• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2000년도 창립총회 및 춘계학술발표회
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• pp.125-128
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• 2000

Recently, development of advanced soil monitoring technology has became essential for effective site remediation. Soil gas evaluation is simple and powerful technology which can reduce the environmental impact during the survey of VOC contaminated area. In this research, the feasibility test of SnO$_2$ceramic gas sensor is conducted to improve soil gas measurement technology. As a result, it is successfully proved that this gas sensor has an possibility for soil gas monitoring.

• 한국가스학회지
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• 제21권1호
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• pp.1-5
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• 2017

독성가스 사고 시 토양 침적은 사고피해범위에 영향을 미치는 주요 변수이다. 본 연구에서는 토양의 깊이 및 유기물 함량 비율이 독성가스 염소의 토양 침적 특성에 미치는 영향을 연구하였다. 실험에 이용된 장치로는 미국의 Air Force Research Laboratory에서 구축한 장치를 벤치마킹하였다. 다양한 합성토양을 이용해 유기물의 함량을 변화시키면서 토양 침적실험을 진행하였다. 다양한 합성토양에 일정 농도의 염소를 노출시킨 후, 염소 침적의 정도를 정량화하기 위해 음이온 크로마토그래피를 이용하여 침적량을 측정하였다. 그 결과, 토양 표면에서의 침적량 변화에 비해 깊이에 따른 침적량의 변화 경향은 볼 수 없었으나, 염소 노출 시간에 따른 표면 침적량의 차이는 증가함을 확인 할 수 있었다. 또한, 유기물 함량에 따른 침적량은 유기물 함량이 증가함에 따라 비례관계를 보였다. 토양 표면에서의 염소 침적량의 증가는 주로 토양 내 유기물 함량에 의존함을 확인하였다.

• 한국토양환경학회지
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• 제3권1호
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• pp.3-9
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• 1998

본 연구는 휘발성 유기 화합물로 오염된 가솔린 지역에서 soil-gas의 분석결과로부터 오염도를 유추하는 기법에 대하여 서술 하였다. Soil-gas의 채취방법으로는 펌프를 이용한 1)grab sampling법과 흡착제 trap을 사용한 2)passive sampling법이 있다. Grab sampling법은 특정시간에 특정장소에서의 오염도를 보여주며, 반면에 passive sampling법은 특정위치에서 시간에 따른 오염도의 변화를 보여 준다. Soil-gas의 분석은 1)PID나 FID와 같은 작은 검지기에 의해서 총괄 탄화수소량을 측정할수도 있고 2)기체농도에 따라서 색깔이 변하는 지시약이 채워진 기체검지기 튜브를 사용할수도 있으며 3)여러가지 화합물을 한 번에 분석할수 있는 이동형 GC를 사용할수도 있다. Soil-gas를 이용한 측정법은 매우 값싸며 세밀한 정밀조사를 하기 위한 전단계에서 사용할 수 있는 유용한 방법으로 추천할만하다 하겠다.

• 한국가스학회지
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• 제3권2호
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• pp.43-52
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• 1999

지하에 매설된 도시가스 배관에서의 누출 가스에 대한 확산 거동을 관찰하기 위하여 지중 확산실험조를 제작하여 실험하였다. 실험조는 도시가스 공급위치와 농도의 측정위치를 변화시킬 수 있도록 acryl로 제작하였으며, MOS 센서를 이용하여 도시가스 농도를 측정하였다. 가스의 지하 확산을 측정하기 위한 토질로서 주문진 표준사와 화강풍화토를 이용하였으며, 가스누출 속도 변화에 따른 도시가스 농도 변화를 시간에 따라 측정하였다. 누출점으로부터 센서의 측정위치가 가까울수록 또는 누출 속도가 증가할수록 가스의 감지시간이 감소하였으며, 누출가스 농도의 빠른 증가로 인하여 정상상태시 높은 농도를 나타내었다. 또한, 주문진 표준사보다 다짐에 의해 밀도가 증가한 화강풍화토에서 초기에 농도가 낮게 측정되었으나, 시간이 지남에 따라 농도가 높게 나타났다.

• 한국산림과학회지
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• 제81권2호
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• pp.177-182
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• 1992

미국 Maine 주 저지대 가문비나무-젓나무 경제림 지역의 spodosol 토양의 2개의 토심(O와 B층)에서 토양공기 $CO_2$ 농도를 측정하였다. $CO_2$ 농도 측정은 Draeger 직독(直讀) chromatography법과 가스주입기를 이용한 gas chromatography 법의 두 가지 방법을 사용하였다. 1991년 생육기 동안의 토양공기 $CO_2$ 농도(%)의 평균값은 Draeger법으로 측정된 O층의 0.11로부터 gas chromatography법으로 측정된 B층의 0.29사이의 분포를 보였다. B층과 O층 모두에서 Draeger법에 의한 토양공기 $CO_2$의 농도가 gas chromatography법으로 측정된 값보다 낮은 수치를 보였다. 두 방법에 의해 측정된 값들 상호간에는 두 층 모두에서 고도의 상관관계 (p<0.01)를 보였으며, 시간변화에 따른 변화 유형 역시 평행적인 관계를 보여 주었다. 토양공기 $CO_2$ 농도는 토양온도와 고도의 정의 상관관계를 보였는데 상관계수의 값은 선발된 측정방법 및 토층에 따라 0.13-0.32의 값을 나타냈다.

