국내 생태계 유형별 탄소 저장 및 거동 산정 연구 현황 분석

장인영,정헌모,한상학,안나현,김덕엽,강성룡 한국습지학회 2023 한국습지학회지 Vol.25 No.4

생태계는 탄소순환에 있어 매우 중요한 탄소 저장고이다. 기후변화가 점점 심화됨에 따라, 생태계의 이러한 기능을 활용하여 기후변화를 완화하려는 노력들이 진행되고 있다. 본 연구에서는 국내 생태계를 대상으로 생태계 유형(산림, 농경지, 습지, 초지, 정주지) 및 탄소저장고별(지상부·지하부 생체량, 고사목, 낙엽, 토양유기탄소 및 생태계 전체) 탄소 저장및 거동과 관련된 연구를 목록화 하고 분석하였다. 또한, 선행연구 결과를 모아 각 생태계 유형과 탄소저장고를 대상으로 탄소 저장 및 거동량의 평균값을 산정하였다. 그 결과, 대부분의(66%) 국내 탄소 저장·거동 관련 연구가 산림에서수행된 것을 확인할 수 있었다. 산림에서 수행된 연구 결과를 토대로 탄소저장고별 저장량을 분석한 결과, 식생의 지상부(4,166.66gC m-2)와 지하부(3,880.95gC m-2)와 토양(4,203.16gC m-2)에 많은 양의 탄소가 저장되어 있는 것을 확인하였다. 특히 산림 지하부에 많은 탄소가 저장되어 있는 것을 확인할 수 있었다. 다른 생태계 유형의 경우, 데이터의 제한으로 탄소저장고별 저장·거동량은 확인이 불가능하였다. 다만, 토양유기탄소 저장의 경우 산림과 초지의 데이터가 비교 가능하였는데, 두 생태계가 상대적으로 비슷한 탄소의 양을 저장하고 있는 것으로 나타났다(각각 4,203.16 gC m-2, 4,023.23 gC m-2). 본 연구를 통하여, 상대적으로 다양한 생태계 유형에서의 탄소 연구가 필요함을 확인할 수 있었다. As climate change gets severe, the ecosystem acts as an important carbon sink, therefore efforts are being made to utilize these functions to mitigate climate change. In this study, we inventoried and analyzed the previous studies related to carbon storage and flux by ecosystem type (forest, cropland, wetland, grassland, and settlement) and carbon pool (aboveground and belowground biomass, dead wood, Litter, soil organic carbon, and ecosystem) in Korean ecosystems. We also collected the results of previous studies and calculated the average value of carbon storage and flux for each ecosystem type and carbon pool. As a result, we found that most (66%) of Korea's carbon storage and fluxes studies were conducted in forests. Based on the results of forest studies, we estimated the storage by carbon stock. We found that much carbon is stored in vegetation (aboveground: 4,018.32 gC m-2 and belowground biomass: 4,095.63 gC m-2) and soil (4,159.43 gC m-2). In particular, a large amount of carbon is stored in the forest understory. For other ecosystem types, it was impossible to determine each carbon pool's storage and flux due to data limitations. However, in the case of soil organic carbon storage, the data for forests and grasslands were comparable, showing that both ecosystems store relatively similar amounts of carbon (4,159.43 gC m-2, 4,023.23 gC m-2, respectively). This study confirms the need to study carbon in rather diverse ecosystem types.

Influence of carbonized crop residue on soil carbon storage in red pepper field

Lee, Jae-Ho,Eom, Ji-Young,Jeong, Seok-hee,Hong, Seung-Bum,Park, Eun-Jin,Lee, Jae-Seok The Ecological Society of Korea 2017 Journal of Ecology and Environment Vol.41 No.12

