start-ver=1.4
cd-journal=joma
no-vol=15
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=裏表紙・英文目次
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?泉研究所
kn-aut-sei=岡山大学?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=15
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=奥付
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?泉研究所
kn-aut-sei=岡山大学?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=15
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
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?泉研究所
kn-aut-sei=岡山大学?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=15
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=岡山大学温泉研究所報告第15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=岡山大学温泉研究所
kn-aut-sei=岡山大学温泉研究所
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=15
cd-vols=
no-issue=
article-no=
start-page=48
end-page=52
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=STUDIES ON BALNEOTHERAPY OF DIABETES MELLITUS (�U). EFFECT　OF INTERNAL USE OF GERO HOT SPRING ON THE ALIMENTARY HYPERGLYCEMIA IN ALLOXAN-DIABETIC RABBITS
kn-title=糖尿病の温泉治療に関する研究 �U.アロキサン糖尿家兎の食餌性過血糖と下呂?泉（単純硫化水素泉）の飲用
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=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. �T. 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.
en-copyright=
kn-copyright=

en-aut-name=MorinagaHiroshi
en-aut-sei=Morinaga
en-aut-mei=Hiroshi
kn-aut-name=森永寛
kn-aut-sei=森永
kn-aut-mei=寛
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=15
cd-vols=
no-issue=
article-no=
start-page=34
end-page=47
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=STUDIES ON BALNEOTHERAPY OF DIABETES MELLITUS (�T). EFFECT OF THE RADIOACTIVE THERMAL BATH UPON THE CARBOHYDRATE METABOLISM AND THE LEUCOCYTE PICTURE IN ALLOXAN-DIABETIC RABBITS.
kn-title=糖尿病の温泉治療に関する研究 �T.放射能泉入浴とアロキサン糖尿家兎の糖質代謝並に白血球像の変動
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=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).
en-copyright=
kn-copyright=

en-aut-name=MorinagaHiroshi
en-aut-sei=Morinaga
en-aut-mei=Hiroshi
kn-aut-name=森永寛
kn-aut-sei=森永
kn-aut-mei=寛
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=15
cd-vols=
no-issue=
article-no=
start-page=29
end-page=33
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=RHEUMATOID ARTHRITIS AND THORN'S TEST
kn-title=リウマチとTHORN氏テスト
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=In a course of balneotherapy of rheumatoid arthritis, there was no proper standard to judge the therapeutic effect. In this circumstance, Thorn's test and a measurement of red cell sedimentation rate were applied to ten patients with rheumatoid arthritis before and after balneotherpy, and it was found that, although patients before therapy showed a low value of Thorn's test and a faster rate of red cell sedimentation, after released from　various symptoms by balneotherapy they had a higher value of Thorn's test and a slower rate of red cell sedimentation. Therefore, these two tests above described may be used as a standard for a judgement of the effect of　balneotherapy to patients with rheumatoid arthritis.
en-copyright=
kn-copyright=

en-aut-name=IzumiTomokuni
en-aut-sei=Izumi
en-aut-mei=Tomokuni
kn-aut-name=泉友圀
kn-aut-sei=泉
kn-aut-mei=友圀
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所外科
END

