start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page= end-page= dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title= kn-title=表紙・目次 en-subtitle= kn-subtitle= en-abstract= kn-abstract= en-copyright= kn-copyright= en-aut-name= en-aut-sei= en-aut-mei= kn-aut-name=岡山大学溫泉研究所 kn-aut-sei=岡山大学溫泉研究所 kn-aut-mei= aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil= END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=1 end-page=5 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=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 kn-title=温泉地の井戸水中並びに土壤に附着しているCl(-), SO(4)(2-)について（第1報）　鳥取県三朝溫泉 en-subtitle= kn-subtitle= en-abstract= kn-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. en-copyright= kn-copyright= en-aut-name=UmemotoShunji en-aut-sei=Umemoto en-aut-mei=Shunji kn-aut-name=梅本春次 kn-aut-sei=梅本 kn-aut-mei=春次 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化学部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=6 end-page=9 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=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 kn-title=温泉地の井戸水中並びに土壤に附着しているCl(-), SO(4)(2-)について（第2報）　鳥取県関金溫泉 en-subtitle= kn-subtitle= en-abstract= kn-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. en-copyright= kn-copyright= en-aut-name=UmemotoShunji en-aut-sei=Umemoto en-aut-mei=Shunji kn-aut-name=梅本春次 kn-aut-sei=梅本 kn-aut-mei=春次 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化学部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=10 end-page=15 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=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 kn-title=温泉地の井戸水中並びに土壤に附着しているCl(-), SO(4)(2-)について（第3報）　島根県志学溫泉，湯抱溫泉 en-subtitle= kn-subtitle= en-abstract= kn-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. en-copyright= kn-copyright= en-aut-name=UmemotoShunji en-aut-sei=Umemoto en-aut-mei=Shunji kn-aut-name=梅本春次 kn-aut-sei=梅本 kn-aut-mei=春次 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化学部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=16 end-page=19 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=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 kn-title=温泉地の井戸水中並びに土壤に附着しているCl(-), SO(4)(2-)について（第4報）　島根県玉造溫泉 en-subtitle= kn-subtitle= en-abstract= kn-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. en-copyright= kn-copyright= en-aut-name=UmemotoShunji en-aut-sei=Umemoto en-aut-mei=Shunji kn-aut-name=梅本春次 kn-aut-sei=梅本 kn-aut-mei=春次 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化学部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=20 end-page=23 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=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 kn-title=温泉地の井戸水中並びに土壤に附着しているCl(-), SO(4)(2-)について（第5報）　鳥取県浜村溫泉，勝見溫泉 en-subtitle= kn-subtitle= en-abstract= kn-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. en-copyright= kn-copyright= en-aut-name=UmemotoShunji en-aut-sei=Umemoto en-aut-mei=Shunji kn-aut-name=梅本春次 kn-aut-sei=梅本 kn-aut-mei=春次 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化学部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=24 end-page=27 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=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 (VI) DISTRICT NEAR THE SPRING IN KITADANI VILLAGE, TOTTORI PREFECTURE, JAPAN kn-title=温泉地の井戸水中並びに土壤に附着しているCl(-), SO(4)(2-)について（第6報）　鳥取県北谷村の湧水附近 en-subtitle= kn-subtitle= en-abstract= kn-abstract=In Fukudome, Kitadani Village, the chloride, sulfate and phosfate content and water temperatures of well waters and the amounts of chloride and sulhte fixed to the soil were determined with the samples collected from various parts near the spring which contains much inorganic salts. The chloride, sulfate and phosfate content of the well water samples collected from the district which surrounds the spring, were higher than those from its neighhonrhood, but for the water temperatures of the well water samples, no difference was recognized. As the existence of other sources which would supply the chloride, sulthte and phosfate to the well water is not expected, the difference in the chloride, sulfate and phosfate content of well waters between the samples collected from the A district and its neighbourhood, seems to be due to the effects of the spring which contains much inorganic salts or its sources. en-copyright= kn-copyright= en-aut-name=UmemotoShunji en-aut-sei=Umemoto en-aut-mei=Shunji kn-aut-name=梅本春次 kn-aut-sei=梅本 