• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2020년도 학술발표회
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• pp.396-396
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• 2020

기후변화는 여러 수자원 문제를 야기하며, 특히 가뭄으로 인해 농업용 저수지의 물관리는 점점 중요해지고 있다. 여러 둑높이기 농업용 저수지 중 나주호는 수혜면적에 비해 유역면적이 작아 저수율관리에 어려움을 겪고 있다. 실제로 2017년과 2018년 가뭄이 발생함에 따라 저수율이 20 %까지 저하되었으며, 수혜구역내 간이 양수장, 양수 저류 등 가뭄대책이 시행되었다. 그럼에도 불구하고 나주호의 저수율이 회복되지 않아 단수를 실시하는 등 물관리에 어려움을 겪었다. 이 연구에서는 저수지인 나주호를 대상으로 기상자료, 나주호의 저수율, 공급량 자료를 바탕으로 CAT 모형을 적용 가뭄년도의 유입량 변화를 추정하였다. 검보정의 경우 CAT 3.0 버전에 포함된 SCE-UA 최적화기법을 이용하였다. 그 결과, 2008년부터 2019년까지의 평균 연간 유입량은 6,549 만㎥으로 분석되었으며, 평균 연간 유출율은 48 %로 조사되었다. 하지만, 가뭄이 발생하였던 2017년도의 경우 평균 연간 유입량이 2,070 만㎥, 유출율은 27 %로 조사되었다.

• 한국기후변화학회지
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• 제7권1호
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• pp.77-84
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• 2016

Seedling stage is particularly important for tree survival and is easily influenced by warming. Therefore, air temperature being increased due to climate change may affect physiological traits and growth of seedlings. This study was conducted to investigate the physiological and growth responses of Larix kaempferi seedlings to open-field experimental warming. 1-year-old and 2-year-old L. kaempferi seedlings were warmed with infrared lamps since April 2015 and April 2014, respectively. The seedlings in the warmed plots were warmed to maintain the air temperature to be $3^{\circ}C$ higher than that of the control plots. Physiological responses (stomatal conductance, transpiration rate, net photosynthetic rate and total chlorophyll content) and growth responses (root collar diameter (RCD), height and biomass) to experimental warming were measured. Physiological and growth responses varied with the seedling ages. For 2-year-old L. kaempferi seedlings, stomatal conductance, transpiration rate and net photosynthetic rate decreased following the warming treatment, whereas there were no changes for 1-year-old L. kaempferi seedlings. Meanwhile, total chlorophyll content was higher in warmed plots regardless of the seedling ages. Net photosynthetic rate linked with stomatal conductance also decreased due to the drought stress and decrease of photosynthetic efficiency. In response to warming, RCD, height and biomass did not show significant differences between the treatments. It seems that the growth responses were not affected as much as physiological responses were, since the physiological responses were not consistent, nor the warming treatment period was enough to have significant results. In addition, multifactorial experiments considering the impact of decreased soil moisture resulting from elevated temperatures is needed to explicate the impacts of a wide range of possible climate change scenarios.

• 농업과학연구
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• 제31권2호
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• pp.135-148
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• 2004

