result 5240 件
| JaLCDOI | 10.18926/bgeou/40067 |
|---|---|
| Title Alternative | The Best Textbook of Japanese-language Teaching in the Late Ch'ing Era; Japanese-language textbook by GUO Zupei & XIONG Jinshou |
| FullText URL | bgeou_144_063_074.pdf |
| Author | Yoshida, Norio| Liu, Jianyun| |
| Abstract | 1899年春,東本願寺が中国の華中方面にいくつかの東文学堂を設立した｡金陵東文学堂はそのなかでもっとも成功した一例である｡本稿は,金陵東文学堂の卒業生により作成された『日語独習書』(1903)を掘り起こし,その著者と成立刊行の経過,作成原則,構成,内容.特徴などを考察し,同時期の植民地台湾の日本語教科書との関連性を検討した｡そして,本書の活末中国の日本語教育における重要な位置と意義を明らかにし,日本語教育史研究における活末東文学堂の口語指導用の教材史料の不十分による研究の空自を埋める｡ |
| Keywords | 日本語教育史 日語独習書 金陵東文学堂 清末中国 |
| Publication Title | 岡山大学大学院教育学研究科研究集録 |
| Published Date | 2010-06-25 |
| Volume | volume144 |
| Start Page | 63 |
| End Page | 74 |
| ISSN | 1883-2423 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002314155 |
| Author | Hamano, Ryosuke| Inagaki, Masaru| Nishie, Manabu| Tokunaga, Naoyuki| Tsunemitsu, Yosuke| Ohtsuka, Shinya| Iwakawa, Kazuhide| Iwagaki, Hiromi| Sonobe, Hiroshi| |
|---|---|
| Published Date | 2010-08-02 |
| Publication Title | 岡山医学会雑誌 |
| Volume | volume122 |
| Issue | issue2 |
| Content Type | Journal Article |
| Author | Yoshioka, Miho| |
|---|---|
| Published Date | 2010-03-25 |
| Publication Title | |
| Content Type | Thesis or Dissertation |
| Author | Enko, Kenki| |
|---|---|
| Published Date | 2010-03-25 |
| Publication Title | |
| Content Type | Thesis or Dissertation |
| JaLCDOI | 10.18926/21349 |
|---|---|
| Title Alternative | SPECTROPHOTOMETRIC DETERMINATION OF ZIRCONIUM |
| FullText URL | pitsr_029_001_006.pdf |
| Author | Okuno, Takaharu| Sakanoue, Masanobu| |
| Abstract | Neo-Thorin was previously presented by the other authers as a color-developing reagent for the spectrophotometric determination of zirconium. 1) To determine the optimum condition for the use of this method, the effects of pH, time and temperature, and the interference of several ions were checked. The following conclusions were derived from the experimental results: Absorption curve-- The zirconium Neo-Thorin complex salt shows a maximum absorption at 580 mμ against Neo-Thorin (Figs. 1 and 2). Effect of pH-- The complex salt gives a maximum absorption at pH 1. 7 (Fig. 3). Effect of time and temperature-- Color absorption is stable for a period of 15 to 200 minutes after color development at room temperature. Heating over 40°C is harmful, because of the formation of a purple precipitation. Interference by several ions-- Cations UO(2)(2+) and Fe(3+) besides Th(4+), considerably interfer with color development. The absorption of 2000 μg U corresponds to that of 10 μg Zr (Fig. 4). However, interference by Fe(3+) becomes negligible if hydroxylamine hydrochloride is added. 2) As a result of the above conclusions, the following procedure is recommended: Procedure recommended-- A few ml of sample solution, 1 ml of 20% hydroxylamine hydrochloride and 1 ml of dilute acid, if necessary, are mixed and diluted to 9 ml. To this solution, 1 ml of 0.05% Neo-Thorin is added. The pH value of the final solution is 1.7. From 15 to 200 minutes after mixing, color absorption is measured at 575 mμ. In the range of 0 to 150 μg Zr per 10 ml, the color absorption of the complex salt obeys Beer's law (Fig. 5). 3) In demonstration, this method was applied to the determination of zirconium in a uranium mineral. Table 1 shows the zirconium content of beta-uranophane from Katamo Mine, Tottori-ken. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1961-06-25 |
| Volume | volume29 |
| Start Page | 1 |
| End Page | 6 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002310976 |
| JaLCDOI | 10.18926/21334 |
|---|---|
| Title Alternative | The Geochemistry of Rocks from Asama Volcano, Japan. New Approaches in the Quantitative Interpretation of the Chemical Composition of Volcanic Rocks |
| FullText URL | pitsr_032_001_085.pdf |
| Author | Matsui, Yoshito| |