kn-aut-mei=春次 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化学部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=28 end-page=31 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=STUDY ON RADON CONTENT OF WATERS AND EARTH TEMPERATURES IN FUKUDOME KITADANI VILLAGE, TOTTORI PREFECTURE, JAPAN kn-title=鳥取県東伯郡北谷村福富附近に於ける放射能並びに地温について en-subtitle= kn-subtitle= en-abstract= kn-abstract=In Fukudome, Kitadani Village, Tottori Prefecture, the radon content of well waters and waters in rice-field and earth temperatures were determined. The radon content of waters in "A" district was higher than that in its neighbourhood, and earth temperatures of "A'" district were higher than those in its neighbourhood. Furthermore, "A" district coincides nearly with "A'" district. These results seem to be dne to the effects of the spring which issues in A (or N) district and supplies a water of high salinity. en-copyright= kn-copyright= en-aut-name=SugiharaTakeshi en-aut-sei=Sugihara en-aut-mei=Takeshi kn-aut-name=杉原健 kn-aut-sei=杉原 kn-aut-mei=健 aut-affil-num=1 ORCID= en-aut-name=MifuneMasaaki en-aut-sei=Mifune en-aut-mei=Masaaki kn-aut-name=御船政明 kn-aut-sei=御船 kn-aut-mei=政明 aut-affil-num=2 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化学部 affil-num=2 en-affil= kn-affil=岡山大学溫泉研究所化学部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=32 end-page=36 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=ON THE DISTRIBUTION OF THE NITRATE CONTENT IN THE MISASA HOT SPRINGS, TOTTORI PREFECTURE kn-title=鳥取県三朝温泉の硝酸塩の分布 en-subtitle= kn-subtitle= en-abstract= kn-abstract=The author determined the nitrate content in Misasa Hot-Springs, sampled from August to October, 1952, In all the well-waters, the amounts of nitrate were higher than 1mg/l, and the highest nitrate content was 9.6mg/l in the well-water in front of Mr. Aoki, s house. In the hot-springs, the author found 10 springs containing more than 1 mg/l of nitrate, and the highest nitrate content was 9.0 mg/l in the Hakuro-Yu, but the lotvest content was about 0 mg/l in the Iwasaki Hot-Springs. In Ishiyu and "Yamadaku-KyodoYu" during the stay of irrigation water in rice-fields from the rain season to September, the amounts of flow incrensed, but the content of radon and chloride decreased. On the other hand, in Hisui-no-yu, the chloride content decreased and the radon content increased with the amount of flow. Moreover, the amounts of nitrate were considerably high in the Ishiyu and Yamndaku-KyodoYu Hot Springs, but fairly low in the Hisui-no-Yu. So the author expects that some relation may be found between the variation of the radon content and the amounts of nitrate. The water samples, which nitrate contents were high, showed a tendency to have a high phosfate content generally. en-copyright= kn-copyright= en-aut-name=SugiharaTakeshi en-aut-sei=Sugihara en-aut-mei=Takeshi kn-aut-name=杉原健 kn-aut-sei=杉原 kn-aut-mei=健 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化学部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=37 end-page=42 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=ON THE DETECTION OF RADIOACTIVE SPRING BY GROUND WATER kn-title=地下水による放射能泉の探査について en-subtitle= kn-subtitle= en-abstract= kn-abstract=The author determined the radon content in the ground waters of Misasa and its vicinity by the I. M. fontactoscope from August to November, 1952. The results and conclusions are as follocvs : A close correlation was observed between the radon contents in the spring-waters and that in the ground-waters near the springs, so it seems possible to prospect the existence of radioactive springs by determination of the radon content in groundwaters in the place where no radioactive spring was found as yet. The highest radon content in 53 samples was 741 Mache (2697×10(-10) Curie/l) of the Mr, shigemasa Matsubara's well-water, and this record ecceeds the highest radon content in thermal waters of Misasa known up to the present time. Though the temperature of its well-water was 24.0°C in the afternrnoon of November 25th, 1952, the hot-springs of Yamadaku-kyodoYu, Gunzeshinsenryo, Koyoen, and so on, issue neare by the well. Therefore, the author points out that if a boring is tried in the place where the well is the centre, a most strongly radioactive hot spring in the world may issue. en-copyright= kn-copyright= en-aut-name=SugiharaTakeshi en-aut-sei=Sugihara en-aut-mei=Takeshi kn-aut-name=杉原健 kn-aut-sei=杉原 kn-aut-mei=健 