• 미생물학회지
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• 제51권1호
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• pp.21-30
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• 2015

본 연구는 논과 밭 토양의 황산염 환원세균의 군집구조와 T-RFLP 패턴을 조사한 논문으로, 유기 농법 토양과 관행 농법 토양 그리고 밭 토양 총 3종류의 토양을 8월과 11월에 채집하여 실험하였다. 토양 성분 분석 결과 총 질소, 총 탄소, 총 인의 값은 모든 토양이 비슷하게 나타났고 계절별로는 수분의 함량은 8월에, 총 탄소는 11월에 가장 높게 나타났다. 황산염 환원세균은 초산보다 젖산을 기질로 이용하는 황산염 환원세균이 더 많이 분포하고, 유기 농법 토양에 황산염 환원세균이 가장 많이 분포하는 것으로 나타났다. 각 토양에서 얻은 총 181개 클론으로 계통학적 분석을 한 결과, 대부분의 클론들은 배양 가능한 황산염 환원세균과는 매우 낮은 상동성을 보였으나, 자연계에서 확인되는 클론들과는 90% 이상의 높은 상동성을 나타내었다. T-RFLP 분석 결과 91, 357, 395, 474 bp의 분포가 가장 높았고, 계절에 따라 황산염 환원세균의 군집 구조가 달라지는 것을 확인하였다.

• 한국토양비료학회지
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• 제49권5호
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• pp.510-516
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• 2016

Soil respiration has been recognized as a key factor of the change of organic matter and fertility due to the carbon and nitrogen mineralization. In this study, we evaluated the effect of soil respiration on the light fraction-C and inorganic N content depending on temperature in soil applied with organic matter. Soil respiration was calculated by using total $CO_2$ flux released from soil applied with $2Mg\;ha^{-1}$ of rice straw compost and rye for 8 weeks incubation at 15, 25, $35^{\circ}C$ under incubation test. After incubation test, light fraction and inorganic N content were investigated. Rye application dramatically increased soil respiration with increasing temperature. $Q_{10}$ value of rye application was 1.69, which was higher 27% than that of rice straw compost application. Light-C and $NO_3-N$ contents were negatively correlated to soil respiration. Light-C in rye application more decreased than that in rice straw compost with temperature levels. These results indicate that temperature sensitivity of soil respiration could affect soil organic mater content and N availability in soil due to carbon availability. Also, light fraction would be useful indicator to evaluate decomposition rate of organic matter in soil under a short-term test.

• 자원환경지질
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• 제45권6호
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• pp.673-684
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• 2012

해양 퇴적물내 함유된 총탄소(total carbon; TC), 총무기탄소(total inorganic carbon; TIC)와 총유기탄소(total organic carbon; TOC)의 정량적 이해는 해양 저서 퇴적 환경 해석을 위한 기본 자료이다. 원소분석기(elemental analyzer; EA)는 내륙 토양 및 해양 퇴적물의 탄소성분 분석에 많이 이용되고 있다. 원소분석기로 분석한 표준시료샘플(soil reference material; SRM)의 탄소 및 질소함량은 평균 2.30%와 0.21%이었으며, 표준편차(standard deviation)는 각각 0.02, 0.01이었다, 상대표준편차(relative standard deviation; RSD)는 각각 0.01, 0.06으로 높은 정밀도를 나타내었다. 형도 부지의 총유기탄소(TOC) 2.0% 이하 샘플에 대해 총유기탄소(TOC)와 총탄소(TC) 분석치의 회귀분석은 기울기가 0.9743인 직선형 관계($R^2$=0.9989, n=38)를 보였으며, 2개 샘플을 제외한 총유기탄소 0.5% 이하의 총유기탄소량 및 평균입도의 관계 회귀분석 결과는 기울기가 0.0444인 직선형 관계($R^2$=0.6937 n=36)를 나타내었다. 형도 표층퇴적물의 총유기탄소(TOC) 함량은 0.10~1.67%(평균 $0.26{\pm}0.37%$) 범위로 S02 정점에서 1.67%, S07 정점에서 1.31%이고 나머지 점점은 1.00% 이하의 총유기탄소(TOC) 함량을 나타냈다. 주상퇴적물 PC 01 정점의 경우 70 cm 부근에서 총유기탄소(TOC)가 가장 높은 0.20%을 보였고, 주상퇴적물 PC 02 정점의 경우 60 cm 부근에서 가장 높은 0.24%를 나타내었다. 따라서 형도 샘플의 총유기탄소(TOC) 0.5% 이상 함유 샘플에 대해서는 탄산염 같은 무기탄소량이 높은 퇴적물 분석시 오차가 발생할수 있지만, 이와 같은 결과로부터 얻어진 유기탄소분석 방법은 해양 퇴적물의 유기탄소분석에 적용 될 수 있다. 그리고 원소분석기(EA) 정밀도 및 정확도로 해양 퇴적물 표층 및 주상 퇴적물 유기탄소분석 분석 실험에 유용 할 것으로 사료된다.

