result 47530 件
JaLCDOI | 10.18926/40379 |
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Title Alternative | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (V) HAMAMURA AND KACHIMI HOT-SPRINGS, TOTTORI PREFECTURE, JAPAN |
FullText URL | 009_020_023.pdf |
Author | Umemoto, Shunji| |
Abstract | In Hamamura and Kachimi Hot-Springs, the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from vmions parts of the mineral spring districts. The chloride and sulfate content and warter temperatures of well waters were higher in the samples collected from the thermal spring districts than in the samples collected from its neighbourhood, but for the amounts of chloride and sulfate fixed to the soil, no difference was recognized. As the existence of other sources whlch would supply the chloride, sulfate and heat to the well waters 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 he due to the effects of the thermal springs. |
Publication Title | 岡山大学温泉研究所報告 |
Published Date | 1953-01 |
Volume | volume9 |
Start Page | 20 |
End Page | 23 |
ISSN | 0369-7142 |
Related Url | http://ousar.lib.okayama-u.ac.jp/metadata/40388 |
language | Japanese |
File Version | publisher |
NAID | 40017532512 |
JaLCDOI | 10.18926/40378 |
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Title Alternative | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (IV) TAMATSUKURI HOT-SPRINGS, SHIMANE PREFECTURE, JAPAN |
FullText URL | 009_016_019.pdf |
Author | Umemoto, Shunji| |
Abstract | In Tamatsukuri Hot-Springs, the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from various parts of the mineral spring districts. For the values which were determined with samples collected from the thermal spring districts and its neighbourhood, no difference was recognized. This result is quite different from the results given in the previous reports of the present author. But this fact may be explaned as the effects of the sea warter, and the further study is being continued. |
Publication Title | 岡山大学温泉研究所報告 |
Published Date | 1953-01 |
Volume | volume9 |
Start Page | 16 |
End Page | 19 |
ISSN | 0369-7142 |
language | Japanese |
File Version | publisher |
NAID | 40017532512 |
JaLCDOI | 10.18926/40377 |
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Title Alternative | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (III) SIIGAKU AND YUGAKAI HOT-SPRINGS, SHIMANE PREFECTURE, JAPAN |
FullText URL | 009_010_015.pdf |
Author | Umemoto, Shunji| |
Abstract | 1) In Shigaku Hot-Springs, the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from various parts of the thermal spring district and its neighbourhood. The amounts of chloride and sulfate fixed to the soil were greater in the samples from the thermal spring district than in those from its neighbourhood. As the existence of other sources which would supply the chloride and foulfate to the soil is not expected, the difference in the amounts of chloride and sulfate, between the samples from the thermal spring district and it; neighbourhood, seems to be due to the effects. of thermal springs. 2) In Yugakai Hot-Springs the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from various parts of the mineral spring district. The water temperatures of well water samples from the district which has the mineral springs with higher temperatures, were higher than those from the district which has the mineral springs with lower temperatures, but for the chloride and sulfate content of the well water samples and the amounts of chloride and sulfate fixed to the soil, no difference was detected. As the existence of other sources which would supply the heat to the water is not expected, the difference in the water temperatures, between the samples from the district which has the mineral springs with higher temperatures and the district which has the mineral springs with lower temperatures, seems to be due to the effects of the mineral springs. On the other hand, for the chloride and sulfate content of well water samples and the amounts of chloride and sulfate fixed to the soil, no difference is recognized. |
Publication Title | 岡山大学温泉研究所報告 |
Published Date | 1953-01 |
Volume | volume9 |
Start Page | 10 |
End Page | 15 |
ISSN | 0369-7142 |
Related Url | http://ousar.lib.okayama-u.ac.jp/metadata/40388 |
language | Japanese |
File Version | publisher |
NAID | 40017532512 |
JaLCDOI | 10.18926/40376 |
