検索結果 613 件
JaLCDOI | 10.18926/AMO/30389 |
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フルテキストURL | fulltext.pdf |
著者 | Miura, Mochiyoshi| Kohda, Shigeki| Mino, Yoshio| Aoyama, Hideyasu| |
抄録 | The purpose of this study was to determine the aerobic training intensity from the maximal and submaximal running exercise in 21 untrained adult men. To accomplish this, we evaluated the relationship between physiological (oxygen intake and heart rate) and physical parameters (running speed) of training intensity, and determined the training intensity at the submaximal exercise. Oxygen intake and heart rate were measured by a treadmill test. The maximal oxygen intake (VO2 max), and the aerobic threshold (AerT) and anaerobic threshold (AT) were measured to determine respiratory gas exchange. Running capacity was measured by a 12-min running and treadmill test. For the maximal exercise, there was a significant correlation (r = 0.88, P < 0.01) between VO2 max and 12-min running distance (speed). In addition, the oxygen intake and heart rate at AerT and AT in the submaximal exercise were linearly correlated with running speed. Three levels of training intensity at the submaximal exercise were termed: light, moderate, and heavy. Since AerT was the lower limit intensity and AT was the upper limit, we took the middle of their values as the moderate intensity. The end point for the determination of the training intensity at the submaximal exercise was estimated to be 85% VO2 max and 180 beats.min-1. |
キーワード | aerobic exercise training intensity aerobic threshold anaerobic threshold submaximal exercise |
Amo Type | Article |
出版物タイトル | Acta Medica Okayama |
発行日 | 1995-04 |
巻 | 49巻 |
号 | 2号 |
出版者 | Okayama University Medical School |
開始ページ | 107 |
終了ページ | 112 |
ISSN | 0386-300X |
NCID | AA00508441 |
資料タイプ | 学術雑誌論文 |
言語 | 英語 |
論文のバージョン | publisher |
査読 | 有り |
PubMed ID | 7618488 |
Web of Science KeyUT | A1995QV69800007 |
JaLCDOI | 10.18926/AMO/30330 |
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フルテキストURL | fulltext.pdf |
著者 | Watanabe, Sadahiro| |
抄録 | Cepharanthine, a biscoclaurine alkaloids which interact with biomembranes, has been found to inhibit platelet aggregation. The effects of this drug on morphological and physiochemical phenomena following collagen-induced platelet stimulation were investigated. In the presence of cepharanthine, stimulated platelets became spherical, but did not form pseudopoda , nor did they become aggregated. Physiochemical reactions such as accelerated oxygen consumption, release of membrane-bound Ca2+, release of Ca2+ into the extracellular medium and deporalization of the membrane potential were all inhibited by cepharanthine. Using D,L-dipalmitoyl phosphatidylcholine liposomes as the substrate, cepharanthine was shown to inhibit phospholipase A2 activity. These results suggest that the changes in the membrane following the interaction of collagen with its receptor are important for platelet activation. Cepharanthine may inhibits these membrane state changes, thus blocking all subsequent reactions. |
キーワード | platelet aggregation cepharanthine electron microscopy phospholipase A<sub>2</sub> liposome |
Amo Type | Article |
出版物タイトル | Acta Medica Okayama |
発行日 | 1984-04 |
巻 | 38巻 |
号 | 2号 |
出版者 | Okayama University Medical School |
開始ページ | 101 |
終了ページ | 115 |
ISSN | 0386-300X |
NCID | AA00508441 |
資料タイプ | 学術雑誌論文 |
言語 | 英語 |
論文のバージョン | publisher |
査読 | 有り |
PubMed ID | 6731025 |
Web of Science KeyUT | A1984SN81800002 |
JaLCDOI | 10.18926/AMO/30298 |
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フルテキストURL | fulltext.pdf |
著者 | Hukuhara, Takesi| Okada, Hiromasa| |
