検索結果 1263 件
| JaLCDOI | 10.18926/40361 |
|---|---|
| タイトル（別表記） | Studies of the radio-active springs. XXV The effect of Thoron spring bath on Rotter's reaction |
| フルテキストURL | rbl_003_018_020.pdf |
| 著者 | 大島 良雄| |
| 抄録 | In the preliminary papers the author reported that the Thoron in thermal water passes throngh the skin and stimulates the subcutaneous connective tissue cells. Sotozono proved that the reduced ascorbic acid content in the blood increases after the Radonspring bath. Before and after thermal bath the author measured the time necessary for the complete decoloration of intradermally injected dichlorphenol-indophenol solution. Compared with the plain water bath at a same temperature, the Thoron spring bath seems to have a tendency to reduce the time necessary for the decoloration. |
| 出版物タイトル | 放射能泉研究所報告 |
| 発行日 | 1950-07-25 |
| 巻 | 3巻 |
| 開始ページ | 18 |
| 終了ページ | 20 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002484885 |
| JaLCDOI | 10.18926/40360 |
|---|---|
| タイトル（別表記） | Studies of the radio-active springs : XXIV Effect of the internal use of the radio-active waters on alimentary hyperglycemia, influence cf the aging of mineral water |
| フルテキストURL | rbl_003_015_017.pdf |
| 著者 | 森永 寛| |
| 出版物タイトル | 放射能泉研究所報告 |
| 発行日 | 1950-07-25 |
| 巻 | 3巻 |
| 開始ページ | 15 |
| 終了ページ | 17 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002484884 |
| JaLCDOI | 10.18926/40353 |
|---|---|
| タイトル（別表記） | STUDIES ON THE AGING OF THE MINERAL WATERS (Ill) VARIATION OF SILICATE IN THEMINERAL WATERS |
| フルテキストURL | pitsr_012_006_010.pdf |
| 著者 | 杉原 健| |
| 抄録 | 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. |
| 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 | 6 |
| 終了ページ | 10 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002484889 |
| JaLCDOI | 10.18926/40352 |
|---|---|
| タイトル（別表記） | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE A;\lD SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (VIII) MATSUZAKI, TOGO AND ASOZU HOT SPRINGS, TOTTORI PREFECTURE, JAPAN |
| フルテキストURL | 012_001_005.pdf |
| 著者 | 木村 健二郎| 梅本 春次| |
| 抄録 | In Matsuzaki, Togo and Asozu Hot Springs which issue around the Pond Togo, the chloride and sulfate content and water temperatures of well waters and the amount of chloride and sufate fixed to the soil were determined with samples collected from various parts of the thermal spring districts and its neighborhood. The chloride and sulfate content and water temperatures of the well water samples collected from the thermal spring districts were higher than those from its neighbourhood, but for the amounts of chloride and sulfate fixed to the soil, no difference was detected. As the existence of other sources which would supply the chloride, sulfate and heat to the water 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 be due to the effects of thermal springs. |
| 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 | 1 |
| 終了ページ | 5 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532436 |
| JaLCDOI | 10.18926/40345 |
|---|---|
| タイトル（別表記） | BALNEOLOGICAL STUDIES USING RADIOACTIVE ISOTOPES (3) |
| フルテキストURL | pitsr_013_018_023.pdf |
| 著者 | 横田 剛男| 芦沢 峻| |
| 抄録 | 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. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1953-12 |
| 巻 | 13巻 |
| 開始ページ | 18 |
| 終了ページ | 23 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40340 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002484880 |
| JaLCDOI | 10.18926/40344 |
|---|---|
| タイトル（別表記） | STUDIES ON VITRIOL SPRINGS (4) ON THE COPPER, ZINC, NICKEL, AND COBALT CONTENTS OF BLOOD AFTER THE INTERNAL USE OF A VITRIOL WATER |
| フルテキストURL | 013_015_017.pdf |
| 著者 | 大島 良雄| 芦沢 峻| |
