• 한국농공학회지
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• 제26권4호
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• pp.37-51
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• 1984

The purpose of this study is to find out the determination method of designed duty of water in the rice fields through the comparison of the net unit duty of water at the late reduction division to heading stage with that at the planting stage. The data used for analysing this problem are the data of precipitation and gauge evaporation observed by Cheong-ju Meterological Center, the coefficient of evapotranspiration by College of Agriculture, Chung Buk University and the data of transplanting progressing in Boun area. The results obtained from this analysis are summarized as follows. 1.The occurring year of 1/10 probability value for available precipitation, gauge evaporation and mean maximum daily evapotranspiration during growing season is the year of 1977. 2.The 1/10 probability values of mean maximum evapotranspiration per day under the production rate of 1, 400kg/l0a and 1, 500kg/10a based on the weight of dry matters are 9. 2mm/day and 9. 6mm/day, respectively. 3.The net unit duty of water required in the fields that the maximum planting rate exists is more than the one in the fields that the planting rate is uniform in the planting stage. 4.The determination of net unit duty of water in the late reduction division to heading stage or the planting stage depends upon the daily evapotranspiration and percolation rate in the late reduction division to heading stage or the water depth required for planting and daily consumptive use of water after planting at the planting stage. Therefore the use of figure 5-(1) to figure 5-(6) can easily make the determination of the designed net unit duty of water out of above two kinds of net unit duty of water.

• 방사성폐기물학회지
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• 제14권1호
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• pp.21-33
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• 2016

Estimation of groundwater hydrologic cycle pattern is one of the most critical issues in sustainable management of groundwater resources in coastal area. This study estimated groundwater percolation by using the water balance methodology and hydrogeological characteristics of land use and soil. Evapotranspiration was computed by using the Thornthwaite method, and surface runoff was determined by using the SCS-CN technique. Groundwater storage change was obtained as 229 mm/a (17.8% of the average annual rainfall, 1286 mm/a), with 693 mm/a (60.1%) of evapotranspiration and 124 mm/a (9.6%) of surface runoff. Rainfall and groundwater storage change was highly correlated, comparing with the relationships between rainfall and evapotranspiration, and between rainfall and surface runoff. This result indicates that groundwater storage change responds more sensitively to precipitation than evapotranspiration and surface runoff.

• 한국수자원학회논문집
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• 제48권10호
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• pp.831-843
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• 2015

본 연구에서는 MODIS 위성 기반 증발산량의 적정성을 평가하기 위해 Revised RS-PM 알고리즘으로 일증발산량 지도를 작성하여 에디 공분산 기반의 증발산량과 비교 분석하였다. 또한, 작성된 MODIS 기반의 일증발산량 지도의 공간적인 특성을 평가하기 위해 전적비교 지점을 기준으로 물 수지 성분을 산정하여 이의 특성을 분석하였다. 에디 공분산 기반의 증발산량은 플럭스 타워에서 관측된 잠열 플럭스를 KoFlux 프로그램으로 좌표변환, 밀도보정을 수행하여 이상치를 제거한 후 정량화하였다. 이상치 특성으로 발생된 빈 구간(no value)의 자료는 FAO-PM, MDV, Kalman Filter의 3가지 방법으로 보충(Gap-filling)하였다. 면적강우량과 유출량은 KICT(2013)로부터 자료를 제공받아 정량화하였으며, 유역 평균증발산량은 Revised RS-PM 알고리즘으로 작성된 일증발산량 지도로부터 산정하였다. 유역의 저류변화량은 토양수분 변화량이 유역을 대표한다는 가정 하에 관측된 토심별 자료에 유효토심을 고려하여 산정하였다. MODIS 위성과 에디 공분산 기반의 증발산량을 비교 분석한 결과, MODIS 위성 기반에서 330.6mm 정도 증발산량이 크게 산정되었으며, Bias와 RMSE는 평균 -0.91, 2.90의 특성을 나타내었다. 전적비교 지점을 기준으로 물 수지를 분석한 결과, 177.43mm 정도의 편차로 인해 물 수지가 폐합되지 못하였다. 에디 공분산 기반의 증발산량과 물 수지 분석 결과를 토대로 적정성을 평가해 볼 때, MODIS 위성 기반의 증발산량은 설마천 유역의 실제 증발산량을 대표하지 못하였다.

