• Journal of Korean Society for Atmospheric Environment
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• 제21권E3호
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• pp.75-85
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• 2005

A mathematical sensitivity analysis of the flow-through dynamic flux chamber technique, which has been utilized usually for various trace gas flux measurement from soil and water surface, was performed in an effort to provide physical and mathematical understandings of parameters essential for the NO flux calculation. The mass balance equation including chemical reactions was analytically solved for the soil NO flux under the steady state condition. The equilibrium concentration inside the chamber, $C_{eq}$, was found to be determined mainly by the balance between the soil flux and dilution of the gas concentration inside the chamber by introducing the ambient air. Surface deposition NO occurs inside the chamber when the $C_{eq}$ is greater than the ambient NO concentration ($C_{0}$) introducing to the chamber; NO emission from the soil occurs when the $C_{eq}$ is less than the ambient NO concentration. A sensitivity analysis of the significance of the chemical reactions of NO with the reactive species (i.e. $HO_{2},/CH_{3}O_{2},/O_{3}$) on the NO flux from soils was performed. The result of the analysis suggests that the NO flux calculated in the absence of chemical reactions and wall loss could be in error ranges from 40 to $85\%$ to the total flux.

• 한국토양비료학회지
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• 제45권6호
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• pp.1179-1186
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• 2012

For better understanding of carbon cycle dynamics of an agro-ecosystem, an accurate assessment of seasonal and daily $CO_2$ flux is essential to understand the relationship between various environmental factors and crop productivity. We developed the automatic sliding canopy chamber (ASCC) system that measured continuous net ecosystem productivity (NEP) over whole growing season under the natural meteorological rhythm. The ASCC was composed of two main parts which were sliding part for measuring NEP, and automatic opening and closing chamber (AOCC) for measuring soil respiration (SR) on the soil surface. The ASCC was developed by using open flow method for measuring soil $CO_2$ efflux. The disturbance of natural meteorological condition was minimized by opening the base frames. In the field test with barley (Hordeum vulgare L.), NEP was calculated at $140mg\;CO_2\;m^{-2}h^{-1}$ on a clear day using continuous data and eliminated the possibility of overestimate about 16% using one hour data during the day time. Unlike other small scale chamber system, installation on cropping-field made it possible to take any modifications which might be caused by natural environmental condition.

• 한국대기환경학회지
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• 제20권6호
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• pp.749-758
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• 2004

Nitrous oxide ($N_2$O) has been known as an important trace gas due to the greenhouse gas and the major source of stratospheric oxide of nitrogen (NO). Soil is the major source of $N_2$O in nature. The physicochemical characteristics of soils affect the emission of $N_2$O from soil. These physicochemical parameters are soil moisture, soil temperature, and soil N content. Since these parameters are correlated to the flux of $N_2$O from soil individually and compositely, there still remain many unknowns in the mechanism to produce $N_2$O in soil and the roles of such physicochemical parameters which affect the soil $N_2$O emission. Soil $N_2$O fluxes were measured at different levels in water filled pore space (WFPS), soil temperature and soil N contents from the same amounts of soils which were sampled from agriculturally managed upland field in a depth of ～30 cm at Kunsan. The soil $N_2$O flux measurements were conducted in a laboratory with a closed flux chamber system. The optimum soil moisture and soil temperature were observed at 60% of WFPS and ～13$^{\circ}C$. The soil $N_2$O flux increased as soil N contents increases during the whole experimental hours (up to 48 hours). However, average $N_2$O flux decreased after ～30 hours when organic carbon was mixed with nitrogen in the sample soils. It is suggested that organic carbon could be important for the emission of $N_2$O, and that the ratio of N to C needs to be identified in the process of $N_2$O soil emission.

• 한국조경학회지
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• 제35권2호통권121호
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• pp.49-54
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• 2007

This research was performed to investigate the effect of formaldehyde removal and confirm the utility of plants as indoor environment improvement systems. The plant materials used in this study were Fatsia japonica, Ardisia japonica, Ardisia pusilla and Davallia mariesii. Plants were placed in an airtight chamber under artificial formaldehyde. The initial formaldehyde concentration in the chamber was $500{\pm}30ppb$, and the conditions of $1,500{\sim}2,000lux$ light, $25{\pm}5^{\circ}C$ temperature and $80{\sim}90%$ humidity were maintained. Each chamber was treated as no plant, plant-only and Plant+soil. The total leaf number for Davallia mariesii, Ardisia japonica, Ardisia pusilla, and Fatsia japonica was 40.8, 48.6, 62.3, and 11.8 respectively. The total leaf space n of those plant materials were $2,385cm^2,\;1,252cm^2,\;2,468cm^2\;and\;1,262cm^2$ respectively. The formaldehyde concentration was reduced to $80{\sim}90%$ of the initial concentration in plant-only and Plant+Soil treatment chamber of all species in 12 hours. In the plant-only chamber, Fatsia japonica had removed formaldehyde density by 95% after 12 hours while Ardisia japonica had removed 90%. In the case of Ardisia pusilla, the early removal rate was higher in the plant-only treatment chamber than the Plant+Soil treatment chamber. The formaldehyde removal rate of Davallia mariesii was 98% after 12 hours. In the Plant+Soil treatment chamber, the amount of removal of formaldehyde per time of Davallia mariesii, Ardisia japonica, Ardisia pusilla, and Fatsia japonica was 20.42ppb/hr, 16.28ppb/hr, 2.5.42ppb/hr, 10.28ppb/hr respectively. In the plant-only, That was 22.50ppb/hr, 20.97ppb/hr, 20.83ppb/hr, 20.97ppb/hr respectively.