| Abstract | In dealing with the geochemistry of volcanic rocks, it appears imperative, first, to refine the procedure of rock analysis with respect to both major and minor components, and second, to improve present methods of interpreting analytical data on common rock suites such as basalts, andesites and dacites. In regard to the first problem, the rapid method of silicate analysis as described by Shapiro and Brannock (1956) and by Riley (1958) deserves special attention. With such a method it is possible to estimate the accuracy and precision of data with far greater ease than is possible with a classical one, yet without any loss of quality. For the determination of some components, however, it is felt that the procedures recommended previously lack precision and/or simplicity. In Part I of this paper, new methods are suggested for these components. The sum of Mg, Ca and Mn is titrated with EDTA in the presence of Al, Fe and other metals, using thymolphthalein complexone as indicator at pH 10-10.5. The sum of Al and Fe is determined by the back-titration of excess EDTA with the standard Cu solution. PAN is used as indicator at pH about 4, and tartrate is added as the masking agent of Ti. Na and K are determined by flame photometry using very dilute solutions (1-5ppm Na or K), without the separation of other metals and without the use of the internal standard. Sr is included in the scheme of analysis, and is determined by flame photometry according to the standard addition technique. These procedures are tested for their accuracy using the standard samples G-1 and W-1 (Tables 3, 5, 9, 12 and 15). Procedures for other components are also described in the text in full detail. The system of analytical procedures recommended is shown in Table 16. To investigate the problem of the interpretation of compositional variation, typical rocks from Asama volcano and the surrounding area were selected, namely, andesites and dacites of calc-alkaline type. Twenty-one samples, described in Tables 18 and 19, are analyzed according to the above procedures. Results are shown in Table 20. Variation diagrams are presented in Figs. 3 to 5. Since it may be questioned whether the "trend" seen in the diagrams implies a genetic relationship, a least squares approximation technique has been introduced in order to determine whether the composition of the main components of a rock (F) can be expressed by the linear combination of a selected set of compositions of a magma and the phenocrysts crystallized from it : F(o)=F(1)x(1)+F(2)x(2)+······+F(m)x(m) ······(1) where F(1), F(2), ... denote the compositions of a magma and minerals, and F(o) is the calculated composition of F. These calculations lead to the conclusion that there are at least two series of rocks in Asama (Tables 25 to 30 and Fig. 9), distinguished from each other mainly by their K(2)O content. Those rocks showing features of assimilation (Aramaki, 1963) all belong to the K(2)O-rich series. Contents of minor components such as TiO(2), MnO, P(2)O(5) and SrO are analyzed by the linear regression technique in two ways, for example : TiO(2)(o)=C(1)x(1)+C(2)x(2)+ ······(2) and TiO(2)(o)=aMgO+bFe(o) +cK(2)O ······(3) These methods are found useful in discriminating rocks of different ongm and in distinguishing the characteristic behavior of each component. Results of calculations (Tables 31 to 34) support the conclusion reached by calculations based on the contents of major components. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1963-10-25 |
| Volume | volume32 |
| Start Page | 1 |
| End Page | 85 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002310984 |
| JaLCDOI | 10.18926/21331 |
|---|---|
| Title Alternative | Statistical Obserbation on the Hydrotherapy in Japan |
| FullText URL | pitsr_033_039_050.pdf |
| Author | Kitayama, Minoru| Ezawa, Hidemitsu| |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1964-03-25 |
| Volume | volume33 |
| Start Page | 39 |
| End Page | 50 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002311028 |
| JaLCDOI | 10.18926/21329 |
|---|---|
