• 대한환경공학회지
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• 제32권11호
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• pp.1030-1037
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• 2010

본 연구에서는 비점오염물질 관리를 위한 적정 수변완충폭의 산정 방안과 산정된 수변완충지역에 식재되는 식생 유형에 따른 탄소 축적 효과를 비교하여 수변지역을 친환경적으로 관리하기 위한 방안을 제시하였다. 낙동강 중.하류지역인 낙본 K 유역을 대상으로 수행한 연구 결과 대상 하천에 30~600 m 범위의 수변 폭이 필요한 것으로 분석되었으며, 산출된 수변완충지대 조성 지역에서 논, 밭, 초지, 나대지 등 수변 조성이 용이한 지역은 총 1,776.51 ha로 산출된 지역의 약 50%로 나타났다. 조성이 용이한 1776.51 ha에 활엽수림으로 수변완충지역을 조성할 경우 약 14,526 ton, 혼효림으로 조성할 경우 11,826 ton, 침엽수림으로 조성할 경우 8,382 ton, 다년생 초지로 조성할 경우에는 3,349 ton의 탄소가 각각 매년 축적되는 것으로 나타났다. 본 연구의 결과 산정된 수변완충지역에 매년 흡수하는 이산화탄소량은 자동차 약 5천대에서 배출되는 이산화탄소량과 비슷하며, 4인 기준 가정 약 2만 가구에서 나오는 이산화탄소량과 유사한 양으로 파악되었다.

• 한국관개배수회지
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• 제47호
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• pp.75-75
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• 2011

• 한국미생물학회:학술대회논문집
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• 한국미생물학회 2004년도 International Meeting of the Microbiological Society of Korea
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• pp.19-20
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• 2004

• 전산구조공학
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• 제36권4호
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• pp.4-7
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• 2023

• 한국토양비료학회지
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• 제48권6호
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• pp.736-743
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• 2015

Organic matter plays important roles in soil ecosystem in terms of carbon and nitrogen cycles. Due to recent concerns on climate change, carbon sequestration in agricultural land has become one of the most interesting and debating issues. It is necessary to understand behavior of soil carbon for evaluating decomposition or sequestration of organic matter and analyzing potential carbon decomposition pattern about the kinds of organic matter sources to cope with well. In order to evaluate decomposition of soil carbon according to organic material during cultivating rice in paddy field, we treated organic material such as hairy vetch, rice straw, oil cake fertilizer, and manure compost at $50{\times}50{\times}20cm$ blocks made of wood board, and analyzed carbon contents of fulvic acid and humic acid fraction, and total carbon periodically in 2013 and 2014. Soil sampling was conducted on monthly basis. Four Kinds of organic matter were mixed with soil in treatment plots on 2 weeks before transplanting of rice. The treatment of animal compost showed the highest changes of total carbon, which showed $7.9gkg^{-1}$ in May 2013 to $11.6gkg^{-1}$ in October 2014. Fulvic acid fraction which is considered to easily decompose ranged from 1 to $2gkg^{-1}$. Humic acid fraction was changed between 1 to $3gkg^{-1}$ in all treatments until organic material had been applied in 2014. From May to August in the second year, the contents of humic acid fraction increased to about $4gkg^{-1}$. The average of humic fraction carbon at treatments of animal compost was recorded highest among treatments during two years, $2.1gkg^{-1}$. The treatment of animal compost has showed the lowest ratio of fulvic acid fraction, humic acid fraction compared with other treatments. The average ratio of fulvic fraction carbon in soil ranged from 16 to 20%, and humic fraction carbon ranged from 19 to 22%. In conclusion, animal compost including wood as bulking agent is superior in sequestrating carbon at agricultural land to other kinds of raw plant residue.

• 한국가스학회지
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• 제16권6호
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• pp.55-66
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• 2012

$CO_2$ 감축은 최근 문제되고 있는 온실가스를 감축시킬 수 있는 직접적인 수단이 되고 있으며, 이러한 방법으로는 CCS 기술이 현실적인 대안기술로 부상하고 있다. 특히 전 세계적으로 널리 분포되어 있고 많은 양의 $CO_2$ 를 격리할 수 있는 심부 대염수층을 대상으로 활발한 연구가 진행 중이다. 이에 본 연구에서는 심부 대염수층에 대한 $CO_2$ 지중격리시 예비 타당성 평가 수행을 위하여 인공신경망을 이용한 효율성 평가 모델을 개발하였다. 모델 개발에 앞서 심부 대염수층을 대표할 수 있는 기본 모델을 선정하고 상용시뮬레이터 GEM을 활용하여 민감도 분석을 수행하였으며, 분석 결과를 바탕으로 심부 대염수층에 영향을 미치는 주요 인자 및 영향범위를 선정하였다. 인공신경망 학습을 위한 격리 시나리오 구성 결과 용해트랩과 잔류트랩에 의한 $CO_2$ 격리를 확인할 수 있었으며, 인공신경망 모델 자체 검증 결과 0.99이상의 높은 상관계수를 나타내어 심부 대염수층에서의 $CO_2$ 지중격리 효율성 평가에 활용 가능함을 확인하였다.