• 한국토양환경학회지
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• 제3권3호
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• pp.75-86
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• 1998

쓰레기매립장에서 복토층을 통하여 대기중에 유출하는 가스를 현장에서 단시간내에 측정이 가능한 밀폐형 chamber법을 제시하였다. 또한, 최종복토층에서의 유출가스 실측치를 모델해석으로 모사하여 다음의 결과를 얻었다. 1) 시간변화에 따른 chamber내(H=10-30 cm)의 농도 변화는 30분이내로, G.C의 분석시간을 고려하여 5분단위로 분석한다. 2)메탄산화 반응의 영향으로 $CH_4$/$CO_2$비가 복토층 표면근처에서 급격히 변화한다. 3)매립지 표면의 flux가 F =$10^{-5}$mol/($m^2$.s)일 경우에는 메탄산화반응에 의해 가스조성에의 영향이 있으나, F =$10^{-6}$moll($\textrm{m}^2$.s)의 경우에는 복토층내의 메탄가스 농도가 상대적으로 적으므로 메탄산화반응에의 영향이 적다.

• 헤리티지:역사와 과학
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• 제42권3호
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• pp.66-87
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• 2009

적석목곽묘는 목곽 외부에 석재를 쌓거나 채운 다음 목개 위에 일정한 두께로 적석하고 점토로 밀봉한 구조이다. 경주 중심부라는 한정된 공간 속에 거의 모든 지배자가 지속적으로 한 묘제를 사용하였다는 점, 타 지역에서 확인되는 적석 형태와 전혀 다르다는 점 등에서 경주식 적석목곽묘로 정의하고자 한다. 적석목곽묘는 경주 중심부에서 5C 전반대부터 축조되기 시작한다. 평면형태, 목곽, 이중곽, 석재충전, 석단, 순장 등은 이전시기의 목곽묘에서 계보를 잇고 있다. 이외에 석축과 목주, 적석, 성토분구는 적석목곽묘의 출현과 함께 새롭게 나타나는 요소이다. 특히 석축과 목주는 황남대총을 비롯한 지상식 초대형분에서만 확인된다. 석축과 목주, 적석은 모두 성토 분구 축조과정 속에서 하나의 공정을 이루고 있다. 석축은 지상에 설치된 목곽의 외벽을 견고하게 유지시켜 주면서 성토 분구의 하중을 분산 수용한다. 목주는 석축의 붕괴를 방지하기 위한 보조장치로서 횡가목, 버팀목 등과 함께 사용되었다. 적석은 일정 크기의 석재를 갖고 일정한 두께로 목개 상부에 덮었다. 그리고 그 위에 점토로 밀봉한 다음 분구를 성토하였다. 적석은 경주지역의 입지적 특성이 반영된 것으로 파악된다. 경주 중심부의 적석목곽묘는 하천부지가 넓고 평탄한 형산강 동안을 따라 분포한다. 기반층은 대부분 모래와 냇돌로 구성되어 있다. 따라서 성토분구는 모래성분을 많이 함유하고 있다. 목개를 횡가한 다음 바로 성토할 경우 유수에 의한 붕괴 가능성 또한 크다. 고분의 외형을 유지하면서 내부구조물의 파괴를 방지하기 위하여 적석과 점토밀봉이 이루어진 것으로 판단된다. 상부의 봉토가 유실되더라도 하부의 적석은 형태를 어느 정도 유지할 것이기 때문이다. 성토분구는 국가 혹은 단위정치체가 성장단계에 진입하면서 나타나는 하나의 특징이다. 국가 출현단계 이후 성장단계에 진입하면서 사회구조에 변화가 나타나고 이와 맞물려 새롭게 출현한 지배등급에서 전대의 목곽묘와는 다른 적석목곽묘를 축조하기 시작한 것으로 판단된다. 이 과정에서 분구를 함께 성토한 것으로 파악되며, 지배등급의 성격에 따라 규모와 구조에서 차이를 보인다. 평면형태, 곽과 석단, 순장자의 수, 유물의 양과 질 등은 지배등급의 사회적 지위를 반영하고 있다. 따라서 적석목곽묘는 신라가 성장단계에 접어든 시점에 전대의 묘제로부터 분화 발전된 양상을 보이면서 나타난것으로 생각된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2008년도 추계 학술발표회
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• pp.1278-1284
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• 2008

