないので珪ばん比が異常に小さいが,ウラン鉱床近辺においてモンモリロナイト化に伴なう珪化帯が認められず,珪酸の逸脱が考えられる.鉱量的にみて,両鉱床の主体をなすウラン鉱物が燐顧塩鉱物であり,珪酸塩鉱物が少ないことなどから,モンモリロナイト化作用と鉱化作用との間には,直接関連がないものと考察される. |
| 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 | 21 |
| 終了ページ | 40 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310993 |
| JaLCDOI | 10.18926/21320 |
|---|---|
| タイトル（別表記） | Radioactive Anomaly in the Okutsu Kaoline Mine, Okayama Prefecture |
| フルテキストURL | pitsr_034_001_010.pdf |
| 著者 | 奥野 孝晴| 渡辺 晃二| |
| 抄録 | 奥津カオリン鉱床は花崗緑岩中の熱水交代性の塊状粘土鉱床であって, 中心部に白色粘土鉱体, それをとりまいて石英沸石帯,更にその外側に緑簾石帯からなる変質の帯状分布が存在する. 放射能異常は外側変質帯の緑簾石帯に集中しており, そこにトリウムの濃集が認められる. 本鉱床の放射性元素の濃集は変質帯形成の機構と密接に関連するものとみられる. |
| 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 | 1 |
| 終了ページ | 10 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311015 |
| 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 | 10.18926/21236 |
|---|---|
| タイトル（別表記） | Phlogopites and coexisting pargasites in wehrlite from the northern Kanto mountains, central Japan |
| フルテキストURL | pitsr_043_001_013.pdf |
| 著者 | 田崎 耕市| 猪俣 道也| |
| 抄録 | Coexisting interstitial phlogopites and pargasites in iron rich wehrlite from the northern Kanto mountains were studied. The textural relationｓ between those interstitial hydrous minerals and major constituent minerals, such as olivines and clinopyroxenes suggest the crystallization of the former from the intergranular residual liquids. The modal amounts of phlogopites in wehrlite are less than 1%, and that of pargasites range from 2 to 5%. Microprobe analyses have been carried for those hydrous minerals and the major constituent minerals. namely, olivine, clinopyroxene and idiomorphic zoned chromite. Olivines in wehrlite from the northern Kanto mountains have rather iron-rich nature and range from Foso to Fo(80) and those coexisting with the hydrous minerals are Fo(82.5) in average. Clinopyroxenes from mica bearing wehrlite contain about 2.5% Al(2)O(3). 17% MgO and 5.5% FeO. Tentative cation per cent of Ca, Mg and Fe are calculated as Ca(42.6) Mg(48.1) Fe(9.3) in average. The present probe analyses show high magnesian nature of the interstitial phlogopites. In addition, these phlogopites are conspicuous by their high TiO(2) content ranging from 4.6 to 5.2%. Mg/Mg + Fe versus Ti relation plotted in Fig. 4 revealed that the present phlogopite are similar to that of the alkaline pyroxenite nodules from the Lashaine volcano, northern Tanzania. Pargasites in mica bearing wehrlite are also rich in TiO(2) (3.0～4.7%), whereas pargasitic common hornblende from hornblendite or gabbro are rather low in TiO(2) (0.9～1.7%). Mg/Mg+Fe+Mn versus Ti relations of amphiboles illustrate that Ti contents increase with decrease of Mg/Mg+Fe +Mn. Two different increasing trend for Ti conten t are also noticed. Idiomorphic chromites show distinct compositional variation from core to rim. Total FeO increases about 16% at rim, whereas TiO(2), Al(2)O(3) and MgO decrease at the rim. Possible crystallization scheme of those hydrous minersls is proposed in Fig. 10, where the maximum stability limits of phlogopite and hornblende are shown with the curve for begining of melting of basalt. Separation of liquid fraction from cumulate phase with a small trapped intergranular liquid might occur at point A. The liquid fraction then might move upward through the course II. In cumulate phase, intergranular liquid might crystallize pargasitic amphibole by the reaction with olivine and clinopyroxene through the course I in Fig. 10. Intergranular liquid might decrease with production of amphiboles and K(2)O might concentrate in residual liquid. At final stage of crystallization, residual liquid rich in K(2)O might crystallize as phlogopite by the reactions with olivine. Decrease of Ti02 content at the nm of idiomorphic chromite might be related to the formations of Ti-rich hydrous minerals. |
| 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 | 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 | 120002311004 |
| JaLCDOI | 10.18926/21229 |
|---|---|
| タイトル（別表記） | A report on the physically handicapped persons caused by rheumatoid arthritis in Tottori Prefecture, Japan |
| フルテキストURL | 044_055_060.pdf |
| 著者 | 北山 稔| |
| 抄録 | The physically handicapped persons caused by rheumatoid arthritis were studied in Tottori prefecture in July 1973. The following results were obtained ; 1. The hand i capped per sons of 265, who were recognized as the handicapped by the government authori ties, were observed. The prevalence rate was 4.7 to 10,000 of the population and 15 to 1, 000 of the total number of the hand i capped. 2. The prevalence rate of the handicapped to the total number of patients with rheumatoid arthritis was 15.4%. 3. On a reginal distribution, the prevalence rate of the handicapped to the regional population were calculated between from 0.20‰ to 0.77‰. The result showed that it was higher at rural than at urban districts. 4. The prevalence rate to population gradually increased with aging, especially over the fiftieth years. The prevalence rate of the number of serious handicapped (class 1+2) to the total number of handicapped was regnlarly at 40% between 30 and 60 years of age, but it increased over 70 years of age. 5. The sex ratio of fernIe to male was 3.3 : 1 on the total handicapped and 2.9 : 1 on the serious handicapped persons. On the other hand, the ratio was 5.1 : 1 on the group under 59 year s of age and 2.4 : 1 on the groupe over 60 years of age at the total handicapped. And then, the ratio was 5.0 : 1 on the younger group and 2.6 : 1 on the older group at the serious handicapped persons. |
