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우라늄系列 非平衡 年代測定法과 韓半島 南海 上白島 現生 堆積層의 年代測定에 關한 硏究
Won Mok Jae(諸元穆),Chul Lee(李澈),Keung Shik Park(朴肯植),Seung Whan Choo(朱昇煥) 대한자원환경지질학회 1985 자원환경지질 Vol.18 No.3
Uranium-thorium separation technique from shallow sediment and α-source electrode-position technique are established in the present work, and uranium series disequilibrium dating method is applied to the quaternary piston core from Sangback-do, South Sea of Korean Peninsula. The age of the piston core (depth 200~300cm) sampled from Latitude 34°06′37″, Longitude 127°37′37″ was determined as ranging from 9.0±2.2 to 22.9±3.3Ky B.P, i.e., Later Pleistocene, older than Holocene which was stratigraphically known in the previous study. The sedimentation rate in the area is regularly increased according to the depth of the sedimentation layer. Except a few split sections of the piston core the sedimentation rates are avarage 7.2cm/1,000 years. Where sedimentation layer is deeper, then sedimentation rate tend to be slower. It must be pointed in age calculation that initial ²³⁰Th/²³⁴U radioactivity ratio is much influenced when detrital material was introduced in the sample. The ²³⁰Th/²³⁴U activity ratio measured in the present work is 0.06 at ²³²Th=0, and this value shows higher analytical errors because of the low-radioactivity of ²³⁰Th in the samples.
Determination of the Formation Constants of Metal Complexes with Organic Acids by Adsorption Method
제원목,Jae, Won-Mok Korean Chemical Society 1971 대한화학회지 Vol.15 No.4
The adsorption method for the determination of the formation constants of the metal complexes with organic acids was developed by using membrane filters. The adsorption method involved the measurements of radioactivities of the adsorbed metal on membrane filters and the filtrate solution after the radioactive metal ion were filtered through membrane filters in the presence of organic ions of varying concentration. Comparing the adsorption method with the ion exchange method, it was seen that the adsorption method was simpler and faster than the ion exchange method. As an example of the metal complex with organic acid yttrium citrate complex was chosen, and the formation constant of the complex obtained by the adsorption method showed $K_f=2.0{\times}10^{-4}(l. mole^{-1})$ at a pH of 7. Also the present study revealed that the carrierfree state of yttrium in aqueous solution was present in the completely ionized state.
Studies on Carrier-Free Yttrium-90 with Membrane Filters
제원목,Jae, Won-Mok Korean Chemical Society 1970 대한화학회지 Vol.14 No.4
The state of carrier-free yttrium-90 has been studied by filtration method with membrane filters. The studies include the adsorption ratio of carrier-free yttrium-90 on membrane filters by the change of PH, concentration of yttrium-90, and the pore size of member filters. The adsorption followed to Freundlich adsorption isotherm. The adsorption mechanism was proposed by the adsorption of transient state as an ionic form of $Y^{3+}$, and the experimental results were explained satisfactorily by the proposal. The adsorbed state of yttrium was present in the forms of yttrium such as $Y^{3+},\;Y(OH)^{3+},\;Y(OH)^{2+},\;Y(OH)^+_3,\;and\;Y(OH)_3$,and the existing ratios of the forms of yttrium were sharply changed by PH. It seems to be valid tha the carrier-free yttrium-90 exists mostly in $Y^{3+}$ state.
Studies on Carrier-Free Silver-111 with Membrane Filters
제원목,Jae, Won-Mok Korean Chemical Society 1973 대한화학회지 Vol.17 No.5
무단체 Ag-111의 상태를 여과법에 의하여 연구하였다. 이 연구는 막여과자에 의하여 수용액에 있어서 Ag-111의 pH 및 농도변화에 대한 효과를 조사하였다. 이 연구결과 막여과지에 대한 Ag-111의 부착은 Freundlich 흡착 등온식에 따르고 Ag-111의 흡착상태는 AgOH 형태로 존재하며 높은 pH에서 흡착성이 없는 $Ag(OH)_{2}-$는 Ag의 흡착을 방해하는 것으로 생각된다. 또한 무단체 Ag-111는 수용액중에서 $Ag^+$상태로 존재하고 있다. The state of carrier-free silver-111 has been studied by applying filtration method. The studies involved that the effects of pH and concentration of silver-111 in aqueous solution have been determined with membrane filters. The present studies revealed that the retainment of silver-111 on membrane filters followed Freundlish adsorption isotherm, and the adsorbed state of silver-111 was present in the form of AgOH. Also it was supposed that the formation of the non-adsorbed hydroxide of$Ag(OH)_{2}-$ may prohibit the existance of AgOH at higher pH, and it seems to be valid that the carrier-free silver-111 in aqueous solution exists in$Ag^+$state.
