• Nuclear Engineering and Technology
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• 제47권6호
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• pp.738-745
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• 2015

The catalytic exchange of hydrogen isotopes between hydrogen and water has been known to be a very useful process for the separation of tritium from tritiated water. For the process, a highly active hydrophobic catalyst is needed. This study provides an effective fabrication method of size-controlled platinum/poly[styrene-divinylbenzene-tri(propylene glycol) diacrylate] [Pt/poly(SDB-TPGDA)] hydrophobic catalyst beads with a narrow size distribution. Platinum nanoparticles were prepared by ${\gamma}$-ray-induced reduction in the aqueous phase first, and then uniformly dispersed in SDB-TPGDA comonomer after the hydrophobization of platinum nanoparticles with alkylamine stabilizers. The porous Pt/poly(SDB-TPGDA) hydrophobic catalyst beads were synthesized by the UV-initiated polymerization of the mixture droplets prepared in a capillary-based microfluidic system. The size of as-prepared catalyst beads can be controlled in the range of $200-1,000{\mu}m$ by adjusting the flow rate of dispersed and continuous phases, as well as the viscosity of the continuous phase. Sorbitan monooleate and cyclohexanol were used as coporogens to control the porosities of the catalyst beads.

• 대한화학회지
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• 제37권9호
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• pp.800-805
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• 1993

정도관리용 생체기준물질 중의 극미량원소에 대한 분석법을 확립하였다. 생체시료를 질산-과산화수소 혼합산화제와 함께 테플론 가압분해용기에 넣어 마이크로파 오븐에서 분해하는 시료전처리법(microwave digestion)을 사용하였다. 시료를 분해시키기 전에 정량할 극미량금속의 안정 동위원소를 첨가하여 동위원소희석 질량분석법을 적용하였다. 혈액과 소나무잎 기준물질에 이러한 분석방법을 적용하여 기준값과 일치되는 결과를 얻었다.

• Nuclear Engineering and Technology
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• 제31권4호
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• pp.423-431
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• 1999

A radiotracer technique has been developed to monitor the rotational movement of two piston rings in one cylinder during engine operation. The rings were labeled with two different kinds of radioisotopes, i.e. $^{60}$ Co and $^{192}$ Ir, for identification of the top ring from the second ring. The radiotracers were implanted in a small hole bored on the inner side of each piston ring. The rings were installed in a single cylinder hydrogen engine and three Nal scintillation detectors were mounted around the engine block to measure the gamma radiation. The angle of ring-gap orientation was determined from the radiation counts measured with the three detectors during engine operation. Two windows (upper window for $^{60}$ Co and lower window for $^{192}$ Ir) were set on each ratemeter to count radiation from the two isotopes separately. Procedure to convert the radiation counts to the position of the ring gap was established. With the software programmed with MS-Visualbasic, radiation counts were compared with the reference responses that were measured at angular intervals of 10$^{\circ}$for each piston ring in advance of the experiment. The result was used for the evaluation of the relationship between the orientation of ring-gaps and oil consumption. It was found that an increase in the oil consumption rate of a specific operation condition was closely related to the relative phase angle of the two piston rings.

• Ocean and Polar Research
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• 제38권4호
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• pp.331-338
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• 2016

Many studies using tracers have been conducted to understand a physical process in a system. Rain-on-snow could accelerate snowmelt processes, which influences the hydrological process in both temperate and polar regions. Hydrological and ecological conditions will be affected by the amount and timing of discharge reaching the bottom of a snowpack. The discharge consists of the rain-on-snow, pore water penetrating into the snowpack and natural meltwater. In this study, after a rain-on-snow experiment, we conducted an isotopic hydrograph separation to distinguish rainwater and pore water from meltwater. Using the isotopic data of snow and meltwater from Lee et al. (2010), two components were separated based on the assumption that rainwater and pore water are new water and natural meltwater is old water. After the second rain-on-snow experiment, the maximum contributions of rainwater and pore water reached up to 69% of the discharge and then decreased. During the study period, the measured total discharge was 4153 L and 40% (based on hydrogen isotope) of rainwater and pore water was calculated in the discharge, which is not consistent with what Lee et al. (2016) calculated using chemical separation (63%). This inconsistency can be explained by how an end-member was defined in both approaches. The contributions of artificial rainonsnow and pore water to melwater discharge range between the two methods. This study will suggest a mixing calculation from isotopic compositions of the Southern Ocean.