This study carried out bender element tests in a calibration chamber in order to estimate the characteristics of soil specimen prepared in a calibration chamber. Basically, the purpose of bender element test is to measure the shear wave velocity. Bender element test cannot only confirm the status of soil specimen deposited in a chamber, but also estimate the consolidation process indirectly. In order to carry out bender element test in a calibration chamber, a pair of bender elements was installed inside the chamber, using the 'ㄷ' shaped frame. For the sandy soils having various relative densities in various stress conditions, the maximum shear modulus was estimated. From the comparison with bender element test results in a triaxial testing device, testing device and procedure was validated.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2002년도 봄 학술발표회 논문집
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• pp.673-678
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• 2002

Laboratory calibration chamber tests for cone penetrometers, pressuremeters and dilatometers in cohesionless soil specimens have been conducted by numerous researchers. However, there have been only few applications to compacted or preconsolidated cohesive soils. Therefore, for the first time, Calibration Chamber System was developed in Korea University. This can be attributed to the extremely time consuming and laborious process involved in the preparation of large cohesive soil specimens in addition to other complexities involving instrumentation for pore pressure monitoring and the need for maintaing saturation by back pressure. Chamber System with similar principle as LSU Chamber System was made of more strengthen and complementary form by increasing system diameter(1.2m), carrying out 1st and 2nd consolidation process in one system for smooth and safe work, accurate Data Aquisition.

• 한국측량학회지
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• 제37권6호
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• pp.555-562
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• 2019

본 논문에서는 근접 사진측량에 기반하여 모형 토조 내 지반의 변위를 측정하기 위한 연구를 진행하였다. 알루미늄 프레임 및 투명 아크릴로 제작된 실내 모형 토조 내에 토사를 채워 넣고, 하중 재하 장치를 이용한 하중 재하를 통한 토사의 변위를 사진측량 기법으로 측정하였다. 토조 내의 토사는 영상 기반 자동 매칭을 위하여 검은 모래 약 40%, 일반 모래 약 60% 혼합하여 영상 대비의 정도를 높일 수 있도록 계획하였다. 전처리 과정으로서 실험실 카메라 캘리브레이션을 통해 내부표정요소를 도출하였고, 토조 프레임에 배치된 기준점을 이용한 후방교회법을 통해 외부표정요소를 예측하였다. 이후 영상 매칭을 통해 하중 전, 후의 토사 변위 패턴을 측정하였으며, 영상 매칭 시 활용되는 매칭 윈도우 크기 및 영상 스무딩 정도를 변경 적용하여 그 결과를 평가해보았다. 실험 결과, 매칭 윈도우 크기 65×65픽셀의 경우 안정적인 변위 도출이 가능하였으며, 영상 스무딩은 매칭의 과대 오차를 감소하는 효과를 보여주었다. 이를 통해 사진 측량을 통한 토조 내 지반 변위 패턴을 도출할 수 있었다.

• 한국대기환경학회지
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• 제29권6호
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• pp.789-800
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• 2013

$N_2O$ and $CH_4$, Greenhouse gas emission, Forest soil, Closed chamber technique, Soil uptake $N_2O$ and $CH_4$ are important greenhouse gases (GHG) along with $CO_2$ influencing greatly on climate change. Their soil emission rates are highly affected by bio-geo-chemical processes in C and N through the land-atmosphere interface. The forest ecosystems are generally considered to be net emission for $N_2O$; however, net sinks for $CH_4$ by soil uptake. Soil $N_2O$ and $CH_4$ emissions were measured at Mt. Taewha in Gwangju, Kyeonggi, Korea. Closed chamber technique was used for surface gas emissions from forest soil during period from May to October 2012. Gas emission measurement was conducted mostly on daytime (from 09:00 to 18:00 LST) during field experiment period (total 25 days). The gas samples collected from chamber for $N_2O$ and $CH_4$ were analyzed by gas chromatography. Soil parameters were also measured at the sampling plot. GHG averages emissions during the experimental period were $3.11{\pm}16.26{\mu}g m^{-2}hr^{-1}$ for $N_2O$, $-1.36{\pm}11.3{\mu}gm^{-2}hr^{-1}$ for $CH_4$, respectively. The results indicated that forest soil acted as a source of $N_2O$, while it acted like a sink of $CH_4$ on average. On monthly base, means of $N_2O$ and $CH_4$ flux during May (spring) were $8.38{\pm}48.7{\mu}gm^{-2}hr^{-1}$, and $-3.21{\pm}31.39{\mu}gm^{-2}hr^{-1}$, respectively. During August (summer) both GHG emissions were found to be positive (averages of $2.45{\pm}20.11{\mu}gm^{-2}hr^{-1}$ for $N_2O$ and $1.36{\pm}9.09{\mu}gm^{-2}hr^{-1}$ for $CH_4$); which they were generally released from soil. During September (fall) $N_2O$ and $CH_4$ soil uptakes were observed and their means were $-1.35{\pm}12.78{\mu}gm^{-2}hr^{-1}$ and $-2.56{\pm}11.73{\mu}gm^{-2}hr^{-1}$, respectively. $N_2O$ emission was relatively higher in spring rather than other seasons. This could be due to dry soil condition during spring experimental period. It seems that soil moisture and temperature mostly influence gas production and consumption, and then emission rate in subsoil environment. Other soil parameters like soil pH and chemical composition were also discussed with respect to GHG emissions.