• Ecology and Resilient Infrastructure
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• 제10권4호
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• pp.161-170
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• 2023

본 연구에서는 제주도에서 자생하는 준맹그로브인 황근 (Hibiscus hamabo)과 갯대추나무 (Paliurus ramosissimus)의 탄소 저장량을 원격탐사로 추정하고 기후요인에 의하여 공간변이를 예측하는 인공지능 모델을 구축하고자 하였다. 준맹그로브의 지상부 탄소 축적량은 Global Ecosystem Dynamics Investigation (GEDI) 라이다에 의하여 제공되는 지상부 생물량 밀도(aboveground biomass density, AGBD)를 Sentinel-2 영상으로부터 추출한 normalized difference vegetation index (NDVI)으로 해상도를 상향하여 추정하였다. 제주도에서 단위면적당 탄소 축적량은 황근이 16.6 t C/ha, 갯대추나무가 21.1 t C/ha이었다. 제주도 전 해안에서 준맹그로브의 탄소 축적량은 11.5 t C로 추정되었다. 환경요인에 따른 준맹그로브의 탄소 축적량을 예측하기 위하여 랜덤 포레스트 기술을 적용하였다. 제주도 준맹그로브림의 분포면적 대비 지상부 생물량의 잔차를 계산하였다. 이 잔차에 영향을 미치는 주요 환경요인으로는 가장 습한 달의 강수량, 가장 더운 달의 최고온도, 등온성 및 가장 습한 달의 평균 온도가 선정되었다. 제주도에서 랜덤 포레스트 분석으로 예측된 준맹그로브의 탄소 축적량은 12.0 t C/ha - 27.6 t C/ha 범위의 공간적 변이를 나타내었다. 본 연구에서 개발된 탄소 축적량의 원격탐사 추정법과 환경요인에 따른 인공지능 예측법은 한반도에서 탄소흡수원으로서 맹그로브의 보전과 조성에 필요한 기초자료로 활용할 수 있을 것이다.

• Journal of the korean society of oceanography
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• 제34권3호
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• pp.144-150
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• 1999

Slope sedimentation on the modern west Florida continental margin is controlled by pelagic carbonate accumulation and off-shelf sedimentation of neritic carbonates and terrigenous fines. Production and deposition of pelagic carbonates by planktonic foraminifera and coccoliths have played a significant role in the total slope sedimentation and are mainly promoted by sea-surface productivity. Organic carbon data reflect the relatively high biological productivity in surface waters, indicating high accumulation of biogenic calcareous sediments. The surface-water productivity in the study area is supported by the relation among microfossil assemblages, carbonate mineralogy and sedimentary organic carbon.

• 한국기후변화학회지
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• 제5권4호
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• pp.339-348
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• 2014

Agro-ecosystem plays an important role in the mitigation of atmospheric $CO_2$ concentration through photosynthesis and soil carbon fixation. The perennial crops have capacity of carbon accumulation because they have lived for years in the same position. Carbon dioxide fixation occurs in the fruit orchard by photosynthesis and soil carbon sequestration. The objectives of this review are to introduce the fruit orchard as a carbon dioxide sink and to summarize the methods that measure $CO_2$ flux in the orchard. There are three difference methods (chamber, biomass, and eddy covariance method) to measure $CO_2$ exchanges on sites. However, there is no standard method suitable for fruit cultivation condition in Korea. Thus the standard method have to be developed in order to exactly estimate the carbon accumulation. In foreign studies, the carbon assessments were conducted in apple, peach, olive, grape orchard and so on. On the other hand the estimation of $CO_2$ exchange was carried out for apple and mandarine orchard in Korea. According to these results, fruit orchard is a $CO_2$ sink even though amount of carbon accumulation is smaller than the forest. To introduce certainly fruit orchard as greenhouse gas sink, long-term monitoring and further study have to be conducted under each planting condition.

• Journal of Forest and Environmental Science
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• 제34권1호
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• pp.12-23
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• 2018

Quantitative information on biomass and available nutrients are essential for developing sustainable forest management strategies to regulate atmospheric carbon. An attempt was made at Chilapatta Reserve Forest in Duars region of West Bengal to quantify its above and below ground carbon along with available "N", "P" and "K" in the soil. Stratified random nested quadrats were marked for soil, biomass and litter sampling. Indirect or non-destructive procedures were employed for biomass estimation. The amount of these available nutrients and organic carbon quantified in soil indicates that the forest soil is high in organic carbon and available "K" and medium in phosphorus and nitrogen. The biomass, soil carbon and total carbon (soil C＋C in plant biomass) in the forest was 1,995.98, 75.83 and $973.65Mg\;ha^{-1}$. More than 90% of the carbon accumulated in the forest was contributed by the trees. The annual litter production of the forest was $5.37Mg\;ha^{-1}$. Carbon accumulation is intricately linked with site quality factors. The estimated biomass of $1,995.98Mg{\cdot}ha^{-1}$ clearly indicates this. The site quality factor i.e. tropical moist deciduous with optimum availability of soil nutrients, heavy precipitation, high mean monthly relative humidity and optimum temperature range supported luxuriant growth which was realized as higher biomass accumulation and hence higher carbon accumulated.

