• 한국터널지하공간학회 논문집
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• 제20권6호
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• pp.1177-1192
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• 2018

본 연구의 목적은 한랭지역에서 운영 중인 터널구조물의 누수를 유도배수하기 위하여 기존 유도배수시스템을 향상시키는 것이다. 유도배수시스템은 유도배수판, 방수재료인 Hotty-gel, Hotty-gel 돌출 방지판, 공압타카, 고정핀, 집수관, 유도배수관, 철망 및 뿜어 붙임 모르타르로 구성되어 있다. 유도배수시스템은 현장 적용성 및 시공성을 평가하기 위하여 재래식 콘크리트 라이닝 터널에서 시험 시공되었다. 재령 7일, 14일, 21일, 28일, 2개월, 3개월, 4개월, 5개월, 6개월, 7개월 및 8개월에 약 1,000 ml의 붉은색 물을 유도배수시스템 배면에 주입하여 유도배수시스템의 방수과 유도배수 성능을 평가하였다. 현장 성능 평가 실험이 진행된 8개월 동안 터널이 위치한 지역의 일일 평균 온도는 $-16.0~25.6^{\circ}C$로 측정되었고, 일일 최저 온도는 $-21.3^{\circ}C$, 일일 최고 온도는 $30.8^{\circ}C$였다. 유도배수시스템의 유도배수판에서는 누수가 발생하지 않았지만 재령 14일부터 유도배수관에서 누수가 발생하였다. 유도배수관 누수는 고압의 공압타카와 고정핀 사용으로 두께 0.2 cm인 연성플라스틱 재질의 유도배수관이 변형되었고, 누수 방지를 위한 Hotty-gel의 두께와 폭이 충분하지 않아서 발생한 것으로 판단된다.

• 한국산림과학회지
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• 제94권6호
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• pp.370-376
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• 2005

능이(Sarcodon aspratus)는 자연산 식용버섯으로 참나무와 공생하는 균근성 버섯으로 알려져 있다. 본 연구는 토양수분과 기상인자가 능이 발생에 미치는 관계를 구명하기 위하여 실시하였다. 충북 제천시 한수면 송계리 월악산내에 2개소를 선정하여 2000년부터 2002년까지의 토양수분과 기상인자를 조사하여 능이 발생에 미치는 영향을 구명하였다. 능이 발생지와 비발생지의 토양수분과 지온을 1시간 간격으로 계측하여 분석하였다. 능이 발생 전후의 토양수분은 능이 발생지의 평균토양수분이 14.3%이고, 능이 비발생지의 평균토양수분은 16.4%로 능이 발생지의 평균토양수분이 2.1% 낮은 경향이었다. 능이 발생지의 평균지중온도는 $16.8^{\circ}C$이고, 능이 비발생지의 평균지중온도는 $16.5^{\circ}C$로 큰 차이는 없으나 능이 발생지의 평균지중온도가 $0.3^{\circ}C$ 높게 유지되었다. 능이의 발생에는 토양수분, 일최고온도, 일최저온도, 일최저지온이 영향을 미친다고 판단되며 송이의 경우와 유사한 경향이었다. 능이의 발생시기는 8월말~9월초에서 10월 초순경까지 발생하며 최근 기상이변과 엘리뇨 등의 영향으로 발생시기가 일정하지 않고 변화가 많았다. 송이의 경우와 같이 능이 발생이후에 일최저지온이 $20^{\circ}C$ 이상으로 유지되는 일수가 지속되면 원기생성과 능이 자실체 생장에 불리한 것으로 판단된다.

• 한국산림과학회지
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• 제111권3호
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• pp.357-364
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• 2022