Rice is not only main food but also key farm income source of Korean farmers. In spite of the above facts, rice productivity was decreased on account of drought in every 2 or 3 years interval owing to the vulnerability of irrigation facilities throughout Korea in the past decades. As an context of the first five year economic development plan, all weather farming programme including 4 big river basin comprehensive development projects and large and medium sized irrigation water development projects were carried out successfully. Therefore the area of irrigated paddy were increased from 58% in 1970 to 76.2% in 1999. In the past decades, the Government had invested heavy financial funds to develop irrigation water but as an factor share analysis, the contribution rates of irrigation water and investment for farmland base development project have not been identified yet in national agricultural economic level. It is very scarce to find out the papers concerned to macro-economic factor share analysis or contribution rates of water and investment cost to rice production value in Korea considering the production function of the quantity of irrigation water and investment cost as independent variables. Accordingly this paper covered and aimed at identifying (1) derivation of rice production function with the time serial data from 1965 to 1999 and the contribution rates of irrigation water and total investment cost for farmland base development project. The analytical model of the contribution rates was adapted the famous Cobb-Douglass production function. According to the model analysis, the contribution rate of irrigation water to rice production in Korea was shown 37.8% which was equivalent to 0.28 of the production elasticity of water. The contribution rate of farmland base development project cost was revealed 22% and direct production cost of rice was contributed 60% in the growth of rice production and farm mechanization costs contributed to 18% of it respectively. The two contribution rates comparing with the direct production cost were small but without irrigation water and farmland base development, application of high-pay off inputs and farm mechanization might be impossible. Considering the food security and to cope with the frequent drought, rice farming and investment for the irrigation water development should be continued even in WTO system.

• 한국수자원학회논문집
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• 제46권6호
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• pp.613-627
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• 2013

본 연구에서는 지속기간별(1-, 3-, 6-, 12-, 24개월)로 가장 가뭄이 심한 해의 5월 건조현상을 지역별로 분석하기 위해 1973년부터 2006년까지 우리나라 53개 기후관측지점에서 관측된 월별 기후자료를 이용하여 FAO Penman-Monteith 기준잠재증발산량(RET)을 산정하였다. 그리고 강수량(P)에 대한 RET의 비(P/RET)를 이용하여 건조지수(aridity index)와 P/RET의 변동지수(variation index, VI)를 산정하고, 표준강수지수(standard precipitation index, SPI)와 비교하였다. 우리나라 지역별 건조현상을 파악하기 위해 53개 기후관측지점을 20개 연구지역으로 구분하여 분석하였다. 또한 지역별 건조지수의 추세분석을 위해 Mann-Kendall 추세분석, Spearman rank test 그리고 Sen's slope을 적용하였다. 분석 결과에 의하면 각 지속기간별로 P/RET의 변동지수(VI)와 표준강수지수사이에 양호한 상관관계를 보였다. 또한 우리나라 전역에 걸쳐서 지속기간이 단기화 될수록 5월 기후가 더욱 건조한 것으로 나타났다. 3개월이나 6개월 지속기간의 경우 대부분 지역에서 유의하거나 혹은 유의하지 않은 수준에서 건조지수의 감소추세를 보였다. 반면에 12개월 및 24개월 지속기간의 경우 유의한 건조지수의 감소추세를 보이는 지역은 없는 것으로 나타났다.

• 한국농공학회지
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• 제26권2호
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• pp.47-58
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• 1984

The study results of the mosture consumption character and irrigation effect of tomato, red pepper and chinese cabbage, in case the soil moisture is kept with different moisture content by the soil properties(loam, sandy loam, sand), are summarized as follows: 1. The available rainfall under bare soil condition had an order of sand>sandy loam> loam and their average was 64.2%. 2. Total moisture consumption under bare soil condition had an order of loam>sandy loam>sand and their average was 4.2mm. 3. The amount of irrigated water to keep certain soil moisture under bare soil condition showed minimum in sand and maximum in loam. It is considered because the capillary phenomenon was more developed in loam. 4. Total moisture consumption of tomatoes under premature cultivation showed 925mm in maximum and had on order of loam>sandy loam>sand. In the aspect of re-irrigation point, it had an order of PF 1.5> PF 1.7>PF 2.1. In case the twenty years's drought frequency was taken into account, the target amount of irrigation water meeded for premature cultivation was 916mm and its average daily moisture consumption was 10.8mm. 5. Total moisture consumption of red pepper under open cultivation showed 1145mm in maximum and had an order of loam>Sandy loam>sand. In the aspect of re-irrigation frequency was taken into consideration the target amount of irrigation water was 1,174.8mm and its average daily moisture consumption was 8.0mm. 6. Total moisture consumption of autumn chinese cabbages was 349mm in maximum and had an order of loam>sandy loam>sand. In the aspect of re-irrigation point, it had an order of PF 1.5>PF 2.1>PF 2.7. In case the twenty year's drought frequency was taken into account, the target amount of irrigation water needed for chinese cabbage cultivation was 259.5mm and its average daily moisture consumption was 6.5mm. 7. It is effective to keep the soil moisture of tomato from PF 1.5 to PF 2.1 in loam and the soil moisture control was effective in sandy loam than red pepper and chinese cabbage. In sand, the production was severaly decreased and the re-irrigation point of PF 1.5 was effective.