• Journal of Forest and Environmental Science
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• 제29권4호
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• pp.249-256
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• 2013

The aim of the study was to reveal the scope and benefits derives from establishing carbon forests in a country like Bangladesh. Carbon forestry is the modernized forestry practice that evolves no cutting of trees or vegetation rather conserves them in the wood. Trees might be the source of carbon sink at large scale by establishing carbon forests. To find out how and in what extent forests of Bangladesh could contribute to global emission reduction, tree species of economic importance were taken into account about their carbon sequestration potential. Data source was a secondary one. Bangladesh has subtropical evergreen and deciduous forest tree species. Here trees can sequester almost 45-55 percent organic carbon in their biomass. On an average, trees in different types of stands can sequester 150-300 tC/ha. Carbon value of these forests might be 7,500-15,000 USD per hactre (assuming 50 USD per equivalent $tCO_2$). Thus, accounting tree carbon credits of total forested lands of Bangladesh, there might be a lump sum value of $1.89{\times}10^{10}-3.79{\times}10^{10}$ USD. If soil carbon is added, this amount would jump. Alternatively, there are two times higher spaces as marginal lands than this for starting carbon forestry. However, carbon forestry concept is still a theoretical conception unless otherwise their challenges are addressed and solved. Despite of this, forests of Bangladesh might be the key showcase for conserving biodiversity in association with carbon capture. Protected areas in Bangladesh are of government wealth, however, degraded and denuded waste and marginal lands might be the best fit for establishing carbon forests.

• 유기물자원화
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• 제25권1호
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• pp.87-92
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• 2017

본 실험의 목적은 토양탄소 격리 기술을 개발하기 위한 바이오차 팰렛 시용에 따른 고추 생육 효과를 평가하는 것이다. 처리는 고추 수확 후 총 탄소 함량, 암모늄태 질소의 농도 및 총 바이오매스량 비교를 위해 일반적인 영농 방법으로서 대조구, 돈분 팰렛, 바이오차와 돈분 퇴비 혼합 비율별 바이오차 팰렛 시용구 (9:1, 8:2, 6:4, 4:6, 2:8)로서 구성되어 있다. 바이오차 팰렛의 사용량은 고추 재배를 위한 추천 시용량 (440 kg/10a)기준으로 혼합 비율에 관계없이 8.8 g/pot이었다. 실험 결과로서 총 탄소 함량은 대조구와 비교하여 처리구에서 1.8-2.6배 낮게 나타났다. 암모늄태 질소의 농도는 대조구와 비교하여 처리구들 사이에 유의차가 인정되지 않았으며, 질산태 질소는 모든 처리구에서 검출되지 않았다. 그렇지만, 총 바이오매스량은 다른 처리구에서는 낮게 나타났다 할지라도 대조구와 2:8 바이오차 팰렛 처리구 사이에는 유의차가 인정되지 않았다. 따라서 이 바이오차 팰렛 시용은 농사 활동에 있어서 탄소격리를 위해서는 더욱더 연구되어야 한다.

• 태양에너지
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• 제20권2호
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• pp.75-84
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• 2000

Global wanning induced by greenhouse gases such as carbon dioxide is a serious problem for mankind. Carbon dioxide ocean disposal is one of the promising options to reduce carbon dioxide concentration in the atmosphere because the ocean has vast capacity for carbon dioxide sequestration. However, the dissolution rate of liquid carbon dioxide in seawater must be known in advance in order to estimate the amount of carbon dioxide sequestration in the ocean. Therefore, the solubility, the surface concentration, the droplet size and other factors of liquid carbon dioxide at various depths are calculated. The results show that liquid carbon dioxide changes to carbon dioxide bubble around 500 m in depth, and the droplet is completely dissolved below 500 m in depth if carbon dioxide droplet is released both at 1000 m in depth with the initial droplet diameter of 0.011 m or less and at 1500 m in depth with the diameter of 0.015 m or less. In addition, the hydrate film acts as a resistant layer for the dissolution of liquid carbon dioxide. The surface concentration of carbon dioxide droplet with the hydrate film is about 50% at 1500 m in depth and about 60% at 1000 m in depth of the carbon dioxide solubility. Also, the ambient carbon dioxide concentration in the plume is an another crucial parameter for complete dissolution at the intermediate ocean depth, and the injection of liquid carbon dioxide from a moving ship is more effective than that from a fixed pipeline.

• Journal of Forest and Environmental Science
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• 제37권2호
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• pp.116-127
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• 2021

Predicting carbon distribution of soil aggregates is difficult due to complexity in organo-mineral formation. This limits global warming mitigation through soil carbon sequestration. Therefore, knowledge of land use effect on carbon stabilization requires quantification of soil mineral cations. The study was conducted to quantify carbon and base cations on soil mineral fractions in Natural Forest, Plantation Forest and Farm Land. Five 0.09 ha were demarcated alternately along 500 m long transect with an interval of 50 m in Natural Forest (NF), Plantation Forest (PF) and Farm Land (FL). Soil samples were collected with soil cores at 0-15, 15-30 and 30-45 cm depths in each plot. Soil core samples were oven-dried at 105℃ and soil bulk densities were computed. Sample (100 g) of each soil core was separated into >2.0, 2.0-1.0, 1.0-0.5, 0.5-0.05 and <0.05 mm aggregates using dry sieve procedure and proportion determined. Carbon concentration of soil aggregates was determined using Loss-on-ignition method. Mineral fractions of soil depths were obtained using dispersion, sequential extraction and sedimentation methods of composite soil samples and sieved into <0.05 and >0.05 mm fractions. Cation exchange capacity of two mineral fractions was measured using spectrophotometry method. Data collected were analysed using descriptive and ANOVA at α_0.05. Silt and sand particle size decreased while clay increased with increase in soil depth in NF and PF. Subsoil depth contained highest carbon stock in the PF. Carbon concentration increased with decrease in aggregate size in soil depths of NF and FL. Micro- (1-0.5, 0.5-0.05 and <0.05 mm) and macro-aggregates (>2.0 and 2-1.0 mm) were saturated with soil carbon in NF and FL, respectively. Cation exchange capacity of <0.05 mm was higher than >0.05 mm in soil depths of PF and FL. Fine silt (<0.05 mm) determine the cation exchange capacity in soil depths. Land use and mineral size influence the carbon and cation exchange capacity of Gambari Forest Reserve.