• Water Engineering Research
• /
• 제4권1호
• /
• pp.31-43
• /
• 2003

The impacts of climate change on soil moisture in sub - Arctic watershed simulated by using the hydrologic model. A range of arbitrary changes in temperature and precipitation are applied to the runoff model to study the sensitivity of soil moisture due to potential changes in precipitation and temperature. The sensitivity analysis indicates that changes in precipitation are always amplified in soil moisture with the amplification factor for flow. The change in precipitation has effect on the soil moisture in the catchment. The percentage change in soil moisture levels can be greater than the percentage change in precipitation. Compared to precipitation, temperature increases or decreases alone have impacts on the soil moisture. These results show the potential for climate change to bring about soil moisture that may require a significant planning response. They are also indicative of the fact that hydrological impacts affecting water supply may be important in consider-ing the cost and benefits of potential climate change.

• 한국토양비료학회지
• /
• 제28권3호
• /
• pp.266-269
• /
• 1995

볏짚을 사용한 구(볏짚 5톤+NPK:110-70-80kg/ha)와 볏짚을 사용하지 아니한 구(NPK : 110-70-80kg/ha)에서 벼의 출수기에 2시간 간격으로 메탄 배출량을 24시간 측정하고 지온(地溫)과 기온(氣溫)의 변화(變化)에 따른 상관관계(相關關係)를 고찰하였다. 1. 볏짚을 사용하지 아니한 삼요소구(三要素區)에서는 메탄배출은 지온(地溫)의 변화와 상응하게 변화하나 기온 상승이 급격한 오전 11시부터 오후 5시까지는 메탄배출량이 기온상승에 부응하는 증가경향을 보이지 않았다. 2. 볏짚을 시용한 삼요소구(三要素區)에서는 메탄 배출의 일 변화 양상이 지온의 변화와는 상관이 적고 기온이 상승하는 오전 11시~오후 5시에 매탄배출량이 급격히 증가하여 기온의 변화와 상관이 깊어 보였다. 3. 메탄 배출에는 지온(地溫) 외에도 기온(氣溫)과 메탄생성의 기질(基質)이 되는 유기물(有機物)의 존재(存在)가 중요함이 인정되었다.

• Journal of the Korean Data and Information Science Society
• /
• 제20권4호
• /
• pp.649-654
• /
• 2009

기온과 더불어 지중온도는 기후 변동 및 농업 환경 예측의 중요한 기준이 되고 있다. 이 논문 에서는 대구지역의 1932년부터 1990년도까지의 토심 0.5m 지중온도의 연평균 변화와 1961년부터 2008년까지의 기온 자료를 이용하여 연평균 기온변화를 살펴보고, 지중온도와 기온의 관계 모델을 도출하였다. 이 모델을 통하여 현재 측정되지 않는 대구의 지중온도를 기온을 이용하여 복원하였으며 그 결과 지중온도는 매년 약 $0.028^{\circ}C$의 증가를 보이고 있다는 사실을 확인할 수 있었다. 복원을 통한 지중온도의 예측은 대구 지역 기후 변화 예측의 중요한 기준이 되며, 농업 환경의 변화에 대한 FTA 협약, 지구온난화 등에서 발생가능한 상황의 대비책을 마련할 수 있는 정보가 되겠다.

• 한국조경학회지
• /
• 제35권3호
• /
• pp.105-113
• /
• 2007

This study was conducted to analyze the effects of environmental factors such as soil moisture, light intensity, temperature and humidity on changes in cambial electrical resistance. To improve data quality, cambial electrical resistance was continuously measured at fixed points by using a data logger isolated from alternating current. The relationship between environmental factors and changes in cambial electrical resistance was also analyzed. The results are as follows: 1. Cambial electrical resistance is highly correlated to the temperature of the measured area(r=-0.934). Therefore, temperature compensation is needed to analyze the effects of other environmental factors on cambial electrical resistance changes. 2. If temperature is compensated for, the change of cambial electrical resistance is highly correlated to water vapor pressure(r=-0.836). 3. If temperature and humidity are compensated for, the change of cambial electrical resistance is highly correlated to intensity of light(r=-0.738). 4. Diurnal deviation of soil water potential is not more significantly related than the change of cambial electrical resistance. However, in the long-term, soil water potential and cambial electrical resistance are highly correlated(r=-0.831). This indicates that soil moisture significantly influences the long-term change of cambial electrical resistance.

• The Korean Journal of Ecology
• /
• 제23권2호
• /
• pp.117-123
• /
• 2000

Changing patterns and the possibility of climate change in the area of Cheiudo island, the southernmost Island in Korea, were analyzed using daily temperature and Precipitation data observed at the Cheiu Regional Meteorological Office from May 1923 to December 1998. A hydrologic simulation model "BROOK" was used to simulate and analyze the dynamics of daily soil moisture content and soil moisture deficit by applying the daily weather data. During the period, significantly increasing pattern was observed in temperature data of both annual and monthly basis, while no significantly changing pattern was observed in precipitation data. During the last 76 years. mean annual temperature was observed to have risen about 1.4$^{\circ}C$, which may show the Possibility of the initiation of climate change on the island whose validity should be tested in future studies after long-term studies on temperature. Based on the simulation, due to increased temperature, significant increase was predicted in evapotranspiration. while no significant decrease was detected in simulated soil moisture content during the period. Changing pattern of annual soil moisture content was markedly different from those of precipitation. In some dominant trees, negative effects of the drought of the late season for the previous year were shown to be statistically significant to radial growth of the tree for the current year. As annual variation of radial growth of trees is mainly affected by the soil moisture content. the information on the dynamics of soil moisture deficit possibly provides us with useful information for the interpretation of tree growth decline on the mountain. mountain.