우라늄계열(系列) 비평충(非平衝) 연대측정법(年代測定法)과 한반도(韓半島) 남해(南海) 상백도(上白島) 현생(現生) 퇴적층(堆積層)의 연대측정(年代測定)에 관(關)한 연구(硏究)
제원목,이철,박긍식,주승환,Jae, Won Mok,Lee, Chul,Park, Keung Shik,Choo, Seung Whan 대한자원환경지질학회 1985 자원환경지질 Vol.18 No.3
Uranium-thorium separation technique from shallow sediment and ${\alpha}$-source electrodeposition technique are established in the present work, and uranium series disequilibrium dating method is applied to the quaternary piston core from Sangback-do, South Sea of Korean Peninsula. The age of the piston core (depth 200~300cm) sampled from Latitude $34^{\circ}06^{\prime}37^{{\prime}{\prime}}$, Longitude $127^{\circ}37^{\prime}37^{{\prime}{\prime}}$ was determined as ranging from $9.0{\pm}2.2$ to $22.9{\pm}3.3$ Ky B.P, i.e., Later Pleistocene, older than Holocene which was stratigraphically known in the previous study. The sedimentation rate in the area is regularly increased according to the depth of the sedimentation layer. Except a few split sections of the piston core the sedimentation rates are avarage 7.2cm/1,000 years. Where sedimentation layer is deeper, then sedimentation rate tend to be slower. It must be pointed in age calculation that initial $^{230}Th/^{234}U$ radioactivity ratio is much influenced when detrital material was introduced in the sample. The $^{230}Th/^{234}U$ activity ratio measured in the present work is 0.06 at $^{232}Th=0$, and this value shows higher analytical errors because of the low· radioactivity of $^{230}Th$ in the samples.
Adsorption Kinetics of Carrier-Free Yttrium-90 on Membrane Filters
제원목,Won Mok Jae Korean Chemical Society 1972 대한화학회지 Vol.16 No.1
The adsorption kinetics on a membrane filter have been studied by an introduction of acid or alkali in yttrium-90 solution. The change of the adsorption in the filtration process was determined by the filtrate activities with using a microsyringe filter holder connected with a syringe. The over all reaction rate obeyed a reversible first order reaction, and the rate constants thus obtained, showed the values of $k_1$ = 0.12 $sec^{-1}$ and $k_1'$ = 0.039 $sec^{-1}$. As a result of the present studies, it would be reasonable that the rate determining step of the adsorption reaction was the hydrolysis reaction of the adsorbed yttrium ions.
Citrate Complexes of Alkaline Earth Metals in Aqueous, Acetone-Water and Ethanol-Water Solutions
최상업,배영일,제원목,Choi, Sang-Up,Pae, Young-Il,Jae, Won-Mok Korean Chemical Society 1970 대한화학회지 Vol.14 No.1
양이온 교환수지와 시트르산 이온($Cit^{3-}$)이 들어있는 용액에서 방사성 알칼리 토류 금속 이온이 수지와 용액 사이에 어떻게 분배되는가를 실온에서 조사함으로써 그들 금속 이온의 시트르산 착물형성에 관한 연구를 하였다. 용매로서 $H_2O$, 아세톤-$H_2O$ 및 에탄올-$H_2O$를 사용하였다. 용액의 pH는 7.2-7.5로 조절하였고 이온 강도는 0.10-0.12로 유지하였다. 본 연구의 결과 $Ba^{++}$과 $Sr^{++}$은 어떤 용매계에서도 1:1착물(M $Cit^-$)을 형성하는 것을 알았다. 그리고 $Ca^{++}$은 수용액에서는 1:1착물을 형성하지만 혼합 용매계에서는 1:1착물(Ca $Cit^-$)과 1:2착물(Ca $Cit_2^{4-}$)을 형성함을 알았다. 그리고 이들 착물의 안정도는 $Ba^{++}\;<\;Sr^{++}\;<\;Ca^{++}$ 의 순으로 커지며 또 혼합용매의 유기 성분의 농도 증가순으로 커짐을 알았다. Formation of the complexes of alkaline earths with citrate ions in aqueous, acetone-water and ethanol-water solutions was studied at room temperature by the equilibrium exchange technique. This technique involved the measurements of distribution of radioactivity between cation exchange resin and solution phase after the radioactive metal ions were equilibriated with the cation exchange resin in the presence of citrate ions ($Cit^{3-}$) of varying concentrations. The pH of the solutions was controlled to 7.2-7.5, and the ionic strength of the solutions was kept at 0.10-0.12. The present study revealed that both barium and strontium ions formed the one to one citrate complexes, $[M Cit]^-$ in all solvent systems examined. It was also observed that calcium ions formed the one to one citrate complex in aqueous solution. In acetone-water and ethanol-water solutions, however, calcium ions were observed to form both one to one and one to two complexes, $[Ca Cit]^-$ and $[Ca\;Cit_2]^{4-}$. The results of the present study indicated also that relative stabilities of the complexes increased in the order; $Ba^{++}\;<\;Sr^{++}\;<\;Ca^{++}$, and in the order of increasing concentration of the organic components in the mixed solvent systems.