• Bulletin of the Korean Chemical Society
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• 제35권3호
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• pp.753-757
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• 2014

The nucleophilic substitution reactions of Y-aryl N,N-dimethyl phosphoroamidochloridates with substituted anilines and deuterated anilines are kinetically investigated in acetonitrile at $65.0^{\circ}C$. A stepwise mechanism with a rate-limiting leaving group departure from the intermediate is proposed based on the positive ${\rho}_{XY}$ value. The deuterium kinetic isotope effects involving deuterated anilines show secondary inverse with all the nucleophiles, rationalized by a dominant backside nucleophilic attack.

• 전기의세계
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• 제13권1호
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• pp.30-33
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• 1964

최근 우리나라의 isotope사용은 의학 및 농학을 비롯하여 여러 분야에서 활발히 움직이고 있으나 공업면의 응용에는 아직 거의 없는 실정에 놓여있는 것이다. 그것은 계측기의 성능이 종래의 다른 방식과 비교할 때 대단히 우수하여 계측만으로의 목적으로는 좋은 평가를 받았든 것이나 process공업의 목적으로는 측정 절단 그리고 제어를 하는 복잡한 체계로서 시작하여야 되는 고로 다소 고도의 기술을 요하는 난점이 있었기 때문이었다. 따라서 본지에서는 실제 isotope가 process공업에 응용될때 문제되는 점 즉 process제어 정밀도의 우려를 가려내는 검출단의 성능과 각 공업에서 사용할 수 있는 계측기의 제어계를 간단히 해설하여 보기로 한다.

• Bulletin of the Korean Chemical Society
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• 제29권11호
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• pp.2125-2128
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• 2008

• 대한자원환경지질학회:학술대회논문집
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• 대한자원환경지질학회 2003년도 춘계 학술발표회 논문집
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• pp.20-23
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• 2003

Low-sulfidation style ore deposits, the major source of Au, Ag, and Hg, are formed from neutral-pH, reduced hydrothermal solutions close to equilibrium with their host rocks. The waters are low-salinity (〈1 wt % NaCl equiv.) but relatively gas rich (1-2 wt % $CO_2$), and are largely meteoric water. However, the contribution of magmatic components to the epithermal system, its temporal importance, and its relation to the source of ore metals are largely controversial. (omitted)

• 한국어업기술학회:학술대회논문집
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• 한국어업기술학회 2001년도 춘계 수산관련학회 공동학술대회발표요지집
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• pp.407-408
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• 2001

Stable isotope technique in matrine science is becoming powerful tool to roveal the environmental characteristics surrounding organisms during their past life histories. general, the isotopic data can be used for estimations of habitat temperature, migratory patterns and habitat location, metabolic rates, and investigations of food chains (Kalish, 1991). (omitted)

• 대한화학회지
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• 제63권5호
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• pp.387-391
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• 2019

• 대한수의사회지
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• 제9권3호
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• pp.67-70
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• 1965

• 자원환경지질
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• 제33권6호
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• pp.469-489
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• 2000

The hydrogeochemical and isotopic studies on deep groundwater (below a 550 m depth from the ground surface) in the Munkyeong area, Kyeongbuk province were carried out. Two types of deep groundwater (${CO_2}$-rich groundwater and alkali groundwater) occur together in the Munkywong area. ${CO_2}$-rich groundwater (Ca-${HCO_3}$ type) is characterized by low pH (5.8~6.5) and high TDS (up to 2,682 mg/L.), while alkali groundwater (Na-${HCO_3}$ type) shows a high pH (9.1~10.4) and relatively low TDS (72~116 mg/L). ${CO_2}$-rich water may have evolved by ${CO_2}$ added at depth during groundwater circulation. This process leads to the dissolution of surrounding rocks and Ca, Na, Mg, K and ${HCO_3}$ concentrations are eniched. The low $Pco_2$ ($10^{-6.4}$atm) of alkali groundwaters seems to result from the dissolution of silicate minerals without a supply of ${CO_2}$. The ${\delta}^{18}O$ and ${\delta}^D$values and tritium data indicate that two types of deep groundwater were both derived from pre-thermonuclear meteoric water and have evolved through prolonged water-rock interaction. The carbon isotope data show that dissolved carbon in the ${CO_2}$-rich water was possibly derived from deep-seated ${CO_2}$ gas, although further studies are needed. The ${\delta}^{34}S$ values of dissolved sulfate show that sulfate reduction occurred at great depths. The application of various chemical geothermometers on ${CO_2}$-rich groundwater shows that the calculated deep reservoir temperature is about 130~$l75^{\circ}C$. Based on the geological setting, water chemistry and environmental isotope data, each of the two types of deep groundwater represent distinct hydrologic and hydrogeochemical evolution at depth and their movement is controlled by the local fracture system.

• 분석과학
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• 제27권3호
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• pp.140-146
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• 2014

후 컬럼 동위원소 희석법(PCID, post column isotope dilution)을 HPLC-ICP/MS (high performance liquid chromatography-inductively coupled plasma/mass spectrometry)에 적용한 정량법에서 내부 표준물을 동시에 사용하여 정확도와 정밀도를 개선하였다. 전통적인 여러 정량법과 후 컬럼 동위원소 희석법을 비교하여 볼 때에 PCID의 경우에 컬럼내에서 발생하는 오차가 가장 큰 요인으로 작용하였음을 알 수 있었다. PCID에서 내부 표준물을 사용하여 컬럼내에서의 손실에 대한 오차를 효과적으로 보정하고 정확도와 정밀도를 개선할 수 있었다. 셀레늄 화학종인 SeMet을 시료로 사용하고 내부 표준물로 MeSecys 또는 $Se^{4+}$를 이용한 결과, 사용하지 않은 경우와 비교하면 상대오차는 각 각 31%와 13%에서 모두 1% 대로 낮아져 정확도가 크게 개선되었으며, 상대 표준편차는 5.1%와 6.9%에서 각각 1.5%와 0.2%로 정밀도 또한 크게 개선되었다. PCID에서 내부 표준물을 사용하였을 때의 정량분석법의 장점을 다른 분석법과 비교 토의하였다.

• Mass Spectrometry Letters
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• 제3권2호
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• pp.54-57
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• 2012

Mass spectrometric analysis was carried out using multicollector inductively coupled plasma mass spectrometry (MC-ICP-MS) for the precise and accurate determination of the isotope ratios of ultratrace levels of uranium dissolved in 3% $HNO_3$. We used the certified reference material (CRM) 112-A at a trace level of 100 pg/mL for the uranium isotopic measurement. Multiple collectors were utilized for the simultaneous measurement of uranium isotopes to reduce the signal uncertainty due to variations in the ion beam intensity over time. Mass bias correction was applied to the measured U isotopes to improve the precision and accuracy. Furthermore, elemental standard solution with certified values of platinum, iridium, gold, and thallium dissolved in 3% $HNO_3$ were analyzed to investigate the formation rates of the polyatomic ions of $Ir^{40}$ $Ar^+$, $Pt^{40}$ $Ar^+$, $Tl^{40}$ $Ar^+$, $Au^{40}$ $Ar^+$ for the concentration range of 50-400 pg/mL. Those polyatomic ions have mass-to-charge ratios in the 230-245 m/z region that it would contribute to the increase of background intensity of uranium, thorium, plutonium, and americium isotopes. The effect of the polyatomic ion interference on uranium isotope measurement has been estimated.