• Biotechnology and Bioprocess Engineering:BBE
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• 제11권3호
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• pp.215-222
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• 2006

The Lowry method was used in this study to measure protein in Haemophilus influenzae type b (Hib) conjugate vaccines (polyribosylibitol phosphate-tetanus toxoid; PRP-TT) using deoxycholic acid (DOC) to induce protein precipitation. Trichloroacetic acid (TCA) did not induce precipitation adequately from the Hib conjugate bulk and the freeze-dried Hib conjugate product. Its yield was approximately 50%. The matrix structure of Hib conjugate inhibits precipitation by TCA. Although the Lowry method can be carried out without precipitation in Hib conjugate bulk when no residual impurities (adipic acid dihydrazide [ADH], 1-ethyl-3-(3-dimethylamino-propyl) carbodiimide-HCI [EDAC], phenol and cyanogens bromide [CNBr], etc.) are present, it cannot be used for Hib conjugate products that contain sucrose 8.5%, because 8.5% concentration of sucrose enhanced the protein concentration. DOC- and HCl-induced precipitation is an alternative method for evaluating the protein content of the Hib conjugate bulk and the Hib conjugate product. The precipitation was optimal with a final concentrate of 0.1% for DOC at $4^{\circ}C$ and pH 2. This Lowry method, using DOC/HCI precipitation to induce protein precipitation, was confirmed a consistent, reproducible, and valid test for proteins in Hib conjugate bulk and its freeze-dried product.

• 한국산림과학회지
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• 제97권3호
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• pp.229-236
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• 2008

본 연구는 산림생태계내 물질순환의 한 경로인 수간류를 대상으로 수종에 따른 수간류량과 pH값의 특성을 살펴보기 위해 강원도 평창군에 위치한 중왕산 지역에서 2004년과 2005년에 매년 6월부터 10월까지 임외강우와 활엽수종인 신갈나무, 거제수나무, 음나무, 물푸레나무와 대표적 조림수종인 낙엽송 등 5개 수종의 수간류의 유입량과 pH값을 분석하였다. 수종별 수간류량은 신갈나무에서 조사기간 동안 9.9 mm가장 많았고, 거제수나무, 음나무, 낙엽송, 물푸레나무가 각각 7.5 mm, 5.9 mm, 3.8 mm, 3.2 mm였다. 임외강우량이 증가할수록 수간류량도 증가하였으며, 단기간 집중호우가 많이 발생한 2004년에 임외강우의 증가에 따른 수간류의 증가량이 적게 나타났다. 각 수종별 수간류의 pH값은 물푸레나무에서 평균 5.56으로 가장 높았으며, 음나무 5.64, 거제수나무 5.80, 신갈나무 5.91, 낙엽송 5.25 순이었다. 대체로 임외강우의 pH값이 증가함에 따라 수간류의 pH값도 증가하였으며, 임외강우의 평균 pH값은 6.39로 모든 수종의 pH값이 임외강우의 pH값보다 낮았다.

• 한국대기환경학회:학술대회논문집
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• 한국대기환경학회 2004년도 춘계학술대회 논문집
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• pp.135-136
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• 2004

• 한국대기환경학회지
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• 제20권3호
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• pp.381-396
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• 2004