• 한국농업기계학회:학술대회논문집
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• 한국농업기계학회 2000년도 동계 학술대회 논문집
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• pp.228-233
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• 2000

• Journal of Biosystems Engineering
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• 제28권2호
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• pp.151-156
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• 2003

This study was performed to investigate the effect of light quality on evapotranspiration and graft-taking characteristics of watermelon grafted seedlings using blue, red and far-red light-emitting diodes (LED). At initial stage of graft-taking, blue light increased the evapotranspiration rate (EVTR) of grafted seedlings as compared to effects of red and far-red on EVTR of grafted seedlings. Grafted seedlings graft-taken under red and blue LED showed the high graft-taking of 100% and 96%, respectively. However, grafted seedlings graft-taken under far-red LED showed the graft-taking of 80% and survival of 60% with low seedlings quality after hardening. The stem of grafted seedlings graft-taken under red light was elongated but blue light suppressed the stem elongation. The leaf area of grafted seedlings graft-taken under red light was increased. It is concluded that the effect of light quality using LED on graft-taking of watermelon grafted seedlings was significantly recognized. Considering the duration of quality of grafted seedlings graft-taken under artificial lighting, LED could be used as an effective lighting sources to validate the continuance of seedling quality.

• 한국농공학회지
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• 제27권1호
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• pp.62-70
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• 1985

The purpose of this study is to investigate the basic data such the total, the daily maximum, and the peak stage of consumptive use of water and also the soil moisture extraction pattern for irrigation plan of tobacco during the growing period. The plots at which this study was conducted are divided into three fertilization levels of 30g, 60g, and 90g. Each block for three levels is divided as vinyl mulching and irrigation plot, vinyl mulching and nonirrigation plot, and nonmulching and irrigation plot. The results obtained are summarized as follows: 1. The evapotranspiration amount of mulching-irrigation plots are similar to that of mulching-nonirrigation plots. While, the evapotranspiration amount of mulching plots are different obviousely from that of nonmulching plots. Therefore, a significance was recognized between the mulching plots and the nonmulching plots. 2. The amount of evapotranspiration in case of 60g and 90g fertilization level was larger than that of 30g. But the 60g plots and the 90g plots showed little differences. 3. In the total amount of evapotranspiration for each of the experimental plots during the growing period, nonmulching-irrigation plot showed the largest value of 332.9mm, second the mulching-irrigation plot, 284. 9mm, and the mulching-nonirrigation plot, the smallest as 255. 9mm. 4. In the monthly average amount of evapotranspiration for each of the treatment plots, the mulching-irrigation the mulching-nonirrigation, and the nonmulching-irrigation plot showed 3. 6mm, 3. 2mm and 4. 2mm respectively. The daily maximum amount of evapotranspiration showed 5. 1mm, 4. 5mm, and 6.4mm for the mulching-irrigation, the mulching-nonirrigationl, and the nonmulching-irrigation plot respectively. 5. It was confirmed that the higher correlationship exists between the weight of dried leaves and the amount of evapotranspiration, and between the weight of dried leaves and the coefficient of evapotranspiration with the function of logarithms. The coefficient of evapotranspiration have a tendency to increase in proportion to the leaf area index. 6. The maximum coefficient of evapotranspration and the largest leaf area index showed 1. 45 and 5.5 respectively. The stage appeared maximum values was assumed to be before and after flowering. 7. The soil moisture extraction pattern has changed by the depth of root zone for the tobacco's growing. The soil moisture extraction influenced on the 20cm depth of soil after 15 days passed, the 30cm depth after 25 days passed and the whole root zone after 45 days passed from planting. It was shown in the only mulching-irrigation plot after S5days passed from planting that the rate of soil moisture extraction of 20cm layer was larger than that of 10cm layer.