Background: Because of climate change, interest in the development of carbon pools has increased. In agricultural ecosystems, which can be more intensively managed than forests, measures to control carbon dioxide ($CO_2$) emission and absorption levels can be applied relatively easily. However, crop residues may be released into the atmosphere by decomposition or combustion. If we can develop scientific management techniques that enable these residues to be stocked on farmland, then it would be possible to convert farmlands from carbon emission sources to carbon pools. We analyzed and investigated soil respiration (Rs) rate characteristics according to input of carbonized residue of red peppers (Capsicum annuum L.), a widely grown crop in Korea, as a technique for increasing farmland carbon stock. Results: Rs rate in the carbonized biomass (CB) section was $226.7mg\;CO_2\;m^{-2}h^{-1}$, which was 18.1% lower than the $276.9mg\;CO_2\;m^{-2}h^{-1}$ from the red pepper residue biomass (RB) section. The Rs rate of the control was $184.1mg\;CO_2\;m^{-2}h^{-1}$. In the following year, Rs in the CB section was $204.0mg\;CO_2\;m{-2}h^{-1}$, which was 38.2% lower than the $330.1mg\;CO_2\;m^{-2}h^{-1}$ from the RB section; the control emitted $198.6mg\;CO_2\;m^{-2}h^{-1}$. Correlation between Rs and soil temperature ((Ts) at a depth of 5 cm) was $R^2=0.51$ in the RB section, which was higher than the other experimental sections. A comparison of annual decomposition rates between RB and CB showed a large difference, 41.4 and 9.7%, respectively. The results showed that carbonization of red pepper residues reduced the rates of decomposition and Rs. Conclusions: The present study confirmed that the Rs rate can be reduced by carbonization of residue biomass and putting it in the soil and that the Rs rate and Ts (5 cm) were positively correlated. Based on the results, it was determined that approximately $1.2t\;C\;ha^{-1}$ were sequestered in the soil in the first year and $3.0t\;C\;ha^{-1}$ were stored the following year. Therefore, approximately $1.5t\;C\;ha^{-1}year^{-1}$ are expected to be stocked in the soil, making it possible to develop farmlands into carbon pools.

Influence of carbonized crop residue on soil carbon storage in red pepper field

이재호,엄지영,정석희,홍승범,박은진,이재석 한국생태학회 2017 Journal of Ecology and Environment Vol.41 No.12

Background: Because of climate change, interest in the development of carbon pools has increased. In agricultural ecosystems, which can be more intensively managed than forests, measures to control carbon dioxide (CO2) emission and absorption levels can be applied relatively easily. However, crop residues may be released into the atmosphere by decomposition or combustion. If we can develop scientific management techniques that enable these residues to be stocked on farmland, then it would be possible to convert farmlands from carbon emission sources to carbon pools. We analyzed and investigated soil respiration (Rs) rate characteristics according to input of carbonized residue of red peppers (Capsicum annuum L.), a widely grown crop in Korea, as a technique for increasing farmland carbon stock. Results: Rs rate in the carbonized biomass (CB) section was 226.7 mg CO2 m− 2 h− l, which was 18.1% lower than the 276.9 mg CO2 m− 2 h− l from the red pepper residue biomass (RB) section. The Rs rate of the control was 184.1 mg CO2 m− 2 h− l. In the following year, Rs in the CB section was 204.0 mg CO2 m− 2 h− l, which was 38.2% lower than the 330. 1 mg CO2 m− 2 h− l from the RB section; the control emitted 198.6 mg CO2 m− 2 h− l. Correlation between Rs and soil temperature ((Ts) at a depth of 5 cm) was R2 = 0.51 in the RB section, which was higher than the other experimental sections. A comparison of annual decomposition rates between RB and CB showed a large difference, 41.4 and 9.7%, respectively. The results showed that carbonization of red pepper residues reduced the rates of decomposition and Rs. Conclusions: The present study confirmed that the Rs rate can be reduced by carbonization of residue biomass and putting it in the soil and that the Rs rate and Ts (5 cm) were positively correlated. Based on the results, it was determined that approximately 1.2 t C ha− 1 were sequestered in the soil in the first year and 3.0 t C ha− 1 were stored the following year. Therefore, approximately 1.5 t C ha− 1 year− 1 are expected to be stocked in the soil, making it possible to develop farmlands into carbon pools.

DC-conductivity of thin films of 1,4-cis-polybutadiene doped with SiC

S.W. Tkaczyk 한국물리학회 2009 Current Applied Physics Vol.9 No.6

In this paper the results of DC-conductivity investigation of 1,4-cis-polybutadiene thin films doped with 5% weight of silicon carbonate (SiC) of nanocrystalline form with the size of grains being about 20 nm are presented. The aim of the study was to receive a knowledge about the electrical properties and DC-conductivity mechanisms depending on film thickness, temperature and electric field magnitude. The investigated films thickness ranged from 1 to 12 ㎛. The investigations were carried out for both undoped and doped with nanocrystalline SiC polymers. The current flow through the material bulk changed from 10-12 to 10-4 A with applied electric fields of 0 to 3 × 107 V/m and temperature of the film varying from 15 to 325 K. It was observed that the magnitude of the current flow through the investigated material bulk is governed by a phase state of the polymer and the presence of SiC in the bulk. The charge transport through the material bulk is controlled by the Poole-Frenkel phenomenon as well as by hopping. The determined activation energies were between kT and 0.36 eV. In this paper the results of DC-conductivity investigation of 1,4-cis-polybutadiene thin films doped with 5% weight of silicon carbonate (SiC) of nanocrystalline form with the size of grains being about 20 nm are presented. The aim of the study was to receive a knowledge about the electrical properties and DC-conductivity mechanisms depending on film thickness, temperature and electric field magnitude. The investigated films thickness ranged from 1 to 12 ㎛. The investigations were carried out for both undoped and doped with nanocrystalline SiC polymers. The current flow through the material bulk changed from 10-12 to 10-4 A with applied electric fields of 0 to 3 × 107 V/m and temperature of the film varying from 15 to 325 K. It was observed that the magnitude of the current flow through the investigated material bulk is governed by a phase state of the polymer and the presence of SiC in the bulk. The charge transport through the material bulk is controlled by the Poole-Frenkel phenomenon as well as by hopping. The determined activation energies were between kT and 0.36 eV.