• 공업화학
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• 제32권5호
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• pp.581-588
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• 2021

In this study, soil slurry bioreactors were used to treat soils containing 16 polycyclic aromatic hydrocarbons (PAHs) for 35 days. Five different soil samples were taken from manufactured gas plant (MGP) and coal tar disposal sites. Soil properties, such as carbon content and particle distribution, were measured. These properties were significantly correlated with percent biodegradation and degradation rate. The cumulative amount of PAH degraded (P), degradation rate (K_m), and lag phase (𝜆) constants of PAHs in different MGP soils for 16 PAHs were successfully obtained from nonlinear regression analysis using the Gompertz equation, but only those of naphthalene, anthracene, acenaphthene, fluoranthene, chrysene, benzo[k]fluoranthene, benzo(a)pyrene, and benzo(g,h,i)perylene are presented in this study. A comparison between total non-carcinogenic and carcinogenic PAHs indicated higher maximum amounts of PAH degraded in the former than that in the latter owing to lower partition coefficients and higher water solubilities (S). The degradation rates of total non-carcinogenic compounds for all soils were more than four times higher than those of total carcinogenic compounds. Carcinogenic PAHs have the highest partitioning coefficients (K_oc), resulting in lower bioavailability as the molecular weight (MW) increases. Good linear relationships of K_m, 𝜆, and P with the octanol-water partitioning coefficient (K_ow), MW, and S were used to estimate PAH remaining, lag time, and biodegradation rate for other PAHs.

• 유기물자원화
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• 제22권3호
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• pp.33-40
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• 2014

본 연구의 목적은 옥수수 재배 기간 동안 퇴비 및 바이오차를 시용한 토양에서 질소 무기화와 질산화율을 평가하였으며, 또한 유거수에 의한 총 탄소 및 질소 유실량을 산정하는 것이었다. 본 실험에 사용된 토성은 식양토였고, 비료 시용량은 토양검정 시비량으로서 $230-107-190kg\;ha^{-1}$($N-P_2O_5-K_2O$)이었으며, 바이오차 시용량은 토양무게 기준 0.2%이었다. 토양 시료는 15일 간격으로 채취하였으며, 시험구는 우분, 돈분 및 호기액비 처리구 와 각각의 처리구에 바이오차를 혼용하였다. 질소 무기화 및 질산화율은 일반적으로 파종 후 45일 토양 시료를 제외하고 유기성 퇴비만 시용한 구에 비해 바이오차를 혼용한 구에서 더 낮게 나타났으며, 호기액비 처리구에서 가장 높게 관측되었다. 유거수에 의한 총 탄소의 유실은 $1.5{\sim}3.0kg\;ha^{-1}$범위이었으며, 바이오차를 혼용한 돈분처리구에서만 $0.4kg\;ha^{-1}$ 저감되는 것으로 평가되었다. 또한 바이오차를 혼용함으로서 총 질소량이 돈분 및 호기소화액 처리구에서 각각 4.2 (15.1%) 와 $3.8(11.8%)kg\;ha^{-1}$이 줄어드는 것으로 나타났다.