• 세라미스트
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• 제22권4호
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• pp.357-367
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• 2019

Secondary Ion Mass Spectrometry(SIMS) is an analytical method that measures the distribution and concentration of elements or compounds by analyzing the mass of secondary ions released by irradiating ion beams with energy of hundreds eV to 20 keV on the sample surface. Unlike other similar analytical instruments, SIMS directly detect the elemental ions that constitute a sample, allowing you to accurately identify components and obtain concentration information in the depth direction. It is also a great feature for measuring isotopes and analyzing light elements, especially hydrogen. In particular, with the development of materials science, there is an increasing demand for trace concentration analysis and isotope measurements in the micro-regions of various materials. SIMS has a short history compared to other similar methods; nevertheless, SIMS is still advancing in hardware and is expected to contribute to the development of materials science through research and development of advanced analytical techniques.

• 자원환경지질
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• 제41권1호
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• pp.15-32
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• 2008

강화 석모도 지역 석모도 온천수의 영족기체와 온천수의 지화학적 진화와 기원을 해석하고 온천수의 지화학적 특성을 규명하기 위해 온천수, 지하수, 지표수의 수리화학, 안정 동위원소, 영족기체 동위원소 분석이 이루어졌다. 온천수와 지하수의 pH는 각각 $6.42{\sim}6.77,\;6.01{\sim}7.71$로 약산성을 보이고 있다. 석모도 온천 지역의 온천수의 유출수온은 $43.3{\sim}68.6^{\circ}C$이다. 온천수의 전기전도도는 $60,200{\sim}84,300{\mu}S/cm$으로 비교적 높은 값이며 석모도 온천수가 해수와 혼합되어졌음을 암시하고 있다. 석모도 온천수의 화학 조성은 Na-Ca-Cl형이다. 반면, 지하수와 지표수는 각각 Na(Ca)-$HCO_3$, Na(Ca)-$SO_4$형과 Ca-$HCO_3$ 형으로 구분된다. 석모도 온천수의 산소와 수소 동위원소비는 각각 $-4.41{\sim}-4.47%o$와 $-32.0{\sim}-33.5%o$로 순환수 기원이다. 지하수에서의 산수 수소 동위원소비는 각각 $-7.07{\sim}-8.55%o,\;-50.24{\sim}-59.6%o$이다. 석모도 온천수에 $^{18}O$와 $^2H$가 부화된 특성은 온천수가 담수와 해수의 혼합대에서 유래되었음을 암시하고 있다. 석모도 온천수 중의 황산염이온의 황 동위원소비는 $23.1{\sim}23.5%o$로 이 지역 해수의 황 동위원소비(20.2%o)와 유사하다. 이는 온천수의 황이 해수의 황산염으로부터 유래되었음을 의미한다. 석모도 온천수의 $^3He/^4He$ 비는 $1.243{\times}10^{-6}{\sim}1.299{\times}10^{-6}cm^3STP/g$로 온천수 중의 He 가스가 부분적으로 맨틀에서 유래되었음을 보여준다. 온천수에서의 아르곤 동위원소비$(^{40}Ar/^{36}Ar=298{\times}10^{-6})cm^3STP/g$는 대기기원의 값을 보인다.

• Korean Chemical Engineering Research
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• 제56권2호
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• pp.169-175
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• 2018

본 연구는 핵융합 배가스 중 삼중수소가 포함된 화합물인 메탄($CQ_4$) 및 물($Q_2O$)로부터 수소동위원소를 회수하기 위한 공정에 관한 것이다(Q는 수소, 중수소, 삼중수소). 수증기-메탄 개질반응과 수성가스 전환반응을 이용하여 $CQ_4$와 $Q_2O$를 $Q_2$로 변환시키고, 후속하는 팔라듐 분리막으로 생성된 $Q_2$를 회수한다. 본 연구에서는 $CQ_4$ 및 $Q_2O$ 중 하나의 물질인 $CH_4$ 및 $H_2O$로부터 수소 회수를 위해 촉매반응기, 팔라듐 분리막, 순환펌프로 구성된 순환루프를 적용하였다. 촉매반응온도 및 순환유량을 변화시켜가며 $CH_4$ 및 $H_2O$의 전환율을 측정하였다. $CH_4$ 중 수소 회수는 촉매반응온도 $650^{\circ}C$, 순환유량 2.0 L/min 조건에서 99% 이상의 $CH_4$ 전환율을확인하였고, $H_2O$ 중수소 회수는촉매반응온도 $375^{\circ}C$, 순환유량 1.8 L/min 조건에서 96% 이상의 $H_2O$ 전환율을 확인하였다. 이와 더불어, 향후 핵융합 실증로(K-DEMO)에서의 $CQ_4$ 발생량을 예측하고, 이에 대한 처리공정을 제안하였으며, HAZOP (Hazard and Operability) 분석을 실시하여 공정의 위험요소와 운전상의 문제점을 도출하고 해결방안을 제시하였다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2000년도 추계학술대회
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• pp.232-236
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• 2000