Effect of the Application of Carbonized Biomass from Crop Residues on Soil Chemical Properties and Carbon Pools

이선일,박우균,김건엽,최용수 한국토양비료학회 2015 한국토양비료학회지 Vol.48 No.5

Objective of this study was to investigate the effect of carbonized biomass from crop residues on chemical properties of soil and soil carbon pools during soybean cultivation. The carbonized biomass was made by field scale mobile pyrolyzer. A pot experiment with soybean in sandy loam soil was conducted for 133 days in a greenhouse, by a completely randomized design with three replications. The treatments consisted of four levels including the control without input and three levels of carbonized biomass inputs of 9.75 Mg ha-1, C-1 ; 19.5 Mg ha-1, C-2 ; 39 Mg ha-1, C-3. Soil samples were collected and analyzed pH, EC, TC, TN, inorganic-N, available phosphorus and exchangeable cations of the soils. Soil pH, Total-N and available phosphorus contents correspondingly increased with increasing the carbonized material input. The contents of soil carbon pools were 19.04 Mg C ha-1 for C-1, 26.19 Mg C ha-1 for C-2, 33.62 Mg C ha-1 for C-3 and 12.01 Mg C ha-1 for the control at the end of experiment, respectively. Increased contents of soil carbon pools relative to the control were estimated at 7.03 Mg C ha-1 for C-1, 14.18 Mg C ha-1 for C-2 and 21.62 Mg C ha-1 for C-3 at the end of experiment, respectively, indicating that the soil carbon pools were increased with increasing the input rate of the carbonized biomass. Consequently, it seems that the carbonized biomass derived from the agricultural byproducts such as crop residues could increase the soil carbon pools and that the experimental results will be applied to the future study of soil carbon sequestration.

Effect of the Application of Carbonized Biomass from Crop Residues on Soil Chemical Properties and Carbon Pools

Sun-Il Lee,Woo-Kyun Park,Gun-Yeob Kim,Yong-Su Choi 한국토양비료학회 2015 한국토양비료학회지 Vol.48 No.5

Objective of this study was to investigate the effect of carbonized biomass from crop residues on chemical properties of soil and soil carbon pools during soybean cultivation. The carbonized biomass was made by field scale mobile pyrolyzer. A pot experiment with soybean in sandy loam soil was conducted for 133 days in a greenhouse, by a completely randomized design with three replications. The treatments consisted of four levels including the control without input and three levels of carbonized biomass inputs of 9.75 Mg ha<SUP>-1</SUP>, C-1 ; 19.5 Mg ha<SUP>-1</SUP>, C-2 ; 39 Mg ha<SUP>-1</SUP>, C-3. Soil samples were collected and analyzed pH, EC, TC, TN, inorganic-N, available phosphorus and exchangeable cations of the soils. Soil pH, Total-N and available phosphorus contents correspondingly increased with increasing the carbonized material input. The contents of soil carbon pools were 19.04 Mg C ha<SUP>-1</SUP> for C-1, 26.19 Mg C ha<SUP>-1</SUP> for C-2, 33.62 Mg C ha<SUP>-1</SUP> for C-3 and 12.01 Mg C ha<SUP>-1</SUP> for the control at the end of experiment, respectively. Increased contents of soil carbon pools relative to the control were estimated at 7.03 Mg C ha<SUP>-1</SUP> for C-1, 14.18 Mg C ha<SUP>-1</SUP> for C-2 and 21.62 Mg C ha<SUP>-1</SUP> for C-3 at the end of experiment, respectively, indicating that the soil carbon pools were increased with increasing the input rate of the carbonized biomass. Consequently, it seems that the carbonized biomass derived from the agricultural byproducts such as crop residues could increase the soil carbon pools and that the experimental results will be applied to the future study of soil carbon sequestration.

