start-ver=1.4
cd-journal=joma
no-vol=20
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1958
dt-pub=195801
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=20
cd-vols=
no-issue=
article-no=
start-page=1
end-page=41
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1958
dt-pub=195801
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=DIE KLINISCHEN UND EXPERIMENTELLEN UNTERSUCHUNGEN ?BER DIE PELOIDTHERAPIE BEI GYN?KOLOGISCHEN ENTZ?NDUNGEN
kn-title=婦人科的慢性炎症の鉱泥療法に関する研究
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=Die resortive Behandlung bei schwerheilbaren chronischen Entz?ndungen der Adnexe und des Uterus besteht aus verschiedenen W?rmeapplikationsmethoden. Effekt der Peloidtherapie als eine von diesen Methoden wurde untersucht. Die Untersuchung besteht aus klinischer Beobachtung ?ber die Peloidpackung und tier experimentellem Studium ?ber Peloidbad. A) ?ber die Peloidpackung. 1. Heileffekt der Packung.
35 F?lle, die an chronischer Entz?ndung der Adnexe und des Uterus gelitten hatten, wurden mit warmer Peloidpackung an Lenden oder Unterbauch t?glich einmal f?r 2 oder 3 Wochen behandelt. Bei den 28 F?llen von diesen 35 F?llen wurde die gute Folge, wie zum Beispiel Nachlass der Schmerzen und der Induration, bemerkt, Da einige F?lle von diesen 28 F?llen schwache Reaktion auf die anderen verschiedenen Therapie wie Ultrakurzwellenbestrahlung gezeigt hatten, Packung mit Peloid muss eine erfolgreichste Therapie in besonderen F?llen sein, 2, Physiologische Untersuchungen ?ber den Einfluss der Packung bei obigen Kranken, Gesteigerte Blutsenkungsgeschwindigkeit normalisierte sich, und Leukozytenzahl zeigte keine Zeichen der Verschlechteung w?hrend der Kur, Keine nennenswerte Ver?nderung des Elektrokardiogramms wurde w?hrend und nach Applikation der Peloid gefunden, und bei Kranken mit hohem Blutdruck fiel der Blutdruck vor?bergehend w?hrend Applikation der Peloid, Steigerung der Hauttemperatur und der Uterustemperatur bei Packung waren gr?sser als bei Ultrakurzwellenbestrahlung und Heissluftbad, und diese Erscheinungen wurden auch von tierexperimentellen Untersuchungen festgestellt,
Ausscheidung der Phenolsulfonphthalein, die in die Bauchh?hle des Kaninchens sich eingespritzt hatte, wurde von Packung an Unterbauch beschleunigt, So stellt diese klinischen und tierexperimentellen Untersuchungen fest, dass
Peloidpackung stark resorptiv durch ihre hyper?misierenden Wirkung nach die Tiefe des Krankheitsherdes ist, und zwar es den Kranken zu keiner Last in verschiedenen Seiten fallt, B) ?ber das Peloidbad, Verfasser hatte ein St?ckchen der spongiOsen Gelatine, die ?blich als blutstillendes Material bei Operation gebraucht wird, an Peritoneum der Ratten angen?ht, und liess diese Ratten die Peloidb?der t?glich einmal 20 minutenlang f?r 4 Wochen nehmen Inzwischen wurden die Ratten w?chentlich get?tet, und die spongi?se Gelatine wurde mit umgebener Granulation aus Bauchh?hle herausgenommen, und dann wurde histologisch untersucht. Gleichzeitig wurden Arten der freien Zellen in der Bauchh?hle
und die Neutralrotf?rbung:::intensit?t der Hystiozyten in lockerem Bindegewebe der
Unterhaut als Merkmal f?r Abwehrkraft des Organismus untersucht, Es war festgestellt, dass bei Peloidb?dern der Verlauf der durch spongi?se Gelatine hervorgerufene Entz?ndung sich verk?rzt, und das St?ckchen der Gelatine wird schnell abgesorviert, und zugleich Abwehrkraft sich steigert, Bei diesen Experimente wurden die stark sauere sulfurhaltge Quellenschlamme (Konyajigoku zu Beppu) und die neutrale Schlamme der Seeboden (Toogooike zu Tottoriken) gebraucht, aber kein wesentlicher Wirkungsunterschied zwischen beide
Schlamme wurde gefunden.
en-copyright=
kn-copyright=

en-aut-name=OkadaToshio
en-aut-sei=Okada
en-aut-mei=Toshio
kn-aut-name=岡田俊郎
kn-aut-sei=岡田
kn-aut-mei=俊郎
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学医学部産婦人科教室
END

start-ver=1.4
cd-journal=joma
no-vol=20
cd-vols=
no-issue=
article-no=
start-page=42
end-page=47
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1958
dt-pub=195801
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=DIFFERENTIAL THERMAL ANALYSIS OF HYDROUS FERRIC OXIDE FORMED BY DIRECT NEUTRALIZATION OF FERRIC CHLORIDE SOLUTION
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=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.
en-copyright=
kn-copyright=

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=1
ORCID=

affil-num=1
en-affil=
kn-affil=Division of Chemistry, Balneological Laboratory, Okayama University
END

start-ver=1.4
cd-journal=joma
no-vol=20
cd-vols=
no-issue=
article-no=
start-page=48
end-page=54
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1958
dt-pub=195801
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=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
kn-title=鳥取県三朝温泉の温泉水中の二価鉄及び可還元鉄の密栓放置による濃度変化について
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=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.
en-copyright=
kn-copyright=

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=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=20
cd-vols=
no-issue=
article-no=
start-page=55
end-page=61
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1958
dt-pub=195801
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=On the Underground Temperatures and Radioactivities at One Meter Depth in the Misasa Hot Spring Area
kn-title=三朝温泉地域の地下1m深さにおける温度分布並びに放射能について
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=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).
en-copyright=
kn-copyright=

en-aut-name=SomaTokuzo
en-aut-sei=Soma
en-aut-mei=Tokuzo
kn-aut-name=相馬徳蔵
kn-aut-sei=相馬
kn-aut-mei=徳蔵
aut-affil-num=1
ORCID=

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