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著者 Sakawa Masatoshi| Matsuoka Shimpei| Kato Kosuke| Ishimaru Keiichi| Ushiro Satoshi|
発行日 2009-11-12
出版物タイトル Proceedings : Fifth International Workshop on Computational Intelligence & Applications
2009巻
1号
資料タイプ 会議発表論文
JaLCDOI 10.18926/19625
タイトル(別表記) STUDIES ON BALNEOTHERAPY OF DIABETES MELLITUS (Ⅱ). EFFECT OF INTERNAL USE OF GERO HOT SPRING ON THE ALIMENTARY HYPERGLYCEMIA IN ALLOXAN-DIABETIC RABBITS
フルテキストURL 015_048_052.pdf
著者 森永 寛|
抄録 The author investigated the effect of the internal use of the hot spring water of Gero (Gifu Prefecture, Japan), which contained Cl' 167 mg./L., HCO(3)' 66.0 mg./L. and titrated sulphur 0.6 mg./L. (pH: 6.2) at the time of this experiment, upon the alimentary hyperglycemia in alloxan-diabetic rabbits. 1. The author injected alloxan of 150 mg. per kg. of body weight intravenously into normal rabbits and performed the experiment 5~6 weeks after the injection. At the time of the experiment, the fasting blood sugar levels of alloxan-diabetic rabbits ranged from 107 to 211 mg./dl. (170 mg./dl. on the average). 2. Thirty ml. of 10% glucose solution in thermal water or in plain water per kg. of body weight was administered to the rabbits by stomach tube, and blood sugar level was determined before and 1/2, 1, 2, 3, 4 and 5 hours after the administration. The rejection interval (5%) of the glucose tolerance in 17 normal rabbits is shown in Fig. Ⅰ. Glucose tolerance curves of these alloxan-diabetic rabbits were out of the limit of the normal range. 3. Gero Hot Spring water had no inhibitory action upon the alimentary hyperglycemia of alloxan-diabetic rabbits.
出版物タイトル 岡山大学温泉研究所報告
発行日 1955-03-25
15巻
開始ページ 48
終了ページ 52
ISSN 0369-7142
言語 日本語
論文のバージョン publisher
NAID 120002309141
JaLCDOI 10.18926/19621
タイトル(別表記) STUDIES ON BALNEOTHERAPY OF DIABETES MELLITUS (Ⅰ). EFFECT OF THE RADIOACTIVE THERMAL BATH UPON THE CARBOHYDRATE METABOLISM AND THE LEUCOCYTE PICTURE IN ALLOXAN-DIABETIC RABBITS.
フルテキストURL 015_034_047.pdf
著者 森永 寛|
抄録 The author investigated the effect of the radioactive thermal bath upon the carbohydrate metabolism and the leucocyte picture in alloxan-diabetic rabbits. 1. The author injected 100-200 mg. of alloxan per kg. of body weight intravenously into normal rabbits and produced alloxan diabetes. The triphasic blood sugar response to the injection of alloxan is illustrated in Table 1. and Fig. 1. About a week after the injection of alloxan, the fasting blood sugar values ranged 127 to 331 mg./dl. (Table 3.). 2. In this experiment the alloxan-diabetic rabbits were put in radioactive hot spring and plain water bath, 42-44℃. in temperature. The radioactive hot springs put in use are "Hisui-no-Yu" and "Kenkyusho-sen" (the Loboratory-Spring), both in Misasa Spa, the chemical compositions of which are given in Table 2. 3. In any case, the blood sugar level rose temporarily after the thermal baths for 5 minutes, but the 24-hour blood sugar value after taking a bath was lower in "Hisui-no-Yu" (Rn: 300-400 Mache units) than in "Kenkyusho-sen" (Rn: 10-30 Mache units) (Table 3 and Fig. 2). 4. The glucose tolerance was found to be abnormal in alloxan-diabetic rabbits even 3 months after the injection of alloxan, but this abnormal carbohydrate metabolism tended to become normal by the radioactive thermal bath (Table 5, 6 and Fig. 3, 5.). 5. The radioactive thermal bath in "Hisui-no-Yu" caused increase of leucocyte counts of alloxan-diabetic rabbits more remarkably than the bath in "Kenkyusho-sen" (Table 8. and Fig. 6).