Effect of the Application of Carbonized Biomass from Crop Residues on Soil Chemical Properties and Carbon Pools

Lee, Sun-Il,Park, Woo-Kyun,Kim, Gun-Yeob,Choi, Yong-Su 한국토양비료학회 2015 한국토양비료학회지 Vol.48 No.5

Objective of this study was to investigate the effect of carbonized biomass from crop residues on chemical properties of soil and soil carbon pools during soybean cultivation. The carbonized biomass was made by field scale mobile pyrolyzer. A pot experiment with soybean in sandy loam soil was conducted for 133 days in a greenhouse, by a completely randomized design with three replications. The treatments consisted of four levels including the control without input and three levels of carbonized biomass inputs of $9.75Mg\;ha^{-1}$, C-1 ; $19.5Mg\;ha^{-1}$, C-2 ; $39Mg\;ha^{-1}$, C-3. Soil samples were collected and analyzed pH, EC, TC, TN, inorganic-N, available phosphorus and exchangeable cations of the soils. Soil pH, Total-N and available phosphorus contents correspondingly increased with increasing the carbonized material input. The contents of soil carbon pools were $19.04Mg\;C\;ha^{-1}$ for C-1, $26.19Mg\;C\;ha^{-1}$ for C-2, $33.62Mg\;C\;ha^{-1}$ for C-3 and $12.01Mg\;C\;ha^{-1}$ for the control at the end of experiment, respectively. Increased contents of soil carbon pools relative to the control were estimated at $7.03Mg\;C\;ha^{-1}$ for C-1, $14.18Mg\;C\;ha^{-1}$ for C-2 and $21.62Mg\;C\;ha^{-1}$ for C-3 at the end of experiment, respectively, indicating that the soil carbon pools were increased with increasing the input rate of the carbonized biomass. Consequently, it seems that the carbonized biomass derived from the agricultural byproducts such as crop residues could increase the soil carbon pools and that the experimental results will be applied to the future study of soil carbon sequestration.

배 과수원에서 전정가지 유래 탄화물 시용이 토양 탄소 축적에 미치는 영향

이선일 ( Sun Il Lee ),이종식 ( Jong Sik Lee ),김건엽 ( Gun Yeob Kim ),최은정 ( Eun Jung Choi ),서상욱 ( Sang Uk Suh ),나운성 ( Un Sung Na ) 한국환경농학회 2016 한국환경농학회지 Vol.35 No.3

과수원에서 발생하는 전정가지 부산물로부터 생산한 바이오매스 탄화물의 토양내 처리효과를 구명하기 위하여 배 전정가지를 활용하여 탄화물을 생산하고 이를 배 과원 토양에 투입하여 토양 화학성 변화와 토양 탄소 저장 잠재량을 비교 검토하였다. 배 전정가지 유래 탄화물은 방향족 화합물 형태를 유지하고 탄소함량도 62%로 매우 높았으며, 과원 토양의 유기물함량은 탄화물의 투입량이 많을수록 통계적으로 유의하게 증가하였다. 탄화물 투입 166일 후 토양 탄소저장 잠재량은 바이오매스 탄화물 시용 수준이 높을수록 증가하는 경향을 나타냈으며, 통계적으로 유의한 차이를 나타냈다. 대조 구, C-1 그리고 C-2 처리구에서 각각 토양 탄소저장 잠재량은 40.1, 49.3 그리고 57.8 Mg/ha으로 나타났다. 토양 탄소저장 잠재량은 탄화물 투입량에 따라 고도로 높은 상관관계(P < 0.001)를 나타내며 증가하였다. 기울기가 1.496인 1차 회귀방정식을 나타냈으며, 탄화물 투입량이 100 kg/ha 높아 질수록 토양 탄소 저장 잠재량은 0.1496 Mg/ha 증가하였다. 이러한 결과를 미루어 볼 때 장기간 동안 지속적으로 바이오 매스 탄화물을 시용한다면 토양 탄소의 중요한 공급원이 되며 결론적으로 농경지가 토양 탄소저장원으로서의 역할을 할 수 있을 것으로 판단된다. BACKGROUND: Carbonized biomass is increasingly used as a tool of soil carbon sequestration. The objective of this study was to evaluate soil carbon storage to application of carbonized biomass derived from pear tree pruning. METHODS AND RESULTS: The carbonized biomass was a mobile pyrolyzer with field scale, which a reactor was operated about 400~500℃ for 5 hours. The treatments were consisted of a control without input of carbonized biomass and two levels of carbonized biomass inputs as 6.06 Mg/ha, C-1 and 12.12 Mg/ha, C-2. It was shown that the soil carbon pools were 49.3 Mg/ha for C-1, 57.8 Mg/ha for C-2 and 40.1 Mg/ha for the control after experimental periods. The contents of accumulated soil carbon pool were significantly (P < 0.001) increased with enhancing the carbonized biomass input amount. The slopes (1.496) of the regression equations are suggested that carbon storage from the soil was increased about 0.1496 Mg/ha with every 100 kg/ha of carbonized biomass input amount. CONCLUSION: Our results suggest that application of carbonized biomass would be increased the soil carbon contents due to a highly stable C-matrix of carbonized biomass. More long-term studies are needed to be proved how long does carbon stay in orchard soils.

