• Journal of Korean Society for Atmospheric Environment
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• 제14권E호
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• pp.9-17
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• 1998

Oxides of nitrogen play important roles in atmospheric chemistry. Soil has been recognized as a major natural source of NO, and its emission depends on soil parameters such as soil nitrogen availability, soil moisture and temperature. It is necessary to understand effects of these controlling parameters on soil NO emission. In order to understand soil moisture effects on NO emission, variations of NO concentration and existence of its equilibrium concentration were observed from ammonium fertilized Japanese upland soil prepared for different soil moisture conditions. The closed chamber technique was employed for this study. The significant increases in NO with soil moisture were found. Maximum was occurred at sample ID4 (55% of water-filled pore space (WFPS)), but it decreased as soil moisture increased. No significant NO concentration was emitted from soil sample without fertilizer, but there was significant NO in fertilized soil samples. The magnitudes of NO from soil increased with time and reached at steady state within ten minutes approximately. These results suggest that nitrogen input from fertilizer takes charge in the first step of sharp increase in NO emission, and then soil moisture becomes important factor to control NO emission from the soils. NO concentrations from soil were compared to those one-day after the experiment. Results from the comparison analysis suggest that the soil NO flux might have been stimulated by soil disturbances like mixing, and this is much more effective in dry soils rather than in wet soils. It was found that much less NO came out from soils after a day; suggesting that most of NO was released from the soils within a day after fertilizer application during our experiment. The length of NO releasing time span may depend on the amounts of fertilizer applied, soil moisture condition, and other soil physical parameters.

• 자원리싸이클링
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• 제7권4호
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• pp.27-34
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• 1998

본 연구에서는 NiCuZn Ferrite(NCZF) 제조공정의 제어에 대하여 연구하였다. $700^{\circ}C$, 3시간 하소한 NCZF를 약 60시간 볼밀링하여 약 $0.5\mu\;extrm{m}$ 입자크기로 분쇄한 후 분무 건조하여 과립화하였다. NCZF의 충전율에 따른 겉보기 고화속도 및 초기투자율에 미치는 영향을 조사한 결과 다음과 같은 결과를 얻었다. 1. 성형압력 유지시간 1분에서 성형압력을 약 20~170 ㎫로 변화시켜 제조한 NCZF 토로이달 상의 출발시편은 성형압이 증가하면서 입자의 충전율은 48.6%에서 56.8%로 증가하였다. 2. 일정 소성온도에서 NCZF의 충전율이 높아질수록 고화속도가 높아지고, 일정 성형압력에서 소성온도가 높아질수록 NCZF의 겉보기 고화속도는 빨라졌다. NCZF의 충전율과 소성온도가 높고, 소성시간이 길어지면 bulk density는 증가하였다. 3. 고정된 조성에서 소성온도($875~925^{\circ}C$)와 소성시간(0~5시간)의 조합에 의해 제조된 NCZF의 초기투자율은 bulk density와 semi-log상에서 직선적인 비례관계를 가지며 NCZF입자의 충전율에 크게 의존하였다. NCZF입자의 충전율과 이들을 소성하였을 때의 bulk density를 알면 초기투자율을 예측할 수 있었다. log $\mu$i=$G1{\times}BD$+$G2{\times}충전율$+b(0), G1;0.8394, G2;-3.6233, (b);0.7053.

• 한국세라믹학회지
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• 제53권1호
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• pp.43-49
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• 2016

This analyzed a Young's modulus (E), a thermal expansion coefficient (TEC, ${\beta}$) and a thermal conductivity (${\kappa}$) of the material with simple cubic particulate inclusion using two model structures: a parallel structure and a series structure of laminated layers. The derived ${\beta}$ equations were applied to calculate the ${\beta}$ value of the W-MgO system. The accuracy was higher for the series model structure than for the parallel model structure. Young's moduli ($E_c$) of sintered porous alumina compacts were theoretically related to the development of neck growth of grain boundary between sintered two particles and expressed as a function of porosity. The series structure model with cubic pores explained well the increased tendency of $E_c$ with neck growth rather than the parallel structure model. The thermal conductivity of the three phase system of alumina-mullite-pore was calculated by a theoretical equation developed in this research group, and compared with the experimental results. The pores in the sintered composite were treated as one phase. The measured thermal conductivity of the composite with 0.5-25% porosity (open and closed pores) was in accordance with the theoretical prediction based on the parallel structure model.

