• 한국토양비료학회지
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• 제47권5호
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• pp.345-350
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• 2014

This study was conducted to investigate the changes in daily surface temperature of red pepper leaf compared to air and soil surface temperature. The maximum, minimum and average daily temperatures of red pepper leaf were 27.80, 11.40 and $19.01^{\circ}C$, respectively, which were lower by 0.10, 7.60 and $3.86^{\circ}C$ than air temperature, respectively, and lower by 15.00, 0.0 and $4.38^{\circ}C$ than soil surface temperature, respectively. Mean deviations of the difference between measured and estimated temperature by the E&E Model (Eom & Eom, 2013) for the air and surface temperature of red pepper leaf and soil were 0.64, 1.82 and $4.77^{\circ}C$, respectively. The relationships between measured and estimated scaled factor of the air and surface temperature of red pepper leaf and soil were very close to the 1:1 line. Difference between air and surface temperature of red pepper leaf showed a linear decreasing function with the surface temperature of red pepper leaf. Difference between soil surface temperature and air and surface temperature of red pepper leaf linearly increased with the soil surface temperature.

• 한국물환경학회지
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• 제28권1호
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• pp.137-147
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• 2012

Land surface temperature in ecohydrology is a variable that links surface structure to soil processes and yet its spatial prediction across landscapes with variable surface structure is poorly understood. And there are an insufficient number of soil temperature monitoring stations. In this study, a grid-based land surface temperature prediction model is proposed. Target sites are Andong and Namgang dam region. The proposed model is run in the following way. At first, geo-referenced site specific air temperatures are estimated using a kriging technique from data collected from 60 point weather stations. Then surface soil temperature is computed from the estimated geo-referenced site-specific air temperature and normalized difference vegetation index. After the model is calibrated with data collected from observed remote-sensed soil temperature, a soil temperature map is prepared based on the predictions of the model for each geo-referenced site. The daily and monthly simulated soil temperature shows that the proposed model is useful for reproducing observed soil temperature. Soil temperatures at 30 and 50 cm of soil depth are also well simulated.

• 한국환경복원기술학회지
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• 제8권6호
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• pp.34-44
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• 2005

The objective of this study is to analyze the thermal properties of various green roof type. The experimental districts, have different soil thickness, soil type, the existence of module and the different kinds of vegetation, had installed. A measurement was conducted in Seoul University to investigate the thermal impacts of rooftop greening. The measurement point of temperature were 30, located in soil surface, middle of the soil layer, under the module, hard surface and soffit surface of each experimental district. The experimental investigation lasted from 6th August to 29th August, a total of 24 days. The results showed that green roof can contribute thermal benefits by soil and vegetation and reduce building energy consumption by a role of insulation. It's also better to make soil thickness over 20cm and various vegetation that should be more effective. The district installed only soil also could be effective for reducing the temperature of roof surface. Therefore, the increase of soil thickness and various vegetation could reduce more temperature of roof surface and building energy consumption. Also, it's helpful to reduce temperature that plant coverage rate be raised.

• 대한토목학회논문집
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• 제14권3호
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• pp.535-542
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• 1994

원격 측정 방법은 지표로부터 방출된 방사선의 관측으로부터 지표면의 특성을 추정하는데 기초를 두고 있으며 이 방법을 사용하여 연구되어지는 수문학적 인자에는 지표면 온도, 증발산, 토양 함수비, 강우 그리고 강설 등이 있다. 본 연구에서는 관측된 광명온도와 모의된 광명온도로부터 피복이 안된 토양의 함수비 산정에 대한 방법을 소개한다. 피복이 안된 토양에서의 초단파 방출은 함수비, 토양의 온도와 표면 조도에 의존하게 된다. 이 방법은 표면 조도의 영향을 고려하기 위한 Fresnel 반사 계수의 수정과 함께 방사선 전달 모델(radiative transfer model)에 기본을 두고 있는데 피복이 안된 매끈한 표면과 서로 다른 표면 조도를 가진 표면에 대해 분석을 실시한다. 연구의 결과는 표면 조도의 영향이 토양의 광명온도를 증가시키고 광명온도와 함수비 사이의 감소경사를 작게함을 보여주고 있다.