抄録 | In decerebrated cats the impulse discharges were detected by means of an unipolar microelectrode from a single inspiratory neuron in the respiratory centers, and the change in discharge produced by administration of stimulating, as well as depressant agents, was studied. The results were summarized as follows. 1) Inhalation of the air containing all. excess of carbon dioxide, as well as the air deficient of oxygen and the intravenous administration of a small dose of caffeine, aminocordine and lobeline produced a) a remarkable increase of frequency of impulses in the stage of constant frequency of the volley, b) a rapid increase of frequency of impulses in the stage of crescent frequency of the volley and c) a shortening of the duration of the volleys, as well as of silent periods. 2) In narcosis by a moderate dose of morphine, as well as in the recovery stage from apnea produced by over-ventilation, there were observed the phenomena which were exactly opposite to those described in 1). 3) It was concluded that a most essential sign by which one can discern whether the activity of the respiratory Genters is raised or depressed, is the changes of the frequency of impulses produced from an inspiratory neuron. The expense of this research was defrayed from the grant in aid of the Ministry of Education. |
Amo Type | Article |
出版物タイトル | Acta Medicinae Okayama |
発行日 | 1956-07 |
巻 | 10巻 |
号 | 3号 |
出版者 | Okayama University Medical School |
開始ページ | 151 |
終了ページ | 163 |
NCID | AA00041342 |
資料タイプ | 学術雑誌論文 |
言語 | 英語 |
論文のバージョン | publisher |
査読 | 有り |
著者 | 堀 彰宏| |
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発行日 | 2010-03-25 |
出版物タイトル | |
資料タイプ | 学位論文 |
JaLCDOI | 10.18926/21324 |
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タイトル(別表記) | Determination of Dissolved Gases in the Ground Water at Mt. Daisen |
フルテキストURL | pitsr_034_053_062.pdf |
著者 | 渡辺 晃二| 奥野 孝晴| |
抄録 | 鳥取県大山火山の西北麓の地下水中に潜存するガス成分比は Ar : 0.34~0.40 (cc/l) 1.48~1.64 (%) O(2) : 6.69~9.08 (cc/l) 27.92~35.30 (%) N(2) : 15.16~17.23 (cc/l) 63.22~67.92 (%) の範囲内で定量できる.また,飽和度は次の如くである. O(2) : 87.8~113.9 (%) N(2) : 110.5~123.2 (%) この結果を地表水と比較して,O(2)の飽和度は小さいが,量的な差異はあまりみられず,地表水と地下水の中間的な性質を示している.地質構造,地形が溶存ガス成分比に及ぼす影響は,地下水の流通経路が長距離とみなされる場合に若干のO(2)の消費が認められ,短距離で湧出したと思われるものにはO(2)の飽和度が大きい傾向がある.また,水理地質的にみて,地質と湧出量には密接な関連を見出せるが,ガス成分には影響を与へてはいない. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1964-10-25 |
巻 | 34巻 |
開始ページ | 53 |
終了ページ | 62 |
ISSN | 0369-7142 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002310987 |
JaLCDOI | 10.18926/21228 |
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タイトル(別表記) | Continuous in-vIvo measurement of the brain tissue and the ischemic muscle gas tension using MEDSPECT, MS-8 |
フルテキストURL | pitsr_043_029_036.pdf |
著者 | 川上 俊爾| 山根 義久| 野一色 泰晴| 古元 嘉昭| 寺本 滋| 妹尾 嘉昌| 金子 克也| 杉本 誠起| 高橋 俊二郎| |
抄録 | I MEDSPECT is a medical mass spectrometer for continuous in-vivo measurement of tissue, blood and respiratory gases. Interfacing catheter for tissue in measurement has Teflon membrane. The permeability and perfusion rate for various gases through its membrane varied with temperature. The temperature coefficient of Teflon catheter in the range of 15℃-40℃ is approximately constant with -2% of correction per degree for oxygen and carbon dioxide. Linear correlation was confirmed experimentally. II The brain tissue gas tensions were measured in ten dogs with intra-venous anesthesia at normothermia and deep hypothermia using perfusion cooling, including circulatory arrest for 30 minutes at 20°C of cerebral temperature. On average, the brain tissue P(O2) was 15mmHg in normothermia when the arterial P(O2) showed 95mmHg and the brain tissue P(CO2) was 49mmHg when the arterial PC02 showed 30mmHg. The brain tissue carbon dioxide tension gradually decreased by cooling and increased during circulatory arrest for 30 minutes; from 45mmHg to 72mmHg. The brain tissue oxygen tension increased during cooling from 15mmHg to 41mmHg and decreased in the circulatory arrest; from 41mmHg to 36mmHg. III The ischemic muscle gas tension was measured in a 22-year-old man, who was suffered from thromboangiitis obliterans bilaterally, and had the popliteal autovein bypass surgery 3 months ago. Control oxygen tensions in the both anterior tibial muscles showed about the same; 35mmHg and 36mmHg respectivelly, and the P(O2) of the non-operated side showed remarkable low level of 18mmHg as compared with the side of arterial reconstruction surgery after 5-minutes ankle exercise. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1974-03-25 |