Assessment of Carbon Sequestration Potential in Degraded and Non-Degraded Community Forests in Terai Region of Nepal

Rajeev Joshi,Hukum Singh,Ramesh Chhetri,Karan Yadav 강원대학교 산림과학연구소 2020 Journal of Forest Science Vol.36 No.2

This study was carried out in degraded and non-degraded community forests (CF) in the Terai region of Kanchanpur district, Nepal. A total of 63 concentric sample plots each of 500 m2 was laid in the inventory for estimating above and below-ground biomass of forests by using systematic random sampling with a sampling intensity of 0.5%. Mallotus philippinensis and Shorea robusta were the most dominant species in degraded and non-degraded CF accounting Importance Value Index (I.V.I) of 97.16 and 178.49, respectively. Above-ground tree biomass carbon in degraded and non-degraded community forests was 74.64±16.34 t ha-1 and 163.12±20.23 t ha-1, respectively. Soil carbon sequestration in degraded and non-degraded community forests was 42.55±3.10 t ha-1 and 54.21±3.59 t ha-1, respectively. Hence, the estimated total carbon stock was 152.68±22.95 t ha-1 and 301.08±27.07 t ha-1 in degraded and non-degraded community forests, respectively. It was found that the carbon sequestration in the non-degraded community forest was 1.97 times higher than in the degraded community forest. CO2 equivalent in degraded and non-degraded community forests was 553 t ha-1 and 1105 t ha-1, respectively. Statistical analysis showed a significant difference between degraded and non-degraded community forests in terms of its total biomass and carbon sequestration potential (p<0.05). Studies indicate that the community forest has huge potential and can reward economic benefits from carbon trading to benefit from the REDD+/CDM mechanism by promoting the sustainable conservation of community forests.

Effect of Long Term Fertilization on Soil Carbon and Nitrogen Pools in Paddy Soil

Lee, Chang Hoon,Jung, Ki Youl,Kang, Seong Soo,Kim, Myung Sook,Kim, Yoo Hak,Kim, Pil Joo Korean Society of Soil Science and Fertilizer 2013 한국토양비료학회지 Vol.46 No.3

Fertilizer management has the potential to promote the storage of carbon and nitrogen in agricultural soils and thus may contribute to crop sustainability and mitigation of global warming. In this study, the effects of fertilizer practices [no fertilizer (Control), chemical fertilizer (NPK), Compost, and chemical fertilizer plus compost] on soil total carbon (TC) and total nitrogen (TN) contents in inner soil profiles of paddy soil at 0-60 cm depth were examined by using long-term field experimental site at $42^{nd}$ years after installation. TC and TN concentrations of the treatments which included N input (NPK, Compost, NPK+Compost) in plow layer (0-15 cm) ranged from 19.0 to 26.4 g $kg^{-1}$ and 2.15 to 2.53 g $kg^{-1}$, respectively. Compared with control treatment, SOC (soil organic C) and TN concentrations were increased by 24.1 and 31.0%, 57.6 and 49.7%, and 72.2 and 54.5% for NPK, Compost, and NPK+Compost, respectively. However, long term fertilization significantly influenced TC concentration and pools to 30 cm depth. TC and TN pools for NPK, Compost, NPK+Compost in 0-30 cm depth ranged from 44.8 to 56.8 Mg $ha^{-1}$ and 5.78 to 6.49 Mg $ha^{-1}$, respectively. TC and TN pools were greater by 10.5 and 21.4%, 30.3 and 29.6%, and 39.9 and 36.3% in N input treatments (NPK, Compost, NPK+Compost) than in control treatment. These resulted from the formation and stability of aggregate in paddy soil with continuous mono rice cultivation. Therefore, fertilization practice could contribute to the storage of C and N in paddy soil, especially, organic amendments with chemical fertilizers may be alternative practices to sequester carbon and nitrogen in agricultural soil.