• Journal of Forest and Environmental Science
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• 제36권1호
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• pp.25-36
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• 2020

Area exclosure is a widely practiced intervention of restoring degraded lands though its impact in sequestering terrestrial and soil carbon is scanty. The study was initiated to investigate the effect of exclosure of different ages on carbon sequestration potential of restoring degraded dryland ecosystems in eastern Tigray, northern Ethiopia. Twelve plots each divided into three layers were randomly selected from 5, 10 and 15 years old exclosures and paired adjacent open grazing land. Tree and shrub biomasses were determined using destructive sampling while herb layer biomass was determined using total harvest. The average total biomass obtained were 13.6, 24.8, 27.1, and 55.5 Mg ha^-1 for open grazing, 5 years, 10 years, and 15 years exclosures respectively. The carbon content of plant species ranged between 48 to 53 percent of a dry biomass. The total carbon stored in the 5 years, 10 years and 15 years age exclosures were 39 Mg C ha^-1, 46.3 Mg C ha^-1, and 64.6 Mg C ha^-1 respectively while in the open grazing land the value was 24.7 Mg C ha^-1. Carbon stock is age dependent and increases with age. The difference in total carbon content between exclosures and open grazing land varied between 14.3-40 Mg C ha^-1. Although it is difficult to extrapolate this result for a longer future, the average annual carbon being sequestered in the oldest exclosure was about 2.7 Mg C ha^-1 yr^-1. In view of improving degraded area and sequestering carbon, area exclosures are promising options.

• 자원리싸이클링
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• 제23권2호
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• pp.46-52
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• 2014

본 논문은 마이크로파와 고온발열체에 의한 유류오염토양의 정화효율에 관한 연구를 정리한 것이다. 수분의 함량은 처리량에 따라 측정이 되었는데 상대적으로 짧은 시간에 300 g에 도달했다. TPH(Total Petroleum Hydrocarbons)처리 속도는 SiC 발열체를 단독으로 사용했을 때와 비교하였을 때, SiC와 활성탄을 4 kW/kg에서 동시에 사용했을 때 70.1%의 제거율로 가장 높은 값을 보여주었다. 특히, 3 kW/kg때를 제외하고는 전력이 증가할수록 처리속도도 증가하였다. SiC와 활성탄으로 제작된 발열체를 사용할 경우, 내부 온도가 $300^{\circ}C$를 초과하였으며, 4 kW로 2분동안 유지되었을 때 온도가 다시 하락하였으나, 8분이후에는 다시 온도가 상승하였다. 이러한 결과를 기초로 하여, 샘플을 처리하기 위한 에너지량은 마이크로파의 전력에 따라 계산이 되었으며, TPH처리 상수는 유류오염토양의 처리 특성에 관한 다양한 실험에 의해 측정이 되었다.

• 한국환경복원기술학회지
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• 제10권6호
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• pp.62-69
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• 2007

This study has been carried out to estimate aboveground carbon contents in an average 30-years-old Betula platyphylla and 32-years-old Juglans mandshurica stands in Chungju, Chungbuk Province. Nine sample trees were cut in each forest and soil samples were collected. Carbon concentration in stemwood, stembark, branch, and foliage were ranged from 54.6% to 57.0% in Betula platyphylla and 53.5% to 56.9% in Juglans mandshurica stands. Aboveground carbon contents was estimated by the equation model logWt=A+BlogD where Wt is oven-dry weight in kg and D is DBH in cm. Total aboveground carbon contents was 34.31t/ha in Betula platyphylla stand and 21.10t/ha in Juglans mandshurica stand. Aboveground net primary carbon production was estimated at 2.31t/ha/yr in Betula platyphylla stand and 2.03t/ha/yr in Juglans mandshurica stand.