| 抄録 | Sotozono proved that the administration of daily 20cc of Fujino Mineral Water (an acid vitriol water containing copper, zinc, nickel and cobalt) has a remarkably beneficial effect on several kinds of hypochromic anemia. It contains 9.56gms of iron, 0.007gm of zinc, 0.005gm of copper 0.001gm of nickel, and 0.006gm of cobalt in one liter. 20 - 40cc of Fujino water was diluted 5 - 10 fold with plain water and administered to the fasting patients perorally. Blood samples were taken from cubital vein before, 1, 2, 4, 6, 24, 48, and 72 hours after the intake of the vitriol water. Copper, zinc, nickel and cobalt contents of the blood samples were measured by Ashizawa' s dithizone- chromatographic method. It was shown that copper, nickel, and cobalt contents of blood rose unexpectedly high temporarily, in a manner that did not correspond to their amount in the given mineral water. So that the mobilization of copper, nickel, and cobalt in the body after the intake of the mineral IVrter was susrected. Zinc content of blood showed no constant tendency. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1953-12 |
| 巻 | 13巻 |
| 開始ページ | 15 |
| 終了ページ | 17 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002484879 |
| JaLCDOI | 10.18926/40343 |
|---|---|
| タイトル（別表記） | STUDIES ON VITRIOL SPRINGS (3) EFFECT OF THE INTERNAL USE OF VITRIOL WATER OF FUJINO ON THE GASTRIC ACIDITY |
| フルテキストURL | pitsr_013_009_014.pdf |
| 著者 | 森永 寛| |
| 抄録 | Fujino Spring is the foremost acid vitriol spring of Japan in ferrous and ferric ion contents. Six years ago the author reported that its internal use had an remarkable hemopoietic effect on hypochromic anemia and delayed the curve of alimentary hyperglycemia in rabbit. Twenty ml. of this vitriol water was diluted with plain water to two hundred ml. and was given to twenty one patients by stomach tube at 37°C. Gastric acidity of the patients was measured at 30 minutes intervals during the following 150 minutes after the administration of the water. In six cases of normal acidity no significant difference was proved between the effects of the mineral water and of caffein control (0.2g. in 200 ml.). In six cases of hyperacidity it seemed that the vitriol water decreased in the acidity curve compared with control. In nine patients of hypo- and anacidity both free and total acidity curve was elevated by the use of the mineral water compared with caffein control. The internal use of Fujino Spring in moderate dilution with plain water regulated the gastric acidity. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1953-12 |
| 巻 | 13巻 |
| 開始ページ | 9 |
| 終了ページ | 14 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002484879 |
| JaLCDOI | 10.18926/40342 |
|---|---|
| タイトル（別表記） | ON THE EXISTENCE OF RADIUM B, RADIUM C AND THORIUM B IN MISASA HOT SPRINGS |
| フルテキストURL | pitsr_013_005_008.pdf |
| 著者 | 佐藤 三雄| |
| 抄録 | 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. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1953-12 |
| 巻 | 13巻 |
| 開始ページ | 5 |
| 終了ページ | 8 |
| ISSN | 0369-7142 |
| 言語 | 英語 |
| 論文のバージョン | publisher |
| NAID | 120002484878 |
| JaLCDOI | 10.18926/40341 |
|---|---|
| フルテキストURL | pitsr_013_001_005.pdf |
| 著者 | Umemoto, Shunji| |
| 抄録 | Various colormetric methods for determining magnesium in natural waters have been studied, and the methods using 8-oxyquinolin, ammonium molybdate and titan yellow were studied most frequently(1)), following the studies on the interfering ions(2)). Brilliant yellow(3)), l-amino-2-naphthol-6-sulfonic acid(4)) and other new reagents were also used. E. D. T. A. was used, but the determination by using this reagent is not exact. Present reagent already reported by T. Ashizawa(5)), magneson II, is insoluble in water, soluble in alkali and hardly soluble in ethanol. In the existence of magnesium ion, the color of solution varies from pink-violet (in alkali) and orange (in ethanol) to blue-violet. This variation of color was evaluated photometrically by Shimadzu photoelectric spectrophotometer, and moreover the grades of interference by interfering ions were clarified. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1953-12 |
