한라산 아고산대 구상나무군락의 물질생산과 탄소수지

장래하 ( Rae Ha Jang ),최재윤 ( Jae Yun Choi ),유영한 ( Young Han You ) 한국환경생태학회 2014 한국환경생태학회 학술대회지 Vol.2014 No.2

본 연구는 우리나라 한라산 아고산대에서 구상나무림의 물질생산, 탄소분포와 탄소수지에 대하여 알아보기 위해 수행되었다. 구상나무림의 현존량은 2009, 2010, 2011, 2012 와 2013에 각각 98. 88, 106. 42, 107. 67, 108. 31와 91. 48ton/ha 유기탄소량은 44. 5, 47. 89, 48. 45, 48. 74와 41. 17 ton C/ha 이었다. 순생산량은 2009, 2010, 2011, 2012 년에 각각 11. 40, 7. 41, 0. 05 와 -9. 46 ton ha-1yr-1 이었고, 유기탄소 순생산량은 5. 13, 3. 33, 0. 02와 -4. 25 ton C ha-1yr-1 이었다. 2009~2013년 연간 낙엽생산량은 각각 2. 42, 4. 02, 2. 94, 5. 47, 2. 67 ton ha-1yr-1이었고, 낙엽생산량의 유기탄소량은 1. 09, 1. 80, 1. 32, 2. 46, 1. 20 ton C ha-1yr-1. 연간 임상낙엽량 6. 09, 5. 40, 4. 45, 2. 57 ton/ha 임상냑엽량의 유기탄소량은 2. 74, 2. 43, 2. 00, 1. 16 ton C/ha. 토양 20cm까지의 유기탄소축척량은 각각 55. 77, 54. 90, 50. 69, 44. 42, 41. 87 ton C ha-120cm-1. 2012년 토양호흡을 통해 배출된 유기탄소량은 2011, 2012년에 각각 4. 42, 4. 14 ton Cha-1yr-1 이었다. 한라산 구상나무림에서는 2011년에 총 0. 01 ton C ha-1yr-1의 유기탄소를 대기로 방출하였고 2012년에 -8. 39 ton C ha-1yr-1의 유기탄소를 대기로 배출하였다.

한라산 아고산대 구상나무림에서 연간 물질생산과 유기탄소량 변화1a

장래하 ( Rae Ha Jang ),조규태 ( Kyu Tae Cho ),유영한 ( Young Han You ) 한국환경생태학회 2014 한국환경생태학회지 Vol.28 No.6

