• 한국농림기상학회지
• /
• 제11권4호
• /
• pp.247-251
• /
• 2009

강우가 토양 호흡에 미치는 영향을 평가하기 위해, 일본 서부에 위치한 활엽수림에서 2001년 2월 20일부터 11월 19일까지 강우를 차단한 상태에서 토양 $CO_2$ 플럭스를 측정하였다. 강우가 차단된 관측지의 토양 호흡($F_c$)의 일변화는 0.2m 깊이의 토양 온도의 일변화와 매우 비슷하였으며, 자정에 최고값을 보이고 정오에서 이른 오후 사이에 최저값을 나타내었다. 이러한 뚜렷한 일변화 패턴은 같은 관측지에서 강우가 차단되지 않은 상태에서 관측된 선행연구의 결과(뚜렷한 일변화의 부재)와 대조되었다. 또한, 자연상태의 가능토양호흡(potential soil respiration, $F_{cal}$)의 크기와 비교할 때, 강우가 차단된 관측지의 토양호흡은 매우 큰 차이(예를 들면, 토양수분이이 부족할 때 약 50% 감소)를 보였다. 이 연구결과는 강우가 토양 $CO_2$ 플럭스의 크기뿐만이 아니라 토양온도의 연직 프로파일을 바꿈으로써 토양호흡의 일변화 양상에도 영향을 미침을 보여준다.

• Journal of Ecology and Environment
• /
• 제42권2호
• /
• pp.77-84
• /
• 2018

Background: For understanding and evaluating a more realistic and accurate assessment of ecosystem carbon balance related with environmental change or difference, it is necessary to analyze the various interrelationships between soil respiration and environmental factors. However, the soil temperature is mainly used for gap filling and estimation of soil respiration (Rs) under environmental change. Under the fact that changes in precipitation patterns due to climate change are expected, the effects of soil moisture content (SMC) on soil respiration have not been well studied relative to soil temperature. In this study, we attempt to analyze relationship between precipitation and soil respiration in temperate deciduous broad-leaved forest for 2 years in Gwangneung. Results: The average soil temperature (Ts) measured at a depth of 5 cm during the full study period was $12.0^{\circ}C$. The minimum value for monthly Ts was $-0.4^{\circ}C$ in February 2015 and $2.0^{\circ}C$ in January 2016. The maximum monthly Ts was $23.6^{\circ}C$ in August in both years. In 2015, annual precipitation was 823.4 mm and it was 1003.8 mm in 2016. The amount of precipitation increased by 21.9% in 2016 compared to 2015, but in 2015, it rained for 8 days more than in 2016. In 2015, the pattern of low precipitation was continuously shown, and there was a long dry period as well as a period of concentrated precipitation in 2016. 473.7 mm of precipitation, which accounted for about 51.8% of the precipitation during study period, was concentrated during summer (June to August) in 2016. The maximum values of daily Rs in both years were observed on the day when precipitation of 20 mm or more. From this, the maximum Rs value in 2015 was $784.3mg\;CO_2\;m^{-2}\;h^{-1}$ in July when 26.8 mm of daily precipitation was measured. The maximum was $913.6mg\;CO_2\;m^{-2}\;h^{-1}$ in August in 2016, when 23.8 mm of daily precipitation was measured. Rs on a rainy day was 1.5~1.6 times higher than it without precipitation. Consequently, the annual Rs in 2016 was about 12% higher than it was in 2015. It was shown a result of a 14% increase in summer precipitation from 2015. Conclusions: In this study, it was concluded that the precipitation pattern has a great effect on soil respiration. We confirmed that short-term but intense precipitation suppressed soil respiration due to a rapid increase in soil moisture, while sustained and adequate precipitation activated Rs. In especially, it is very important role on Rs in potential activating period such as summer high temperature season. Therefore, the accuracy of the calculated values by functional equation can be improved by considering the precipitation in addition to the soil temperature applied as the main factor for long-term prediction of soil respiration. In addition to this, we believe that the accuracy can be further improved by introducing an estimation equation based on seasonal temperature and soil moisture.