• Environmental Engineering Research
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• 제20권3호
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• pp.246-253
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• 2015

The effects of carbon-to-nitrogen (C/N) ratio in simulated rice straw hydrolysates using glucose and ammonium chloride on polyhydroxyalkanoates (PHA) accumulation by Cupriavidus necator was investigated. In general, PHA accumulation rate was higher under higher degrees of N-deficient conditions (e.g., C/N ratio of 360:1) than lower degrees of N-deficient conditions (e.g., C/N ratio of 3.6:1 and 36:1). Also, the most PHA accumulation was observed during the first 12 h after the PHA accumulation initiation. This study showed that the similar PHA accumulation could be achieved by using different accumulation periods depending on C/N ratios. N source presence was important for new cell production, supported by approximately ten times greater PHA accumulation under the N-deficient condition ($NH_4Cl$ 0.01 g/L) than the N-free (without $NH_4Cl$) condition after 96 h. C/N ratio of the rice straw hydrolysate was approximately 160:1, based on the glucose content, and this accumulated $0.36{\pm}0.0033g/L$ PHA with PHA content of $21{\pm}3.1%$ after 12 h. Since external C or N source addition for C/N ratio adjustment increases production cost, an appropriate accumulation period may be used for PHA accumulation from organic wastes, based on the PHA accumulation patterns observed at various C/N ratios and C and N concentrations.

• 한국생물공학회:학술대회논문집
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• 한국생물공학회 2000년도 추계학술발표대회 및 bio-venture fair
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• pp.346-349
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• 2000

In order to investigate the characteristics for RNA accumulation, continuous cultures of S. cerevisiae MTY62 under the carbon-limitation or carbon-phosphate-limitation were performed. In the carbon-limited chemostat, the highest RNA content of 144 mg-RNA/g-dry cell was observed at the dilution rate of $0.30\;hr^{-1}$. In the carbon and phosphate-limited chemostat, the culture condition with the dilution rate of $0.25\;hr^{-1}$ gave the maximal RNA content of 209 mg-RNA/g-dry cell. The accumulation rate of RNA $(mg-RNA/L\;{\cdot}\;hr)$ was decreased at higher dilution rate in the carbon and phosphate-limited chemostat.

• 한국초지조사료학회지
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• 제13권1호
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• pp.58-65
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• 1993

가을에 파종한 사초용유채(Brassica napus Subsp. oleifera cv. Swiss)의 생육기간 동안의 질소대사와 관련하여 건물수량 및 조단백질의 축적정도를 규명하기 위해. 생육기간중 수량 및 조단백질 함량을 측정하고, 엽내 carbon, nitrogen 및 hydrogen 함량을 비교. 분석하였다. 월동기인 '91년 11월 7일부터 '92년 2월 4일 동안의 생초량 및 건물량의 축적은 매우 적었으며, 엽내 C함량은 건물 1g당 382mg에서 435mg으로 증가하였으나. 질소 및 조단백질 함량은 55mg에서 46mg 및 345mg에서 289mg으로 각각 감소하였다. 월동후 춘계 재생초기(2월 3일부터 3월 30일까지) 동안 생초수량의 점차적인 증가에 따라 엽내 C함량은 일당 37mg의 감소를 보였으나, 월동기 동안 감소 되었던 N함량은 다소 증가를 보였다. 영양생장기(3월 31일)부터 추태기인 4월 16일까지 일당 개체당 생초 및 건물축적량은 각각 5.2g 및 0.5g으로 전 생육기간중 가장 높았는데, 엽내의 C/N 의 정상적인 균형을 유지하며 직선적인 증가를 보였고, 조단백질 함량 역시 지속적인 축적이 있었다. 이 시기 이후 개화최성기('92년 5월 19일)까지 엽내 C, N, H 및 조단백질 함량은 공히 유의적인 감소를 보였는데, 특히 N과 조단백질 함량이 추태기에 비해 각각 45.7% 및 46%의 감소로 뚜렷하였다 이들 결과들은 월동기나 월동 후 초기재생 기간중 식물체내 C/N 균형의 현저한 변화를 가져오며, 춘계 영양생장기에서 추태기 동안(3월 31일부터 4월 16일까지)가장 원활한 물질대사에 따라 엽내의 건물 및 조단백질 축적이 왕성하다는 것을 보여준다. 따라서 예취이용의 적기는 추태기이며 생육기간 중 추비적기는 춘계 영양생장기 이전으로 사료된다.