본 연구는 미국의 미시간주 산지로부터 도입한 종자를 이용하여 국내 6개 지역에서의 토양 물리·화학적 성질 및 기상인자에 따른 루브라참나무 초기 생장 특성을 분석하고자 수행되었다. 조사지는 화성, 양평, 평창, 삼척, 충주, 김제이며 2014년에 루브라참나무 묘목(1-0묘)은 3,000본 ha^-1 밀도로 식재되었다. 2021년도에 조사된 6개 지역 8년생 루브라참나무의 평균 수고, 근원경 및 재적생장은 각각 3.52 m, 3.84 cm, 0.0023 m³로 나타났다. 조사된 국내 6개 지역 중에서 경기도 화성시에 식재된 루브라참나무의 생장이 가장 우수하며 강원도 평창군의 생장이 가장 저조하였다. 토양특성 조사에서 조림지 토양 내 모래의 비율은 21.4~64.1%, 미사는 24.9~61.1%, 점토는 9.7~21.2%로 확인되었으며, pH는 전체적으로 4.15~4.80의 범위로 약산성을 나타내었다. 지역별로는 화성이 4.15로 가장 낮았고 삼척 지역이 4.80으로 가장 높았다. 조림지 토양의 물리·화학적 특성 및 기상인자와 생장 특성과의 상관분석을 진행한 결과, 토양인자들 중 pH는 근원경과 부의 상관을 나타냈으며 다른 토양인자들은 생장특성과 유의한 상관관계가 나타나지 않았다. 반면, 일 최고기온과 3~10월의 평균온도 등의 기상인자는 생장특성과 강한 정의 상관을 나타냈으며, 해발고와 지형, 3~10월의 강우 일수는 부의 상관을 보였다. 특히 화성지역은 가장 높은 일 최고온도와 3~10월의 평균온도, 낮은 고도와 산록에 가까운 지형으로 인해 가장 우수한 초기생장을 보이는 것으로 나타났다. 생장이 가장 저조했던 평창의 경우 높은 고도와 낮은 일 최저기온 등으로 인한 겨울철 동해 피해와 야생동물에 의한 수목 피해가 생장에 부정적인 영향을 주었던 것으로 분석되었다. 주성분 분석에서는 제 3 주성분까지 84.7%의 설명력을 나타냈으며, 생장특성인 근원경 및 재적과 생장이 가장 우수했던 화성지역이 강한 상관관계를 보였다. 종합적으로 국내 6개 지역 중에서 화성 지역의 루브라참나무 초기 생장이 가장 우수한 것으로 나타났으며, 조림지 토양의 물리·화학적 특성보다는 온도나 고도와 같은 기상과 관련된 인자가 생장특성과 상관관계가 높다는 것을 확인할 수 있었다. 이 결과는 루브라참나무 국내 조림 적지 판정 및 환경 특성에 따른 초기생장 특성 예측에 필요한 유용한 정보로 이용될 수 있을 것으로 판단된다.

• The Korean Journal of Ecology
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• 제24권6호
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• pp.335-339
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• 2001

The dynamic model was developed to simulate the photosynthetic rate of Phragmites communis stands in coastal ecosystem. The model was composed of the compartments of both climatic and biological variables. The former were photosynthetic photon flux density(PPFD), daily maximum- and minimum-temperature. The latter were combinations of the specific physiological responses of plant organs with the biomass of each organs. The PPFD and air temperature were calculated and using those values, gas exchange rate of each plant organ was calculated at every hour. The carbon budget was constructed using the modelled predictions. Analysis of annual productivity and fluxes showed that yearly gross population productivity, yearly population respiration and yearly net population productivity were 33.4, 21.3 and 12.1 $CO_2ton{\cdot}ha^{-2}{\cdot}yr^{-1}$, respectively. The final result was tested over two stands, produced promising predictions with regards to the levels of production attained. The model can be used to determine production potential under given climatic conditions and could even be applied to plant canopies with analogous biological characteristics.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2005년도 Proceedings of ISRS 2005
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• pp.178-181
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• 2005

The positioning accuracy of the Global Positioning System (GPS) has been improved considerably during the past two decades. The main error sources such as ionospheric refraction, orbital uncertainty, antenna phase center variation, signal multipath, and tropospheric delay have been reduced substantially, if not eliminated. In this study, the GPS data collected by the GPS receivers that were established as continuously operating reference stations by International GNSS Service (IGS), Ministry of the Interior (MOl), Central Weather Bureau (CWB), and Industrial Technology Research Institute (ITRI) Of Taiwan are utilized to investigate the impact of atmospheric water vapor on GPS positioning determination. The surface meteorological measurements that were concurrently acquired by instruments co-located with the GPS receivers include temperature, pressure and humidity data. To obtain the influence of the GPS height on the proposed impact study. A hydrodynamic ocean tide model (GOTOO.2 model) and solid earth tide were used to improve the GPS height. The surface meteorological data (pressure, temperature and humidity) were introduced to the data processing with 24 troposphere parameters. The results from the studies associated with different GPS height were compared for the cases with and without a priori knowledge of surface meteorological measurements. The finding based on the measurements in 2003 is that the surface meteorological measurements have an impact on the GPS height. The associated daily maximum of the differences is 1.07 cm for the KDNM station. The impact is reduced due to smoothing when the average of the GPS height for the whole year is considered.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2004년도 학술발표회
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• pp.1142-1146
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• 2004

The objective of this study is to the test applicability of SLURP on Soyanggang-dam watershed. The area of this watershed is $2,694km^2$ and mean elevation and slope is 650 m and $23^{\circ}$ respectively. Topographical parameters were derived from DEM using TOPAZ and SLURPAZ. NDVI was calculated from multi-temporal NOAA/AVHRR images. The daily meteorological data and hydrograph during $1999\~2001$ were selected for model calibration and performance tests. Weather elements (dew-point temperature, solar radiation, maximum and minimum temperature, relative humidity) were required from the S meteorological stations near the study area. The model parameters of each land cover class were optimized by sensitivity analysis and SCE-UA method. Runoff rate shows $49.33\%\~64.06\%$. Simulated results during 4 years were estimated by Nash-Sutcliffe efficiency and WMO volume error. Nash-Sutcliffe efficiency shows $0.61\~0.75$ and WMO volume error shows $6.1\%-18.8\%$.