出版物タイトル 岡山大学温泉研究所報告
発行日 1955-03-25
15巻
開始ページ 34
終了ページ 47
ISSN 0369-7142
関連URL http://ousar.lib.okayama-u.ac.jp/21510
言語 日本語
論文のバージョン publisher
NAID 120002314143
JaLCDOI 10.18926/19607
タイトル(別表記) EFFECT OF WATER LEVEL OF RIVER ON MINERAL SPRING (Continued)
フルテキストURL 015_011_015.pdf
著者 梅本 春次|
抄録 From February to September 1954, observations were made of the rates of flow and the water temperatures at a spring called "Tanaka-no-Yu", Misasa Hot Springs, Tottori Prefecture. Simultaneously with these observations, the water level of the River Misasa and that of an irrigation stream nearby were also determined. The procedures for the observations were the same as in the previous report. Comparing the results here obtaind wite those previously obtaind, and referring to the conclusions in the previous report, the author has been led to the following conclusions. From the observations in the period from February to September, 1954, as from those in the period from June, 1953 to January, 1954, a positive correlation was found between the rate of flow and the water teperature, the correlarion coefficient being 0.828 (highly significant). The analsis of variance of the obseryed results showed that the rate of flow and the water temperature appear to be affected by the water levels of the River and of the irrigation stream, and also by their interaction. This conclusion supports what was deduced in the previous report. The average water levels of the River and of the irrigation stream, the average rates of flow and the average water temperatures, for the period from June to September in 1953, were compared with those for the period from June to September in 1954. The differences in the average water levels of the River, the average rates of flow and the average water temperatures are significant; while that in average water levels of the stream is not significant. From this it may be concluded that the increase in the rate of flow and the rise of the water temperature were resulted from the upheaval of the water level of the River, which followed the construction of a dam there.
出版物タイトル 岡山大学温泉研究所報告
発行日 1955-03-25
15巻
開始ページ 11
終了ページ 15
ISSN 0369-7142
言語 日本語
論文のバージョン publisher
NAID 120002309149
JaLCDOI 10.18926/19605
タイトル(別表記) STUDIES ON CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO SOIL IN THE MINERAL SPRING DISTRICTS (X) MATSUZAKI, TOGO AND ASOZU HOT SPRINGS AND HAMAMURA AND KACHIMI HOT SPRINGS (Continued)
フルテキストURL 015_006_010.pdf
著者 梅本 春次|
抄録 At Matsuzaki, Togo and Asozu Hot Springs and at Hamamura and Kachimi Hot Springs, the amounts of chloride and sulfate fixed to soil were determined with samples which were colleted from various parts of the thermal spring zone and its outside area, more than ten days after rainfall, so as to eliminate its possible effect. The amounts of sulfate were determined by terbidimetry with BaCl(2) solution and those of chloride were determined by mercuric thiocyanate method. In the average amounts of chloride and sulfate, no differences were found between the samples collected from the thermal spring zone and its outside area. The same fact was described in the 5th and 8th reports, but errorneously ascribed to an effect of rainfall. From the present study it has been ascertained that the fact is independent of rainfall.
出版物タイトル 岡山大学温泉研究所報告
発行日 1955-03-25
15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 120002309043
JaLCDOI 10.18926/19602
タイトル(別表記) STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO SOIL IN THE MINERAL SPRING DISTRICTS (IX) SAGINOYU HOT SPRINGS, SHIMANE PREFECTURE, JAPAN.
