http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
소아 신질환에서 요 β₂-Microgloburin치와 사구체여과율 및 인산세뇨관재흡수율과의 상관관계
이한영,신재훈,김창렬,이우길 대한신장학회 1987 Kidney Research and Clinical Practice Vol.6 No.1
Urinary B2-microglobulin Q4-MG) was measured and compared the correlation between that and glomerular filtration rate (GFR) or tubular reabsorption of phos- phate (TRP$gt; in 72 patients with various renal diseases who were admitted to Hanyang University Hospital from January 1984 to March 1986. As a control group, the urinary B2-MG and GFR and TRP in 24 patients hospitalized due to other diseases (exclude known renal diseases, chronic inflammatory diseases, autoimmune diseases and malignancies) during the same period were also measured. The results were as follows: 1) The mean levels of urinary B2-MG were 225.4±41. 7 mg/24 hr in acute poststreptococcal glomerulonephritis, 192.7±36.6 pg/24 hr in nephrotic syndrome, and 241. 5±59.4 pg/24 hr in urinary tract infection which were markedly increased over that of control group (90.1±10. 1 pg/24 hr), (p=0.003, 0.003 and 0.012, respectively). 2) The GFR and TRP were not significant difference between renal diseases and control groups. 3) The urinary B2-MG levels enal diseases and control groups were not correlated with GFR or TRP.
Garnet-Orthopyroxene Geothermometer and Geological Applications
이한영,Lee, Han Yeang The Korean Society of Economic and Environmental G 1988 자원환경지질 Vol.21 No.1
석류석과 사방휘석의 평형관계를 20-45kb, $975-1400^{\circ}C$, FMAS시스템에서 상호역반응 실험을 통해서 연구하였으며 반응 촉매제로써 사용한 PbO와 0.55 $PbF_2$의 혼합물은 매우 효과적이었다. Fe-Mg의 교환반응은 이 실험온도, 압력범위 내에서는 조성성분의 영향을 받지 않는다. 실험결과와 석류석의 혼합 모델을 사용한 석류석-사방휘석의 지질온도계는 다음과 같다. $$T^{\circ}C=(1971+11.91P(Kb)+1510(X_{Ca}+X_{Mn})^{Gt}/(lnK_D+0.96)-273$$. Equilibrium relations between garnet and orthopyroxene have been investigated by reversal experiments in the range of 20-45Kb and $975-1400^{\circ}C$ in the $FeO-MgO-Al_2O_3-SiO_2$(FMAS) system. A mixture of PbO with about 55 mol per cent $PbF_2$ was used as a flux and proved very effective. The Fe-Mg exchange reaction seems to have little or no compositional dependence at these conditions. Combination of the experimental results with the garnet mixing model of Ganguly and Saxena(1984) yields the following geothermometric expression for the common natural assemblages that can be represented essentially within the system $FeO-MgO-CaO-MnO-Al_2O_3-SiO_2$. $$T^{\circ}C=(1971+11.91P(Kb)+1510(X_{Ca}+X_{Mn})^{Gt}/(lnK_D+0.96)-273$$.