result 9424 件
| JaLCDOI | 10.18926/40386 |
|---|---|
| Title Alternative | A CLINICAL, STUDY ON HEARTBURN |
| FullText URL | pitsr_009_054_063.pdf |
| Author | Sotozono, Masazumi| |
| Abstract | 402 consecutive patients with various disorders of digestive tract were investigated concerning heartburn and 184 cases (45%) proved to have heartburn. No significant relationship was established between the heartburn and gastric acidity or the kinds of digestive diseases. Heartburn was not only seen in hyperacidity but also often seen in hyp-and anacidity or normacidity. No significant correlation was observed between the heartburn and the rate of emptying the gastric content. Flow back of bile in stomach juice was relatively often seen in cholecystopathic patients with heartburn, but no such relationship was proved in other kinds of patients. Experimentally beartburn was evoked in the patients with heartburn by administration of 30 cc of 1% sodium bicarbonate solution in the stomach or ten cc in oesophagus, but not by the same quantity of hydrochloric acid (N/20), lactic acid (N/20), 10% syrup, 50% polytamine solution, physiological saline, or 5% bile dilution. A habit of eating fast was observed relatively often in heartburn patient. Profession of the most of the above examined patients was farmer and they noted some causative relation to large intake of food rich in carbohydrate (sweetpotato, rice-cake, etc. ). The most frequent time for heartburn to beginn was one to three hours after a meal. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1953-01 |
| Volume | volume9 |
| Start Page | 54 |
| End Page | 63 |
| ISSN | 0369-7142 |
| Related Url | http://ousar.lib.okayama-u.ac.jp/metadata/40388 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002484891 |
| JaLCDOI | 10.18926/40355 |
|---|---|
| FullText URL | fulltext.pdf |
| Author | 森永 寛| |
| Publication Title | 放射能泉研究所報告 |
| Published Date | 1949 |
| Volume | volume1 |
| Start Page | 1 |
| End Page | 74 |
| language | Japanese |
| File Version | publisher |
| JaLCDOI | 10.18926/40353 |
|---|---|
| Title Alternative | STUDIES ON THE AGING OF THE MINERAL WATERS (Ill) VARIATION OF SILICATE IN THEMINERAL WATERS |
| FullText URL | pitsr_012_006_010.pdf |
| Author | Sugihara, Takeshi| |
| Abstract | When silicate content is determined by the colorimetric method, the silicate content in the mineral waters and sodium silcate solution decreases in addition of ammonium hydroxide and sodium carbonate respectively, and moreover after addition of aluminium ion in the samples, when aluminium hydroxide is precipitated from ammonium hydroxide solution, total silicates in various forms are coprecipitated with it. The silicate content in the mineral waters that are kept in concentrations of 0.1～0.4 normality of sodium hydroxide showed special variations with times. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1953-09 |
| Volume | volume12 |
| Start Page | 6 |
| End Page | 10 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002484889 |
| JaLCDOI | 10.18926/40345 |
|---|---|
| Title Alternative | BALNEOLOGICAL STUDIES USING RADIOACTIVE ISOTOPES (3) |
| FullText URL | pitsr_013_018_023.pdf |
| Author | Yokota, Takeo| Ashizawa, Takashi| |
| Abstract | By using labelled sodium sulfate or calcium sulfate (sulfate containing S(35)) the transition of sulfate ion into the body across the skin was investigated soon after taking a bath in sodium sulfate or calcium sulfate solution under varing conditions. Mice were used for experiments. The percutaneous absorption of sulfate ion proved to decrease gradually in the course of serial baths in sodium sulfate solntion and was accelerated by making a fresh burn on the skin of the bathed animals, but it showed a tendency to decrease as the wound became more and more healed. The application of basic dye to the skin (e.g. 1% methylenblue or 1% fuchsin solution) increased the transition of sulfate ion into the test animal. Little difference was proved between the bath in sodium sulfate and calcium sulfate solution with respect to the penetration of sulfate ion. Passage of sulfate ion from the bath water through the skin was a little promoted by the use of sodium sulfate solution than by the use of calcium sulfate solution. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1953-12 |
| Volume | volume13 |
| Start Page | 18 |
| End Page | 23 |
| ISSN | 0369-7142 |
| Related Url | http://ousar.lib.okayama-u.ac.jp/metadata/40340 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002484880 |
| JaLCDOI | 10.18926/40342 |
|---|---|
| Title Alternative | ON THE EXISTENCE OF RADIUM B, RADIUM C AND THORIUM B IN MISASA HOT SPRINGS |
| FullText URL | pitsr_013_005_008.pdf |
| Author | Sato, Mitsuo| |