| 巻 | 13巻 |
| 開始ページ | 1 |
| 終了ページ | 5 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40340 |
| 言語 | 英語 |
| 論文のバージョン | publisher |
| NAID | 120002484877 |
| JaLCDOI | 10.18926/40326 |
|---|---|
| タイトル（別表記） | ASOZU (WEAK COMMON SALT SPRING), HAMAMURA (SULPHATED BITTER SPRING), KAlKE (CALCIUM CHLORIDE CONTAINING SALINE SPRING) AND FUJINO (ACID ALUM VITRIOL SPRING) SPRING WATERS AND THE ALIMENTARY HYPERGLYCEMIA |
| フルテキストURL | pitsr_014_022_029.pdf |
| 著者 | 森永 寛| |
| 抄録 | There are many experimental reports and clinical observations about the internal use of thermal waters on carbohydrate metabolism, and alkaline springs, alkaline common salt springs and sulphur springs are used for the balneological therapy of diabetic patients. The author reported that the internal use of the radon springs of Japan, such as Misasa, Ikeda and Masutomi thermal waters promoted the action of insuline and inhibited the experimental hyperglycemia in rabbits, and he suggested that these radioactive waters also would be able to utilize for the diabetic treatment. On the other hand, trace elements such as Cu, Zn and Mn have protective effects against disturbed carbohydrate metabolism of diabetic body. Some thermal waters contain these trace elements in various degrees, and Oshima & Ashizawa observed that after the drinking of Fujino mineral water the iron, copper, nickel and cobalt content in blood rose temporarily. In this report, the author investigated the influence of the drinking of Asozu (weak common salt spring), Hamamura (sulphated bitter spring), Kaike (calcium chloride containing saline spring) and Fujino (acid alum vitriol spring) Spring waters upon the alimentary hyperglycemia in rabbits. Thirty ml. of 10% glucose solution in thermal water (Fujino Water was diluted twice with plain water) or in plain water per kg. of bodyweight was administered to the rabbit by stomach tube and blood sugar level was determined before, 1/2, 1, 2, 3 and 4 hours after the administration. The results were as follows: 1. The drinking of Asozu Spring water inhibited the alimentary hyperglycemia compared with the plain water as a control. 2. Hamamura Spring had a tendency to decrease the blood sugar level. 3. Kaike Spring water had no inhibitory a.ction upon the alimentary hyperglycemia. 4. In spite of the existence of trace elements, Fujino mineral water had no significant effect. The author supposed that this was due to its high acidity. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1954-03 |
| 巻 | 14巻 |
| 開始ページ | 22 |
| 終了ページ | 29 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002462903 |
| JaLCDOI | 10.18926/40325 |
|---|---|
| タイトル（別表記） | EFFECT OF WATER LEVEL OF RIVER ON MINERAL SPRING |
| フルテキストURL | pitsr_014_015_021.pdf |
| 著者 | 梅本 春次| |
| 抄録 | 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. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1954-03 |
| 巻 | 14巻 |
| 開始ページ | 15 |
| 終了ページ | 21 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002462902 |
| JaLCDOI | 10.18926/40324 |
|---|---|
| タイトル（別表記） | RADON CONTENT OF HOT SPRINGS IN TOTTORI PREFECTURE, JAPAN |
| フルテキストURL | 014_001_014.pdf |
| 著者 | 大島 良雄| 山田 尚春| 御船 政明| |
| 抄録 | 1. Radon content of 166 thermal waters in IWAI, TOTTORI YOSHIOKA, HAMAMURA, TOGO, SEKIGANE, MISASA, and KAlKE Hot Springs was measured by I. M. Fontactoscope in the years 1950-1951. Of which 66 samples showed a radon content over 30×10(-10) curie units per liter. Namely, 50 springs in Misasa, 6 in Sekigane, 9 in Hamamura, and one in Togo belonged to the radioactive spring in the definition by Ministry of Social Welfare. The highest Radon content (1150×10(10) curie units per liter) was recorded in Hisuino-Yu in Misasa, where five springs had a radon content over 360×10(-10) curie units per liter. 2. No marked difference was proved between the results obtained this time and the data in the former reports concerning the radon content of these thermal springs. 3. Radon content proved higher in the springs which issue from granite than in the springs of other districts. No definite relation was proved between the radon content and water temperature. The radon content was generally high in simple thermals or in weak sodium chloride springs, low in sulfated springs and in saline springs which had a comparatively high sulfate content. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1954-03 |