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Title Alternative | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (II) SEKIGANE HOT-SPRINGS, TOTTORI PREFECTURE, JAPAN |
FullText URL | 009_006_009.pdf |
Author | Umemoto, Shunji| |
Abstract | In Sekigane Hot-Springs, the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from the various parts of the thermal spring district and its neighbourhood. The chloride and sulfate content of the well water samples collected from the thermal spring district were higher than those from its neighbourhood, and no difference was found for the water temperatures. The amonnts of chloride fixed to the soil in the samples collected from the thermal spring district were greater than those from its neighbourhood, and the amounts of sulfate in the samples collected from the thermal spring district were extremely greater than those from its neighhourhood. As the existence of other sources which would supply the chloride and sulfate to the water and soil is not expected, the difference in the chloride and sulfate content and water temperatures, between the sa.mples from the thermal spring district and its neighbourhood, seems to be due to the effects of thermal springs. |
Publication Title | 岡山大学温泉研究所報告 |
Published Date | 1953-01 |
Volume | volume9 |
Start Page | 6 |
End Page | 9 |
ISSN | 0369-7142 |
language | Japanese |
File Version | publisher |
NAID | 40017532512 |
JaLCDOI | 10.18926/40375 |
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Title Alternative | STUDIES ON THE CHLORIDE AND SULFATE CONTENT OF WELL WATERS AND THE AMOUNTS OF CHLORIDE AND SULFATE FIXED TO THE SOIL IN THE MINERAL SPRING DISTRICTS (I) MISASA HOT-SPRINGS, TOTTORI PREFECTURE, JAPAN |
FullText URL | 009_001_005.pdf |
Author | Umemoto, Shunji| |
Abstract | In Misasa Hot-Springs, the chloride and sulfate content and water temperatures of well waters and the amounts of chloride and sulfate fixed to the soil were determined with the samples collected from various parts of the thermal spring district and its neighbourhood. The chloride and sulfate content and water temperatures of the well water samples collected from the thermal spring district were higher than those from its neibourhood, and the amounts of chloride fixed to the soil were greater in the samples collected from the thermal spring district than in those from its neighbourhood, but for the amounts of sulfate fixed to the soil, no difference was detected. As the existence of other sources which would supply the chloride and sulfate to the water and soil is not expected, the difference in the chloride and sulfate content and water temperatures, between the samples collected from the thermal spring district and its neighbourhood, seemes to be due to the effects of thermal springs. |
Publication Title | 岡山大学温泉研究所報告 |
Published Date | 1953-01 |
Volume | volume9 |
Start Page | 1 |
End Page | 5 |
ISSN | 0369-7142 |
Related Url | http://ousar.lib.okayama-u.ac.jp/metadata/40388 |
language | Japanese |
File Version | publisher |
NAID | 40017532512 |
Author | 岡山大学溫泉研究所| |
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Published Date | 1953-01 |
Publication Title | 岡山大学温泉研究所報告 |
Volume | volume9 |
Content Type | Others |
Author | 岡山大学溫泉研究所| |
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Published Date | 1952-11 |
Publication Title | 岡山大学温泉研究所報告 |
Volume | volume8 |
Content Type | Others |
Author | 岡山大学溫泉研究所| |
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Published Date | 1952-08 |
Publication Title | 岡山大学温泉研究所報告 |
Volume | volume7 |
Content Type | Others |
Author | 岡山大学溫泉研究所| |
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Published Date | 1952-03 |
Publication Title | 岡山大学温泉研究所報告 |
Volume | volume6 |
Content Type | Others |
Author | 岡山大学溫泉研究所| |
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Published Date | 1952-03 |
Publication Title | 岡山大学温泉研究所報告 |
Volume | volume6 |
Content Type | Others |
Author | 岡山大學溫泉研究所| |
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Published Date | 1951-08 |
Publication Title | 岡山大学温泉研究所報告 |
Volume | volume5 |
Content Type | Others |
Author | 岡山大學放射能泉研究所| |
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Published Date | 1951-03 |
Publication Title | 放射能泉研究所報告 |
Volume | volume4 |
Content Type | Others |
Author | 岡山大學放射能泉研究所| |
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Published Date | 1951-03 |