국가장기생태사업(LTER)의 일환으로 한라산 아고산대 구상나무림의 물질생산과 탄소분포의 특성을 밝히고자 2009년부터 2013년까지 현존량, 유기탄소분포, 낙엽생산, 임상낙엽량과 토양 유기탄소 축척량을 조사하였다. 식물현존량은 상대생장법에 의해 보고된 물질생산 식을 이용하여 측정하고 이를 이산화탄소의 고정량으로 환산하였다. 2009, 2010, 2011, 2012 와 2013년의 현존량은 각각 98.88, 106.42, 107.67, 108.31 와 91.48 ton ha-1 였다. 이 기간 동안의 유기탄소는 지상부 생물량에 35.95, 38.69, 38.96, 39.46, 33.2 ton C ha-1, 지하부 생물량에 8.54, 9.2, 9.49, 9.28, 7.97 ton C ha-1 이 각각 분포하였다. 5년 동안 낙엽 생산을 통해 1.09, 1.80, 1.32, 2.46 와 1.20 ton C ha-1 의 유기탄소가 생태계로 유입되었다. 2010, 2011, 2012와 2013년의 임상낙엽층의 유기탄소량은 2.74, 2.43, 2.00 와 1.16 ton Cha-1였고, 토양 20cm깊이까지의 유기탄소 축적량은 55.77, 54.90, 50.69, 44.42 와 41.87 ton C ha-120cm-1였다. 이와 같이 현존량과 유기탄소량이 2009~2012년까지 매년 증가하였지만 태풍이 있었던 2013년에는 감소하였다. 이러한 현상은 자연적 교란이 한국의 아고산대 생태계에 크게 영향을 미친다는 것을 의미한다. Annual biomass production and amount of organic carbon in Abies koreana forest at Mt. Halla were conducted as a part of Korea National Long-Term Ecological Research (KNLTER). We measured standing biomass change of litter, soil production and organic carbon amounts of the forest floor and soil layer of A. koreana forest in Mt. Halla from 2009 to 2013 in permanent plots. Standing biomass, which was determined by allometric method, was converted into CO2. The standing biomass in A. koreana forest was 98.88, 106.42, 107.67, 108.31, 91.48 ton ha-1 in 2009, 2010, 2011, 2012 and 2013 year, respectively. The amount of annual carbon allocated to above ground was 35.95, 38.69, 38.96, 39.46, 33.2 ton C ha-1 and below ground biomass was 8.54, 9.2, 9.49, 9.28, 7.97 ton C ha-1 in 2009, 2010, 2011, 2012 and 2013 year, respectively. Amount of organic carbon returned to the forest via litterfall was 1.09, 1.80, 1.32, 2.46 and 1.20 ton C ha-1 in 2009, 2010, 2011, 2012 and 2013. Amount of organic carbon in annual litter layer on forest floor was 2.74, 2.43, 2.00 and 1.16 ton C ha-1 in 2010, 2011, 2012 and 2013 year, respectively. Amount of organic carbon within 20cm soil depth was 55.77, 54.9, 50.69, 44.42 and 41.87 ton C ha-120cm-1 in 2009, 2010, 2011, 2012 and 2013 year, respectively. Then standing biomass and organic carbon distribution increased steadily until 2012. But there declined in 2013 because of the typhoon Bolaven. Thus, standing biomass and organic carbon distribution of this subalpine forest were largely affected by natural disturbance factor.

Valuation of ecosystem services in the organic carbon of the Pinus densiflora forest at Mt. Namsan, Seoul Metropolitan City

Lee, Eung-Pill,Lee, Soo-In,Jeong, Heon-Mo,Han, Young-Sub,Lee, Seung-Yeon,Park, Jae-Hoon,Jang, Rae-Ha,Hong, Youg-Sik,Jung, Young-Ho,Kim, Eui-Joo,Lee, Sang-Hun,You, Young-Han The Ecological Society of Korea 2019 Journal of Ecology and Environment Vol.43 No.4

Background: Standing biomass, litter production, rate of litter decomposition, amount of litter on forest floor, and amount of soil organic carbon distribution were investigated from March 2016 to November 2018 in order to evaluate the ecosystem value through organic carbon distribution in the Pinus densiflora forest at Namsan, Seoul Metropolitan City. Results: The amount of organic carbon in the Pinus densiflora forest was 261.09 ton C ha^-1 during the research period, and fixed organic carbon in plant through net photosynthesis was 3.2 ton C ha^-1 year^-1. The organic carbon in plant was 62.77 ton C ha^-1 (24.04%), in litter on the forest floor was 3.65 ton C ha^-1 (1.40%), and in soil was 194.67 ton C ha^-1 (74.56%). The value of plant, litter on forest floor, and soil organic carbon distribution were each 6,277,000 won ha^-1, 365, 000 won ha^-1, and 19,467,000 won ha^-1. The value per ton of fixed organic carbon in plant through net photosynthesis was 320,000 won ha^-1 year^-1 and the value of ecosystem services stored in carbon in the Namsan forest ecosystem was about 26.1 million won ha^-1 for 3 years. Conclusions: The results of this study suggest that the pine forests of Namsan rapidly decompose leaves due to the high atmospheric temperature and accumulate a large amount of organic carbon in the soil to provide climate control regulatory service function.