| Title Alternative | Causes and Prevention of Intestinal Adhesions Part 3. Experimental Study of Prevention of Intestinal Adhesions |
| FullText URL | pitsr_033_001_028.pdf |
| Author | Ohtani, Mitsuru| |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1964-03-25 |
| Volume | volume33 |
| Start Page | 1 |
| End Page | 28 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002310982 |
| Author | Institute for Thermal Spring Research, Okayama University| |
|---|---|
| Published Date | 1964-03-25 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume33 |
| Content Type | Others |
| JaLCDOI | 10.18926/21321 |
|---|---|
| Title Alternative | Fluorescent X-ray Spectrometric Determination of Uranium,Zirconium, Yttrium and Strontium in Solution |
| FullText URL | pitsr_034_011_020.pdf |
| Author | Okuno, Takahara| |
| Abstract | ウラン鉱床の成因およびウラン鉱物の生成状況を解明するためには,ウラン含有量と同時に,ジルコニウム,イットリウム,ストロンチウムなどの含有量の多少を知ることが,人形峠周辺の鉱床の研究過程において重要となった.これら諸元素の定量をかなりの精度で微量の場合にまで迅速に行なうため,溶液法による蛍光X線分析法を検討した.試料は細粉としたのち,王水などの強酸で分解し,残りはロ過除去してのち,濃縮して一定容となし,その一部をあらたに試作した液体試料保持台(内容積1.8ml,液層の厚さ2.5mm)に入れて測定を行なう.タングステン管球を用い,45KV,22mAの条件で,理学電機製の装置(結晶はLiF)を用い,固定計数法によって各螢光X線(ULα,ZrKα,SrKα,YKα)の強度を計測する.各元素の標準溶液について,最適の角度,バックダウランド値,強度と濃度の関係を検討し,比較的低濃度(20μg/ml前後)まで,検量線の直線性によって,精度よく定量し得ること を知った.さらにこれら諸元素の混合溶液についても検討し,ZrKα に対するウランおよびストロンチウムの影響,さらに共存元素として含有量の多い鉄の影響をしらべ,蛍光X線法により定量した鉄の存在量による諸元素の測定値に対する補正を検討した.以上の諸検討にもとずいて,本法の迅速性を活用し,実際の各種試料について諸元素の定量を行ない,興味ある結果を得られることを知った. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1964-10-25 |
| Volume | volume34 |
| Start Page | 11 |
| End Page | 20 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002311018 |
| JaLCDOI | 10.18926/21216 |
|---|---|
| Title Alternative | Genetic relationship between the Hiroshima and Ryoke granites as indicated by some geochemical evidence |
| FullText URL | pitsr_045_033_046.pdf |
| Author | Honma, Hiroji| |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1976-03-25 |
| Volume | volume45 |
| Start Page | 33 |
| End Page | 46 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002310988 |
| JaLCDOI | 10.18926/21205 |
|---|---|
| Title Alternative | Hydrogen and oxygen isotopic ratios of thermal and mineral springs in Arima area |
| FullText URL | pitsr_043_015_028.pdf |
| Author | Matsubaya, Osamu| Sakai, Hitoshi| Tsurumaki, Michiji| |
| Abstract | Saline waters of thermal and mineral springs in Arima area, at Takarazuka, and in Ishibotoke area of Kawachinagano City indicate wide ranges of δD and δ(18)O values (Table 1). Excellent linearity exists between the δD and δ(18)O values (Fig. 1) and between the δ(18)O value and the chloride concentration (Fig. 2). These facts as well as the chemical evidence of the previous investigators strongly support the view that Arima springs are admixtures of a single deep brine and local ground water (TSURUMAKI, 1964). The deep brine may have the δ(18)O value of +8.0～+8.5‰, the δD value of -25～-30‰, and the chloride concentration of 1.20～1.25 eq/l, which were estimated from the water of the maximum salinity so far reported. Because the thermal and mineral springs in Arima area closely associate with the upper Cretaceous granitic rocks, and the estimated δ(18)O value of the deep brine is similar to a value of water in isotopic equilibrium with those granitic rocks at 500～600℃, the deep brine of Arima might have been the magmatic water of those granitic rocks. The mineral springs at Takarazuka and in Ishibotoke area also show the similar linearity among Cl(-), δ(18)O and δD to those in Arima area. Therefore it is assumed that the mineral springs at Takarazuka may be of the same origin as that in Arima area, and the mineral springs in Ishibotoke area might have been the fluid associated with Ryoke metamorphic rocks. Alternatively, the deep brine in Arima area may be isotopically and chemically similar to the saline formation waters in Illinois basin (GRAF et al., 1966). The high δD values and salinities of those formation waters were attributed