Due to global climate change, Korea is experiencing flooding and drought severely. It is hard to manage water resources because intensive precipitation during short periods and drought are commonly occurred in Korea, recently. Severe drought occurred in 2015 and 2017 in the islands, and coastal and inland areas in Korea, and the citizens experienced decreased water supply and emergency water service by using bottled water. Therefore, the Korean government provided additional governmental funds such as the grant of drought disaster. In this study, we tried to calculate the cost of water for drought response based on the cost of tap water for the regional local governments in Korea and the grant of drought disaster by the Ministry of the Interior and Safety in Korea, etc. The estimated costs of water for drought responses in coastal and inland areas which have a chance to apply alternative water sources such as brackish or seawater desalination and water reuse in Korea were higher than in other areas in Korea. Additionally, as the novel approach of drought response, the 300 m3/day-scale desalination vessel was suggested to provide desalinated water for the islands in Korea. The estimated expenses of water supply for the target island areas (Sinan-gun and Jindo-gun) by the desalination vessel was lower than those by emergency water service by using bottled water.

It is necessary to develop a mobile water production system in order to provide stable water supply in case of disasters such as floods or earthquakes. In this study, we developed a modular mobile water production system capable of producing water for various uses such as domestic water and drinking water while improving applicability in various raw water sources. The water production system consists of three stages of filtration (sand filtration - activated carbon filtration - pressure filtration) to produce domestic water and an additional reverse osmosis process to produce drinking water. In laboratory and field experiments, the domestic water production system showed excellent treatment efficiency for particulate matter, but showed limitations in the treatment of dissolved substances such as dissolved organic matter. In addition, ultraviolet irradiation was considered as additional disinfection step, because it does not form precipitates of manganese oxides after disinfection. Reverse osmosis process was added to increase the removal efficiency of dissolved substances and the treated water satisfied drinking water quality standards. Fluorescence analysis of dissolved organic matter showed that the fulvic acid-like substances in raw water was successfully removed in the reverse osmosis process. The mobile water production system developed in this study is expected to be used not only in water supply in case of disaster, but also widely used in islands and rural area.

본 연구에서는 정밀관수를 위한 관수시간, 점적라인 설치 등 관수시스템 설계를 위한 기초 데이터를 얻고자 점적관수 시 토성에 따른 물의 수분함량변화를 공간적, 시간적 변이의 차이를 구명하였다. 20cm의 간격의 노즐로 설치된 1열 점적관을 이용 관수 하였을 경우 양토와 사양토내의 수분은 중심을 따라 대칭 형태를 유지하면서 이동하였으나 수분확산 폭은 양토가 더 넓고 속도가 느린 경향을 나타내었다. 상대적으로 높은 모래성분 함량을 갖는 양질사토의 경우는 낮은 수분 보유력으로 인하여 위치별 수분함량의 변화는 상대적으로 낮았으며 그만큼 물 빠짐정도가 큰 것으로 나타났다. 관수개시점과 종말점을 고려하였을 때 사양토의 경우 20cm 깊이에서 관수개시 30분 후에 수분의 포화가 이루어졌으나 양토와 양질사토의 경우는 약 80분이 소요되어 효율적인 수분공급 측면에서 관수시간은 토성별로 달리해야 하는 것으로 나타났다. 깊이 10cm에서의 시간에 다른 토양수분의 감쇠특성은 지수함수의 형태를 나타내었으며 토양별 안정된 상태에서의 수분함량은 양토, 사양토, 양질사토 각각 17.6%, 6.2%, 4.2%로 예측되어 토성에 따라 잔여수분함량은 차이가 있음을 확인하였다. 토양수분함량과 토양수분퍼텐셜과의 관계를 나타내는 수분특성곡선은 시험 토양의 경우 모두 높은 결정계수를 갖는 지수함수로 근사가 가능하여 수분퍼텐셜을 이용하여 측정하는 재배시스템에서 대응하는 수분함량 예측에 유용한 관계식을 얻었다.

This study was conducted to assess water movement in paddy-upland rotation soil scheduled for ginseng cultivation through the measurement of infiltration and permeability of soil water. Soil sample was divided with four soil layers. The first soil layer (to 30cm from top soil) was loamy sand, the second and the third soil layers (30~70 ㎝) were sand, and the fourth (〈 120 ㎝) was sandy loam. The soil below 130 ㎝ of fourth soil layer was submerged under water. The shear strength, which represents the resisting power of soil against external force, was 3.1 kPa in the first soil layer. This corresponded to 1/8 of those of another soil layer and this value could result in soil erosion by small amount of rainfall. The rates of infiltration and permeability depending on soil layers were 39.86 cm hr-1 in top soil, 2.34 cm hr-1 in 30~70 ㎝ soil layer, 5.23 cm hr-1 and 0.18 cm hr-1 in 70~120 ㎝ soil layer, with drain tile, and without drain tile, respectively. We consider that ground water pooled in paddy soil and artificial formation of soil layer could interrupt water canal within soil and affect negatively on water movement. Therefore, we suggest that to drain at 5 m intervals be preferable when it makes soil dressing or soil accumulation to cultivate ginseng in paddy-upland rotation soil to reduce failure risk of ginseng cultivation.

낙동강 유역의 용수수급 불균형을 해결하기 위한 한 대안으로서 한강과 낙동강 유역을 서로 연계하여 한강에서 낙동강 유역으로의 물이동 가능성을 검토하였다. 검토방법으로는 낙동강 유역의 용수부족량을 추정한 뒤 한강 유역에서의 여유량을 모의기법과 최적화기법을 사용하여 추정하였다. 모의기법으로는 HEC-5를 사용하여 중,소규모댐을 검토하고, 최종적으로 동적계획법을 사용하여 다목적댐에 대하여 검토하였다. 또한, 경제적 측면에서 한강-낙동강 유역간 물이동과 낙동강