| 巻 | 14巻 |
| 開始ページ | 1 |
| 終了ページ | 14 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532457 |
| JaLCDOI | 10.18926/40319 |
|---|---|
| タイトル（別表記） | REPORT OF THE CHEMICAL ANALYSIS OF MISASA HOT SPRINGS, TOTTORI PREFECTURE |
| フルテキストURL | 016_001_018.pdf |
| 著者 | 大島 良雄| 御船 政明| 山田 尚春| 上山 昭子| |
| 抄録 | The water samples of 55 springs of Misasa were analysed in the years 1950～1951. The temperatures of the waters ranged from 44° to 85° C. Radon content ranged from 34.1 to 2360×10(-10) curies per liter. pH 6.2～7.5. Evaporation residue: 534～1940 mg/kg. K(+) :10.4～47.3mg/kg. Na(+) : 140.4～574mg/kg. Ca(2+) : 7.56～49.06mg/kg. Mg(2+) : 0.11～15.3mg/kg.. Fe(2+) : 0.10～0.67mg/kg. Cl(-) : 138～854mg/kg. SO(4)(2-) : 29.2～187mg/kg. HCO(3)(-) : 74.8～370mg/kg. HBO(2)(-) : 1.80～19.6mg/kg. S(2)O(3)(2-) : o.62～3.69mg/kg. Radon sources seem to exist at shallow places under the ground and the radon in the thermal wacer is supposed to have been derive partly from the ground water which also contains considerable amount of radon. A close linear correlation (r=0.751) was proved between the sulfate and the chloride ion contents. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1956-01 |
| 巻 | 16巻 |
| 開始ページ | 1 |
| 終了ページ | 18 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40318 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532473 |
| JaLCDOI | 10.18926/40313 |
|---|---|
| タイトル（別表記） | EFFECT OF INTERNAL USE OF THERMAL WATER OF YUMURA AND MUSASHI HOT SPRINGS UPON THE ALIMENTARY HYPERGLYCEMIA IN RABBITS |
| フルテキストURL | pitsr_017_008_012.pdf |
| 著者 | 森永 寛| |
| 抄録 | The author investigated the effect of the internal use of thermal water of Yumura (weak alkaline spring, Hyogo Prefecture) and Musashi (weak common salt spring, Fukuoka Prefecture) Springs upon the alimentary hyperglycemia in rabbits. Sixty ml. of spring water, and of plain water as control, with 10% glucose in solution was administered to rabbits by stomach tube, and the blood sugar level was determined before and 1/2, 1, 2 and 3 hours after the administration. In all cases, the thermal water was revealed to inhibit the alimentary hyperglycemia significantly by comparing the results obtained with the thermal water and those with the plain water control. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1956-03 |
| 巻 | 17巻 |
| 開始ページ | 8 |
| 終了ページ | 12 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002462898 |
| JaLCDOI | 10.18926/40312 |
|---|---|
| タイトル（別表記） | o-PHENANTHROLINE METHOD APPLIED TO THE DETERMINATION OF IRON IN NATURAL WATERS |
| フルテキストURL | pitsr_017_001_007.pdf |
| 著者 | 田中 重男| |
| 抄録 | 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. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1956-03 |
| 巻 | 17巻 |
| 開始ページ | 1 |
| 終了ページ | 7 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40311 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002462897 |
| JaLCDOI | 10.18926/40273 |
|---|---|
| タイトル（別表記） | On the Underground Temperatures and Radioactivities at One Meter Depth in the Misasa Hot Spring Area |
| フルテキストURL | pitsr_020_055_061.pdf |
| 著者 | 相馬 徳蔵| |