In order to understand the precipitation acidity and chemical composition of ion species in Iksan area as well as to know the difference of chemical characteristics in precipitation samples from the viewpoint of precipitation sampling method, precipitation samples were collected by wet-only automatic precipitation sampler and bulk manual precipitation sampler in Iksan, from March 2003 to August 2003. The mean pH of precipitation was 5.0. There was a little significant difference in the mean value of pH between automatic and manual sampler. However, pH values of some precipitation samples were lower in automatic sampler than in manual sampler, especially in case of precipitation samples with small rainfall for March 2003. The mean concentrations of each ions in precipitation were generally a little higher in precipitation samples collected by the manual sampler than in those collected by the automatic sampler because of accumulation of dry deposition on the surface of glass funnel installed at the manual sampler during the sampling period or no rainfall. Dominant species determining the acidity of precipitation, were N $H_4$$^{[-10]}$ and nss-C $a^{2+}$ for cations and nss-S $O_4$$^{2-}$ and N $O_3$$^{[-10]}$ for anions. The mean concentration of N $H_4$$^{+}$ and nss-C $a^{2+}$ were 31 $\mu$eq/L and 9 $\mu$eq/L for the automatic sampler and 40 ueq/L and 16 ueq/L for the manual sampler, respectively. In addition, nss-S $O_4$$^{2-}$ and N $O_3$$^{[-10]}$ were 27 $\mu$eq/L and 13 $\mu$eq/L for the automatic sampler and 32 $\mu$eq/L and 17 $\mu$eq/L for the manual sampler, respectively. Although the concentrations of the acidifying ions of nss-S $O_4$$^{2-}$ and N $O_3$$^{[-10]}$ were about 3 times higher than those for foreign pristine sites, precipitation acidity were estimated to be natural due to the neutralization reaction of the alkaline species of N $H_4$$^{+}$ and nss-C $a^{2+}$ with its higher concentrations. Considering the ratios of nss-S $O_4$$^{2-}$/N $O_4$$^{[-10]}$ nss-S $O_4$$^{2-}$, it was found that ammonium sulphate was dominant in Iksan precipitation. The major non-sea salt ions were maximum concentrations for March, but decreased with increasing of precipitation amount.on amount.

• 한국환경과학회지
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• 제13권5호
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• pp.469-478
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• 2004

Atmospheric bulk (wet and dry) samples were monthly collected in an urban environment (Daeyeon-dong) of Busan over a year, to assess the deposition flux and seasonality of dioxin-like polychlorinated biphenyls (DLPCBs) using stainless steel pots. Deposition fluxes of DLPCBs in bulk samples were determined using high resolution gas chromatography coupled to high resolution mass spectrometry (HRGC/HRMS). Particle deposition fluxes in the urban environment varied from 23 to 98 $mg^2$/year (mean 41 $gm^2$/year). DLPCB deposition fluxes in atmospheric bulk samples ranged from 0.09 to 0.77 ng-$TEQ/m^2$/year (mean 0.35 ng-$TEQ/m^2$/year). Seasonal atmospheric deposition fluxes of DLPCBs were high in winter and low in summer. Atmospheric deposition fluxes of particles and DLPCBs in this study were comparable to or slightly lower values than those of different locations in the world. Monthly DLPCB profiles in deposition bulk samples were similar over a year. Non-ortho PCBs were higher contributions to the total DLPCBs fluxes than mono-ortho PCBs. In particular, PCB 126 had the highest concentrartion (>75%) in all deposition samples, followed by PCB 169 and PCB 156. A highly positive correlation was found among the deposition fluxes of DLPCB species, suggesting the possibility of that the DLPCB contamination originated from one source. The deposition fluxes of DLPCBs were not significantly correlated with temperature and the amount of precipitation even though the summer season with the highest temperature and the largest amount of precipitation showed the lowest DLPCB deposition flux.

• 한국분말재료학회지
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• 제13권3호
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• pp.178-186
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• 2006

The effect of use of $H_2O$ as PCA(process control agent) to prevent the carbon contamination during mechanical alloying process and the precipitation behavior in Ni-20Cr-20Fe-5Nb bulk alloy after aging were investigated. NbC and $Cr_2O_3$ were formed during mechanical alloying and consolidation processes in the Ni-20Cr-20Fe-5Nb alloy in which methanol($CH_3OH$) was added as PCA. Formation of NbC in this alloy decreased the amount of Nb dissolved in the Ni matrix. The use of $H_2O$ as PCA in Ni-20Cr-20Fe-5Nb alloy prevented the formation of NbC and increased the hardness. The increase of hardness in this alloy was attributed to the increased amount of Nb dissolved in the Ni matrix. After aging treatment for 20 hours at $600^{\circ}C\;and\;720^{\circ}C$ of Ni-20Cr-20Fe-5Nb bulk alloy in which $H_2O$ added as PCA, ${\gamma}"$$(Ni_3Nb,\;tetragonal)\;and\;{\delta}\;(Ni_3Nb,\;orthorhombic)$ precipitates were formed, respectively. The precipitation temperatures of ${\gamma}"$ and ${\delta}$ in this bulk alloy were lower than those in commercial IN 718 alloy. It seemed that the lower precipitation temperatures for ${\gamma}"$ and ${\delta}$ in this bulk alloy than in commercial IN 718 alloy were due to severe plastic deformation during mechanical alloying.