• 대한의용생체공학회:의공학회지
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• 제19권3호
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• pp.215-224
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• 1998

본 논문은 급성 간 부전 환자나 간이식 대기상태에 있는 환자에 이용하기 위한 체외 간 보조장치를 개발하기 위한 기초 실험에 관한 것이다. 밀도 33kg/m, 평균 직경 500um, 60-70%의 window를 가진 폴리우레탄 폼을 15% NCO-프리폴리머로 제조하였다. 폴리우레탄 폼에 접종된 간세포는 3일 후에 거의 모두 100-150um 크기의 구상체를 형성하였다. BSA 코팅을 한 폴리우레탄 폼은 BSA로 코팅하지 않은 폴리우레탄 폼보다 간세포 구상체 형성 시간이 더 짧았다. 폴리우레탄 폼에 형성된 간세포 구상체의 간 기능을 증명하기 위하여 암모니아 제거율과 요소 및 알부민 분비율을 측정하였다. 폴리우레탄 폼은 간세포 구상체 배양에 적합하며, 폴리우레탄 폼 내에서의 간세포 구상체 배양은 체외 간 보조장치로의 개발 가능성이 높다.

• 한국전기전자재료학회논문지
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• 제15권5호
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• pp.406-411
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• 2002

Ni-Zn ferrite is required to have predominant and stable characteristics in the range of high frequency for the power line communication, so that microstructures and magnetic properties such as power loss and initial permeability in $Ni_{0.8}Zn_{0.2}Fe_2O_4$ were investigated in terms of variable $Bi_2O_3,CaO$ and $V_2O_5$ contents. $Bi_2O_3$ and $V_2O_5$ liquid phase created during sintering process promoted sintering and grain growth but much of the closed pore existed in the grains. The grain size of the specimens with $V_2O_5$ of over 0.5 wt% decreased as the result of "pinning effect"and the resonance frequency increased with CaO of 0.3we%. The high initial permeability of 81.52%, resonance frequency of 17.05 MHz and low power loss of 17,858 kW/$\textrm{m}^3$ were obtained from the samples with $Bi_2O_3$ of 0.5, CaO of 0.3, and $V_2O_5$ of 0.7 wt%.

• Nuclear Engineering and Technology
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• 제34권4호
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• pp.323-330
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• 2002

Various types of compounds were tested with the aspects of decomposition and formation of residue in a $CO_2$ or 7H$_2$+93$N_2$ atmosphere. The evaporation temperature range of each compound was determined from thermogravimetric curve. Decomposition of dicarbon amide, stearic acid, acrowax and zinc stearate was studied by thermogravimetry in $CO_2$ or in 7H$_2$+93$N_2$ atmosphere. All compounds were decomposed in $CO_2$ atmosphere at lower than 40$0^{\circ}C$, but the residue, ZnO remained for zinc stearate. ZnO did not decompose in $CO_2$ atmosphere up to 130$0^{\circ}C$, but reduced into Zn metal and disappeared in the temperature range of $600^{\circ}C$ to 120$0^{\circ}C$ in 7H$_2$+93$N_2$ atmosphere. The effect of residue, which trapped in closed pores of sintered pellet, on the thermal stability was studied using the resintering test at 1$700^{\circ}C$ in 7H$_2$+93$N_2$ atmosphere. In the case of oxidative sintered pellet with admixing zinc stearate, the cavity formation accompanied with a density drop after resintering is due to the pressure of the Zn gases trapped in the isolated pores.