Publication Title | 放射能泉研究所報告 |
Volume | volume4 |
Content Type | Others |
Author | 岡山大學放射能泉研究所| |
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Published Date | 1950-07-25 |
Publication Title | 放射能泉研究所報告 |
Volume | volume3 |
Content Type | Others |
Author | 岡山大學放射能泉研究所| |
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Published Date | 1950-07-25 |
Publication Title | 放射能泉研究所報告 |
Volume | volume3 |
Content Type | Others |
JaLCDOI | 10.18926/40364 |
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Title Alternative | Direct colorimetric and volumetric determination of calcium with new reagent |
FullText URL | rbl_003_039_042.pdf |
Author | Ashizawa, Takashi| |
Abstract | The anthor found that azocal-A reacts only with calcium, and devised a direct colorimetric, and a direct titration method for calcium determination using azocal-A as an indicator, and obtained a satisfactory result. Accuracy : detectable amount in NaOH……0.28 γ, of Ca ; detectable amount in NH(4)OH……2 γ, of Ca. Sensibility……1 : 125,000 & 1 : 17,500 respectively. Interfering substances : Fe, U, Ni, Co, Hg, Ag, citrate, tartarate, oxalate, large amount of NH(4) salts, Sr, Mg. Not interfering subst. : Ba, F, acetate and silicate. Reagents : Saturated soln. of azocal-A in weak NaOH soln.. Spot test procedure : Place a drop of the acid or neutral test soln. upon white spot plate, add 1 drop of azocal-A soln., and mix them. If a yellow color appears, calcium is present. Colorimetric method: Transfer water sample containg not more than 0.05 mg of calcium, and not more than 5 mg of Fe, Mn, Mg, etc. to a 20 cc colorimetric tube, add 0.5-1 cc of azocal-A soln. and 0.5 cc of 6N-NaOH soln.. Allow it to stand for 10 minutes. Then compare the resulted yellow color with standard Ca soln. prepared similarly and simultaneously. Volumetric method : Amount determinable : 0.1 g of calcium. Transfer 40 cc of sample containg 5-100 mg to a 100 cc Erlenmeyer's flask, add 0.5 cc of 6N-HCl, add azocal-A to the amount of pink color as caused by methyl orange in acid soln.. Make alkaline with 1 cc of 6N-NaOH. Add 10 cc alcohol to every 40 cc of the sample solution. Then its color turns to yellow. Titrate with 0.1 N oxalate soln.. 1.0 cc of 0.1 N oxalate soln. is equivalent to 2.0 mg of Ca. Absorption band of the acid soln. at 4900 A, alkaline soln. at 5000 A, Ca-compound at 4300 A. The azocal-A is o-carboxy-benzol-azo-2-naphtol 3, 6-disulfonic acid prepared from anthranilic acid and R-salt. |
Publication Title | 放射能泉研究所報告 |
Published Date | 1950-07-25 |
Volume | volume3 |
Start Page | 39 |
End Page | 42 |
language | Japanese |
File Version | publisher |
NAID | 120002484888 |
JaLCDOI | 10.18926/40363 |
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Title Alternative | Studies on vitriol springs : 5. Polynuclear complex iron salts in vitriol waters |
FullText URL | rbl_003_035_038.pdf |
Author | Ashizawa, Takashi| |
Publication Title | 放射能泉研究所報告 |
Published Date | 1950-07-25 |
Volume | volume3 |
Start Page | 35 |
End Page | 38 |
language | Japanese |
File Version | publisher |
NAID | 120002484887 |
JaLCDOI | 10.18926/40362 |
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Title Alternative | Chemical studies on Misasa Hot Spring (1-8) |
FullText URL | rbl_003_021_034.pdf |
Author | Ashizawa, Takashi| |
Publication Title | 放射能泉研究所報告 |
Published Date | 1950-07-25 |
Volume | volume3 |
Start Page | 21 |
End Page | 34 |
language | Japanese |
File Version | publisher |
NAID | 120002484886 |
JaLCDOI | 10.18926/40361 |
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Title Alternative | Studies of the radio-active springs. XXV The effect of Thoron spring bath on Rotter's reaction |
FullText URL | rbl_003_018_020.pdf |
Author | Oshima, Yoshio| |
Abstract | 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. |
Publication Title | 放射能泉研究所報告 |
Published Date | 1950-07-25 |
Volume | volume3 |
Start Page | 18 |
End Page | 20 |
language | Japanese |
File Version | publisher |
NAID | 120002484885 |
JaLCDOI | 10.18926/40360 |
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Title Alternative | 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 |
FullText URL | rbl_003_015_017.pdf |
Author | Morinaga, Hiroshi| |
Publication Title | 放射能泉研究所報告 |
Published Date | 1950-07-25 |
Volume | volume3 |
Start Page | 15 |
End Page | 17 |
language | Japanese |
File Version | publisher |
NAID | 120002484884 |