巻 | 43巻 |
開始ページ | 29 |
終了ページ | 36 |
ISSN | 0369-7142 |
関連URL | http://eprints.lib.okayama-u.ac.jp/21235 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002311036 |
著者 | 本間 弘次| 酒井 均| |
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発行日 | 1976-03-25 |
出版物タイトル | 岡山大学温泉研究所報告 |
巻 | 45巻 |
資料タイプ | データ・データベース |
JaLCDOI | 10.18926/21205 |
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タイトル(別表記) | Hydrogen and oxygen isotopic ratios of thermal and mineral springs in Arima area |
フルテキストURL | pitsr_043_015_028.pdf |
著者 | 松葉谷 治| 酒井 均| 鶴巻 道二| |
抄録 | 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. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1974-03-25 |
巻 | 43巻 |
開始ページ | 15 |
終了ページ | 28 |
ISSN | 0369-7142 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002310971 |
JaLCDOI | 10.18926/21194 |
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タイトル(別表記) | Stable isotope study of the hotsprings and volcanoes of Hokkaido, Japan |
フルテキストURL | pitsr_047_055_067.pdf |
著者 | 松葉谷 治| 酒井 均| 上田 晃| 堤 真| 日下部 実| 佐々木 昭| |
抄録 | Stable isotope ratios of hydrogen, oxygen, carbon and sulfur of precipitation, thermal and mineral waters, and volcanic gases were measured. The isotopic data combined with chemical and geological information were discussed in terms of origin and evolution of the hotsprings and volcanic gases. The hotsprings along the Uchiura Bay, Oshima Peninsula are mostly near-neutral NaCl-type thermal water and may be divided into three groups : (1) thermal waters isotopically similar to the precipitation of this area, (2) those similar in D/H to the local meteoric waters but enriched by 2 to 3‰ in (18)O compared to the latter, and (3) those enriched significantly in both D and (18)O relative to the local meteoric waters. The first and second types of thermal water probably form from local meteoric water which percolates through "Green Tuff" formations and acquires dissolved chemicals from them. However, high salt concentration and the oxygen isotope shift (thesecond type) may imply that the NaCl-type water of volcanic origin might be involved. On the other hand, the waters of the third group can be explained by mixing of modern sea water into the second type thermal water (in case of Yachigashira) or by incorporation of fossil sea water of Tertiary origin into modern meteoric water (Nigorigawa). Except for Esan, Noboribetsu and Atosanupuri volcanic systems, waters from all the hotsprings and volcanic fumaroles associated with Quaternary volcanic rocks are meteoric in origin. Thermal waters at Esan, Noboribetsu and Atosanupuri have δD = -30~-50 and δ(18)O = -1~+ 3‰ and are enriched in D and (18)O relative to local meteoric water of the respective area. The origin of these waters and the mechanism (s) controlling the isotope ratios could not be made clear by the present study. Interesting is the finding that at Esan, Noboribetsu and Atosanupuri, thermal waters are enriched in D and (18)O relative to near-by fumarolic gases. The enrichment factor is 18 to 26‰ for hydrogen and 4 to 6‰ for oxygen, implying that more than one stages of liquidvapor separation are taking place in underground hydrothermal systems. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1978-03-25 |
巻 | 47巻 |
開始ページ | 55 |
終了ページ | 67 |
ISSN | 0369-7142 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 40000321119 |
JaLCDOI | 10.18926/21162 |
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タイトル(別表記) | No occcurrence of the oxygen isotope exchange with quartz glass of reaction tube through the conversion of oxygen into carbon dioxide in an externally heated carbon furnace |
フルテキストURL | pitsr_050_041_042.pdf |
著者 | 松葉谷 治| |