• 한국환경복원기술학회지
• /
• 제26권3호
• /
• pp.19-28
• /
• 2023

The purpose of this study is to estimate carbon dioxide emissions from soil microbial respiration by forest type of Sobaeksan National Park. As a result of estimating the annual soil microbiological respiration volume by forest type in Sobaeksan National Park, broad-leaved forests, coniferous forest, artificial forests were similar to around 19.5 CO₂-ton/ha/yr. In the case of coniferous forests in sub-alpine and grassland near Birobong Peak, 12.2 CO₂-ton/ha/yr and 8.1 CO₂-ton/ha/yr, respectively, were lower than general forest areas. And as a result of analyzing the changes in soil microbiological respiration rate according to forest type in Sobaeksan National Park, the soil microbiological respiration rate in coniferous forests, broad-leaved forests, artificial forests, and sub-alpine areas was the highest in the July survey in summer and the lowest in November in late autumn. The change in soil microbial respiratory volume according to the measurement time in Sobaeksan National Park was the highest between 12:00 and 16:00, when the soil temperature was generally the highest among the days. It is known that the soil temperature is relatively low and the amount of soil microbial respiration decreases during winter, and the change in respiratory volume over the measurement time during the day was the smallest in November, when the amount of soil microbial respiration was relatively smaller than the May-September survey. However, this study has limitations in revealing the causal relationship of various environmental factors that affect the soil microbial respiration. Therefore, it is suggested that long-term research and investigation of various factors affecting soil respiration are needed to understand the carbon cycle of forest ecosystems.

• 미생물학회지
• /
• 제8권1호
• /
• pp.13-20
• /
• 1970

Chenges in respiration of the soils collected from the reclaimed tidal soil in Chogi-ri, Kanghwa Island and treated with organic matters are presented. The measurement of the respiration for the smaples, which were incubated for 0,2,4 and 5 weeks, were carried out by using Warburg's respirometer. While the respirations of the samples added by organic matters were increased 6.7 - 28.0 times compared with that 0 week during the incubation in case of 5-year soil, the respiration in case of 3-year soil were increased 3.3-11.8 times. Thus, the effect of adding organic matters on the respiration of the experimented soils, as this indicates, was much higher for the soil of 5-year area than that of 30-year area. And for the organic matters Salicornia was most effective and then Suaeda and Oryzae. The samples treated with Salicornia and Suaeda showed their highest respiration rate at the 4th week, but the one with Oryzae was measured to increase progressively during 5 weeks experimented. Regarding the salinity, content of organic matters and number of bacteria, in each intact soil experimented, 5-year soil samples had much poor habitat then 30-year soil for the activity of soil microorganisms, but according to the result mentioned above, it is firmly believed that the addition of organic matters on the saline soil is one of the best means to change the reclaimed tidal land into arable land with less time duration.

• 한국토양비료학회지
• /
• 제50권5호
• /
• pp.472-481
• /
• 2017

Agricultural field near at the abandoned metal mine and industrial area has a high possibility to be polluted by heavy metals. However, concern about chemical properties including heavy metal concentration has been increased and biological properties such as soil respiration has been minimal in heavy metal polluted field. Therefore, main objective of this research was to evaluate soil respiration as an indicator of heavy metal pollution in agricultural field. Total of 60 sampling sites including each 30 sites of abandoned metal mine and industrial area were selected and heavy metal concentration, soil respiration, and chemical properties were measured. Results showed that heavy metal concentration in metal mine area was ranged Cu: $6.21~85.23mg\;kg^{-1}$, Pb: $23.84{\sim}1,044.72mg\;kg^{-1}$, As: $1.88{\sim}691.44mg\;kg^{-1}$, Zn: $18.72{\sim}527.55mg\;kg^{-1}$, Cd: $0.58{\sim}4.27mg\;kg^{-1}$, and Cu: $0.29{\sim}30.62mg\;kg^{-1}$, Pb: $4.41{\sim}19.77mg\;kg^{-1}$, As: $2.23{\sim}11.76mg\;kg^{-1}$, Zn $39.98{\sim}109.59mg\;kg^{-1}$, Cd $0.29{\sim}0.57mg\;kg^{-1}$ for industrial area respectively. While no sampling site was exceed the threshold value of each heavy metals in industrial field, metal mine area was highly polluted with Pb, As, Zn, and Cd. Soil respiration in the metal mine and industrial area was ranged $12.05{\sim}299.80mg\;O_2\;kg^{-1}$ and $27.68{\sim}330.94mg\;O_2\;kg^{-1}$, respectively. Correlation analysis between heavy metal concentration in soil and soil respiration showed that negative correlation was observed in metal mine area while no correlation was observed in industrial area. This result might indicate that as heavy metal concentration was increased, microbial activity in soil was decreased resulting decrease of soil respiration rate. Overall, soil respiration can be used as indicator of heavy metal pollution in soil and more biological properties need to be evaluated to better understand heavy metal pollution in soil.