• 한국산림과학회지
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• 제102권3호
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• pp.315-322
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• 2013

이 연구는 하동 송림 내 토양과 입지특성을 분석하고, 이용자들에 대하여 설문 조사를 실시함으로써 향후 송림의 토양복원 및 합리적 관리방안을 제시하고자 수행하였다. 하동 송림에서 평균토양용적밀도는 휴식년제지역($1.39g/cm^3$)이 비휴식년제지역($1.31g/cm^3$)보다 약간 높게 나타났다. 하동 송림의 휴식년제 지역에서 산책길의 토양용적밀도($1.74g/cm^3$)는 임내($1.39g/cm^3$)보다 약 1.3배 높은 값을 나타내었으며, 토양의 공극률은 산책길(34.6%)이 임내(47.7%) 보다 1.4배 낮았다. 비휴식년제지역에서 산책길의 토양용적밀도($1.53g/cm^3$)는 임내($1.31g/cm^3$)보다 약 1.2배 높았으며, 토양의 공극률은 송림의 산책길(42.6%)이 임내(50.5%) 보다 1.2배 낮은 값으로 나타났다. 또한 하동 송림(산책길)에서 토양의 공극률은 휴식년제지역(34.6%)이 비휴식년제지역(42.6%)보다 낮게 나타났다. 송림 지표토양의 토양경도는 휴식년제지역, 비휴식년제지역은 각각 10.5, $8.5kgf/cm^2$로 토양용적밀도의 결과와 유사한 결과를 나타내었다. 송림의 토양 화학성(토성, 토양pH, 유기물함량, 전질소, 양이온치환용량, 치환성양이온)은 식물이 성장하는데 영향을 미치는 적정함량에 부족한 것으로 나타났다. 송림을 탐방하는 이용자들은 휴양 및 경관조망이 주를 이루고 있고, 송림의 소나무 숲 생태계를 유지 보전하기 위한 관리를 위해서 휴식년제의 실시와 아울러 음주가무, 흡연, 오물투기 등 송림에서 행해지는 이러한 사항에 대한 단속 및 금지에 대한 교육이 필요한 것으로 응답하였다. 설문 응답자들은 현재 송림의 소나무 숲 생태계는 비교적 양호하다고 판단하지만 소나무 숲 생태계를 보전하기 위한 보다 적극적인 관리와 아울러 소나무숲 하층식생으로 자생종 화본과식물의 도입을 요구하는 것으로 나타났다.

• 열처리공학회지
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• 제32권5호
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• pp.201-211
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• 2019

Low carbon steel (S20C steel) and SPCC steel sheet have been austenitic nitrided at $700^{\circ}C$ in a closed pit type furnace by changing the flow rate of ammonia gas and heat treating time. When the flow rate of ammonia gas was low, the concentration of residual ammonia appeared low and the hardness value of transformed surface layer was high. The depth of the surface layer, however, was shallow. With increasing the concentration of residual ammonia by raising up the ammonia gas flow, both the depth of the surface layer and the pore depth increased, while the maximum hardness of the surface layer decreased. By introducing a large amount of ammonia gas in a short time, a deep surface layer with minimal pores on the outermost surface was obtained. In this experiment, while maintaining 10~12% of residual ammonia, the flow rate of inlet ammonia gas, 7 liter/min, was introduced at $700^{\circ}C$ for 1 hour. In this condition, the thickness of the surface layer without pores appeared about $60{\mu}m$ in S20C steel and $30{\mu}m$ in SPCC steel plate. Injecting additional methane gas (carburizing gas) to this condition played a deteriorating effect due to promoting the formation of vertical pores in the surface layer. For $1^{st}$ transformed surface layer for S20C steel, maintaining 10~12% residual ammonia condition via austenitic nitriding process resulted in ${\varepsilon}$ phase with relatively high nitrogen concentration (just below 4.23 wt.%N) among the mixed phases of ${\varepsilon}+{\gamma}$. The ${\varepsilon}$ phase was formed a specific orientation perpendicular to the surface. For $2^{nd}$ transformed layer for S20C steel, ${\gamma}$ phase was rather dominant (just above 2.63 wt.%N). For SPCC steel sheet, there appeared three phases, ${\gamma}$, ${\alpha}(M)$ and weak ${\varepsilon}$ phase. The nitrogen concentration would be approximately 2.6 wt.% in these phases condition.