Budget and distribution of organic carbon in Taxus cuspidata forest in subalpine zone of Mt. Halla

Jang, Rae-Ha,Jeong, Heon-Mo,Lee, Eung-Pill,Cho, Kyu-Tae,You, Young-Han The Ecological Society of Korea 2017 Journal of Ecology and Environment Vol.41 No.1

Background: In order to investigate organic carbon distribution, carbon budget, and cycling of the subalpine forest, we studied biomass, organic carbon distribution, litter production, forest floor litter, accumulated soil organic carbon, and soil respiration in Taxus cuspidata forest in Halla National Park from February 2012 to November 2013. Biomass was calculated by using allometric equation and the value was converted to $CO_2$ stocks. Results: The amount of plant organic carbon was $13.60ton\;C\;ha^{-1}year^{-1}$ in 2012 and $14.29ton\;C\;ha^{-1}year^{-1}$ in 2013. And average organic carbon introduced to forest floor through litter production was $0.71ton\;C\;ha^{-1}year^{-1}$. Organic carbon distributed in forest floor litter layer was $0.73ton\;C\;ha^{-1}year^{-1}$ on average and accumulated organic carbon in soil was $51.13ton\;C\;ha^{-1}year^{-1}$ on average. In 2012, Amount of released $CO_2$ from soil to atmosphere was 10.93 ton $CO_2ha^{-1}year^{-1}$. Conclusions: The net ecosystem production based on the difference between net primary production of organic carbon and soil respiration was $-1.74ton\;C\;ha^{-1}year^{-1}$ releasing more carbon than it absorbed.

Organic carbon distribution and budget of dominant woody plant community in the subalpine zone at volcanic Jeju Island, Korea

Jang, Rae-Ha,Lee, Seung-Yeon,Lee, Eung-Pill,Lee, Soo-In,Kim, Eui-Joo,Lee, Sang-Hun,You, Young-Han The Ecological Society of Korea 2019 Journal of Ecology and Environment Vol.43 No.4

Background: The Northern Hemisphere forest ecosystem is a major sink for atmospheric carbon dioxide, and the subalpine zone stores large amounts of carbon; however, their magnitude and distribution of stored carbon are still unclear. Results: To clarify the carbon distribution and carbon budget in the subalpine zone at volcanic Jeju Island, Korea, we report the C stock and changes therein owing to vegetation form, litter production, forest floor, and soil, and soil respiration between 2014 and 2016, for three subalpine forest ecosystems, namely, Abies koreana forest, Taxus cuspidata forest, and Juniperus chinensis var. sargentii forest. Organic carbon distribution of vegetation and NPP were bigger in the A. koreana forest than in the other two forests. However, the amount of soil organic carbon distribution was the highest in the J. chinensis var. sargentii forest. Compared to the amount of organic carbon distribution (AOCD) of aboveground vegetation (57.15 t C ha^-1) on the subalpine-alpine forest in India, AOCD of vegetation in the subalpine forest in Mt. Halla was below 50%, but AOCD of soil in Mt. Halla was higher. We also compared our results of organic carbon budget in subalpine forest at volcanic island with data synthesized from subalpine forests in various countries. Conclusions: The subalpine forest is a carbon reservoir that stores a large amount of organic carbon in the forest soils and is expected to provide a high level of ecosystem services.

Budget and distribution of organic carbon in Quercus serrata Thunb. ex Murray forest in Mt. Worak

Lee, Seung-Hyuk,Jang, Rae-Ha,Cho, Kyu-Tae,You, Young-Han The Ecological Society of Korea 2015 Journal of Ecology and Environment Vol.38 No.4

