• 자원환경지질
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• 제11권3호
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• pp.99-108
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• 1978

The Gum-Ho river basin is one of the densely populated area having more than 35% of the total population and it was also well irrigated since earlier days in the Nackdong river basin. Most of the easily developed source of surface water are fully utilized, and at this moment the basin is at the stage that no more :surface water can be made available under the present rapid development of economic condition. Since surface water supplies from the basin have become more difficult to obtain, the ground water resources must be thoroughly investigated and utilized greatly hereafter. In economic ground of the basin what part could ground water play? In what quantities and, for what uses could it be put? The answer to these questions can be relatively simple;the ground water resources in the basin can be put at almost any desired use and almost anywhere in the basin The area of the basin is at about $2088km^2$ in the middle part of Nackdong river basin and it is located along the Seoul-Pusan express highway. The mean annual rainfall is about 974.7mm, most of which falls from June to September during the monsoon. Accumulated is appeared approximately after every 8 year's accumlated dry period with the duration of 5 years. The water bearing formation in the basin include unconsolidated alluvial deposits in Age of Quaternary, saprolite derived from weathered crystalline rocks, Gyongsang sedimentary formations of the period from late Jurassic to Cretaceouse, and igneouse rocks ranging of the Age from Mesozoic to Cenozoic. The most productive ground water reservoir in the basin is calcareous shale and sandstones of Gyongsang system, which occupies about 66% of the total area. The results of aquifer test on Gyongsang sedimentary formation show that average pumping capacity of a well drilled into the formation with drilling diameter and average depth of $8{\frac{1}{2}}$ inch and 136m is $738m^3/day$ and also average specific capacity of those well is estimated $77.8m^3/D/M$. Total amount of the ground water reserved in the basin is approximately estimated at 37 billion metric tons, being equivalent 18 years total precipitations, among which 7 billion metric tons of portable ground water can be easily utilized in depth of 200 meters.

• 한국농림기상학회지
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• 제22권1호
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• pp.26-46
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• 2020

이 연구의 목표는 관개된 옥수수 밭에서의 복사, 에너지 및 엔트로피의 교환을 평가하고 문서화하는 것이다. 열역학적 관점에서, 우리는 이 농업생태계를 태양 복사로 인해 시스템 내부와 외부 사이에 큰 경도(gradient)가 부여되는 열린 열역학적 시스템으로 간주하였다. 따라서 시스템이 평형에서 멀어질 때, 열역학적 원칙에 따라 비평형 소산 과정(nonequilibrium dissipative process)인 이 생태-사회시스템이 모든 생물, 물리, 화학 및 인위적 구성 요소를 사용하여 태양으로부터 주어진 경도에 저항하여 이를 감소시키도록 움직인다고 가정하였다. 이 가설을 검증하기 위한 첫 단계로서 미국 네브라스카의 옥수수 밭에 위치한 AmeriFlux의 NE1 사이트에서 2003년부터 2014년까지 관측된 플럭스 및 미기상 자료를 사용하여 복사, 에너지 및 엔트로피의 교환을 정량화하였다. 12년 평균한 생장기간의 결과에 따르면, 시스템의 에너지 포획(순복사와 하향단파복사의 비, R_n/R_s↓)은 옥수수의 생장과 함께 증가하였고, 생장기간이 비생장기간보다 약 80% 높았다. 생장기간 동안 시스템 내의 엔트로피 생성(σ)은 평균 9.56 MJ m^-2 K^-1이었고, 주로 하향단파 복사에 의해 결정되었다. 엔트로피 수송(J)은 잠열플럭스, 순장파복사, 현열플럭스의 순으로 기여하였고, 시스템 외부 환경으로 퍼낸 양은 σ의 ~84%에 해당하는 -7.99 MJ m^-2 K^-1이었다. 따라서 매년 생장 기간동안 시스템 내에 순 축적된 엔트로피(dS/dt)는 1.57 MJ m^-2 K^-1이었다. 탄소 흡수 효율(CUE)은 1.25~1.62, 물 사용 효율(WUE)은 1.98~2.92 g C (kg H₂O)^-1이었고 모두 옥수수의 성장과 함께 증가하였다. 극심한 가뭄으로 관개가 더 빈번하게 행해진 2012년의 경우, σ와 J가 모두 평년보다 10% 많은 최대값을 보였고, 그 결과 서로 대부분 상쇄되어 dS/dt는 평년보다 조금 높은 수준에 머물렀다. 가뭄 중에도 빈번한 관개로 인해 엔트로피 수송의 주된 경로가 현열플럭스에서 잠열플럭스로 바뀌면서 생산량과 CUE는 평년 값을 웃돌았으나 물과 빛의 사용 효율은 오히려 낮아졌다. 이러한 결과에 근거하여 관개된 옥수수 생태-사회시스템의 지속가능성의 변화를 평가하기에는 아직 여러가지 문제가 남아있다. 자기-조직화 과정은 시스템과 주변 간의 경도를 효과적으로 감소시키는 역할을 한다. 따라서 엔트로피 자료와 함께, 지속가능성의 척도가 되는 자기-조직화 역량을 나타내는 스펙트랄 엔트로피, 또는 하부시스템의 구조 및 에너지·물질의 흐름의 강도와 방향의 변화를 가늠할 수 있는 역학적 과정망(dynamic process network) 분석 등의 추가 연구가 병행되어야 한다.