• 설비공학논문집
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• 제20권2호
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• pp.128-136
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• 2008

It is necessary to estimate the cooling load of the next day for effective control of ice thermal storage system. In this paper, new methodology is proposed to estimate the cooling load using design parameters of building and predicted weather data. Only six input parameters such as sensible heat coefficient and constant, latent heat coefficient and constant, maximum and minimum temperature are necessary to obtain hourly distribution of cooling load for the next day. Two benchmarking buildings(hospital and research institute) are selected to validate the performance of the proposed method, and the estimated cooling loads in hourly and daily bases are calculated and compared with the measured data for E hospital. The estimated results show fairly good agreement with the measured data for both buildings.

• 한국환경과학회지
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• 제15권8호
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• pp.701-718
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• 2006

The average ratio of the daily UV-B to total solar (75) irradiance at Busan (35.23$^{\circ}$N, 129.07$^{\circ}$E) in Korea is found as 0.11%. There is also a high exponential relationship between hourly UV-B and total solar irradiance: UV-B=exp (a$\times$(75-b))(R$^2$=0.93). The daily variation of total ozone is compared with the UV-B irradiance at Pohang (36.03$^{\circ}$N, 129.40$^{\circ}$E) in Korea using the Total Ozone Mapping Spectrometer (TOMS) data during the period of May to July in 2005. The total ozone (TO) has been maintained to a decreasing trend since 1979, which leading to a negative correlation with the ground-level UV-B irradiance doting the given period of cloudless day: UV-B=239.23-0.056 TO (R$^2$=0.52). The statistical predictions of daily total ozone are analyzed by using the data of the Brewer spectrophotometer and TOMS in East Asia including the Korean peninsula. The long-term monthly averages of total ozone using the multiplicative seasonal AutoRegressive Integrated Moving Average (ARIMA) model are used to predict the hourly mean UV-B irradiance by interpolating the daily mean total ozone far the predicting period. We also can predict the next day's total ozone by using regression models based on the present day's total ozone by TOMS and the next day's predicted maximum air temperature by the Meteorological Mesoscale Model 5 (MM5). These predicted and observed total ozone amounts are used to input data of the parameterization model (PM) of hourly UV-B irradiance. The PM of UV-B irradiance is based on the main parameters such as cloudiness, solar zenith angle, total ozone, opacity of aerosols, altitude, and surface albedo. The input data for the model requires daily total ozone, hourly amount and type of cloud, visibility and air pressure. To simplify cloud effects in the model, the constant cloud transmittance are used. For example, the correlation coefficient of the PM using these cloud transmissivities is shown high in more than 0.91 for cloudy days in Busan, and the relative mean bias error (RMBE) and the relative root mean square error (RRMSE) are less than 21% and 27%, respectively. In this study, the daily variations of calculated and predicted UV-B irradiance are presented in high correlation coefficients of more than 0.86 at each monitoring site of the Korean peninsula as well as East Asia. The RMBE is within 10% of the mean measured hourly irradiance, and the RRMSE is within 15% for hourly irradiance, respectively. Although errors are present in cloud amounts and total ozone, the results are still acceptable.

• 한국환경과학회지
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• 제29권1호
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• pp.45-54
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• 2020

High-resolution meteorological simulations were conducted using a Weather Research and Forecasting (WRF) model with an Urban Canopy Model (UCM) in the Ulsan Metropolitan Region (UMR) where large-scale industrial facilities are located on the coast. We improved the land cover input data for the WRF-UCM by reclassifying the default urban category into four detailed areas (low and high-density residential areas, commercial areas, and industrial areas) using subdivided data (class 3) of the Environmental and Geographical Information System (EGIS). The urban area accounted for about 12% of the total UMR and the largest proportion (47.4%) was in the industrial area. Results from the WRF-UCM simulation in a summer episode with high temperatures showed that the modeled temperatures agreed greatly with the observations. Comparison with a standard WRF simulation (WRF-BASE) indicated that the temporal and spatial variations in surface air temperature in the UMR were properly captured. Specifically, the WRF-UCM reproduced daily maximum and nighttime variations in air temperature very well, indicating that our model can improve the accuracy of temperature simulation for a summer heatwave. However, the WRF-UCM somewhat overestimated wind speed in the UMR largely due to an increased air temperature gradient between land and sea.

• 한국수산과학회지
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• 제40권2호
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• pp.102-107
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• 2007

A remarkable sea surface cooling (SSC) event was observed in the eastern sea of Korean peninsula based on new generation sea surface temperature (NGSST) satellite images in September 2005, when typhoon Nabi passed over the East Sea. The degree of SSC ranged from $1^{\circ}C\;to\;4^{\circ}C$, and its maximum was observed in the southeastern sea area. Daily variations in sea surface temperature at a longitudinal line $(35^{\circ}-41^{\circ}N,\;132^{\circ}E)$, derived from satellite data for September 1-13, 2005, showed that the SSC lasted about 3 days after the typhoon passed in the south of $39^{\circ}N$, whereas it was unclear in the north of$39^{\circ}N$. Water temperature measured by a mooring buoy suggested that the SSC was caused mainly by a vertical mixing of the water column driven by the typhoon, rather than by coastal upwelling.