The carbon cycle came into the spotlight due to the climate change and forests are well-known for their capacity to store carbon amongst other terrestrial ecosystems. The annual organic carbon of litter production, forest floor litter layer, soil, aboveground and belowground part of plant, standing biomass, net primary production, uptake of organic carbon, soil respiration, etc. were measured in Mt. Worak in order to understand the production and carbon budget of Quercus serrata forest that are widely spread in the central and southern part of the Korean Peninsula. The total amount of organic carbon of Q. serrata forest during the study period (2010-2013) was 130.745 ton C ha^-1. The aboveground part of plant, belowground part of plant, forest floor litter layer, and organic carbon in soil was 50.041, 12.510, 4.075, and 64.119 ton C ha^-1, respectively. The total average of carbon fixation in plants from photosynthesis was 4.935 ton C ha^-1 yr^-1 and organic carbon released from soil respiration to microbial respiration was 3.972 ton C ha^-1 yr^-1. As a result, the net ecosystem production of Q. serrata forest estimated from carbon fixation and soil respiration was 0.963 ton C ha^-1 yr^-1. Therefore, it seems that Q. serrata forest can act as a sink that absorbs carbon from the atmosphere. The carbon uptake of Q. serrata forest was highest in stem of the plant and the research site had young forest which had many trees with small diameter at breast height (DBH). Consequentially, it seems that active matter production and vigorous carbon dioxide assimilation occurred in Q. serrata forest and these results have proven to be effective for Q. serrata forest to play a role as carbon storage and NEP.

Soil CO₂ efflux in a warm-temperature and sub-alpine forest in Jeju, South Korea

Jeong, Heon-Mo,Jang, Rae-Ha,Kim, Hae-Ran,You, Young-Han The Ecological Society of Korea 2017 Journal of Ecology and Environment Vol.41 No.6

Background: This study investigated the temporal variation in soil $CO_2$ efflux and its relationship with soil temperature and precipitation in the Quercus glauca and Abies koreana forests in Jeju Island, South Korea, from August 2010 to December 2012. Q. glauca and A. koreana forests are typical vegetation of warm-temperate evergreen forest zone and sub-alpine coniferous forest zone, respectively, in Jeju island. Results: The mean soil $CO_2$ efflux of Q. glauca forest was $0.7g\;CO_2\;m^{-2}\;h^{-1}$ at $14.3^{\circ}C$ and that of A. koreana forest was $0.4g\;CO_2\;m^{-2}\;h^{-1}$ at $6.8^{\circ}C$. The cumulative annual soil $CO_2$ efflux of Q. glauca and A. koreana forests was 54.2 and $34.2t\;CO_2\;ha^{-1}$, respectively. Total accumulated soil carbon efflux in Q. glauca and A. koreana forests was 29.5 and $18.7t\;C\;ha^{-1}$ for 2 years, respectively. The relationship between soil $CO_2$ efflux and soil temperate at 10 cm depth was highly significant in the Q. glauca ($r^2=0.853$) and A. koreana forests ($r^2=0.842$). Soil temperature was the main controlling factor over $CO_2$ efflux during most of the study period. Also, precipitation may affect soil $CO_2$ efflux that appeared to be an important factor controlling the efflux rate. Conclusions: Soil $CO_2$ efflux was affected by soil temperature as the dominant control and moisture as the limiting factor. The difference of soil $CO_2$ efflux between of Q. glauca and A. koreana forests was induced by soil temperature to altitude and regional precipitation.

남산의 소나무림, 신갈나무림, 아까시나무림의 낙엽생산과 토양유기탄소 동태

정헌모 ( Heon Mo Jeong ),김해란 ( Hae Ran Kim ),신동훈 ( Dong Hoon Shin ),이경미 ( Kyoung Mi Lee ),이승혁 ( Seung Hyuk Lee ),한영섭 ( Young Sub Han ),장래하 ( Rae Ha Jang ),이상경 ( Sang Kyeong Lee ),김태규 ( Tae Kyu Kim ),유영한 한국환경생물학회 2013 환경생물 : 환경생물학회지 Vol.31 No.2