• 기술사
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• 제10권2호
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• pp.13-26
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• 1977

The Kum-Ho river basin is one of the densely populated area having more than 35% of the total population and it was also well irrigated since ealier days in the Nackdong River Basin Most of the easily developed source of surface water are fully utilized, and at this moment the basin is at the stage that no more surface water can be made available under the present rapid development of economic condition. Since surface water supplies from the basin have become more difficult to obtain, the ground water resources must be thoroughly investigated and utilized greatly hereafter. In economic ground of the basin what part could ground water play\ulcorner In what quantities and, for what uses could it be put\ulcorner The answer to these questions can be relatively simple; the ground water resources in the basin can be put at almost any desired use and almost anywhere in the basin. The area of the basin is at about 2088km$^2$ in the middle part of Nackdong River Basin and it is located along the Seoul-Pusan Express Highway. The mean annual rainfall is about 974.7m/m, most of which falls from June to September during the monsoon. Accumulated wet period is appeared approximately after every 8 year's accumulated dry-period with the duration of 5 years. The water bearing formations in the basin include unconsolidated alluvial deposits in Age of Quatenary, saprolite derived from weathered crystalline rocks, Kyongsang sedimentary formations of the period from late Jurassic to Cretaceouse, and igneouse rocks ranging of the Age from Mesozoic to Cenozoic. The most productive ground water reservoir in the basin is calcareouse shale and sandstones of Kyongsan system, which occupies about 66% of the total area.

• 한국농공학회지
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• 제45권7호
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• pp.57-69
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• 2003

To evaluate nutrient dynamics with different fertilization in paddy field and develop water quality model, mass balance analysis was performed during growing season of 2001-2002 in field experimental plots irrigated with groundwater. As a result of water balance analysis, most of outflow was surface drainage as about half of total outflow and about 500mm was lost by evapotranspiration. The water budget was well balanced. The runoff from paddy field was influenced by rainfall and forced drain. Especially runoff during early cultural periods more depends on the forced drain. As a result of mass balance analysis, most of nutrient was input by fertilization and lost by plant uptake. Significant amount of nitrogen were supplied by precipitation and input from upper paddy field, comprising 12%∼28% of total inflow. Nutrient loading by surface drainage was occurred showing about 15%∼29% for T-N and 6%∼13% for T-P. The response of rice yield with different fertilization was not significant in this study. Water quality model for paddy field developed using Dirac delta function and continuous source was calibrated and validated to surface water quality monitoring data. It demonstrates good agreement between observed and simulated. The nutrient concentration of surface water at paddy field was significantly influenced by fertilization. During early cultural periods when significant amount of fertilizer was applied, surface drainage from paddy field can cause serious water quality problem. Therefore, reducing surface drainage during fertilization period can reduce nutrient loading from paddy fields. Shallow irrigation, raising the weir height in diked rice fields, and minimizing forced surface drainage are suggested to reduce surface drainage outflow.