| Abstract | The author tried to measure RaB, RaC and ThB in the hot spring waters using G-M counter and proved the existence of RaB and ThB in Misasa Hot Springs. To 100 liters of spring water ahout 20 gms of ferric chloride and then sodium hydroxide were added. Precipitate was dissolved in hydrochloric acid and after adding bismuth and lead, the solution was saturated with hydrogen sulfide. The precipitate of sulfides was filtered and ignited to ashes after drying. The β-activity of the ashes was measured by a mica-window type G-M counter with the recording circuits of scale of 16. Natural background was 50±5 connts per minutes. Six spring waters of Misasa, namely "Spring of Branch Laboratory", "Nakayu", "Gunze" "O-T-R", "Jwayu", and "Tsukiminoyu" were investigated. RaB was detected in all samples. ThB was found only in "Gunze" and "O-T-R". ThB content of "Gunze" was estimated, to be roughly 1×10(-12) Curie units per liter. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1953-12 |
| Volume | volume13 |
| Start Page | 5 |
| End Page | 8 |
| ISSN | 0369-7142 |
| language | English |
| File Version | publisher |
| NAID | 120002484878 |
| Author | 淸水 多栄| |
|---|---|
| Published Date | 1953-12 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume13 |
| Content Type | Others |
| Author | Institute for Thermal Spring Research, Okayama University| |
|---|---|
| Published Date | 1953-12 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume13 |
| Content Type | Others |
| JaLCDOI | 10.18926/40325 |
|---|---|
| Title Alternative | EFFECT OF WATER LEVEL OF RIVER ON MINERAL SPRING |
| FullText URL | pitsr_014_015_021.pdf |
| Author | Umemoto, Shunji| |
| Abstract | From June 1953 to January 1954, the water temperature and amount of flow of a spring called IITanaka-no-Yu", Misasa Hot Springs, Tottori Prefecture, were observed continuously. It issues 10 metres north of the riverside of the River Misasa and a stream runs 3 metres south of it. The water level of the River and the stream were also observed. The water level of the stream have close connection with the water volume of rice-field which surround that spring, because it is a watercourse of irrigation to rice-field. It was found that when the amount of flow increased, the water temperature rose, namely there was a positive correlation between them, and the correlation coefficient was 0.952 (highly significant). The analysis of variance showed that the amount of flow would be affected by the water level of the River but would not be severely affected by that of the stream. The correlation between the amount of flow and the water level of the River was also positive and the correlation coefficient was 0.731 (highly significant). As a result of the analysis of variance, the computation of confidence limit and the analysis of covariance, in summer the averages of the amount of flow and the water temperature would be higher than those in autumn and winter. This difference was seemed to be induced by the water level of the stream. The end of the observation, a dam had been constructed 20 metres down (west) the River and she rised, but the effect of it must be observed after this. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1954-03 |
| Volume | volume14 |
| Start Page | 15 |
| End Page | 21 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002462902 |
| Author | 岡山大学温泉研究所| |
|---|---|
| Published Date | 1956-01 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume16 |
| Content Type | Others |
| JaLCDOI | 10.18926/40312 |
|---|---|
| Title Alternative | o-PHENANTHROLINE METHOD APPLIED TO THE DETERMINATION OF IRON IN NATURAL WATERS |
| FullText URL | pitsr_017_001_007.pdf |
| Author | Tanaka, Shigeo| |
| Abstract | The o-phenanthroline method was tested as to its applicability to the separate determination of iron in natural water: ionic ferrous iron, reducible iron, snd colloidally dispersed iron. In connection with this, the results of the following experiments are given in this paper. 1. Determination of the absorption curve of o-phenanthroline ferrous complex. (Figure 1.) 2. Construction of the calibration curve for a Purfrich's photometer with filter S 50, 15 cm cuvettes. (Figure 2.) 3. Examination of the effects of coexisting anions on the determination of iron by the method of three way layout. (Table 1., Table 2.) 4. Trial determinations of iron in three different states in solution. (Table 3., Table 4. ) 5. Test of the applicability of this method to the determination of ionic ferrous iron and reducible iron in thermal water. (Table 5., Table 6.) From the above, it was revealed that ionic ferrous iron and reducible iron in natural water are separately determinable with sufficient accuracy by the o-phenanthroline method, and that ionic iron and colloidally dispersed iron are also separately determinable, when the dispersed iron is present in amount more than 1.3% of the total iron. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1956-03 |