남산의 소나무림, 신갈나무림 그리고 아까시나무림에서 2008년 1월부터 2009년 12월까지의 월별 낙엽생산량과 토양의 유기탄소량을 조사하였다. 소나무림은 2008년과 2009년 모두 10월에 낙엽생산량이 가장 많았으며, 2008년 1월과 2009년 12월에 낙엽생산량이 가장 적었다. 신갈나무림은 2008년과 2009년 모두 11월에 낙엽생산량이 가장 많았으며, 2월에 낙엽생산량이 가장 적었다. 아까시나무림은 2008년 11월과 2009년 10월에 낙엽생산량이 가장 많았으며, 2008년 1월과 2009년 12월에 낙엽생산량이 가장 적었다. 이것은 한반도 중부에서 상록성의 소나무림이 낙엽성의 참나무숲 보다 더 일찍 낙엽이 진다는 것을 의미한다. 소나무림과 신갈나무림, 아까시나무림의 2년 평균의 낙엽생산량은 7.07, 6.36, 5.02 ton ha-1로 소나무가 가장 많았다. 소나무림과 신갈나무림, 아까시나무림의 2년 평균의 토양유기탄소량은 76.2, 68.6, 72.5 ton C ha-1로 소나무림에서 가장 많았다. 이처럼 소나무숲에서 높게 나타난 것은 남산에서 신갈나무나 아까시나무를 벌목하여 임목밀도가 줄었기 때문이다. The objective of this study was to estimate dynamics of litter production and soil organic carbon of Pinus densiflora forest, Quercus mongolica forest, and Rhobina pseudo-acasia forest at Mt. Nam as a part of Korea National Long-Term Ecological Research (KNLTER) from 2008 to 2009. Litter production of P. densiflora forest was the highest in October 2008, 2009 and the lowest in January 2008 and December 2009. Litter production of Q. mongolica forest was the highest in November and the lowest in February in 2008 and 2009. Litter production of R. pseudo-acacia forest was the highest in November in 2008 and October in 2009 and the lowest in January in 2008 and December in 2009. It means that leaves of P. densiflora forest shed earlier than deciduous oak forests in Korean central region. An average of litter production for 2 years was 7.07, 6.36, 4.66 ton ha-1 in P. densiflora forest, Q. mongolica forest, R. psuedo-acacia forest, respectively. An average of soil organic carbon matter for 2 years was 88.3, 76.5, 84.2 ton ha-1 in P. densiflora forest, Q. mongolica forest, R. psuedo-acacia forest, respectively.

중추신경계 손상시 GFAP의 발현에 대한 고찰

하미숙,박수경,박래준 대구대학교 특수교육재활과학연구소 2007 再活科學硏究 Vol.25 No.1

이 연구는 중추신경 손상에 대한 문헌적 고찰을 통해 아교 섬유성 산 단백질(glial fibrillary acidic protein : GFAP)에 대한 이해와 경과 시간에 따른 발현시기 등을 알아보고자 한다. GFAP는 별아교세포에만 특이적으로 염색되어 별아교세포의 특이적 표지물질(specific marker)로 사용되어 지고 있다. GFAP의 발현정도가 손상 후 1주일째까지 가장 현저히 증가하는 것으로 보아 손상 초기에 물리치료적 중재를 통해 중추신경계의 기능회복에 있어서 좋은 결과를 얻을 수 있다. Purpose : The purpose of this study was to uderstand the glial fibrillary acidic protein through literature review about CNS injury. Method : This is a western bolt analysis, immunocytochemical analysis and double immunofluorescence for glial fibrillary acidic protein were performed after CNS injury. Result : The GFAP expression level in the gray matter increased in the early stage of injury. In contrast the GFAP expressoin level in the gray matter decreased in the late stage of injury. Conclusion : The study of GFAP is the intermediate filament of the glial cells and useful as a marker for the astrocytes. Also, the upregulation of GFAP espression required various physical therapeutic approaches.

모노에탄올아민 전처리에 의한 양모섬유의 저온염색

하민자,이내연 충남대학교 1991 論文集 Vol.14 No.1

The dyeing properties of wool pretreated with monoethanolamine and neutralized with formic acid were investigated. The experiments were performed using Orange Ⅱ(C.I. Acid Orange 7) for various temperatures(40°, 50°, 60℃) at pH 4.7. The apparent diffusion coefficients of preteated wool were larger than untreated wool and the apparent activation energy of diffusion of pretreated and untreated wool were 19.7 K㎈/㏖, 28.3 K㎈/㏖, respectively. According to the dye absorption and dye exheastion curve, the temperature dyeing of preteated wool might be possible at 50℃ for about 1 hours.