• 한국세라믹학회지
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• 제39권3호
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• pp.259-264
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• 2002

본 연구에서는 석탄회로 제조된 인공경량골재에 석회석을 첨가하였을 때 소성온도 및 시간에 따른 소성특성을 관찰하였다. 소성온도의 증가에 따라 quartz($SiO_2$)가 감소한 반면 mullite($3Al_2O_3{\cdot}2SiO_2$)가 증가되었으며, 석회석의 첨가에 의해 clinoptiolite와 pagioclase와 같은 소성에 의한 소성광물이 생성되었다. 석탄회 및 석회석으로 제조된 경량골재의 소성성은 주로 소성시간보다는 소성온도에 의해서 좌우되는 것으로 확인되었다. 또한 소성온도 및 시간의 증가는 골재내 형성된 거대기공의 미세화 및 폐기공의 형성으로 전체 기공부피를 축소시키는 경향을 나타냈다. 1000$^{\circ}$C에서 5분가 소성시킨 경량골재의 표면은 용융 슬래그 층의 융착현상에 의해 개기공이 거의 없었으나 내부는 발포가스에 의해 수 ${\mu}$의 미세기공이 폐기공 형태로 균일하게 분포하였다. 이로부터 석회석이 첨가된 소성 경량골재의 적정 소성조건은 소성온도는 약 1000$^{\circ}$C, 소성시간은 5분이 바람직한 것으로 나타났다.

• 한국대기환경학회지
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• 제27권3호
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• pp.313-325
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• 2011

From October 2009 to June 2010, major greenhouse gases (GHG: $N_2O$, $CH_4$, $CO_2$) soil emission were measured from upland cabbage field at Kunsan ($35^{\circ}$56'23"N, $126^{\circ}$43'14"E), Korea by using closed static chamber method. The measurements were conducted mostly from 10:00 to 18:00LST during field experiment days (total 28 days). After analyzing GHG concentrations inside of flux chamber by using a GC equipped with a methanizer (Varian CP3800), the GHG fluxes were calculated from a linear regression of the changes in the concentrations with time. Soil parameters (e.g. soil moisture, temperature, pH, organic C, soil N) were also measured at the sampling site. The average soil pH and soil moisture were ~pH $5.42{\pm}0.03$ and $70.0{\pm}1.8$ %WFPS (water filled pore space), respectively. The ranges of GHG flux during the experimental period were $0.08\sim8.40\;mg/m^2{\cdot}hr$ for $N_2O$, $-92.96\sim139.38mg/m^2{\cdot}hr$ for $CO_2$, and $-0.09\sim0.05mg/m^2{\cdot}hr$ for $CH_4$, respectively. It revealed that monthly means of $CO_2$ and $CH_4$ flux during October (fall) were positive and significantly higher than those (negative value) during January (winter) when subsoil have low temperature and relatively high moisture due to snow during the winter measurement period. Soil mean temperature and moisture during these months were $17.5{\pm}1.2^{\circ}C$, $45.7{\pm}8.2$%WFPS for October; and $1.4{\pm}1.3^{\circ}C$, $89.9{\pm}8.8$ %WFPS for January. It may indicate that soil temperature and moisture have significant role in determining whether the $CO_2$ and $CH_4$ emission or uptake take place. Low temperature and high moisture above a certain optimum level during winter could weaken microbial activity and the gas diffusion in soil matrix, and then make soil GHG emission to the atmosphere decrease. Other soil parameters were also discussed with respect to GHG emissions. Both positive and negative gas fluxes in $CH_4$ and $CO_2$ were observed during these measurements, but not for $N_2O$. It is likely that $CH_4$ and $CO_2$ gases emanated from soil surface or up taken by the soil depending on other factors such as background concentrations and physicochemical soil conditions.