• The Korean Journal of Ecology
• /
• 제26권5호
• /
• pp.289-296
• /
• 2003

The ecological process-based approach provides a detailed assessment of belowground compartment as one of the major compartment of carbon balance. Carbon net balance (NEP: net ecosystem production) in forest ecosystems by ecological process-based approach is determined by the balance between net primary production (NPP) of vegetation and heterotrophic respiration (HR) of soil (NEP=NPP-HR). Respiration due to soil heterotrophs is the difference between total soil respiration (SR) and root respiration (RR) (HR=SR-RR, NEP=NPP-(SR-RR)). If NEP is positive, it is a sink of carbon. This study assessed the forest carbon balance by ecological process-based approach included belowground compartment intensively. The case study in the Takayama Station, cool-temperate deciduous broad-leaved forest was reported. From the result, NEP was estimated approximately 1.2 t C $ha^{-1} yr^{-1}$ in 1996. Therefore, the study area as a whole was estimated to act as a sink of carbon. According to flux tower result, the net uptake rate of carbon was 1.1 t C $ha^{-1} yr^{-1}$.

• The Korean Journal of Ecology
• /
• 제24권3호
• /
• pp.141-147
• /
• 2001

상수리나무림에서 교란이 가해지지 않은 대조구(Con), 그리고 인위적으로 만든 숲틈(Gap)과 낙엽층 제거지역(Lr) 두 곳을 실험구로 설정하여 토양호흡과 호흡에 영향을 주는 토양온도, 수분, 유기물함량을 조사하였다. Con, Gap, Lr의 토양호흡률은 7월에 가장 높았으며, 이 때 각각의 평균 토양호흡률은 15.6±0.9, 11.2±1.4, 7.7 ± 1.3 CO₂μmol·m/sup -2/·s/sup -1/로 Con에 비해 Gap과 Lr에 서 28.6%와 50.6% 낮았다. Con, Gap, Lr에서 동절기에는 토양호흡률이 각각 0.5±0.0, 0.4±0.1, 0.3 ±0.0 CO₂μmol·m/sup -2/·s/sup -1/로 지소간 유의한 차이는 없었다. Con, Gap, Lr에서 조사기간의 평균 토양호흡률은 각각 5.0±4.7, 4.3±3.5, 2.8±2.2 CO₂μmol·m/sup -2/·s/sup -1/로 지소간 유의한 차이(P<0.01)가 있었다. Gap과 Lr은 Con에 비해 각각 24%, 44% 감소되었다. 토양으로부터 대기중으로 방출되는 연간 CO₂의 양은 Con, Gap, Lr에서 각각 6.86, 5.84, 3.81 CO₂㎏·m/sup -2/·yr/sup -1/ 이었다 (P<0.01). Gap과Lr는 Con에 비해 각각 14.8, 44.5%감소되었다. 교란의 정도와 관계없이 토양호흡률은 토양온도와 높은 상관관계가 있었다. 낙엽층은 토양생물의 에너지원이 되고 안정한 서식처를 제공하기 때문에 토양호흡과 밀접한 관련이 있는 것으로 판단된다.