• 한국재료학회지
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• 제14권1호
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• pp.9-12
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• 2004

Metallic impurities, such as Fe, Cu, and Au, become generation and recombination centers for minority carriers when combined with oxide precipitates or silicon self-interstitial clusters. As these centers may cause leakage and discharge in silicon devices, their prevention through gettering of the metallic impurities is an important issue. In this article, key aspects of intrinsic gettering, such as oxygen control, wafer cleaning, device area denudation, and bulk oxygen precipitation are discussed, and a practical method of implementing intrinsic gettering is outlined.

• 한국결정성장학회지
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• 제24권6호
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• pp.246-251
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• 2014

최근 태양전지의 효율을 증가시키기 위한 연구가 많이 이루어지고 있으며, 특히 단결정 실리콘 웨이퍼의 경우 높은 효율을 낼 수 있는 소재로써 고효율 태양전지연구에 많이 이용되고 있다. 본 연구에서는 단결정으로 Czochralski(Cz)-Si 성장 시 산소농도를 다르게 하여 산소석출결함의 변화와 그에 따른 셀효율과의 관계를 비교하였다. 산소불순물은 Cz법으로 성장시킨 실리콘의 주된 불순물이다. 산소불순물 존재 시 태양전지 공정에서 산소석출결함이 생성되며 발생된 산소석출결함은 셀효율에 악영향을 미치게 된다. 그러므로 고효율 태양전지를 위한 웨이퍼를 생산하기 위한 산소석출결함 밀도와 셀효율의 상관성을 연구하였다. 또한 산소농도에 따른 산소석출결함을 분석하여 산소석출결함이 발생되지 않는 잉곳 내 산소농도 범위를 연구하여 14.5 ppma 이하에서 Bulk Micro Defect(BMD)가 발생하지 않음을 확인하였다.

• 공업화학
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• 제9권6호
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• pp.846-851
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• 1998

w/o 에멀젼 내에서 균일용액침전반응을 진행시켜 산화아연 미세 입자를 제조하는 실험적 연구를 수행하였다. 질산아연 수용액에 hexamethylene tetramine (HMTA)을 침전제로 첨가한 침전액은 유화제 Span 80에 의해 kerosine과 안정한 w/o 에멀젼을 형성하였다. 얻어진 w/o 에멀젼을 HMTA 분해온도 이상($85^{\circ}C$)으로 가열하여 w/o 에멀젼 내에서 균일용액 침전반응을 진행시키면 산화아연 입자들이 제조되는 것을 확인하였다. 이렇게 제조된 산화아연 입자들은 이중분산 (bi-modal distribution)을 갖는 영역이 존재하기도 하였으나, 균일용액침전법에 비하여 높은 초기 아연농도와 높은 수율에서도 입자가 작고 입도분포가 비교적 좁은 산화아연 입자들을 얻을 수 있었다.

• Ocean and Polar Research
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• 제27권3호
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• pp.237-250
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• 2005

To investigate the air mass modification related with Yeongdong Heavy snowfall events, we examined sensible and latent heat fluxes on the East Sea, the energy exchange between atmosphere and ocean in this study. Sensible and latent heats were calculated by a bulk aerodynamic method, in which NCEP/NCAR reanalysis data and NOAA/AVHRR weekly SST data with high resolution were used. Among winter precipitation events in the Yeongdong region, 19 heavy precipitation events $(1995{\sim}2001)$ were selected and classified into three types (mountain, cold-coastal, and warm types). Mountain-type precipitation shows highly positive anomalies of sensible and latent heats over the southwestern part of the East Set When separating them into the two components due to variability of wind and temperature/ specific Humidity, it is shown that the wind components are dominant. Cold-coastal-type precipitation also shows strong positive anomalies of sensible and latent heats over the northern part and over the central-northern part of the East Sea, respectively. It is shown that the sensible heat anomalies are caused mostly by the decrease of surface air temperature. So it can be explained that cold-coastal-type precipitation is closely related with the air mass modification due to cold air advection over warm ocean surface. But in warm-type precipitation, negative anomalies are found in the sensible and latent heat distributions. From this result, it may be postulated that warm-type precipitation is affected by the internal process of the atmosphere rather than the atmosphere-ocean interaction.