抄録 | Two oxygens of which δ(18)O is +28.83 and -79.57‰, respectively, were converted into carbon dioxide by means of both an external heating method and a Daylight's method where a graphite rod was heated by concentration of light from a slide projecter lamp on the graphite rod, and the δ(18)O of carbon dioxides obtained in the two methods were compared to each other. Except for data affected by memory of the previous sample, the averages in the external heating method were +28.85 and -79.56‰, respectively, and quite consistent with the averages in the Daylight's method, that were +28.81 and -79.67‰, respectively. This concludes that no oxygen isotope exchange occurs between the sample gas and the quartz glass of reaction tube in the external heating method. There is no significant difference in the results in four externally heated carbon furnaces, whereas the memory of previous samples was apparently observed within each furnaces. This memory was larger in the furnaces containing a used graphite rod (Nos. 3 and 4) than those containing new one (Nos. 1 and 2), and also more significant for smaller samples (Run 4 in No. 3). However, if the reaction tube was baked out at a higher temperature (750℃) than the reaction temperature (700℃) before reaction, the memory was mostly eliminated (Run 8 in No.3). |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1980-03-25 |
巻 | 50巻 |
開始ページ | 41 |
終了ページ | 42 |
ISSN | 0369-7142 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002310942 |
JaLCDOI | 10.18926/21159 |
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タイトル(別表記) | An isotope study of hot springs in Nagano Prefecture |
フルテキストURL | pitsr_050_017_024.pdf |
著者 | 松葉谷 治| 酒井 均| 日下部 実| 佐々木 昭| |
抄録 | Water samples from 28 hotsprings and mineral springs in Nagano Prefecture, central Japan, were examined for their stable isotope ratios of hydrogen, oxygen, carbon, and sulfur. Spring waters of Kashio are highly saline and enriched in heavy isotopes of oxygen and hydrogen (δ(18)O=-2.5~-4.6‰, δD=-54~-57‰). Linear relationships among δD, δ(18)O, and Cl(-) suggest that spring waters are the mixtures of a deep brine and local surface water. Extrapolation of the linear relationships indicates that the deep brine is both isotopically and chemically very similar to the deep brine previously suggested for the springs of Arima, Takarazuka, and Ishibotoke of which δD, δ(18)O, and Cl(-) are estimated as -33‰, +8.0‰, and 44g/l, respectively. A common origin may be warranted among these postulated brines, while their provenance is yet to be worked out. The hot springs in Matsushiro are a Na-Ca-Cl type of high carbonate content. Their hydrogen and oxygen isotope ratios (δD=-71~-46‰, δ(18)O=-9.1~-2.0‰) are higher than the local surface water. On the basis of the relationships among δD, δ(18)O, and Cl(-), they are considered to be the mixtures of fossil sea water and certain water of meteoric origin of which Cl(-) is about 4g/l and δ(18)O is higher by about 3‰ than the local surface water. The latter may be meteoric water circulating in the marine sedimentary formations (Green Tuff formations) with soluble sea salts. Isotopic exchange with carbonate minerals in the formations explains its (18)O enrichment. Spring waters from Yashio and Isobe (Gunma Pref.) as well as Yunosawa and Yatate (Akita Pref.) were previously interpreted to be mixtures of fossil sea water and local surface water of low Cl(-) content. Re-examination of their data revealed that the meteoric waters responsible for these springs contain about 3g/l Cl(-), similar to the value obtained for Matsushiro. However, unlike Matsushiro, the meteoric waters in these areas are found to be isotopically similar to the local surface waters. Waters from other hot springs studied here are of simply meteoric origin, thus belonging to the GreenTuff type water previously defined. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1980-03-25 |
巻 | 50巻 |
開始ページ | 17 |
終了ページ | 24 |
ISSN | 0369-7142 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002310953 |
JaLCDOI | 10.18926/21085 |