| 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 | 55 |
| 終了ページ | 60 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310975 |
| JaLCDOI | 10.18926/21228 |
|---|---|
| タイトル（別表記） | Continuous in-vIvo measurement of the brain tissue and the ischemic muscle gas tension using MEDSPECT, MS-8 |
| フルテキストURL | pitsr_043_029_036.pdf |
| 著者 | 川上 俊爾| 山根 義久| 野一色 泰晴| 古元 嘉昭| 寺本 滋| 妹尾 嘉昌| 金子 克也| 杉本 誠起| 高橋 俊二郎| |
| 抄録 | I MEDSPECT is a medical mass spectrometer for continuous in-vivo measurement of tissue, blood and respiratory gases. Interfacing catheter for tissue in measurement has Teflon membrane. The permeability and perfusion rate for various gases through its membrane varied with temperature. The temperature coefficient of Teflon catheter in the range of 15℃-40℃ is approximately constant with -2% of correction per degree for oxygen and carbon dioxide. Linear correlation was confirmed experimentally. II The brain tissue gas tensions were measured in ten dogs with intra-venous anesthesia at normothermia and deep hypothermia using perfusion cooling, including circulatory arrest for 30 minutes at 20°C of cerebral temperature. On average, the brain tissue P(O2) was 15mmHg in normothermia when the arterial P(O2) showed 95mmHg and the brain tissue P(CO2) was 49mmHg when the arterial PC02 showed 30mmHg. The brain tissue carbon dioxide tension gradually decreased by cooling and increased during circulatory arrest for 30 minutes; from 45mmHg to 72mmHg. The brain tissue oxygen tension increased during cooling from 15mmHg to 41mmHg and decreased in the circulatory arrest; from 41mmHg to 36mmHg. III The ischemic muscle gas tension was measured in a 22-year-old man, who was suffered from thromboangiitis obliterans bilaterally, and had the popliteal autovein bypass surgery 3 months ago. Control oxygen tensions in the both anterior tibial muscles showed about the same; 35mmHg and 36mmHg respectivelly, and the P(O2) of the non-operated side showed remarkable low level of 18mmHg as compared with the side of arterial reconstruction surgery after 5-minutes ankle exercise. |
| 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 | 29 |
| 終了ページ | 36 |
| ISSN | 0369-7142 |
| 関連URL | http://eprints.lib.okayama-u.ac.jp/21235 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311036 |
| JaLCDOI | 10.18926/21225 |
|---|---|
| タイトル（別表記） | Some new data on granophyres (the Namariyama quarts-diorites) in the Ningyo-toge area |
| フルテキストURL | pitsr_044_021_032.pdf |
| 著者 | 本間 弘次| |
| 抄録 | A new occurrence of granophyric body was described and its geological significance was discussed with regard to classification of Late Cretaceous to Early Tertiary plutonic activities in the area. |
| 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 | 21 |
| 終了ページ | 32 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002311029 |
| 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 | 10.18926/21213 |
|---|---|
| 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 | 10.18926/21205 |
|---|---|
| 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 | 10.18926/21204 |
|---|---|
| タイトル（別表記） | Determination of manganese in serum by atomic absorption spectrophotometry |
| フルテキストURL | pitser_046_037_043.pdf |
| 著者 | 古野 勝志| |
| 抄録 | The manganese (Mn) concentrations in serum of 40 healthy controls (9 males and 31 females), and of 26 patients with rheumatoid arthritis (4males and 22 females) were determined using a HITACHI MODEL 207 atomic absorption spectrophotometer. Wavelength of Mn determination was setted at 2795 A. Flow rate of acetylene was setted at 3.0 l/min and lamp current was setted at 10 rnA. The serum samples were ashed by IPC MODEL 1003plasma machine, and dissolved in 3N-HCl and evapolate on the hot plate, and redissolved in constant volume of 0.1 N-HCl. These sample solution were aspirated directly into the burner. Mn levels in serum were estimated by standard curve. The mean recoverry rate of ashedsample solution was 100.1%, and that of serum by ashing process was 101.6%. The serum Mn levels in 40 healthy controls and 26 patients with rheumatoid arthritis were 2.19 ± 0.34 (S.D.), 3.04 ± 1.01 (S.D.) μg/100ml respectively. The serum Mn levels in rheumatoid arthritis were significantly higher than healthy control levels (p<0.001). In 10 of 26 cases (38%) with rheumatoid arthritis, the serum Mn levels were shown to be above the upper limit of 5% rejection limit of healthy controls. |
| 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 | 37 |
| 終了ページ | 43 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310997 |