• 한국대기환경학회지
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• 제23권2호
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• pp.225-241
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• 2007

A closed flux chamber system was used for measuring major greenhouse gas (GHG) emission from tideland and/or wetland soils in estuarine area at Saemankum, Kunsan in southwestern Korea during from months of February to June 2006. Hourly averaged GHG soil emissions were measured two to three times a day during the ebb tide hours only. Site soils were analyzed for soil parameters (temperature, pH, total organic contents, N and C contents in soil) in the laboratory. Soil GHG fluxes were calculated based on the GHG concentration rate of change measured inside a closed chamber The analysis of GHG was conducted by using a Gas Chromatography (equipped with ECD/FID) at laboratory. Changes of daily, monthly GHGs' fluxes were examined. The relationships between the GHG emissions and soil chemical contents were also scrutinized with respect to gas production and consumption mechanism in the soil. Soil pH was pH $7.47{\pm}0.49$ in average over the experimental period. Organic matter contents in sample soil was $6.64{\pm}4.98\;g/kg$, and it shows relatively lower contents than those in agricultural soils in Kunsan area. Resulting from the soil chemistry data, soil nitrogen contents seem to affect GHG emission from the tidal land surface. The tidal soil was found to be either source or sink for the major GHG during the experimental periods. The annual average of $CH_{4}\;and\;CO_{2}$ fluxes were $0.13{\pm}0.86\;mg\;m^{-2}h^{-1}\;and\;5.83{\pm}138.73\;mg\;m^{-2}h^{-1}$, respectively, which will be as a source of these gases. However, $N_{2}O$ emission showed in negative flux, and the value was $-0.02{\pm}0.66\;mg\;m^{-2}h^{-1}$, and it implies tidal land surface act as a sink of $N_{2}O$. Over the experimental period, the absolute values of gas fluxes increased with soil temperature in general. Averages of the ambient gas concentration were $86.8{\pm}6.\;ppm$ in $CO_{2},\;1.63{\pm}0.34\;ppm\;in\;CH_{4},\;and\;0.59{\pm}0.15\;ppm\;in\;N_{2}O$, respectively. Generally, under the presence of gas emission from agricultural soils, decrease of gas emission will be observed as increase in ambient gas concentration. We, however, could not found significant correlation between the ambient concentrations and their emissions over the experimental period. There was no GHG compensation points existed in tide flat soil.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.377-380
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• 2004

To identify the effect of landfill waste for groundwater and unsaturated air environment, soil gas survey and hydrogeochemical study were executed. The geology of the study area is granite and aquifer is mainly composed of sandy soil. The results of spatial distribution from soil gas showed the boundary of buried waste and processes and degree of waste decomposition. Groundwater contamination by leachate from landfill is controlled by groundwater flow attributed by the original topography and liner.

• Environmental Analysis Health and Toxicology
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• 제16권3호
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• pp.121-126
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• 2001

Analytical method of benzophenone (BP) in sediment and soil was developed by gas chromatography/mass selective detector/selected ion monitoring (GC/MSD/SIM). The ultrasonic extraction of US EPA (method 3550B) method and liquid-liquid extraction for sediment and soil samples were used for the analysis of BP from sediment and soil. BP was extracted with n-hexane. Organic layer was washed with 5% sodium chloride solution. 1∼2 l of the concentrated solution of organic layer was applied to GC/MSD. The retention time of BP peak was 11.10 min. Recovery (％) of BP by ultrasonication from sediment and soil samples was 96.0∼100.6％ and 40.0∼83.0％, respectively. Recovery of BP by liquid-liquid extraction was 51∼59％ in soil samples. The detection limit of BP in sediment and soil samples were determined to 0.1 ng/g.

• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2006년 창립20주년기념 정기학술대회 및 국제워크샵
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• pp.177-180
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• 2006

This study is to make a basic study if solid zinc (Zn) can be used for buried reference electrode, so we examined the adequacy of zinc as reference electrode by using zinc which showed regular electrode for buried period. The deference of electric potential if zinc electrode for corrosion factor such as soil resistivity or pH didn't show fixed trend and there was no clear trend on the change of measurement period. From field test, it is known that the natural electric potential difference of CSE electrode and zinc electrode is 1,100mV, but the electric potential of zinc electrode for CSE electrode in the natural soil and copying soil was 1,094~1,158mV. There was no fixed trend on the change of measurement period and electric potential difference of zinc electrode for corrosion factors such as soil resistivity or pH. Consequently, there was 40~60mV of electric potential difference in every copying soil during the experiment measurement.

• 한국지하수토양환경학회지:지하수토양환경
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• 제19권6호
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• pp.18-23
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• 2014

The BTEX contamination of soil around gas station in Korea was investigated in 53 gas stations in 2013 by official test method on soil pollution. Each gas station was divided into oil tank area, line area, and surrounding area. The concentration of BTEX in 1066 sites of 53 gas stations was N.D.~ 3437.36 mg/kg. The order of average concentration for area was as follows: line area ($20.91{\pm}144.79mg/kg$) > tank area ($15.11{\pm}110.08mg/kg$) > surrounding area ($10.79{\pm}111.40mg/kg$). It was the number of sampling site exceeding regulatory levels at surrounding area the most at all. The average concentration of xylene was the highest, while that of ethylbenzene was the lowest.