| 抄録 | Methods and Results of Measurements:-- A stick of steel was driven into the ground down to one meter depth, and a narrow pipe of aluminum or brass, closed at the upper end, was inserted and the hole covered by a board and earth. (See Fig.3.) In Fig.2 the locations for the experiments are shown by x. Fig.1 gives the atmospheric temperatures at noon, October4-21,1955, when the experiments were carried out. About three hours after the above setting had been done, the gas in the hole was replaced by a bottle of water, and was collected, by driving sprayer for five minutes with apparatus as shown in Fig.5, in a can in which an autoradiographic plate was set. (See Fig.6.) The temperature in the hole was read by means of a maximum thermometer hung in the hole for ten minutes at one meter depth. Fig.7 shows the distribution of temperatures at one meter depth thus observed. Exactly twenty four hours after the above setting, the autoradiographic plate in the can (a quarter sized Fuji ET-2E plate, 15μ thick, for contact method) was developed. For developing, the plate was immersed in Ilford D-19 for fifteen minutes, then fixed with Fuji-fix for fifteen minutes, washed with running water for forty minutes, and dried. Then those autoradiographic plate was examined under the microscope of magnification ×280, to count the number of tracks of a-particles. The results obtained are shown in Fig.8. Underground Temperature Distribution:-- On the basis of the distribution of temperatures at one meter depth (Fig.7) and of other available boring data, the distribution of undergound temperatures is estimated as shown in Fig.9 (vertical section along the Misasa river). |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1958-01 |
| 巻 | 20巻 |
| 開始ページ | 55 |
| 終了ページ | 61 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002462896 |
| JaLCDOI | 10.18926/40272 |
|---|---|
| タイトル（別表記） | 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 |
| フルテキストURL | pitsr_020_048_054.pdf |
| 著者 | 田中 重男| |
| 抄録 | 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. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1958-01 |
| 巻 | 20巻 |
| 開始ページ | 48 |
| 終了ページ | 54 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002462895 |
| JaLCDOI | 10.18926/40271 |
|---|---|
| フルテキストURL | pitsr_020_042_047.pdf |
| 著者 | 田中 重男| |
| 抄録 | Differential thermal investigation was made of amorphous hydrous ferric oxides, precipitated on neutralization of ferric chloride solution under different laboratory conditions, ranging from DOC to 85°C in temperature, and from 3 to 12 in pH. Each of the differential thermal curves obtained shows an endothermic peak due to the release of adsorbed water, followed by a exothermic peak due to crystallization of anhydrous ferric oxide to hematite. The temperature corresponding to the exothermic peak varies in the range from 240°C to 460°C accrding to the temperatures and pH values of the solution from which the hydrous ferric oxide is precipitated. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1958-01 |
| 巻 | 20巻 |
| 開始ページ | 42 |
| 終了ページ | 47 |
| ISSN | 0369-7142 |
| 言語 | 英語 |
| 論文のバージョン | publisher |
| NAID | 120002462894 |
| JaLCDOI | 10.18926/40267 |
|---|---|
| タイトル（別表記） | Studies on Balneotherapy of Gynecological Chronic Inflammations |
| フルテキストURL | pitsr_021_001_046.pdf |
| 著者 | 石井 氻| |
| 抄録 | 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. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1958-04 |
| 巻 | 21巻 |
| 開始ページ | 1 |
| 終了ページ | 46 |
| ISSN | 0369-7142 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002462893 |
| JaLCDOI | 10.18926/40265 |
|---|---|
| タイトル（別表記） | Studies on Paper-Analysis in the Field of Balneology (I) Studies on Iron in Serum by Means of Parper-Electrophoresis and Paper-Chromatography |
| フルテキストURL | 022_037_054.pdf |
| 著者 | 石橋 丸応| |