to the isotopic and chemical fractionation during the passage of water through sediments. The deep brine in Arima area may be genetically similar to those saline formation waters. If such a saline water could have formed in Osaka basin, it is not surprising to find out the similar brines at Arima and Ishibotoke which are the northwestern and southeastern rims of the basin, respectively. At the present, it cannot be answered which of these two models is more probable. Further studies on other saline springs fluid inclusions of Cretaceous granitic rocks may be useful in order to solve this problem. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1974-03-25 |
| Volume | volume43 |
| Start Page | 15 |
| End Page | 28 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002310971 |
| JaLCDOI | 10.18926/21138 |
|---|---|
| Title Alternative | The Effect of Thermal Spring Water on Drug Absorption in Special Reference to Aspirin and Indomethacin |
| FullText URL | pitsr_052_045_050.pdf |
| Author | Okamoto, Teruko| Hirano, Mitsuhiro| Furuno, Katsushi| |
| Abstract | It is thought that a drug reacts differently with media taken internally. The solubility of Aspirin is assured 600μg/ml in 30min. with Misasa spring water, whereas 400μg/ml with plain water. The parallel difference of 200μg/ml follows 10 min. thereafter. Maximum serum concentratin of 200μg/ml is obtained 2 hours after the internal use of Aspirin with Misasa spring water in parallel difference of 20μg/ml with plain water. In the case of Indomethacin intake, maximum serum concentration of 1.5μg/ml is obtained in 2 hours with plain water, whereas maximum serum concentration of 1μg/ml is obtained in the same period with Misasa spring water. However, the difference of 0.25μg/ml in serum concentration between the media internally taken is seen initially and after 4 hours under high concentration of Indomethacin. We, therefore, assume tentatively that the effect of Aspirin and Indomethacin is supposed to be enhanced with Misasa spring water taken internally. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1982-03-25 |
| Volume | volume52 |
| Start Page | 45 |
| End Page | 50 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002311035 |
| JaLCDOI | 10.18926/21132 |
|---|---|
| Title Alternative | Effect of Hot-Air Room Treatment on Peripheral Leucocytes in Guinea Pigs 1. Effect of Single 30 Min. Hot-Air Room Treatment on Leucocytes Count |
| FullText URL | pitsr_052_001_011.pdf |
| Author | Oda, Yasuhiro| Nishimura, Keiko| Komagoe, Haruki| Tanizaki, Yoshiro| |
| Abstract | Effect of hot-air room treatment on peripheral leucocytes was examined in guinea pigs by observing the numerical changes after the treatment. The results were as follows. 1. Number of totalleucocytes was decreased immediately after hot-air room treatment with a room temperature of 43℃, humidity of 75-87% and rapidly increased from 30 to 120 min after the treatment. Numerical changes of neutrophils showed a same tendency as that of total leucocytes. 2. Lymphocyte count was not changed or slightly decreased after the hot-air room treatment. 3. Number of basophils was decreased 30 min after the treatment and then increased, differing from that of eosinophils which showed a decreased tendency 120 min after the treatment. 4. Numbers of monocytes and Kurloff cells were slightly increased after the treatment. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1982-03-25 |
| Volume | volume52 |
| Start Page | 1 |
| End Page | 11 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002311011 |
| JaLCDOI | 10.18926/21125 |
|---|---|
| Title Alternative | On the Munyeijin potassium salt deposits in Yunnan Province, People's Republic of China |
| FullText URL | pitsr_053_067_076.pdf |
| Author | Jia, Shuyuan| |