• 환경생물
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• 제40권3호
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• pp.239-246
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• 2022

가시상추는 도로변, 초지, 철도변, 주택가, 밭둑 등 도처에서 생육하는 생태계교란식물 중의 하나이다. 가시상추는 일반적으로 가을에 발생하여 로제트 형태로 월동하고 이듬해 초여름에 꽃을 피고 종자를 맺는다. 가시상추의 종자는 20℃ 이상만 되면 휴면성이 없이 즉시 발아할 수 있다. 가시상추 종자 속의 내생세균에 의해 가뭄 견딤성이 강해 도로변에서도 잘 생육할 수 있다. 가시상추는 50주 m^-2이상의 밀도에서 콩 수확량의 60~80% 손실을 일으킬 뿐만 아니라, 다른 생태계교란식물의 선구자 역할을 하여 토착식물과 경쟁하기 때문에 제거하는 것이 좋다. 여러 가지 방제방법 중 화학적 방제법이 가장 효과적이고 널리 사용되고 있다. 토양처리제인 oxyfluorfen와 pendimethalin 등이 가시상추의 발생을 억제하였다. 경엽처리제는 glyphosate, glufosinate-ammonium이 많이 사용되고 있다. 경엽처리제 중 2,4-D, dicamba, MCPA 등에 저항성을 보이는 가시상추가 발생하였기에 작용점이 다른 제초제 살포를 권장하고 있다.

• 자원환경지질
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• 제40권4호
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• pp.389-401
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• 2007

2001년부터 2004년까지 유성 소유역내 강수, 지하수, 지열수의 산소 및 수소 동위원소 조성 변화를 검토하였다. 1975년부터 2006년까지의 강수 패턴을 분석한 결과, 연구지역은 $6{\sim}7$년의 가뭄 주기성을 보였다. 2001년도 가뭄 시기부터 2004년까지 4년간 강수의 산소 수소 동위원소 조성은 점차 무거운 성분으로 변화해가는 양상을 보였다. 연구 지역에서 4년간의 강수량을 고려한 동위원소의 가중 평균간을 구해 보면 ${\delta}^{18}O=-7.7%o,\;{\delta}D=-51%o$로서, 동일 기간 내의 지하수와 지열수의 동위원소보다 무거운 조성 범위를 보였다. 이는 연구 지역의 지수 및 지열수가 동위원소적 관점에서 2-3년 이내의 강수에 의해 큰 영향을 받지 않는 것을 의미한다. 기존 자료들을 검토해 볼 때, 연구지역에서의 지하수와 지열수는 1990년과 1992년이 가장 무거운 동위원소 조성을 보였으며 이후로는 산소 및 수소 동위원소 조성이 점차 가벼워지는 쪽으로 변화해가는 양상을 보였다.