• 한국지반환경공학회 논문집
• /
• 제10권7호
• /
• pp.93-101
• /
• 2009

스탠딩 컬럼웰(Standing Column Well) 히트펌프시스템은 지하수의 열교환으로부터 지열에너지를 생산한다. 모의지열펌프시스템(SHPS)을 제작하고 이를 이용하여 변화하는 토양의 온도를 관찰하고, bleeding 실험 후 SHPS 내에서 토양 미생물의 양과 종의 변화를 파악하였다. 이와 같은 실험을 통해 토양의 온도 변화와 수분의 변화에 의해 토양 내 미생물의 전반적인 양은 감소하였고, 종의 개체수가 감소함을 볼 수 있었다. 열원으로 사용되는 지하수의 성상분석을 통해 사용 전 후의 특성을 파악하고, 지하수 시료를 생활용수 기준으로 수질 분석 하였다. 그 결과 지하수의 수질 자체가 매우 양호하여 지하수 오염은 일어나지 않은 것으로 파악되었다. 또한 지하수 시료의 경우에도 지하수 내 존재하고 있는 미생물의 종과 양의 변화를 파악하여, 열원으로 사용 전 후의 미생물의 종과 양이 변화 한다는 것을 알 수 있었다. 지하수의 온도가 2-3도 증가함에 따라 미생물의 양이 90% 정도 늘어났으며, 토양에 비해 종의 변화는 크지 않음을 확인할 수 있었다.

• 한국환경과학회지
• /
• 제5권6호
• /
• pp.727-738
• /
• 1996

An one dimensional atmosphere-canopy-soil interaction model is developed to estimate of the heat budget parameter in the atmospheric boundary layer. The canopy model is composed of the three balance equations of energy, temperature, moisture at ground surface and canopy layer with three independent variables of Tf(foliage temperature), Tg(ground temperature), and qg(ground specific humidity). The model was verilied by comparative study with OSUID(Oregon State University One Dimensional Model) proved in HAPEX-MOBILHY experiment. Also we applied this model in two dimensional land-sea breeze circulation. According to the results of this study, surface characteristics considering canopy acted importantly upon the simulation of meso-scale circulation. The factors which used in the numerical experiment are as follows ; the change for a sort of soil(sand and peat), the change for shielding factor, and the change for a kind of vegetation.

• 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.

• 생태와환경
• /
• 제46권3호
• /
• pp.409-418
• /
• 2013

최근 기후변화에 따른 지구온난화는 전세계적으로 매우 큰 문제로 인식되고 있다. 이산화탄소의 농도, 온난화정도, 토양 온도, 강우량, 토양수분함량, 탈질작용 등과 같은 요인들은 토양으로부터 아산화질소 ($N_2O$)의 방출에 영향을 미치는 것으로 알려져 있다. 본 연구에서는 산지습지인 오대산 질뫼늪과 정족산 무체치늪 토양으로부터 온도변화에 따른 $N_2O$ 발생을 조사하였다. 7월 채취한 질뫼늪 토양은 온도가 증가함에 따라 $N_2O$ 발생이 증가하였으나 $10^{\circ}C$에서는 유의한 차이를 보이지 않았다. $15^{\circ}C$와 $20^{\circ}C$ 토양은 24시간까지는 증가하는 $N_2O$ 발생양상을 보였으나 그 이후 발생량의 뚜렷한 차이를 보이지 않았다, 전반적으로 온도처리에 따른 유의한 차이만을 보였다. 무제치늪 토양 또한 질뫼늪 토양과 유사한 경향을 보였다. 부가적인 질소원 처리에 대해 두 습지 토양은 다소 증가하는 양상을 보였으나 질소부가나 질소원에 따른 유의한 차이를 보이지 않았다. 결론적으로 이탄토양으로부터 배출하는 $N_2O$의 양은 온도가 상승함에 따라 증가되는 양상을 보였으나 질소원의 종류와 부가량은 $N_2O$ 배출 양상에 큰 차이를 보이지 않은 것으로 조사되었다. 향후 산지 이탄습지 토양의 $N_2O$ 배출양상을 보다 명확히 규명하기 위해서는 질소원의 차이, 질소의 시비, 토양효소 활성이나 질화세균의 활동성을 포함하여 다양한 요인에 대한 복합적인 연구가 진행될 필요가 있을 것이다.

• 생태와환경
• /
• 제56권4호
• /
• pp.440-448
• /
• 2023

This study measured soil respiration in pine forests dominated by Pinus densiflora in Mt. Jeombong, Mt. Namsan, Mt. Jirisan in Republic of Korea from 2009 to 2010. The seasonal variations, along with temperature and soil moisture content, were measured to understand the characteristics at each site. Soil respiration was highest in summer and autumn, closely influenced by the increase in soil temperature. Throughout the measurement period, soil respiration ranged from 205.6 to 312.2 mg CO₂ m^-2 h^-1, with Mt. Namsan showing the highest values and Mt. Jirisan the lowest. A strong correlation was observed between soil respiration and soil temperature, with Q₁₀ values ranging from 2.5 to 3.0. Precipitation significantly affected soil moisture content, and although it appeared to influence soil respiration, no significant correlation was found.