• 토지주택연구
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• 제14권1호
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• pp.83-97
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• 2023

본 연구는 묵논습지의 보전 복원과 탄소축적 기능 증진을 위한 학술적 근거를 제공하기 위해 수행되었다. 묵논습지의 시간적 변화를 분석하고 탄소감축을 목표로 묵논습지 유형분류체계를 구축하고자 하였다. 묵논습지의 유형은 탄소축적 기능에 주목하여 수문학적 환경, 식생, 탄소축적 등 세 가지 변수를 기준으로 분류되었다. 묵논습지의 유형은 수리수문 변수를 기준으로 물유입 포텐셜 높음과 낮음, 식생 변수로는 수생식물 우점과 육상식물 우점, 탄소축적 변수로는 유기물 생산과 토양 유기탄소 집적, 분해 등을 종합해 12개 유형으로 분류했다. 국토지리정보원이 제공하는 항공사진으로 분석한 묵논의 발달 시기는 일반적으로 2010~2015년경에 발생하였으나, 대전1(DJMN01) 묵논습지의 경우 1990년경에 영농이 중단되어 2010년 이후 자연습지와 유사한 구조를 보였다. 대전1(DJMN01) 묵논습지의 최근 40년간 토지피복의 변화는 전체적으로는 산림과 농경지의 비율이 높게 나타나고 있으며, 시간의 흐름에 따라 산림과 농경지가 매우 빠른 속도로 감소하면서 인공초지, 다른 형태의 산림 등의 피복유형으로 변화하는 경향이 있었다.

• Journal of Microbiology and Biotechnology
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• 제19권10호
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• pp.1127-1134
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• 2009

Escherichia coli excretes acetate during aerobic growth on glycolytic carbon sources, which has been explained as an overflow metabolism when the carbon flux into the cell exceeds the capacity of central metabolic pathways. Nonacetogenic growth of E. coli on gluconeogenic carbon sources like succinate or in carbon-limited slow growth conditions is believed an evidence for the explanation. However, we found that a strain defected in the acs (acetyl Co-A synthetase) gene, the product of which is involved in scavenging acetate, accumulated acetate even in succinate medium and in carbon-limited low growth rate condition, where as its isogenic parental strain did not. The acs promoter was inducible in noncatabolite repression condition, whereas the expression of the ackA-pta operon encoding acetate kinase and phosphotransacetylase for acetate synthesis was constitutive. Results in this study suggest that E. coli excretes and scavenges acetate simultaneously in the carbon-limited low growth condition and in nonacetogenic carbon source, and the activity of the acetate consumption pathway directly affects the accumulation level of acetate in the culture broth.

• Journal of the korean society of oceanography
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• 제31권4호
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• pp.207-216
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• 1996

A geochemical study of three piston cores (ST.4, ST.6 and ST.20) taken from the Northwest Pacific (eastern edge of Shikoku Basin) provides information about changes in surface water paleoproductivity and sedimentation during the last 127 kys. Paleoproductivity variations were estimated on the basis of total organic carbon content and carbonate mass accumulation rate. The paleoproductivity based on total organic carbon shows significant spatial variations between glacial and interglacial periods. During the last glacial maximum (LGM) paleoproductivity increased about 1.5 times with deglaciation decrease compared with those of the Holocene at inner side of the Shikoku Basin (ST.4 and ST.6). On the other hand, paleoproductivity at outer side of Shikoku Basin (ST.20) indicating not distinctive increase but deglaciation increase. The C/N ratios fall below 10 for cores ST.4 and ST.6, but C/N ratios between 100 ka and 80 ka in ST.20 which show around 10 or larger values suggest a predominance of marine organic carbon with some admixture of terrigenous materials. The carbonate mass accumulation rate of three cores show different patterns of calcareous record with respect to organic carbon based paleoproductivity variation. In the inner side of Shikoku Basin (ST.4 and ST.6) the carbonate mass accumulation rate decreased during last glacial maximum, and significant increase of carbonate mass accumulation rate is recognized at outer side of Shikoku Basin (ST.20). Thus, this set of data reveals that spatial paleoproductivity variations between inner and outer side of Shikoku Basin during the glacial and interglacial periods.