• 한국수자원학회논문집
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• 제44권4호
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• pp.305-314
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• 2011

북한강 수계의 경우 북한이 임남댐을 개발하여 유역변경식으로 물을 이용하고 있어 하류지역에서 여러 가지 문제가 나타나고 있다. 따라서 남 북한이 공유하천을 효과적으로 관리하기 위해서는 수량이나 수질 등 다양한 분야에서의 협력이 절실히 요구되고 있다. 그러나 남 북공유하천에서 상 하류국가간 물이용의 공평성을 실현하기 위한 노력은 매우 미흡한 실정이다. 본 논문에서는 남북공유하천의 공평한 물이용의 판단기준이 되는 수리권을 검토하기 위해 북한의 임남댐에 의한 영향을 주요 분야별로 심도 있게 분석하였다. 분석결과, 한강유역의 용수공급은 1978년을 이수안전도 평가를 위한 기준갈수년으로 할 경우 임남댐으로 인해 379백만$m^3$/년의 공급부족이 발생하는 것으로 나타났다. 아울러 한강 수계의 발전용댐도 유입량 감소로 인하여 연간발전량이 234GWh/년 감소하게 되었고, 수질은 북한강 삼봉리 지점 기준 BOD 약 0.065 ppm 증가하는 것으로 분석되었다. 결과적으로 남북공유하천에서 북한의 절대영토주권주의에 입각한 불공평한 수자원 이용은 하류국가인 남한에 직 간접적으로 상당한 영향을 미치고 있음을 확인하였다.

• 대한원격탐사학회지
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• 제28권3호
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• pp.267-276
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• 2012

Terminal lakes are widely distributed in the arid and semi-arid Gobi of Mongolia, and serves as important water resource for local people and livestock. However, such lakes are subject to great fluctuations in its size depending on climatic conditions and human water utilization. The Orog Lake is one such example that has shown remarkable fluctuation in recent years. In this study, we investigated the temporal changes of Orog Lake surface area by using 16-day MODIS 250 m NDVI products from 2000 to 2010. The results were compared with climate variability represented by monthly precipitation and temperature. Our results show that the Orog Lake gradually shrank for the period from 2000 to 2010, but with a significant range of seasonal and inter-annual variability. The lake area showed considerable seasonal variations, as it expanded in spring and fall, primarily due to snow melt and summer precipitation, respectively. Extreme drought period from 2000 to 2002 triggered the substantial reduction in lake area, leading to dry-up in year 2005, 2006, 2007, and 2009. After dry-up once occurred in 2005, the lake repeated reappearance and disappearance depending on seasonal and annual precipitation. Our findings implicate that the ground water fluctuated around the lake bottom level since 2005. This suggests the highly vulnerable nature of Orog lake, which greatly depends on future precipitation change.

• 상하수도학회지
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• 제32권3호
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• pp.221-233
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• 2018

Two climate change scenarios, the RCP (Representative Concentration Pathways) 4.5 and the RCP 8.5 in the fifth Assessment Report (AR5) by Intergovernmental Panel on Climate Change (IPCC), were applied in the Yocheon basin area using the SWAT (Soil and Water Assessment Tool) model to estimate changes in flow rates and pollutant loadings in the future. Field stream flow rate data in Songdong station and water quality data in Yocheon-1 station between 2013~2015 were used for model calibration. While $R^2$ value of flow rate calibration was 0.85 and $R^2$ value of water qualities were in the 0.12~0.43 range. The total study period was divided into 4 sub periods as 2030s (2016~2040), 2050s (2041~2070) and 2080s (2071~2100). The predicted results of flow rates and water quality concentrations were compared with results in calibrated periods, 2015s (2013~2015). In both RCP scenarios, flow rate and TSS (Total Suspended Solid) loadings were estimated to be in increasing trend while TN (Total Nitrogen) and TP (Total Phosphorus) loadings showed decreasing patterns. Also, flow rates and pollutant loadings showed larger differences between the maximum and the minimum values in RCP 4.5 than RCP 8.5 scenarios indicating more severe effect of drought and flood, respectively. Dependent on simulation period and rainfall periods in a year, flow rate, TSS, TN and TP showed different trends in each scenario. This emphasizes importance of considerations on time and space when analyzing climate change impacts of each variable under various scenarios.