| Abstract | In Langping-Simao basins of Southwestern Yunnan Province, a number of salt deposits and salt springs are distributed (Fig. 1). The salt-bearing formations are sandstones, silt and mudstones of the Cretaceous to Paleogene ages, although the ages of the potassium-salts deposits seem to be younger. The Munyeijin potassium deposit was found on the eastern side of the Simao basin in early nineteen sixties. Although the salt deposit has been strongly deformed by tectonic movements (Fig. 2), the deposit has salt-dome structure and three depositional stages have been identified in each cycle of depositional sequence. They are, from the bottom to the top, red salts, black and white salts and carnallite-bearing clayey rocks (see Fig. 3). The red colour of the bottom zone is due to globular debris of silt in the red salts, whereas the top clayey rocks are high in organic materials, being characteristic of the residue of the last stage evaporation of a salt lake. Potassium salt is found in all the three zones, filling up the grain gaps of sodium chloride crystals or running through salt beds in veins and veinlets, although the black-white salts are the most fertile in potassium and have been mined for commercial use. Small amounts of carbonates and sulfates (gypsum and anhydrite) also exist as fine, dispersed grains. Thin layers of gypsum are not uncommon in dark portions of the red and black-white salts. Tachhydrite (CaCl(2)・2MgCl(2)・6H(2)O) is also observed in the top clayey deposits. From the field observation, geological, mineralogical, and geochemical considerations, the paleohydrogeological environments which led to the formation of potassium-rich salt deposits at Munyeijin are reconstructed as follows: 1) The depositional stage of the carnallite-bearing sediments: This is the last stage of evaporation of a salt lake. The sediments would have had up to 80 vol. % interstitial waters saturated with carnallite and sylvite. 2) Diagenetic stage: The carnallite-clay deposits were covered by younger salt deposits and the pore water was gradually squeezed out by compression. The pore water penetrated into the underlying sodium chloride deposits, where the pore water precipitated sylvite as the sodium salts were essentially devoid of potassium. Because the pore water contained organic materials (Table 2), the sylvite precipitates were dark in colour. 3) Tectonic stage: The Langping and Simao basins are lined along the Sanjian tectonic belts. The tectonic activity which presumably started in Eocene must be responsible for the intense deformation of the salt beds. Enrichment of potassium along the axis of folding and the anhydrite formation with the axis of crystallization tilted to the plane of salt beds are some of the important paleohydrogeological results of such movements. Several lines of evidence strongly suggest that hydrothermal activity took place widely in Munyejin basin during this stage. The origin of the potassium-bearing brines has been debated in China since the discovery of the deposits. Many lines of evidence suggest it be of marine origin. However, the presence of tachhydrite in the carnallite-bearing clayey deposits requires some additional source(s) of calcium in addition to seawater. The highly saline groundwaters in Triassic through Jurassic formations of Sichuan Province often are rich in Ca(2+) as well as Mg(2+) and K(+) as some examples are shown in Table 3. If such saline ground waters flew into a salt lake and was subjected to evaporation, calcium-bearing salts such as tachhydrite may form at the last stage deposit of the lake. The origin of such groundwaters is an interesting problem to be studied in future. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1983-03-25 |
| Volume | volume53 |
| Start Page | 67 |
| End Page | 76 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002310978 |
| JaLCDOI | 10.18926/21121 |
|---|---|
| Title Alternative | Clinical problems of long-term steroid regimen for bronchial asthma, with reference to steroid-dependent cases |
| FullText URL | pitsr_053_045_049.pdf |