| 抄録 | 1. The author showed by means of paper-electrophoresis using o-nitrosoresorcinmonomethylether (hereafter N. R. M. E.), a colourdeveloping reagent, that iron in serum combines with β-fraction of serum protein. 2. The author proposed a new method for the determination of serum iron by means of paper-chromatography. Procedure is as follows. In a centriguged tube, 0.5 ml. of clear serum is taken, acidified with 0.15 ml. of 20% HNO(3), and allowed to stand for 20 minutes. After addition of 0.2 ml. of saturated solution of CH(3)COONa and 1 ml. of acetic acid-sodium acetate buffer solution (pH: 3.8), the mixture is kept for at least 10 min. and filtered through Toyo-filter-paper No.5 A. The clear filtrate is taken in a stoppered test tube (the inside diameter: 1.2 cm.; height: 15 cm.). To this filtrate are added 0.2 ml. of 20% Hydroxylamine hydrochloride and 0.25 ml. of saturated aqueous solution of N. R. M. E. After being allowed to stand for at least 20 min., the mixture is shaken with 5 ml. of carbon tebrachloride. Then the excess of N. R. M. E. is removed. The supernatant aqueous solution (0.2 ml.) is used for a determination sample. The sample is placed on the paper (Toyo,filter-paper No.51 or 50) in a thin line at a distance of 10 cm. from the edge, and the spots are developed with 90 % ethylalcohol. After development for 4-6 hours, a green-coloured linear spot appsars at a distance of 12-16 cm. from the origin-point. Spot intensity at 670 mμ is measured with Natsume's densitometer, and from this, concentration of Fe can be estimat.ed on the standard graph (Fig. 5). 3, Effects of radioactive thermal spring bathing and internal use of vitriol water upon serum iron levels were studied with the result.s as follows. The above-mentioned author's method of determining the iron level in a small amount of serum is very convenient in investigating iron metabolism in the field of balneotherapy. The author examined changes of iron levels in serum after radioactive thermal bathing as well as after internal use of acid vitriol water. a) The iron levels in serum were maasurecl by the author's method before and 5, 30 and 60 minutes after the radioactive thermal bath (Rn-content: 10-30 Mache, 42-3°C., for 10 min,). The iron levels in the serum of healthy subjects showed no significant change after the thermal bathing. b) Yanahara Mineral Water (an acid vitriol water, pH; 2.2) contains 0.045 gm. of Cl(-), 12.35 gm. of SO(4)(--), 2.5 gm. of Fe(++)+Fe(+++), 0.0938 gm. of Al(+++) and 0.0001 gm. of Cobalt in one liter. i) Thirty ml. of Yanahara, water diluted with plain water to 200 ml. (Fe(++) content: ca. 75 mg.) and administered to health fasting subjects orally. As a control matter, 0.65 gm. of Glukon-F powder (Fe(++) content.: ca. 75 mg.) was then given. Blood samples were taken from the cubital vein before and 1, 3 and 6 hours after the intake of the dtriol water. Iron contents of the serum samples were measured by the author's paper chromatographic method. The results were shown in the table and the figure. The iron contents of the serum after the intake of the mineral water were higher than in the case of the control. ii) Two ml. of Yanahara vitriol water was administered to rabbits with the aid of a stomach tube, and serum iron levels wera determined before and 1, 3, 4 and 6 hours after the administration. An amount of 0.05 gm. of Glukon-F powder was dissolved in 5 ml. of plain water, and this solution was given to rabbits as a control. After the internal use of vitriol water, iron levels in serum rose and remained unexpactedly high for about 1-4 hours, in a manner that did not. correspond to the amount of iron in the given mineral water. So that it was suspected that the iron originally contained in the living subjects had been mobilized by the intake of vitriol water. Iron levels in serum after administration of a solution of Glukon-F powder were lower than in the case of the mineral water. |
| 出版物タイトル | 岡山大学温泉研究所報告 |
| 発行日 | 1958-07 |
| 巻 | 22巻 |
| 開始ページ | 37 |
| 終了ページ | 54 |
| ISSN | 0369-7142 |
| 関連URL | http://ousar.lib.okayama-u.ac.jp/metadata/40263 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 40017532359 |