Multi-regression statistical analyses were applied for the water quality data of shallow alluvial ground water (n = 47) collected from the Youngdeok area, in order to quantitatively generalize the natural (non-anthropogenic) causes of regional water quality variation. Seven samples having the high contamination index ( $C_{a}$ > 3) reflect the striong effects by anthropogenic activity. Most of the alluvial groundwaters have acquired their quality primarily due to the dissolution of carbonate minerals. The results of multi-regression analysis show that chlorine is mainly derived from seawater effect. Sulfur isotopic compositions of dissolved sulfur and the S $O_4$/Cl ratio also enable us to discriminate the samples (n = 18) which are affected by atmospheric input of marine aerosol (sea-spray) and also by mixing between freshwater and seawater. Hydrogen and oxygen isotope data of the samples collected lie close to the local meteoric water line obtained from nearby Pohang city but has lower slope (5.45) on the $\delta$D-$^{18}$ O plot, indicating that alluvial groundwater was recharged from infiltrated meteoric water which has undergone some degree of kinetic evaporation. The estimated initial isotopic composition of the recharged water ($\delta$D = -74.8$^{0}$ /$_{00}$, $\delta$$^{18}$ O = -10.8$^{[-1000]}$ /$_{[-1000]}$ ) suggests that the alluvial ground water recharge largely occurs during summer storm events.s.s.

• 한국진공학회:학술대회논문집
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• 한국진공학회 2011년도 제40회 동계학술대회 초록집
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• pp.421-422
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• 2011

The first part is about development of a liquid target for a neutron source, which is designed to overcome many of the limitations of traditional beam-target neutron generators by utilizing a liquid target neutron source. One of the most critical aspects of the beam-target neutron generator is the target integrity under the beam exposure. A liquid target can be a good solution to overcome damage to the target such as target erosion and depletion of hydrogen isotopes in the active layer, especially for the one operating at high neutron fluxes with no need for water cooling. There is no inherent target lifetime for the liquid target neutron generator when used with continuous refreshment of the target surface exposed to the energetic beam. In this work, liquid target containing hydrogen has been developed and tested in vacuum environment. Potentially, liquid targets could allow a point neutron source whose spatial extension is on the order of 1 to $10{\mu}m$. And the second is about the vacuum ultraviolet (VUV) spectrometer which is designed as a five-channel spectral system for ITER main plasma measurement. To develop and verify the design, a two-channel prototype system was fabricated with No. 3 (14.4 nm~31.8 nm) and No. 4 (29.0 nm~60.0 nm) among the five channels. For test of the prototype system, a hollow cathode lamp is used as a light source. The system is composed of a collimating mirror to collect the light from source to slit, and two holographic diffraction gratings with toroidal geometry to diffract and also to collimate the light from the common slit to detectors. The two gratings are positioned at different optical distances and heights as designed. To study the appropriate detector for ITER VUV system, two different electronic detectors of the back-illuminated charge coupled device and the micro-channel plate electron multiplier were installed and the performance has been investigated and compared in the same experimental conditions. The overall system performance was verified by measuring the spectrums.

• 한국지하수토양환경학회지:지하수토양환경
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• 제26권3호
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• pp.25-36
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• 2021

This study evaluated monthly, seasonal and altitudinal changes of oxygen and hydrogen isotope compositions of wet precipitation samples (n = 238) that were collected for last four years from 7 altitudes (from 265 to 1,500 m above sea level) in the Jeju Samdasoo watershed at the southeastern part of Jeju island, in order to examine the recharge characteristics of groundwater that is pumped out for the production of the Samdasoo drinking mineral water. Precipitation samples showed a clear seasonal change of O-H isotopic composition as follow, due to the different air masses and relative humidity: 𝛿D = 7.3𝛿¹⁸O + 11.3 (R² = 0.76) in the wet season (June to September), while 𝛿D = 7.9𝛿¹⁸O + 9.5 (R² = 0.91) in the dry season (October to May). In contrast, the stable isotope compositions of groundwater were nearly constant throughout the year and did not show a distinct monthly or seasonal change, implying the well-mixing of infiltrated water during and after its recharge. An altitudinal effect of the oxygen isotope compositions of precipitation was also remarkable with the decrease of -0.19‰ (R² = 0.91) with the elevation increase by 100 m. Based on the observed altitudinal change, the minimum altitude of groundwater recharge was estimated as 1,200 m above the sea level in the Jeju Samdasoo watershed.