start-ver=1.4
cd-journal=joma
no-vol=15
cd-vols=
no-issue=
article-no=
start-page=16
end-page=28
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=KLINISCHE UND EXPERIMENTELLE UNTERSUCHUNGEN UBER DIE WIRKUNG VON THERMALBADERN AUF DIE SEXUALFUNKTION VON FRAUEN (7) DER EINFLUSS DES THERMALBADES AUF DIE CHOLINESTERASE AKTIVITAT VON ZWISCHENHIRN, ENDHIRN, LEBER UND SERUM DER RATTE
kn-title=婦人の性機能に及ぼす?泉浴の影響に関する臨床的並びに実験的研究（7） ラツテの腦,肝臓,血�C中Cholinesterase活性値と三朝?泉浴
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=Es ist bekannt, dass die Thermalbader den Einfluss auf die　vegetativen Nervenfunktionen haben. Anderseits sind die　Cholinesterase Aktivitat von Gehirn und die Nervenfunktionen eng miteinander verbunden. Mehrere Arbeiten stellt die Veranderungen der Cholinesterase von　Serum bei Thermalbad fest, aber diese von Gehirn wird kaum　untersucht. Daher um Veranderungen der Zentralnervenfunktionen durch dem Thermalbad zu forschen, wurde die Cholinesterase Aktivitat von Gehirn von Ratten bestimmt, dabei wurde diese von Serum und Leber auch bestimmt. Die mannliche Ratten wurden unmittelbar, oder 30. Minute, oder 60. Minute nach dem Bade (42℃, 10 Minuten)durch Dekapitation getotet, dann wurden Endhirn, Zwischenhirn, Leber und Serum durch Hesterinsche Methode (Abb. 1〜3) untersucht, und wurden mit Kontrolltieren (Tabelle 1.) verglichen. Nach Hesterinsche Methode stellt die Cholinesterase Aktivitat sich als Acetylcholingewicht (mg), das Gewebe 0.1g oder Serum 0.1cc in 30 Minuten zersetzen kann. Art dse Bades- 1. Susswasser - Abb. 4 Tabelle �U. 2. Die schwach radioaktive Therme (MISASA) - Abb. 5 Tabelle �V. 3. Die stark radioaktive Therme (MISASA) - Abb. 6 Tabelle �W. 4. Die letzte Therme (3), aber kein Radon durch monatlangen Aufspeicherung. - Abb 7　Tabelle �X. Resultat - 1) Cholinesterase Aktivitat der　Kontrolltieren - Zwischenhirn 6.25, Endhirn 4.01, Leber 0.29, Serum 0.17 2) In Zwischenhirn, Endhirn wurde die vorubergehende statistisch signifikante Zunahme von Cholinesterase Aktivitat nach dem Bade bemerkt. 3) In Leber, Serum wurde die statistisch signifikante Abnahme von Cholinesterase Aktivitat ausser wenigen Ausnahmen nach dem Bade bemerkt. 4) Diese Erscheinungen waren nicht charakteristisch fur Thermalbad oder Radioaktivitat von　Thermalwasser, aber der Grad und die Zeit dieser Verapderungeh waren verschiedenartig je nach der Art des　Badewassers und des Gewebes, und besonders das Susswasserbad hatte keinen bemerkbaren Einfluss auf Zwischenhir. Cholinesterase von Gehirn gehort zu spezifischer Cholinesterase, die physiologisch grosse Rolle spielt, gegen Leber, Serum, und zwar die Veranderungen in Gehirn nach dem Bade sind viel grosser als in Leber und Serum. Die Zuhahme von Cholinesterase in Gehirn bedeutet den gesteigerten Acetylcholin Stoffwechsel, d.h. erhohte Gehirntatigkeit. Also sind oben genannte Erscheinungen reich an Bedeutng bei Badekur.
en-copyright=
kn-copyright=

en-aut-name=TanakaYosinori
en-aut-sei=Tanaka
en-aut-mei=Yosinori
kn-aut-name=田中良憲
kn-aut-sei=田中
kn-aut-mei=良憲
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所産婦人科
END

start-ver=1.4
cd-journal=joma
no-vol=15
cd-vols=
no-issue=
article-no=
start-page=11
end-page=15
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=EFFECT OF WATER LEVEL OF RIVER ON MINERAL SPRING (Continued)
kn-title=河川の水位が?泉に及ぼす影響について（続報）
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=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.
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=岡山大学温泉研究所化学部
END

start-ver=1.4
cd-journal=joma
no-vol=15
cd-vols=
no-issue=
article-no=
start-page=6
end-page=10
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=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)
kn-title=?泉地の井戸水中並びに土壊に附着しているCl(-),SO(4)(2-)について（第10報） 鳥取縣松崎温泉,東郷?泉,浅津?泉及び浜村?泉,勝見?泉（続報）
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=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.
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=岡山大学温泉研究所化学部
END

start-ver=1.4
cd-journal=joma
no-vol=15
cd-vols=
no-issue=
article-no=
start-page=1
end-page=5
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1955
dt-pub=19550325
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 SOIL IN THE MINERAL SPRING DISTRICTS (IX) SAGINOYU HOT SPRINGS, SHIMANE PREFECTURE, JAPAN.
kn-title=?泉地の井戸水中並びに土壌に附着しているCl-,SO(4)(2-)について（第9報） 島根縣鷺の湯?泉
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=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./?.. 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.
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=

en-aut-name=TanakaShigeo
en-aut-sei=Tanaka
en-aut-mei=Shigeo
kn-aut-name=田中重男
kn-aut-sei=田中
kn-aut-mei=重男
aut-affil-num=2
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所化学部

affil-num=2
en-affil=
kn-affil=岡山大学温泉研究所化学部
END