• 한국농공학회논문집
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• 제52권5호
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• pp.61-68
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• 2010

Jangchan reservoir is located in Okcheon county, Chungbuk province, of which watershed area is $29.4\;km^2$ from outside, and $5.1\;km^2$ from inside watershed, effective storage capacity is $392{\times}10^4\;m^3$, paddy area to be irrigated is 474 ha. To determine inflows from Keumcheon weir located in outside watershed on an optimum level, a repeated procedure which is composed of simulation of inflows to Keumcheon weir, setting of range of water taking at Keumcheon weir, simulation of inflows to Jangchan reservoir, estimation of paddy water from Jangchan reservoir, and simulation of water storages in Jangchan reservoir was selected. Parameters of DAWAST model for simulating inflows to Jangchan reservoir were determined to UMAX of 315 mm, LMAX of 21 mm, FC of 130 mm, CP of 0.018, and CE of 0.007 with absolute sum of errors in reservoir water storages minimized using unconstrained Simplex method because of no inflows data. Inflows to Keumcheon weir were simulated to $2,132{\times}10^4\;m^3$ on an annual average. Optimal range of water taking at Keumcheon weir to transfer to Jangchan reservoir were $0.81{\sim}50\;mm/km^2/d$, which were summed up to $1,397{\times}10^4\;m^3$ in 66% of total on an annual average. Inflows to Jangchan reservoir were simulated to $1,739{\times}10^4\;m^3$ on an annual average of which were 80 % from Keumcheon weir of outside watershed. Requirements to paddy water from Jangchan reservoir were estimated to $543{\times}10^4\;m^3$ on an annual average.

• 한국농공학회논문집
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• 제49권2호
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• pp.3-13
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• 2007

The primary objective of this study was to compare water use efficiencies between subsurface drip irrigation and furrow irrigation. The uniformity of used drip lines was tested to determine if clogging would be a threat to the long-term success of a subsurface drip irrigation system. Three crops, cantaloupe, lettuce, and bell pepper, were grown in four plots for each irrigation system. Significantly less water was applied with subsurface drip irrigation than with furrow irrigation (29.5 % less for cantaloupe and 43.2 % less for bell poppet) in order to produce similar crop yields. Water use efficiencies with subsurface drip irrigation were significantly higher than those with furrow irrigation fur cantaloupe (P-value = 0.018) and bell pepper (P-value ${\leq}$ 0.001). Drip-irrigated lettuce, a shallow-rooted crop, had moderately higher water use efficiency during the first two seasons, while no difference was observed in the third season. After the experiment, the uniformity of the drip lines was 92.1 % on average and classified as good. The high values fur water use efficiency and uniformity indicate that subsurface drip irrigation can be a sustainable method for conserving irrigation water.

• 한국환경농학회지
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• 제37권4호
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• pp.317-323
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• 2018

우리나라 관개논의 여름철 강우기 Middleton's 분산성 점토는 불검출 ~ 4.8%의 범위로 나타났으며 최대값은 점토 함량 18% 이상 토양에서 나타났으나 점토 분산성은 점토 함량 18% 미만 토양에서 높게 나타났다. 대상지역의 60%에서 40마력이상 농기계를 사용한 경작연수가 길수록 분산성 점토 함량이 높은 값을 나타내었다. 단, 치환성 나트륨 함량 퍼센트의 차이가 큰 간척논은 예외로 나트륨함량이 높을수록 분산성 점토가 높았다.

