• 제목/요약/키워드: Cold water region

검색결과 152건 처리시간 0.019초

황제내경(黃帝內經)에 보이는 한(汗)관련 서술(敍述)의 특징(特徵)에 대한 고찰(考察) (A Study on the Characteristics of Descriptions of the Perspiration in "Hwangjenaegyeong(黃帝內經)")

  • 유정아;장우창;백유상;정창현
    • 대한한의학원전학회지
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    • 제23권2호
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    • pp.205-223
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    • 2010
  • In Korean Traditional Medicine(abbreviated to K.T.M.), hyperhidrosis and anhidrosis are the targets of the medical treatment. Furthermore sweating appearance is also one of the important symptoms which explain a particular situation of the patient in K.T.M. And at "Sanghanron(傷寒論)" which is a traditional chief clinical bible written by Jang Gi(張機) later Han dynasty(漢代) in China made full use of the various kinds of diaphoresis[汗法] as a main medical treatment with purgation therapy[下法] and emetic therapy[吐法]. So the sweat in itself not only is the disease, but also is one of the symptoms explain a disease pattern. This thesis inquires into "Hwangjenaegyeong(黃帝內經)" referring to sweat which is the origin of recognition to the sweat in K.T.M. Some theses similar to this research had been made progresses and already reported, but most of them have classified the contents into biology, pathology, diagnosis, treatment after the model of western medical theory. In the aspect of comparative studying with other literature and clinic practical using, we found characteristics of referring to sweat in "Hwangjenaegyeong(黃帝內經)". And we classify the characteristics into some categories as follows. 1. There are some terms which make a title including sweat and symbolize the characteristics, for example sweat of soul[魄汗], sweat of death[絶汗], sweat of streaming[灌汗], sweat of weakness[白汗], sweat of sleep[寢汗], sweat of bright and heat[炅汗], sweat of kidney[腎汗], sweat of escaping[漉汗], cold sweat[寒汗], sweat on the head[頭汗], hyperhidrosis[多汗], heavy sweat[大汗]. But there aren't spontaneous sweat[自汗] or sweat like a thief[盜汗] which are the normal terms referring to sweat in history of K.T.M. And there are several descriptions about sweat appearance such as sweating in half of body[汗出偏沮], sweating in the rear end and thigh and knee[汗出尻陰股膝], hyperhidrosis in the neck and aversion to wind[頸多汗惡風], hyperhidrosis in the head and face and aversion to wind[頭面多汗惡風], cannot stopping the sweating under head[頭以下汗出不可止], make a person sweat to one's feet[令汗出至足], sweating like escaping[漯漯然汗出], sweating like soaking[汗出如浴], sweating become moist[汗出溱溱], hardly escaping sweat[汗大泄], escaping sweating[漉漉之汗], sweat moisten the pores [汗濡玄府], ceaseless sweating like pouring[汗注不休] sweating like pouring and vexation[汗注煩心], damp with sweat[汗汗然], sweating spontaneously[汗且自出], removal of fever with sweat drying[熱去汗稀]. That can be divided into sweat region and sweat form. 2. There are detailed explanations of the principle of perspirations caused by hot weather, hot food, hard working and meeting damp pathogen. 3. There are some explanations of the principle of removing fever due to the excessive heat from internal and external body through sweating by replenishing the body fluid. And many descriptions about overcoming the febrile disease by dropping temperature through sweating and many diaphoresis for curing. 4. There are some descriptions about five Jang organs perspirations and attachment of five mucous body fluid to five Jang organs. 5. There are pathogenic progresses after sweating affected by the Six Atmospheric Influences and water. And detailed explanations of disease mechanism a sweat leading to another disease. 6. There are descriptions about various sweat absent situations.

베링해 중부 지역의 마지막 빙하기 이후 고생산성의 고해상 변화 (High-Resolution Paleoproductivity Change in the Central Region of the Bering Sea Since the Last Glaciation)

  • 김성한;김부근;신혜선
    • 한국해양학회지:바다
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    • 제14권3호
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    • pp.134-144
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    • 2009
  • 베링해 중부 지역에서 획득된 피스톤 코아 PC23A의 퇴적물에서 오팔과 총유기탄소의 함량을 측정하고 집적률을 계산하여 마지막 빙하기 이후의 고생산성 변화를 살펴보았다. 코아 PC23A의 연대는 부유성 유공충의 AMS $^{14}C$ 탄소연대와 방산충 L. nipponica sakaii의 마지막 출현 기준에 의해서 결정되어있으며, 코아 최하단부가 약 61,000년 전으로 계산되었고, 코아 상부는 일부 손실된 것으로 판단된다. 오팔과 총유기탄소 함량은 마지막 빙하기 동안 각각 1-10%, 0.2-1.0%의 범위에서 변동하였으며, 각각 5%와 0.7%의 평균값을 보였다. 반면, 후빙기 동안에 오팔과 총유기탄소 함량은 5-22%, 0.8-1.2%의 범위에서 변동하였으며, 평균값은 각각 8%와 1.0%로 증가된 값을 보여주었다. 마찬가지로 오팔과 총유기탄소의 집적률도 마지막 빙하기($1gcm^{-2}kyr^{-1}$, $0.2gcm^{-2}kyr^{-1}$)동안 보다 후빙기 동안(>$5gcm^{-2}kyr^{-1}$, >$1gcm^{-2}kyr^{-1}$)에 증가하였다. 후빙기 동안 증가된 생산성은 온난한 기후에서 해빙의 발달이 미비하고 높아진 해수면 조건에서 주변 육상으로부터 융빙수의 유입 증가와 남쪽으로부터 알라스카 해류 유입의 증가에 의하여 영양염 공급이 충분한 환경에서 규조류가 번성하였기 때문이다. 반면, 마지막 빙하기 동안에는 낮아진 해수면으로 인하여 알라스카 해류의 유입이 감소하여 영양염의 공급이 제한되고, 낮은 수온과 추운 기후로 인해 광범위하게 발달한 해빙에 의해서 생산성이 감소되었다.