| Volume | volume17 |
| Start Page | 1 |
| End Page | 7 |
| ISSN | 0369-7142 |
| Related Url | http://ousar.lib.okayama-u.ac.jp/metadata/40311 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002462897 |
| Author | 斉藤 信房| |
|---|---|
| Published Date | 1957-03 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume18 |
| Content Type | Conference Paper |
| Author | 湊 秀雄| |
|---|---|
| Published Date | 1957-03 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume18 |
| Content Type | Conference Paper |
| Author | 鈴木 篁| |
|---|---|
| Published Date | 1957-09 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume19 |
| Content Type | Conference Paper |
| Author | 初田 甚一郎| 西村 進| |
|---|---|
| Published Date | 1957-09 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume19 |
| Content Type | Conference Paper |
| Author | Yamaguchi, Kenji| |
|---|---|
| Published Date | 1957-09 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume19 |
| Content Type | Conference Paper |
| Author | 初田 甚一郎| 尹 一| |
|---|---|
| Published Date | 1957-09 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume19 |
| Content Type | Conference Paper |
| JaLCDOI | 10.18926/40272 |
|---|---|
| Title Alternative | THE CHANGE IN CONCENTRATION OF FERROUS IRON AND REDUCIBLE IRON, DISSOLVED IN SPRING WATER AT MISASA HOT SPRINGS, JAPAN, DURING PRESERVATION OF THE WATER SAMPLE IN A SEALED BOTTLE |
| FullText URL | pitsr_020_048_054.pdf |
| Author | Tanaka, Shigeo| |
| Abstract | The two sprigns called "Tanaka-no-Yu" and "Hisui-no-Yu" at Misasa Hot Springs, japan (Fig. 1), suitable for sampling the unpolluted water, the locations of which, are shown in Fig. 2, were chosen for this study. The o-phenanthroline method, details of which were discussed in the previous report by the author (Repts. Balneol. Lab. Okyama Univ., 17, 1, (1956)) was used for the determination of ferrous iron, ferrous iron + reducible iron, and ferrous iron + reducible iron + colloidally dispersed iron (to be referred to as "total irons" in this report). For comparison, the change in concentratin of iron dissolved in distilled water during preservation in a sealed bottle was observed, and the results obtained for the solutions with the pH values of 5.4 and 5.8 are illustrated in Fig.3 and Fig.5, rspectively. Both ferrous and reducible iron disappear within 5 minutes, when the pH of the solution is 6.4. The hydrogen ion concentration was thus seen to give a sensitive effects on the speed of diminution of ferrous and reducible iron dissolved in the distilled water. It should be noticed that no appreciable diminution was observed during the period from 60 min. to 120 min,. It is probable that the diminution of total iron is caused by the adsorption of colloidal iron hydroxides on the wall of glass bottle. The effects of charged anion (SO(4)(--)) on the change in concentration of iron during preservation was also investigated, but no appreciable effect was found. (Fig. 5 and Fig. 6). Fig.7, Fig.8, and Fig.9 show the change in concentration of iron during preservation of the spring water at "Tanaka-no-Yu". The content of iron in the spring water is about 0.3 mg/l, and its pH value is about 7.1. For the first 30 minutes, ferrous iron diminishes rapidly, the slope of the diminution curve being sharp and almost straight. Thereafter the slope becomes gentler, and, after an hour, the slope approaches nearly zero. On the other hand, ferrous iron dissolved in distilled water disappears in a moment at the same pH 7.1. Fig.10, Fig.11, and Fig.12 show the change in concentration of iron during preservation of the spring water at "Hisui-no-Yu". The content of iron in the spring water is about 1.0 mg/l, and its pH value is about 6.4. In this case, the diminution of ferrous iron is not remarkable, and only 20% of the initial quantity diminishes within 2 days. Whereas, in the case of distilled water, the diminution is very rapid at the same pH 6,4, and the ferrous iron disappears completely within 5 minutes. In Fig.13 the speed of diminution of iron in distilled water and that in spring water are compared. The difference here seen may probably be due either to that the ferrous iron in spring water is in a certain complex form not easily oxidizable, or to that the spring water contains some reducing substances. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1958-01 |
| Volume | volume20 |
| Start Page | 48 |
| End Page | 54 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002462895 |
| JaLCDOI | 10.18926/40267 |
|---|---|