• 한국농공학회논문집
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• 제48권5호
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• pp.51-60
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• 2006

In order to examine the heat transfer characteristic of a soil warming system and effects of soil warming on the greenhouse heating load, control experiments were performed in two greenhouses covered with double polyethylene film. One treated the soil warming with an electric heat wire and the other treated a control. Inside and outside air temperature, soil temperature and heat flux, and heating energy consumption were measured under the set point of heating temperature of $5,\;10,\;15,\;and\;20^{\circ}C$, respectively. Soil temperatures in a soil warming treatment were observed $4.1\;to\;4.9^{\circ}C$ higher than a control. Heating energy consumptions decreased by 14.6 to 30.8% in a soil warming treatment. As the set point of heating temperature became lower, the rate of decrease in the heating energy consumptions increased. The percentage of soil heat flux in total heating load was -49.4 to 24.4% and as the set point of heating temperature became higher, the percentage increased. When the set point of heating temperature was low in a soil warming treatment, the soil heat flux load was minus value and it had an effect on reducing the heating load. Soil heat flux loads showed in proportion to the air temperature difference between the inside and outside of greenhouse but they showed big difference according to the soil warming treatment. So new model for estimation of the soil heat flux load should be introduced. Convective heat transfer coefficients were in proportion to the 1/3 power of temperature difference between the soil surface and the inside air. They were $3.41\;to\;12.42\;W/m^{2}^{\circ}C$ in their temperature difference of $0\;to\;10^{\circ}C$. Radiative heat loss from soil surface in greenhouse was about 66 to 130% of total heating load. To cut the radiation loss by the use of thermal curtains must be able to contribute for the energy saving in greenhouse.

• 대한원격탐사학회지
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• 제30권3호
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• pp.375-381
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• 2014

Soil moisture is an essential satellite-driven variable for understanding hydrologic, pedologic and geomorphic processes. The European Space Agency (ESA) has endorsed soil moisture as one of Climate Change Initiates (CCI) and had merged multi-satellites over 30 years. The $0.25^{\circ}$ coarse resolution soil moisture satellite data showed correlations with variables of a water stress index, Temperature-Vegetation Dryness Index (TVDI), from a stepwise regression analysis. The ancillary data from TVDI, Land Surface Temperature (LST) and Normalized Difference Vegetation Index (NDVI) from MODIS were inputted to a multi-regression analysis for estimating the surface soil moisture. The estimated soil moisture was validated with in-situ soil moisture data from April, 2012 to March, 2013 at Andong observation sites in South Korea. The soil moisture estimated using satellite-based LST and NDVI showed a good agreement with the observed ground data that this approach is plausible to define spatial distribution of surface soil moisture.

• 한국농공학회논문집
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• 제59권6호
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• pp.29-37
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• 2017

In this study, we analyzed the impacts of land surface characteristics on spatially and temporally distributed soil moisture values at the Yongdam and Soyang-river dam watersheds in 2014 and 2015. The soil moisture, NDVI (Normalized Difference Vegetation Index) and temperature values at the spatio-temporal scales were estimated using satellite-based MODIS (MODerate Resolution Imaging Spectroradiometer) products. Then the Pearson correlations between soil moisture and land surface characteristics (NDVI, temperature and DEM-digital elevation model) were estimated and analyzed, respectively. Overall, the monthly soil moisture values at the time step were highly influenced by the precipitation amounts. Also, the results showed that the soil moisture has the strong correlation with DEM while the temperature was inversely correlated with the soil moisture. However the monthly correlations between NDVI and soil moisture were highly varied along the time step. These findings indicated that water loss near the land surface are highly occurred by soil and plant activities as evapotranspiration and infiltration during the no/less precipitation period. But the high precipitation amounts reduce the impacts of land surface characteristics because of saturated condition of land surface. Thus these results demonstrated that soil moisture values are highly correlated with land surface characteristics. Our findings can be useful for water resources/environmental management, agricultural drought, etc.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 1999년도 Proceedings of International Symposium on Remote Sensing
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• pp.319-322
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• 1999

Land surface hydrological conditions have been considered to play an important role in the global and regional climate variability. Especially, snow, soil moisture, surface temperature, vegetation and rain are the key parameters which should be observed in the global scale. In this paper, new algorithms for these land surface hydrological parameters have been developed by introducing frequency and polarization dependencies of these parameters in the microwave radiative-transfer equations. The algorithms were applied to the TRMM Microwave Radiometer. (TMI) and validated by using the ground data obtained in the Tibetan Plateau. The estimated snow, soil moisture, surface temperature, water content of vegetation and rain patterns corresponded reasonably to the observed ones.

