• Journal of Wetlands Research
• /
• v.25 no.4
• /
• pp.417-425
• /
• 2023

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.

• Journal of the Korea Organic Resources Recycling Association
• /
• v.30 no.1
• /
• pp.5-11
• /
• 2022

This research evaluated the long-term application effects of different soil amendments on yield, dissolved organic carbon, nitrogen and soil organic carbon stock in rice paddy. The experiment consisted of four different fertilizations; Inorganic fertilization (NPK), NPK+Lime (NPKL), NPK+Silicate (NPKS), NPK+Compost (NPKC). There was no significant difference in rice yield between the treatment groups in 1995, but the rice yields in the NPKL and NPKC treatments in 2019 increased by 4.3% and 14.3% compared to NPK. In terms of soil properties, the pH of NPKS(6.7) and NPKL(6.4) in 2019 increased the most compared to the soil pH before experiment(5.2). The organic matter(OM) content from NPKC treatment increased upto 34 and 27 g kg^-1 in year of 1995 and 2019, respectively, compared to before the test. In NPKS and NPKL treatment, labile carbon and nitrogen content, used as a soil quality indicator, increased by 1.1-1.9 times over the control. From these result, it is suggested that type and application rate of soil amendment should be determined based on the soil analysis before cultivation for sustainable agricultural environment and productivity.

• Korean Journal of Soil Science and Fertilizer
• /
• v.16 no.4
• /
• pp.368-371
• /
• 1983

Energy rich rice straw was subjected to biological processes involving the transformation of added nitrogen. A part of soil ammonium nitrogen was steadily exhausted when energy rich rice straw was decomposed. More vigorous transformation of added nitrogen ocurred during the first 5 days of incubation period than after 10 days of incubation period. Furthermore, transformation of added nitrogen occurred more markedly when more rice straw and less nitrogen were added. Remineralization of immobilized nitrogen did not take place in this experiment with 50 days of incubation.

• Journal of Wetlands Research
• /
• v.12 no.2
• /
• pp.59-65
• /
• 2010

Wetlands are a well known ecosystem which have high spatial-temporal heterogeneity of chemical characteristics. This high heterogeneity induces diverse biogeochemical processes, such as aerobic decomposition, denitrification, and plant productivity in wetlands. Understanding the dynamics of dissolved organic carbon (DOC) and inorganic nitrogen in wetlands is important because DOC and inorganic nitrogen are main factors controlling biological processes in wetlands. In this study, we assessed spatial distribution of DOC and inorganic nitrogen with relation to the different hydrology and vegetation in created wetlands. Both DOC and nitrate contents were significantly higher in vegetated areas than open areas. Different water levels also affected DOC contents and their quality. Average DOC contents were $0.37mg{\cdot}g^{-1}$ in deep riparian (DR) and $0.31mg{\cdot}g^{-1}$ in shallow riparian (SR). These results appeared to be related to the interaction between carbon supply by vegetation and microbial decomposition. On the other hand, inorganic nitrogen contents were not affected by water level differences. This result indicates that presence/absence of vegetation could be a more important factor than hydrology in the spatial dynamics of inorganic nitrogen. In conclusion, we observed that vegetation and hydrology differences induced spatial distribution of carbon and nitrogen which are directly related to biogeochemical processes in wetlands.

• Journal of The Korean Society of Grassland and Forage Science
• /
• v.4 no.3
• /
• pp.220-225
• /
• 1984

In the grassland ecosystem dominated by Phragmites longivalvis in the delta of Nak Dong River, the production, decomposition, and accumulation of organic were estimated by the theoretical analysis. The amounts of organic carbon and organic matter of litter are $1020.43g/m^2\;and\;591.90g/m^2$, respectively. The amounts of organic matter and organic carbon on the grassland floor is $1154.96g/m^2\;and\;669.93g/m^2$, the ratio of annual litter production 'L' to the amount of accumulation on the top mineral soil (F, H and $A_2$ horizons) provided estimates of decay constant k. Constant k is 0.884 in the Phragmites longivalvis community. The vertical levels of organic matter and organic carbon is the highest in 120-140 cm of photosythetic system and in 0-20 cm of non-photosyntic system.

• Journal of Korean Society of Environmental Engineers
• /
• v.35 no.12
• /
• pp.897-905
• /
• 2013

In this study, sorption coefficients (${\log}K_{OC}$, n) for the binding of phenanthrene (PHE) to soil humins, insoluble fraction of soil humc substances (HS), were determined and relationship between the sorption coefficients and structural characteristics of the soil humins were investigated. The soil humins used in the present study were isolated from 7 different soils including 5 domestic soils, an IHSS standard and a peat soil, and characterized by elemental analysis and CPMAS $^{13}C$ NMR method. $^{13}C$ NMR spectral features indicate that the soil humins are mainly made up of aliphatic carbons (57.1~72.3% in total carbon) with high alkyl-C moiety, and the alkyl-C contents ($C_{Al-H,C}$, %) was in order of granite soil Hu (26~42%) > volcanic ash soil, HL Hu (23.9%) > Peat Hu (14.0%). The results of correlation study show that a positive relationship ($r^2$ = 0.77, p < 0.05) between organic carbon normalized-sorption coefficients ($K_{OC}$, mL/g) and alkyl-C contents($C_{Al-H,C}$, %), while negative relationship ($r^2$ = (-)0.74, p < 0.05) between Freundlich sorption parameter (n) and H,C-substituted aromatic carbon contents ($C_{Ar-H,C}$, %). The magnitude of $K_{OC}$ values are also negatively well correlated with polarity index (e.g., PI, N + O)/C) ($r^2$ = (-)0.74, p < 0.1). These results suggest that the binding capacity (e.g., $K_{OC}$) for PHE is increased in soil humin molecules having high contents of alkyl-C or lower polarity, and nonlinear sorption for PHE increased as the H,C-substituted aromatic carbon contents ($C_{Ar-H,C}$, %) in the soil humins increased. The PHE sorption characteristics on soil humins are discussed based on the dual reactive mode of sorption model.