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化學部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=43 end-page=48 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=CHEMICAL STUDTES ON THE RIVER WATERS IN THE INFECTED LOCALITIES WITH KATAYAMA-DISEASE (II) kn-title=片山病発生地域の地表水の化学的研究-2- en-subtitle= kn-subtitle= en-abstract= kn-abstract=In the previous report, one of the authors, T. Sugihara, discussed the results of chemical analysis of waters in the infected localites with Katayama-disease in the whole neighbourllood of Kannabe-cho, Fukayasu-distriict, Hiroshima-Prefecture. In this report, the authors discussed the results obtained in Yamanashi prefecture, and in the area drained by Chikugo River, and found the following facts: 1) The amount of KMnO(4) consumed and the copper content were high as in the previous report. 2) The calcium content was 7.3~22.2 mg/ℓ in the river waters of this report, but it was 18.7~38.2 mg/ℓ in the waters in the places of the previous paper. And in the previous report the author pointed out that the calcium content was fairly higher in the waters in the infected localities with Katayama disease than in the non-infected localities. But as the calcium content was relatively lower this time than in the previous investigation, more research is intended to reach definite conclusion. en-copyright= kn-copyright= en-aut-name=SugiharaTakeshi en-aut-sei=Sugihara en-aut-mei=Takeshi kn-aut-name=杉原健 kn-aut-sei=杉原 kn-aut-mei=健 aut-affil-num=1 ORCID= en-aut-name=AkashiTsutomu en-aut-sei=Akashi en-aut-mei=Tsutomu kn-aut-name=明石務 kn-aut-sei=明石 kn-aut-mei=務 aut-affil-num=2 ORCID= en-aut-name=YokoiShin en-aut-sei=Yokoi en-aut-mei=Shin kn-aut-name=横井信 kn-aut-sei=横井 kn-aut-mei=信 aut-affil-num=3 ORCID= affil-num=1 en-affil= kn-affil=岡山大学溫泉研究所化學部 affil-num=2 en-affil= kn-affil=岡山大学溫泉研究所化學部 affil-num=3 en-affil= kn-affil=岡山大学溫泉研究所化學部 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=49 end-page=53 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=A STUDY ON THE INCIDENCE OF STRUMA IN THE CENTRAL DISTRICT OF TOTTORI PREFECTURE JAPAN 3RD REPORT kn-title=鳥取県中部地方に於ける甲状腺腫について-3- en-subtitle= kn-subtitle= en-abstract= kn-abstract=After 2-3 years from the previous reports, the author reinvestigated the thyroid glands of the grown-up people and of the school children, living in the central district of Tottori Prefecture, where several radio-active hot springs (Misasa, Sekigane and Hamamura) issue. The palpability of the thyroid gland of the grown-up people was 48.6 per cent in average ; this was significantly higher than that of the 1st report. The size of the thyroid gland of the school children has also significantly increased than that of the 2nd report. The influence of the radio-active hot springs upon the thyroid gland was not recognized again. en-copyright= kn-copyright= en-aut-name=OndaSakue en-aut-sei=Onda en-aut-mei=Sakue kn-aut-name=音田作衛 kn-aut-sei=音田 kn-aut-mei=作衛 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学温泉研究所内科 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=54 end-page=63 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title=A CLINICAL, STUDY ON HEARTBURN kn-title=胸やけに就て en-subtitle= kn-subtitle= en-abstract= kn-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. en-copyright= kn-copyright= en-aut-name=SotozonoMasazumi en-aut-sei=Sotozono en-aut-mei=Masazumi kn-aut-name=外園正純 kn-aut-sei=外園 kn-aut-mei=正純 aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil=岡山大学温泉研究所内科 END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page=64 end-page=65 dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title= kn-title=THE SEVENTEENTH ANNUAL CONFERENCE OF THE JAPANESE BALNEO-CLIMATOLOGICAL SOCIETY en-subtitle= kn-subtitle= en-abstract= kn-abstract= en-copyright= kn-copyright= en-aut-name= en-aut-sei= en-aut-mei= kn-aut-name=岡山大学溫泉研究所 kn-aut-sei=岡山大学溫泉研究所 kn-aut-mei= aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil= END start-ver=1.4 cd-journal=joma no-vol=9 cd-vols= no-issue= article-no= start-page= end-page= dt-received= dt-revised= dt-accepted= dt-pub-year=1953 dt-pub=195301 dt-online= en-article= kn-article= en-subject= kn-subject= en-title= kn-title=岡山大学温研報第9号正誤表 en-subtitle= kn-subtitle= en-abstract= kn-abstract= en-copyright= kn-copyright= en-aut-name= en-aut-sei= en-aut-mei= kn-aut-name=岡山大学溫泉研究所 kn-aut-sei=岡山大学溫泉研究所 kn-aut-mei= aut-affil-num=1 ORCID= affil-num=1 en-affil= kn-affil= END