| Author | Komagoe, Haruki| Sudo, Michiyasu| Okada, Chiharu| Tanizaki, Yoshiro| Morinaga, Hiroshi| Kitani, Hikaru| Goda, Yoshinori| Tada, Shinya| Takahashi, Kiyoshi| Kimura, Ikuro| |
| Abstract | Adverse side effects of steroid therapy were investigated in 32 asthmatic patients. Thirty-two patients were classified into three groups according to steroid therapy for the past five years; group 1 has been treated with continuous steroid therapy, group 2 with occasional steroid therapy and group 3 without steroid therapy. The results were as follows. 1. Group 1 showed a low level of serum cortisol at 8-9 a. m. The serum concentration of cortisol in patients with daily steroid regimen was lower as compared to that in patients with alternateday steroid therapy. 2. The daily profile of serum cortisol was low in the steroid dependent asthmatic patients, and little increase of serum cortisol level after the administration of prednisolone was shown in group 1. 3. Serum IgG and IgM levels were significantly low in steroid dependent asthmatic patients. 4. The level of serum potassium was low in group 1. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1983-03-25 |
| Volume | volume53 |
| Start Page | 45 |
| End Page | 49 |
| ISSN | 0369-7142 |
| language | Japanese |
| File Version | publisher |
| NAID | 120002311040 |
| JaLCDOI | 10.18926/21119 |
|---|---|
| Title Alternative | 好塩基球からのヒスタミン遊離に関する研究. 2. ハウスダスト抗原および抗ヒトIgEによるヒスタミン遊離 |
| FullText URL | pitsr_053_029_033.pdf |
| Author | Tanizaki, Yoshiro| Komagoe, Haruki| Sudo, Michiyasu| Mifune, Masaaki| Morinaga, Hiroshi| Kitani, Hikaru| Goda, Yoshinori| Tada, Shinya| Kimura, Ikuro| |
| Abstract | IgE-mediated release of histamine from whole blood was examined in two healthy and four asthmatic subjects by dose-dependent fashion. The significantly increased amount of histamine was released from basophils of both healthy and asthmatic subjects by a limited concentration of anti-IgE. Antigen (house dust) caused histamine release only from basophils of asthmatics who are sensitive to house dust. Basophils from one patients with asthma released no significant amount of histamine by anti-IgE. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1983-03-25 |
| Volume | volume53 |
| Start Page | 29 |
| End Page | 33 |
| ISSN | 0369-7142 |
| language | English |
| File Version | publisher |
| NAID | 120002310980 |
| JaLCDOI | 10.18926/21118 |
|---|---|
| Title Alternative | 好塩基球からのヒスタミン遊離に関する研究. 1 自動分析装置による全血からのヒスタミン遊離の測定 |
| FullText URL | pitsr_053_023_028.pdf |
| Author | Tanizaki, Yoshiro| Komagoe, Haruki| Sudo, Michiyasu| Mifune, Masaaki| Morinaga, Hiroshi| Ohtani, Jun| Kitani, Hikaru| Goda, Yoshinori| Tada, Shinya| Kimura, Ikuro| |
| Abstract | Histamine released from whole blood was determined by an automated fiuorometric histamine analysis system. The increased release of histamine from basophils by anti-IgE was observed in ten healthy subjects and 12 extrinsic asthma patients, while the release in 11 intrinsic asthma patients was significantly less as compared to that in healthy and extrinsic asthma subjects. House dust extract caused a significant increase in the histamine release from basophils of the extrinsic asthma patients who are sensitive to house dust. It was concluded from this study that histamine released from basophils could be easily determined by an automated analysis system and that the method is useful for the diagnosis and study of allergy. |
| Publication Title | 岡山大学温泉研究所報告 |
| Published Date | 1983-03-25 |
| Volume | volume53 |
| Start Page | 23 |
| End Page | 28 |
| ISSN | 0369-7142 |
| language | English |
| File Version | publisher |
| NAID | 120002310945 |
| Author | Institute for Thermal Spring Research, Okayama University| |
|---|---|
| Published Date | 1983-03-25 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume53 |
| Content Type | Others |
| Author | Institute for Thermal Spring Research, Okayama University| |
|---|---|
| Published Date | 1983-03-25 |
| Publication Title | 岡山大学温泉研究所報告 |
| Volume | volume53 |
| Content Type | Others |