• 생물환경조절학회지
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• 제12권3호
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• pp.152-159
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• 2003

본 연구에서는 감자 플러그묘를 생산하고자 개발된 폐쇄형 시스템에서 식물묘 생산에 필요한 관수량, 식물묘와 배지로부터의 증발산량, 기습기에 의한 가습량, 공조기구에 의한 제습량, 환기에 의한 수분손실 등을 정량적으로 분석하고, 수분수지에 미치는 상대습도의 영향을 검토하였다. 기온, 상대습도, 광주기 및 PPF 를 각각 20$^{\circ}C$, 70%, 16/8 h, 200 ${\mu}$mol${\cdot}m^{-2}{\cdot}s^{-l}$로 조절한 조건에서 묘생산 시스템에서의 기습량, 제습량, 관수량 및 증발산량은 각각 167.9 kg${\cdot}m^{-2},\;196.9{\cdot}m^{-2},\;44.3\;kg{\cdot}m^{-2},\;33.5\;kg{\cdot}m^{-2}$로 나타났다. 식물체와 배지가 지닌 수분함량은 각각 $1.2\;kg{\cdot}m^{-2},\;6.9\;kg{\cdot}m^{-2}$ 로 나타났다. 3수준 (60%, 70%, 80%)의 상대습도 처리에 따른 묘생산 시스템내의 가습량, 제습량, 관수량, 증발 산량, 배지와 식물체의 수분함량은 상대습도가 증가할수록 모두 증가하였다. 그러므로 상대습도가 낮아질수록 시스템내의 물사용량은 줄어들었으나, 물이용가능효율은 증가하였다. 제습된 물을 재이용할 경우 시스템의 물이용가능효율은 상대습도 처리에 따라 0.97~1.0으로 나타났다. 따라서 제습된 물을 회수하여 재이용할 수 있는 폐쇄형 시스템의 개발은 식물묘생산에 요구되는 수분소모량을 절감시킬 뿐만 아니라 물소비 절약형 식물생산 방식의 확립에 크게 기여할 것이다.

• 한국농공학회지
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• 제44권5호
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• pp.116-126
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• 2002

Discharge pattern and water quality were investigated in the drainage water from about 10 ha of groundwater-irrigated paddy field in the growing season of 2001. Total discharge quantity was about 1,117.2 mm in which about 75% was caused by management drainage due to cultural practice of paddy rice farming and the rest by rainfall runoff where total rainfall was about 515 mm. Dry-day sampling data showed wide variations in constituent concentrations with average of 26.14 mg/L, 0.37 mg/L, 3.54 mg/L at the inlet, and 43.60 mg/L, 0.34 mg/L, 3.58 mg/L at the outlet for CO $D_{cr}$ , T-P, and T-N, respectively. Wet-day sampling data demonstrated that generally CO $D_{cr}$ followed the discharge pattern and T-P was in opposite to the discharge pattern, but T-N did not show apparent pattern to the discharge. Discharge and load are in strong relationship. And based on regression equation, pollutant loads from groundwater irrigation area are estimated to be 288.34, 1.17, and 5.45 kg/ha for CO $D_{cr}$ , T-P, and T-N, respectively, which was relatively lower than the literature value from surface water irrigation area which implies that groundwater irrigation area might use less irrigation water and result in less drainage water, Therefore, total pollutant load from paddies irrigation with groundwater could be significantly lower than that with surface water. This study shows that agricultural drainage water management needs a good care of drainage outlet as well as rainfall runoff. This study was based on limited monitoring data of one year, and further monitoring and successive analysis are recommended for more generalized conclusion.

• 한국농공학회논문집
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• 제60권3호
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• pp.113-121
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• 2018

The objectives of the research were 1) to develop the low-cost and high efficient desalination system to treat brackish water having high salt contents for irrigation at greenhouses near coast, and 2) to monitor and assess the effects of the brackish water desalination system on soil environment and growth in squash greenhouse cultivation area. The monitoring site was one of the squash greenhouse cultivation farm at Choengam-ri, Jinsang-myun, Gwangyang-si, Jeonnam-Do Monitoring results for groundwater irrigation water quality, and salinity showed a remarkable difference between control and treatment group. The salinity of soil at treatment group was less than at control group. While, the system made possible to increase the squash quantity from 4.7 ea to 6.3 ea at each and the average weight of the harvested squash was increased from 277.2 g to 295.1 g. The applied brackish water desalination system may be appled to reclaim sea or brackish irrigated area as alternative water resources, although long-term monitoring is needed to get more representative results at different level of salinity.