• 농업과학연구
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• 제46권1호
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• pp.137-149
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• 2019

Accurate estimation of reference evapotranspiration (RET) is important to quantify crop evapotranspiration for sustainable water resource management in hydrological, agricultural, and environmental fields. It is estimated by different methods from direct measurements with lysimeters, or by many empirical equations suggested by numerous modeling using local climatic variables. The potential to use some such equations depends on the availability of the necessary meteorological parameters for calculating the RET in specific climatic conditions. The objective of this study was to determine the proper RET equations using limited climatic data and to analyze the temporal and spatial trends of the RET in South Korea. We evaluated the FAO-56 Penman-Monteith equation (FAO-56 PM) by comparing several simple RET equations and observed small fan evaporation. In this study, the modified Penman equation, Hargreaves equation, and FAO Penman-Monteith equation with missing solar radiation (PM-Rs) data were tested to estimate the RET. Nine weather stations were considered with limited climatic data across South Korea from 1973 - 2017, and the RET equations were calculated for each weather station as well as the analysis of the mean error (ME), mean absolute error (MAE), and root mean square error (RMSE). The FAO-56 PM recommended by the Food Agriculture Organization (FAO) showed good performance even though missing solar radiation, relative humidity, and wind speed data and could still be adapted to the limited data conditions. As a result, the RET was increased, and the evapotranspiration rate was increased more in coastal areas than inland.

• 한국생물환경조절학회:학술대회논문집
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• 한국생물환경조절학회 2000년도 학술발표논문집 Proceeding of Bio-Environment control
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• pp.51-54
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• 2000

• 한국환경생태학회지
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• 제25권1호
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• pp.91-101
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• 2011

본 연구는 저토심 옥상녹화에 적용 가능한 초본류 및 지피식물을 중심으로 식물의 광합성작용을 통한 $CO_2$ 흡수량과 증발산량을 정량화하여 도시미기후 관점에서의 옥상녹화식물의 환경성능을 평가하고자 하였다. 이를 위해 옥상녹화용 초본류 7종을 대상으로 적외선 $CO_2$ 가스 분석기에 의한 $CO_2$ 교환 속도 분석을 통해 각 식물의 $CO_2$ 흡수량과 증발산량을 측정하였다. 실험기간은 생장이 활발해지기 시작하는 5월부터 11월까지 매월 2반복 측정하였고, 주변 환경에 예민한 초본류의 특성상, 환경변수가 고정된 실내에서 광도의 변화를 주어 실시하였다. $CO_2$ 흡수량과 증발산량을 산출한 결과 단위엽면적당 $CO_2$ 흡수량은 초본류 중 구절초가 $21.47{\times}10^{-6}g/cm^2/s$, 매발톱꽃이 $12.74\;g{\times}10^{-6}g/cm^2/s$로 높은 흡수율을 보였고, 켄터키블루그래스도 $16.20{\times}10^{-6}g/cm^2/s$로 비교적 높았다. 단위엽면적당 증발산량은 켄터키블루그래스가$8.75{\times}10^{-5}g/cm^2/s$로 가장 많았고, 다음은 매발톱꽃 $8.66{\times}10^{-5}g/cm^2/s$, 구절초 $8.58{\times}10^{-5}g/cm^2/s$ 순으로 나타났다.

• 한국수자원학회논문집
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• 제48권11호
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• pp.915-923
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• 2015

본 연구에서는 유역 물수지 방법을 기반으로 제주도 지역에 적합한 용수량 산정방법을 제안하고, 이를 기반으로 4개 하천유역에 대해 지역 및 고도에 따른 증발산량, 용수량 특성을 평가하였다. SWAT-K 유역모형을 적용하여 1992~2013년 기간에 대해 잠재증발산량과 실제증발산량을 산정하고, 이로부터 유역의 순물소모량을 추정하였다. 고도증가에 따라 잠재증발산량은 선형으로 감소하는 반면, 실제증발산량은 강수량에 의한 토양내 가용수분의 증가로 인해 약 400m 고도까지는 증가하다가 이후 고도에서는 식생, 가용수분의 감소, 저온현상 등으로 인해 감소하는 것으로 나타났다. 고도에 따른 순물소모량은 강정천유역을 제외한 3개 유역에서 고도증가에 따라 순물소모량이 선형적으로 감소하는 것으로 나타났으며, 고도 200m 이하 작물경작지에서의 순물소모량은 연간 559~680m로 분석되었다. 추정된 용수량을 실제 관정 이용량과 비교한 결과, 여름철(6~8월) 양수량은 급수관행으로 인해 크게 증가하는데 비해, 작물경작에 따른 순물소모량은 오히려 감소하는 것으로 나타났다. 이에 대해서는 향후 더 많은 관정 이용량과 추가적인 대상지역을 반영하여 분석이 필요할 것으로 판단된다.