• Journal of Ecology and Environment
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• 제43권2호
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• pp.161-182
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• 2019

Quantifying the amount of carbon pools in forest ecosystems enables to understand about various carbon pools in the forest ecosystem. Therefore, this study was conducted in the Chilimo dry afromontane forest to estimate the amount of carbon stored. The natural forest was stratified into three forest patches based on species composition, diversity, and structure. A total of 50 permanent sample plots of 20 m × 20 m (400 ㎡ ) each were established, laid out on transects of altitudinal gradients with a distance of 100 m between plots. The plots were measured twice in 2012 and 2017. Tree, deadwood, mineral soil, forest floor, and stump data were collected in the main plots, while shrubs, saplings, herbaceous plants, and seedling data were sampled inside subplots. Soil organic carbon (SOC %) was analyzed following Walkely, while Black's procedure and bulk density were estimated following the procedure of Blake (Methods of soil analysis, 1965). Aboveground biomass was calculated using the equation of Chave et al. (Glob Chang Biol_20:3177-3190, 2014). Data analysis was made using RStudio software. To analyze equality of means, we used ANOVA for multiple comparisons among elevation classes at α = 0.05. The aboveground carbon of the natural forest ranged from 148.30 ± 115.02 for high altitude to 100.14 ± 39.93 for middle altitude, was highest at 151.35 ± 108.98 t C ha^-1 for gentle slope, and was lowest at 88.01 ± 49.72 t C ha^-1 for middle slope. The mean stump carbon density 2.33 ± 1.64 t C ha^-1 was the highest for the middle slope, and 1.68 ± 1.21 t C ha^-1 was the lowest for the steep slope range. The highest 1.44 ± 2.21 t C ha^-1 deadwood carbon density was found under the middle slope range, and the lowest 0.21 ± 0.20 t C ha^-1 was found under the lowest slope range. The SOCD up to 1 m depth was highest at 295.96 ± 80.45 t C ha^-1 under the middle altitudinal gradient; however, it was lowest at 206.40 ± 65.59 t C ha^-1 under the lower altitudinal gradient. The mean ecosystem carbon stock density of the sampled plots in natural forests ranged from 221.89 to 819.44 t C ha^-1. There was a temporal variation in carbon pools along environmental and social factors. The highest carbon pool was contributed by SOC. We recommend forest carbon-related awareness creation for local people, and promotion of the local knowledge can be regarded as a possible option for sustainable forest management.

• 한국지하수토양환경학회지:지하수토양환경
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• 제18권7호
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• pp.81-89
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• 2013

Concerns have been raised over the impact of nano materials on soil and groundwater environment with the increasing attention to the potential applications of carbon nano materials in various fields. Particularly, carbon nano materials introduced into water environment readily make complexes with humic acid (HA) due to their hydrophobic nature, so there have been increasing numbers of studies on the interaction between HA and carbon nano materials. In this study, we investigated the solubility of HA and multiwalled carbon nanotubes (MWCNT) in three different surfactant solutions of sodium dodecyl sulfate (SDS), Brij 30 and Triton X-100, and evaluated whether the HA can be effectively desorbed from the surface of MWCNT by surfactant. The objective of this study was to determine the optimal adsorption condition for HA to MWCNT. Futhermore, sodium dodecyl sulfate (SDS), Brij 30, Triton X-100 were used to elucidate the effect of desorption and separation on adsorbed HA on MWCNT. As a result, HA solution with 12.7 mg of total organic carbon (TOC) and 5 mg of MWCNT showed the highest adsorption capacity at pH 3 reacted for 72 hrs. Weight solubilizing ratio (WSR) of surfactants on HA and MWCNT was calculated. HA had approximately 2 times lower adsorption capacity for the applied three surfactants compared to those of MWCNT, implying that the desorption of HA may occur from the HA/MWCNT complex. According to the results of adsorption isotherm and weight solubilizing ratio (WSR), the most effective surfactants was the SDS 1% soluiton, showing 53.63% desorption of HA at pH 3.