• 한국토양비료학회지
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• 제37권3호
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• pp.131-135
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• 2004

본 연구는 일반 기상 측정에서 에너지 수지를 구할 때 이용되는 지중열류 값과 토양 내 10 cm 깊이에서 측정한 토양온도를 활용하여 태양 복사에너지와 지표면 복사 에너지의 도달과 분배에 중요한 역할을 하는 토양표면의 온도를 예측하고자 수행하였다. 2003년 6월 10일부터 6월 24일까지 측정한 지중열류와 토양온도 그래프에서 토양온도나 지중열류는 주기성을 나타내며 일중 최저 지중열류와 최고 토양온도 사이에는 위상편차가 존재한다. 토심 5 cm에서 측정하여 시간별로 평균한 토양온도와 지중열류 사이에는 2시간의 시간지연이 존재하며 토양온도와 시 공간상에서의 지중열류는 정의 상관관계를 보였다. 이는 단위체적 당 열용량과 깊이에 따른 열량의 변화율이 태양에너지와 지표면 복사를 통한 지중열류에 비례한다는 것을 의미한다. 예측된 토양 표면온도는 시간별로 평균하였을 때 그 평균온도가 $20^{\circ}C$를 넘어 여름철의 기온을 반영하였으며 모양도 주기함수 형태를 보였다. 진폭은 $4.5^{\circ}C$로서 10 cm 깊이에서의 진폭인 $3.4^{\circ}C$보다 $1.1^{\circ}C$ 높았으며 최저온도가 나타난 시간은 토양표면의 경우는 오전 8시, 10 cm 깊이에서는 오전 9시였으며 최고온도가 나타난 시간은 토양표면은 16시, 10 cm 깊이는 19시이었다. 시간별로 평균하지 않았을 때의 최고와 최저온도는 각각 33.2, $16.5^{\circ}C$ 였으며, 토양표면온도 분포는 $15-20^{\circ}C$가 5.3%, $20-25^{\circ}C$가 65.6%, $25-30^{\circ}C$가 28.1%, $30-35^{\circ}C$가 1%로 대부분의 온도는 $20-25^{\circ}C$ 범위의 값을 나타냈다. 예측된 토양표면온도의 검증을 위해 토양표면 온도와 10 cm 깊이의 토양온도를 가지고 계산한 산술 평균과 토심 5 cm에서 측정한 토양온도를 비교하였다. 또한, 그 과정을 통해 얻어진 추정회귀모형은 P값이 0.001보다 작아 유의성이 인정 되었다. 회귀모형의 결정계수는 0.968이었고 표준오차는 0.38로 예측된 토양표면온도는 추정 회귀모형에 의해 실제 값에 가깝게 추정할 수 있을 것이다.

• Journal of Ecology and Environment
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• 제35권1호
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• pp.1-7
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• 2012

To calculate and predict soil carbon budget and cycle, it is important to understand the complex interrelationships involved in soil respiration rate (Rs). We attempted to reveal relationships between Rs and key environmental factors, such as soil temperature, using a laboratory incubation method. Soil samples were collected from mature deciduous (MD), mature coniferous (MC), immature deciduous (ID), and immature coniferous (IC) forests. Prior to measure, soils were pre-incubated for 3 days at $25^{\circ}C$ and 60% of maximum water holding capacity (WHC). Samples of gasses were collected with 0, 2, and 4 h interval after the beginning of the measurement at soil temperatures of 5, 15, 25, and $35^{\circ}C$ (at 60% WHC). Air samples were collected using a syringe attached to the cap of closed bottles that contained the soil samples. The $CO_2$ concentration of each gas sample was measured by gas chromatography. Rs was strongly correlated with soil temperature (r, 0.93 to 0.96; P < 0.001). For MD, MC, ID, and IC soils taken from 0-5 cm below the surface, exponential functions explained 90%, 82%, 92%, and 86% of the respective data plots. The temperature and Rs data for soil taken from 5-10 cm beneath the surface at MD, MC, ID, and IC sites also closely fit exponential functions, with 83%, 95%, 87%, and 89% of the data points, respectively, fitting an exponential curve. The soil organic content in mature forests was significantly higher than in soils from immature forests (P < 0.001 at 0-5 cm and P < 0.005 at 5-10 cm) and surface layer (P = 0.04 at 0-5 cm and P = 0.12). High soil organic matter content is clearly associated with high Rs, especially in the surface layer. We determined that the incubation method used in this study have the possibility for comprehending complex characteristic of Rs.