| Title Alternative | Studies on Balneotherapy of Gynecological Chronic Inflammations |
| FullText URL | pitsr_021_001_046.pdf |
| Author | Ishii, Chikara| |
| Abstract | The effects of balneotherapy on gynecological chronic inflammations were examined both clinically and experimentally. Clinical study. Statistical observations were made on the patients with gynecological diseases who visited the spa of Misasa. It was ascertained that, among them, the patients with gynecological chronic inflammati on whose chief complains were hypogastric and Lumbar pains were most common and that, by balneotherapy, their conditions were frequently improved both subjectively and objectively. Experimental study. An experimental foreign body inflammation was evoked by inserting a Sponge into the abdominal cavity of an adult female rat and the effects of hot-spring bath were examined. Acceleration of the absorption of the inflammation, enhancement of phagocytosis of the subcutaneous histiocytes, activation of the fibrohistiocytic system of the subcutaneous connective tissue, and acceleration of return of the free cells in the abdominal cavity were proved. Furthermore, comparative studies were made on the effects of various artificial mineral waters and ultra short waves. It was found that, though they were less effective than natural mineral water, artificial strong saline water, artificial sulfur water, artificial sulfate water, artificial iron water and ultra short waves were effective and that artificial weak saline water, artificial bicarbonate water, artificial humimic acid water, artificial alkaline water, and artificial acidic water were as effective as fresh water. Compared with hot bath, insensible bath was more effective. No significant difference of therapeutic effect was found by bathing once a day or three times a day. In short, balneotherapy had a facilitatory action on the absorption of the inflammatory changes in the abdominal cavity. This should be ascribed not only to the increase in the deep blood flow by warming but also to the general defence mechanism enhanced by cutaneous stimulation. Some differences were also assumed depending on the ions contained in the mineral waters. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1958-04 |
| Volume | volume21 |
| Start Page | 1 |
| End Page | 46 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002462893 |
| JaLCDOI | 10.18926/40259 |
|---|---|
| Title Alternative | Study of Togo -Matsuzaki Hot Springs, Tottori Prefecture |
| FullText URL | pitsr_023_001_022.pdf |
| Author | Umemoto, Shunji| Harada, Mitsuru| Okabe, Shigeru| Miyakoshi, Junichiro| Sakanoue, Masanobu| Tanaka, Masaya| Mifune Masaaki| |
| Abstract | 1. Layers containing thermal water in this district are thin, and lie at different depths (about 35, 55, and 60 meters) from the ground surface. There are evidences to show that these layers are intimately connected with one another. 2. The authors may suppose the existence of a structurally weak zone, along the line from Matsuzaki to Asozu, within which the issuing spots of thermal springs are located. 3. The head water levels of the thermal springs in this district are closely related with that of Lake Togo. Keeping pace with the variations of the water levels of Lake Togo and of artesian wells in its vicinity, the rate of flow of thermal springs vary; and the correlation between these variations is apparent. 4. The pumping suction of thermal water at one spring affects the flow of water at other springs within distances of 150 to 200 meters therefrom, though the direct sources of thermal water supply for the latter springs may be different from that of the former. 5. The spring water in this district is considered to be a mixture of hot water, containing sodium, calcium, chloride, and sulfate ions, and cold water, containing bicarbonate ion. The diversity of chemical constitutions of different spring waters is explained as due to the difference in proportion in which the hot and cold waters are mixed. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1958-10 |
| Volume | volume23 |
| Start Page | 1 |
| End Page | 22 |
| ISSN | 0369-7142 |
| Related Url | http://ousar.lib.okayama-u.ac.jp/metadata/40258 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002462891 |
| JaLCDOI | 10.18926/40245 |
|---|---|
| Title Alternative | Granites in the Neighbourhood of Misasa Town, Tottori Prefecture |
| FullText URL | pitsr_025_001_012.pdf |
| Author | Shibata, Hidekata| Sayama, Mitsuo| |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1959-05 |
| Volume | volume25 |
| Start Page | 1 |
| End Page | 12 |
| ISSN | 0369-7142 |
| Related Url | http://ousar.lib.okayama-u.ac.jp/metadata/40244 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002462887 |
