• 대한한의학방제학회지
• /
• 제15권1호
• /
• pp.185-197
• /
• 2007

Objective : This study was conducted to investigate the effects of Hwangryunhaedok-Tang and Geongangbuja-Tang on the change of interleukin-6 (IL-6) and tumor necrosis $factor-{\alpha}$ ($TNF-{\alpha}$) level induced by LPS I.C.V. injection in mice. Method : We devided group into 6 mice and 6 mice were assingned to each group. In the normal group only saline was administered intragastrically, and in the control group LPS was injected intracerebroventricularly 1 hr after intragastric administration of saline. In the experiment groups Hwangryunhaedok-Tang(0.5g/kg, 1.0g/kg, 3.0g/kg) was administered intragastrically to mice 1 hr prior to LPS(100mg/mouse) I.C.V. injection.. Also Geongangbuja-Tang (0.5g/kg, 1.0g/kg, 3.0g/kg) was administered intragastrically to mice 1 hr prior to LPS(100mg/mouse) I.C.V. injection. To measure the plasma IL-6 and $TNF-{\alpha}$ level of mice, their blood samples were collected from retro-orbital plexus, immediately centrifuged at $4^{\circ}C$, and plasma was removed and stored frozen at $-83^{\circ}C$ for later determination of IL-6 and $TNF-{\alpha}$. The level of IL-6 and $TNF-{\alpha}$ production was measured by enzyme-linked immunosorbent assay in the plasma. Result : Regarding IL-6 level, The 0.5g/kg and the 1g/kg groups of Geongangbuja-Tang decreased IL-6 level. Especially the 3g/kg control group decreased IL-6 level significantly than the normal group(p<0.01). Regarding $TNF-{\alpha}$ level, the 3g/kg group of Geongangbuja-Tang decreased it significantly(p<0.05). Conclusion : These data revealed that Hwangryunhaedok-Tang might not have the anti imflammatory effect and Geongangbuja-Tang(3g/kg)might have the anti imflammatory effect by reducing the plasma IL-6 and $TNF-{\alpha}$ level in mice LPS Injection.EIM (Eighteen Incompatible Medicaments) is an important component in Oriental pharmacology and is directly related to clinical prescriptions. Medical practitioners argued that the definite cause and meaning of EIM was ambiguous and therefore debated the issue of clinical application of the EIM. This study conducted an in-depth literary research on the origin, meaning and contents of EIM with the purpose to contribute in its efforts to be used clinically. Even after thousands of years have past since establishment of Oriental medicine, EIM is still tabooed and was an obstacle that hindered ideologies. Modern herbal medicine texts claim that the use of EIM can reduce treatment effects and promote poisoning and side effects. However, since long ago, there has been medical practitioners who reject this as false. Recently, poisoning caused by EIM has been claimed to be from the toxicity of the drug itself, rather than the result of interaction between the drugs, and therefore they suggest that EIM is not a forbidden domain. In addition, EIM showed a difference in number depending on the era. However, this can be understood not as a definite number, but instead as a warning to be careful during combination of drugs for use as clinical medicine. Historically, there were very few cases in which EIM was used for clinical tests and thus, the clinical value is not, while others applied EIM directly to their bodies, which showed signs for the usefulness and potential of EIM for us. A more concrete and in-depth study must be made on EIM.

• 자원환경지질
• /
• 제26권1호
• /
• pp.21-27
• /
• 1993

유체포유물은 광상의 기원과 물리화학적인 환경 연구에 널리 사용되어져 왔다. 하지만 측정치의 오차와 유체포유물의 밀도와 isochore 등의 계산에 있어 그 과정의 복잡성 때문에 유체포유물에 내포한 물리화학적인 정보를 정확히 알아내는 것은 매우 힘들다. HALWAT, $CO_2$ 그리고 CHNACL 등의 컴퓨터 프로그램들은 (Nicholl and Crowford, 1985) 유체포유물의 밀도와 isochore 등을 복잡한 공식을 이용하여 계산함으로서 유체포유물로 계산될 수 있는 물리화학적인 정보의 정확도를 개선하였다. 본 논문에서는 이들 프로그램을 백악기에 형성된 금학 광산에 대한 최상훈과 소칠섭 (1992)의 유체포유물 측정치와 쥬라기에 형성된 삼황학 광산에 대한 윤성택 (1990)의 유체포유물 측정치에 적용하여 보았다. 컴퓨터 프로그램을 이용하여 결정된 금학광산의 온도-압력조건은 $230^{\circ}{\sim}290^{\circ}C$, 500~800 bar로서 최상훈과 소철섭 (1992)에 의하여 추정된 온도-압력조건인 $280{\sim}360^{\circ}C$, 500~800 bar와 유사하다. 하지만 본 연구에서 결정된 삼황학 광산에 대한 온도-압력 조건은 대략 4~7 kb, $328{\pm}500^{\circ}{\sim}55^{\circ}C$ 이며 이는 윤성택 (1990)에 의하여 추정된 온도-압력 조건인 1.2~1.9kb, $25^{\circ}{\sim}294^{\circ}C$와 차이를 보여준다. 삼황학 광산에서의 온도-압력 추정에 있어서의 차이는 광상의 온도-압력조건 추정에 있어 균일화 온도와 유체포유물의 포획온도를 동일시하고 적당치 못한 isochore의 사용함에 기인한다. 금학광상의 경우는 낮은 압력조건 (<1~2kb)에서 균일화 온도와 유체포유물의 포획온도가 비슷하기 때문에 큰 차이를 보여 주지 않았다. 따라서 1~2kb보다 높은 압력조건에서 형성된 광상에서는 광상의 온도-압력조건 추정에 있어 균일화 온도의 잘못된 적용과 적당치 못한 isochore의 사용을 피하여야 하며 이를 위하여 본 연구에서 소개된 컴퓨터 프로그램 이용을 추천한다.