• 한국산림과학회지
• /
• 제83권3호
• /
• pp.372-379
• /
• 1994

본 연구는 서로 다른 두가지 토양에서 천연갱신되어 자라고 있는 trembling aspen(Populus tremuloides Michx.) 임분의 수확이 토양미생물상 및 토양호흡률에 미치는 영향을 조사하며 토양호흡률이 토양미생물상 변이의 지표로 활용될 수 있는지에 대한 연구 결과이다. 다섯 가지의 수확처리(지상부 전체 임목수확, 겨울철 수확통로, 수확 잔재목 제거, 수확 잔재목 및 낙엽류 제거, 춘계 답압)를 1990년과 1991년 사이의 겨울 및 봄 사이에 시행하였고, 1991년 및 1992년의 2년간에 걸쳐 수확후 산림토양의 동태를 조사하였다. 각 임분의 토양형에 관계없이 토양호흡률은 수확후 약간 감소하거나 변동이 없었으나 미생물수는 수확후 2년동안 점차 증가하였다. 미생물수는 식질토양에서 보다 사질토양에서 보다 급속하고 지속적인 증가양상을 나타내었는데, 이것은 수확 결과 미생물 활성에 영향하는 토양의 이화학적 특성이 식질토양보다는 사질토양에서 큰 변화가 있었음을 시사한다. 그러나, 두가지 종류의 처리(세 수준의 유기물 제거 및 두 수준의 답압 처리)는, 두 지역 모두, 수확후 2년간의 미생물상이나 토양호흡률에 유의차를 나타내지 않았다. 본 연구의 대상임분이었던 trembling aspen은 수확후에도 뿌리의 활력이 떨어지지 않고 맹아발생을 위한 대사를 진행하여, 뿌리의 호흡과 미생물의 호흡을 포함하는 전체 토양 호흡에서 뿌리의 호흡이 차지하는 비율이 높은 결과를 낳아, 전체 토양호흡을 미생물의 활력도 변이의 지표로 활용하기 어려웠다.

• 미생물과산업
• /
• 제19권2호
• /
• pp.49-57
• /
• 1993

Chenges in respiration of the soils collected from the reclaimed tidal soil in Chogi-ri, Kanghwa Island and treated with organic matters are presented. The measurement of the respiration for the smaples, which were incubated for 0,2,4 and 5 weeks, were carried out by using Warburg's respirometer. While the respirations of the samples added by organic matters were increased 6.7 - 28.0 times compared with that 0 week during the incubation in case of 5-year soil, the respiration in case of 3-year soil were increased 3.3-11.8 times. Thus, the effect of adding organic matters on the respiration of the experimented soils, as this indicates, was much higher for the soil of 5-year area than that of 30-year area. And for the organic matters Salicornia was most effective and then Suaeda and Oryzae. The samples treated with Salicornia and Suaeda showed their highest respiration rate at the 4th week, but the one with Oryzae was measured to increase progressively during 5 weeks experimented. Regarding the salinity, content of organic matters and number of bacteria, in each intact soil experimented, 5-year soil samples had much poor habitat then 30-year soil for the activity of soil microorganisms, but according to the result mentioned above, it is firmly believed that the addition of organic matters on the saline soil is one of the best means to change the reclaimed tidal land into arable land with less time duration.

• 한국환경생태학회지
• /
• 제26권5호
• /
• pp.780-786
• /
• 2012

공주 근교의 상수리나무림을 대상으로 단근처리 방법을 적용하여 토양호흡량에 대한 뿌리호흡량의 기여율을 파악하였다. 토양호흡구(control plot)와 미생물호흡구(trenched plot)를 설치하고 2011년 6월부터 2012년 5월까지 IRGA 토양호흡측정기를 사용하여 $CO_2$발생량을 측정하였다. $CO_2$발생량은 하절기에 증가한 후 동절기에 감소하는 경향을 보였다. 토양호흡구와 미생물호흡구의 $CO_2$발생량은 8월에 가장 높았으며, 이때 토양호흡구와 미생물호흡구의 $CO_2$발생량은 각각 1.345, 0.897g $CO_2\;m^{-2}\;hr^{-1}$로 토양호흡구에 비해 미생물호흡구에서 33.31% 낮게 나타났다(P<0.05). $CO_2$발생량은 1월에 가장 낮았으며, 이때 토양호흡구와 미생물호흡구에서 각각 0.097, 0.032g $CO_2\;m^{-2}\;hr^{-1}$로 토양호흡구에 비해 미생물호흡구에서 67.01% 낮게 나타났다(P<0.01). 연간 $CO_2$발생량은 토양호흡구와 미생물호흡구에서 각각 4.320, 2.834kg $CO_2\;m^{-2}\;yr^{-1}$로 나타났다. $CO_2$발생량은 토양호흡구와 미생물호흡구에서 토양온도와 높은 상관관계가 있었다. 토양호흡구와 미생물호흡구간의 $CO_2$발생량 차이로 추정한 뿌리호흡량은 토양호흡량 중 약 34.40%를 차지하는 것으로 나타났다.