• Journal of Wetlands Research
• /
• v.17 no.3
• /
• pp.283-292
• /
• 2015

The total global emission of $CO_2$ from soils is recognized as one of the largest fluxes in the global carbon cycle. Especially it is necessary to quantify the amount of $CO_2$ emitted by the organic material decomposition processes of microorganisms in the soil, because it becomes one of a factor for determining the carbon stocks in the soil. This study was conducted to estimate the impact of the Korean water deer(Hydropotes inermis)' feces to the soil organic matter. Also, effects of Korean water deer' feces on $CO_2$ emissions of soil and land use pattern dependent $CO_2$ flux quantification are studied. The organic materials in the Korean water deer' feces significantly changed organic matter content of soil and influenced the activity of soil microorganisms, both changing of respiration of the soil and physical chemical components in soil. In particular, C/N ratio and the $CO_2$ flux of soil of four regions (Rice paddy, Fallow ground, Salix koreensis community, Phragmites australis community) showed a statistically highly significant correlation (P<0.01) with the presence or absence of feces. $CO_2$ flux of soil affected by the feces was 2-20 times higher than the soil unaffected by the feces. This study has great significance to quantify the extent of the material circulation and its impact to the terrestrial ecosystem and soil zone throughout Korean water deer' feces. Feces of wildlife can affect soil and soil material circulation.

• Korean Journal of Organic Agriculture
• /
• v.19 no.2
• /
• pp.229-243
• /
• 2011

Consumers' interest and government's support for the fruits rapidly increased organic fruit productions. This study was examined to compare the soil physicochemical and microbial properties of orchards soil in conventionally and organically management systems. Organic cultivation had lower soil bulk density, solid phase, and penetration resistance than the conventional cultivation. Soil pH and organic matter contents increased from March to August, and the values were greater in the organic cultivation than the conventional cultivation. Total nitrogen (N) and phosphorous concentrations decreased from March to August, and the organic soils had greater N but lower phosphorous concentrations than the conventional soils. Soil microbial carbon biomass increased 36% and 15% for organic and conventional cultivations, respectively, from March to August. Soil microbial N biomass was greater in June than March or August, and the organic cultivation had a greater biomass N compared to the conventional cultivation. Soil dehydrogenase and chitinase activities were greater in June than in March or August. ${\beta}$-glucosidase activity declined in both cultivations, while the phosphatase activity increased. Organic cultivation had greater enzyme activities in March, June, and August, except for the acid phosphatase activity in June.

• Journal of Korean Society of Forest Science
• /
• v.105 no.1
• /
• pp.1-11
• /
• 2016

Globally, there are more than 2600 species of termites which adapted plenty of terrestrial ecosystems by various strategies such as making termite nest and society. Various studies were recently carried out on termites because they play significant roles in the context of carbon (C) cycle of terrestrial ecosystems. According to the results of previous studies, termite activities influenced the amount of soil organic C, methane emission, and organic matter decomposition. Termite nests, where termite biomass was concentrated, exhibited 1.8 times higher soil organic C concentration than reference soils, and emitted $0.0-6.0kg\;ha^{-1}year^{-1}$ of methane in tropical forests and savannas. Feeding activity of termites, in addition, accelerated coarse woody debris (CWD) decomposition by increasing the surface area to volume ratio of CWD. Especially, CWD decomposition induced by the Rhinotermitidae family appeared to be significant for the C cycle in temperate forests. However, more studies should be conducted on termite-induced CWD decomposition in temperate forests because few studies have dealt with it. The termite-induced CWD decomposition could be measured by preparing disc-shaped CWD samples, excluding access of termites to the CWD samples, and comparing the decomposition rate of the CWD samples with and without the termite exclusion treatment. Studies on the termite-induced CWD decomposition would contribute to further elucidation of the C cycle in temperate forests.

• Journal of the Korean Chemical Society
• /
• v.27 no.1
• /
• pp.31-37
• /
• 1983

The consumption of atmospheric carbon monoxide by soil was measured under laboratory conditions in different types of soils. Laboratory experiments were performed with humus containing high proportion of organic matter, roadside soils, and humus and roadside soils previously exposed to high concentration of CO by reusing in the experiment. CO concentrations in the 18.2 l-reaction vessel were varied from 2,000 ppm to 24,000ppm to estimate the effectiveness of CO consumption at high level of CO. The uptake of CO by soil was measured by gas chromatography using a TCD detector. The control experiments conducted along with the soil experiments evidently indicated that the potting soil is responsible for CO consumption. Humus showed much higher CO uptake rates compared with the soil taken from roadside. The humus reused in the experiment showed somewhat higher rates(15%) of uptake than the fresh one. The soil's ability to remove CO from the test atmosphere reached a maximum near the CO concentration of 13,000 ppm in the range of $9,000~24,000ppm$. The addition of streptomycin did not influence the removal capacity of soil significantly, whereas 10% saline solution remarkably prevented CO uptake of the humus sample.