フルテキストURL 015_001_005.pdf
著者 梅本 春次| 田中 重男|
抄録 At Saginoyu Hot Springs same experiments as those described in previous reports were carried out. Water temperature of Springs is about 50℃. and main constituents dissolved in spring water are calcium sulfate and sodium chloride, its total salt content being 1.5g./ℓ.. Experimental results obtained are shown in the annexed table and map. The results obtained may be discussed in two ways: First, the area marked with ※ is regarded as the spring zone, and a comparison is made by Cochran and Cox's method between this zone and the outside area as to the average contents of chloride and sulfate in well Water, the average water temperatures of well water and the average amounts of chloride and sulfate fixed to soil. The differences in averages of the chloride and sulfate content of well water are significant, while that in average water temperatures is not significant. The differences in the average amounts of chloride and sulfate fixed to soil are not significant. However, the difference in the average amounts of chloride fixed to soi1 is nearly same as that for the 5 % level, and it is seen that the average amount of chloride fixed to soil tends to be higher in the spring zone than in the outside area. Second, the area marked with t is regarded as the spring zone, and a comparison is made in the same way as the above. The differences in the averages of the chloride and sulfate contents and water temperatures of well waters, all being higher in the spring zone, are significant. The differences in average amounts of chloride and Sdlfate fixed to soil are not significant. However, since these differences are nearly same as that for the 5 % level, the average amounts of chloride and sulfate fixed to soil tend to be higher in the spring zone than in the outside area. As the existence of sources which would supply the chloride, sulfate and heat to the water and soil is impossible, the above differences may be due to effects of thermal springs. Since the spring zone may be defined as the zone effected by mineral springs, it is more appropriate to follow the second of the above two ways than to follow the first, and to regard the area marked with t as the spring zone. Then, the differences between the spring zone and the outside area are revealed more remarkably than otherwise. It is an interesing fact that the samples Nos. 3-6, though collected from the spots very near to the springs, do not belong to the spring zone.
出版物タイトル 岡山大学温泉研究所報告
発行日 1955-03-25
15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/21510
言語 日本語
論文のバージョン publisher
NAID 40017532466
JaLCDOI 10.18926/19593
タイトル(別表記) CHEMICAL STUDIES ON MISASA HOT SPRING (18) A PYRITE-POLYSULFIDE THEORY OF SULFUR SPRING
フルテキストURL 007_015_019.pdf
著者 芦沢 峻|
抄録 In Misasa there occur only few weak sulfur springs, their maximum hydrogen sulfide content being about 5mg per liter. The ground of Misasa consists of granite and there is no active volcano in the vicinity. So the author tried to explain the mechanism of the occurrence of sulfur spring in Misasa by a reaction of the primarily alkaline thermal water upon pyrite. Namely: XFeS(2) + 3Na(2)C(O)3 = 2Na(2)S(1-5) + Na(2)S(2)O(3) + 3CO(2) + XFeS(1-2) Thiosulfate in sulfur spring waters should not be taken for a secondary product from hydrogen sulfide as accepted generally, but is most probably a primary product to the latter. The phenomenon of white turbidity in sulfur spring is caused mainly by the sulfur liberated from the polysulfide decomposed by the change in pH and temperture of thermal waters and not by the sulfur liberated from the oxidation of hydrogen sulfide. Some experimental data were shown to support the theory.