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タイトル(別表記) | Automatic measurement of oxygen isotope ratio of water samples |
フルテキストURL | pitsr_056_027_034.pdf |
著者 | 千葉 仁| 酒井 均| 安武 正敏| |
抄録 | The automatic sample preparation system for oxygen isotope analysis of natural water samples was constructed. The system is essentially a modification of that originally designed by W. Dansgaard in the University of Copenhagen. Sixty water samples of 5 ml each are automatically equilibrated with CO(2) of 30 ml NTP each within 4.5 hours. The equilibrated CO(2) gases are successively measured for their oxygen isotopic ratios by an automatic mas-sspectrometer, VG903. The time required for the measurement of the 60 CO(2) samples is about 15 hours; thus approximately 20 hours are required to complete the isotopic measurements of 60 water samples. The accuracy of the oxygen isotopic analyses is about 0.1%. The result of oxygen isotopic analyses by the automatic preparation system agrees with that of the conventional method within about +0.1%. The results indicate that the automatic preparation system is applicable for the oxygen isotope analysis of natural water samples. |
出版物タイトル | 岡山大学温泉研究所報告 |
発行日 | 1985-03-30 |
巻 | 56巻 |
開始ページ | 27 |
終了ページ | 34 |
ISSN | 0369-7142 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002310952 |
著者 | 広瀬 温| |
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発行日 | 1956-11-30 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 68巻 |
号 | 11号 |
資料タイプ | 学術雑誌論文 |
JaLCDOI | 10.18926/19790 |
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タイトル(別表記) | Oxygen inhalation therapy for chronic venous ulcer. -An additional treatment modality- |
フルテキストURL | 060_031_034.pdf |
著者 | 古元 嘉昭| 得能 輝男| 曽田 益弘| 平井 俊一| 森末 真八| 鈴鹿 伊智雄| 砂川 満| 萬 秀憲| |
抄録 | 長期にわたり反復する静脈性潰瘍は,静脈圧亢進により拡張した毛細管の増加とその周辺に滲出したフィブリンの沈着により,血液からの酸素,及び栄養物の供給が妨げられている。医用質量分析装置による皮下組織ガス分圧の評価で経鼻的に100 % の酸素吸入により潰瘍周辺への酸素供給が認められたので,重篤臨床例に対して静脈圧減圧処置に加えて酸素吸入を併用したところ,潰瘍の治癒傾向は著しく速くなり,補助療法としての意義を認めた。 |
キーワード | 慢性静脈性潰瘍 (Chronic venous ulcer) 組織ガス分圧 (Partial pressure of tissue gases) 医用質量分析装置 (Medical mass spectrometer) 酸素拡散 (Oxygen diffusion) 酸素吸入療法 (Oxygen inhalation therapy) |
出版物タイトル | 環境病態研報告 |
発行日 | 1989-07 |
巻 | 60巻 |
開始ページ | 31 |
終了ページ | 34 |
ISSN | 09133771 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002309180 |
著者 | 山口 義雄| |
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発行日 | 1956-09-30 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 68巻 |
号 | 9号 |
資料タイプ | 学術雑誌論文 |
JaLCDOI | 10.18926/19731 |
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タイトル(別表記) | Spa therapy for bronchial asthma 1. Climatotherapy, its clinical effects |
フルテキストURL | 058_031_034.pdf |
著者 | 谷崎 勝朗| 周藤 真康| |
抄録 | 気管支喘息に対する温泉療法,特に温泉所在地(保養地)の環境,すなわち気候条件の喘息に対する影響について,文献的考察を加えた。気候療法としては,主として山岳気候,海洋性気候,洞窟気候などが,喘息の治療に応用されている。これらの気候は,いずれも喘息に対して有効的に作用することが示されているが,それぞれの特徴を持っている。例えば,山岳気候は酸素分圧が低いこと,水蒸気圧が低いことなどが特徴であり,そのため生体がそれに適合するためにはある程度の時間が必要となる。一方海洋性気候は,海塩粒子を含んでおり,海水エロゾル中のカルシウムやマグネシウムなどが良い影響を与えると考えられている。また洞窟気候は,水分含量が均一であり,電解質,特に陰イオンが多く,これが粘膜活性や浄化活性を亢進させると言われている。またいずれの気候療法も,副腎皮質機能の活性化をもたらすと考えられている。 |
キーワード | 気候療法 (climatotherapy) 気管支喘息 (bronchial asthrna) 山岳気候 (mountain climate) 海洋性気候 (sea climate) 洞窟気候 (underground climate) |
出版物タイトル | 環境病態研報告 |
発行日 | 1987-08 |
巻 | 58巻 |
開始ページ | 31 |
終了ページ | 34 |
ISSN | 09133771 |
言語 | 日本語 |
論文のバージョン | publisher |
NAID | 120002308993 |
著者 | 赤井 功一郎| |
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発行日 | 1956-06-30 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 68巻 |
号 | 6号 |
資料タイプ | 学術雑誌論文 |
著者 | 河野 育夫| |
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発行日 | 1958-12-31 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 70巻 |
号 | 12号 |
資料タイプ | 学術雑誌論文 |
著者 | 河野 育夫| |
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発行日 | 1958-12-31 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 70巻 |
号 | 12号 |
資料タイプ | 学術雑誌論文 |
著者 | 田中 孝男| |
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発行日 | 1958-12-31 |
出版物タイトル | 岡山医学会雑誌 |
巻 | 70巻 |
号 | 12号 |
資料タイプ | 学術雑誌論文 |