出版物タイトル 岡山大学温泉研究所報告
発行日 1952-08
7巻
開始ページ 15
終了ページ 19
ISSN 0369-7142
言語 日本語
論文のバージョン publisher
NAID 120002309010
JaLCDOI 10.18926/19590
タイトル(別表記) FLUORINE CONTENT OF THERMAL WATERS IN TOTTORI PREFECTURE AND ITS RELATION TO MOTTLED TOOTH AND GOITER (2nd REPORT)
フルテキストURL 007_012_014.pdf
著者 音田 作衛|
抄録 The fluorine content of 67 samples of mineral waters in Misasa, Asozu, Togo, Hamamura, and Iwai Hot Springs was investigated by Zirconium-Alizarine Sulfonate method. It ranged from 1.5 to 15 mg. per liter, 3-6mg. per liter in the majority. Most of the river and well waters in the same districts contained no measurable amount of fluorifle. In Misasa, Asozu, Togo and Hamamura Hot Springs 68-83 per cent of the schoolchildren who take thermal waters habitually as drinking water suffer from mottled tooth. On the contrary 2-10 per cent of the schoolchildren who do not drink thermal waters habitually showed mottled tooth. In Iwai no inhabitant uses thermal water as drinking water, so that the incidence of mottled tooth among them was only 2.8 per cent. Concerning the incidence of struma in the schoolchildren no relationship was proved between the occurrence of mottled tooth or fluorine content of thermal waters.
出版物タイトル 岡山大学温泉研究所報告
発行日 1952-08
7巻
開始ページ 12
終了ページ 14
ISSN 0369-7142
言語 日本語
論文のバージョン publisher
NAID 120002309086
JaLCDOI 10.18926/19585
フルテキストURL Mem_Fac_Eng_OU_29_1_23.pdf
著者 Kawara, Osami| Fukumoto Kohji|
抄録 In this study we investigated the water quality of surface runoff and groundwater runoff from the basins of the Yodo River and the Asahi River based on that separated by a numerical filter. The water quality of the surface runoff is greatly different from the groundwater runoff. The tendency of concentration change in accordance with river discharges is different from each other. The water qtiality of groundwater runoff changes with river discharges clockwise in many cases. The differences of COD and SS originating from those of population and industrial activities in each basin are found in the lower SS concentrations of the surface runoff and the COD cencentrations of the groundwater runoff. The nutrients and chlorine ion were investigated, too.
出版物タイトル Memoirs of the Faculty of Engineering, Okayama University
発行日 1994-11-30
29巻
1号
開始ページ 23
終了ページ 34
ISSN 0475-0071
言語 英語
論文のバージョン publisher
NAID 120002309068
著者 大橋 亘|
発行日 1956-08-31
出版物タイトル 岡山医学会雑誌
68巻
8号
資料タイプ 学術雑誌論文
著者 大橋 亘|
発行日 1956-08-31
出版物タイトル 岡山医学会雑誌
68巻
8号
資料タイプ 学術雑誌論文
著者 大橋 亘|
発行日 1956-08-31
出版物タイトル 岡山医学会雑誌
68巻
8号
資料タイプ 学術雑誌論文
著者 赤松 收|
発行日 1956-08-31
出版物タイトル 岡山医学会雑誌
68巻
8号
資料タイプ 学術雑誌論文
著者 林 宏|
発行日 1959-04-15
出版物タイトル 岡山医学会雑誌
71巻
5-1号
資料タイプ 学術雑誌論文
著者 林 宏|
発行日 1959-04-15
出版物タイトル 岡山医学会雑誌
71巻
5-1号
資料タイプ 学術雑誌論文
著者 近藤 弘|
発行日 1956-05-31
出版物タイトル 岡山医学会雑誌
68巻
5号
資料タイプ 学術雑誌論文
著者 石井 清|
発行日 1956-05-31
出版物タイトル 岡山医学会雑誌
68巻
5号
資料タイプ 学術雑誌論文
著者 石井 清|
発行日 1956-05-31
出版物タイトル 岡山医学会雑誌
68巻
5号
資料タイプ 学術雑誌論文
著者 田中 稔彦|
発行日 1956-04-30
出版物タイトル 岡山医学会雑誌
68巻
1-4号
資料タイプ 学術雑誌論文
著者 日下 哲雄|
発行日 1959-04-15
出版物タイトル 岡山医学会雑誌
71巻
5-1号
資料タイプ 学術雑誌論文