• 제목/요약/키워드: flooding depths

검색결과 25건 처리시간 0.028초

Ecophysiology of Seed Germination in Chinese Milk Vetch (Astragalus sinicus L.)

  • Shim, Sang-In;Kang, Byeung-Hoa
    • 한국작물학회지
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    • 제49권1호
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    • pp.19-24
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    • 2004
  • Germination and emergence habits of Chinese milk vetch (CMV) were examined to obtain the basic information for the effect of environmental conditions and cultural practices on the seedling density. Seed germination tests with different water potentials, temperatures, and soil and water depths showed the environmental effects on the characters related to seed germination in CMV. Imbibition under different temperatures reflects that initial velocity was rapid at higher temperature, however, the times to full imbibition were not different between 15 and $25^{\circ}$. The optimal germination temperature for CMV germination was ranged from 15 to 20 and the germination was highly affected by water potential of media at relatively high temperature above $20^{\circ}$. When the seeds were sown in flooded condition the germination was not proportionally affected by water depth. In addition, there was no correlation between water depth and oxygen concentration. The germination of seeds flooded by 2cm water depth were poorly germinated compared to other depths. Results indicated that the germination of submerged seeds was more highly influenced by flooding depth than the temperature, it was also affected more strongly at 10 than $20^{\circ}$. Emergence of CMV depending on the thickness of covered soil was poor when the soil layer was greater than 5cm. In the experiment with seeds collected between 22 days after flowering (OAF) and 52 DAF, the highest germination ability of CMV seeds was observed at 39 DAF and germinability was decreased subsequently as seeds became mature. The lower germinability may be due to the enhanced seed dormancy.

Efficient crosswell EM tomography for monitoring geological sequestration of $CO_2$

  • Lee, Ki-Ha;Kim, Hee-Joon;Song, Yoon-Ho
    • 한국지구물리탐사학회:학술대회논문집
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    • 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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    • pp.321-327
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    • 2003
  • [ $CO_2$ ] sequestration in oil reservoirs can be one of the most effective strategies for long-term removal of greenhouse gas from atmosphere. This paper presents an advantage of the localized nonlinear approximation of integral equation solutions for inverting crosswell electromagnetic data, which are observed as a part of pilot project of $CO_2$ flooding at the Lost Hills oil field in central California, U.S.A. To monitor the migration of $CO_2$, we have used 2-D cylindrically symmetric and 2.5-D tomographic inversion methods. These two schemes produce nearly the same images if the borehole separation is large compared with the skin depth. However, since the borehole separation is much less than five skin depths in this $CO_2$ injection experiment, the 2.5-D model seems to be more reliable than the 2-D model. In fact, the pre-injection 2.5-D image is more successfully compared with induction logs observed in the two wells than the 2-D model. From the time-lapse crosswell imaging, we can confirm the replacement of brine with $CO_2$ makes a decrease of conductivity.

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무경운 자운영 피복 논에서 담수 깊이가 잡초발생과 수량에 미치는 영향 (Impacts of Flooding Depths on Weed Occurrence and Yield in No-tillage Paddy Field Covered with Chinese Milk Vetch)

  • 홍광표;이영한
    • 한국토양비료학회지
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    • 제44권2호
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    • pp.176-180
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    • 2011
  • 유기농업을 위한 무경운 논에서 자운영 피복을 통한 담수깊이가 잡초발생과 벼 수량에 미치는 영향을 구명하여 농가현장에 적용할 수 있는 기술을 연구하였다. 무경운 논에서 자운영 피복과 담수깊이를 10 cm로 40일간 유지한 결과 잡초발생량은 $4.8g\;m^{-2}$으로 제초제를 처리한 경운 처리구 $4.1g\;m^{-2}$와 비슷한 수준이었으며 벼 수량은 $3.92Mg\;ha^{-1}$로 경운 처리구 보다 11% 감소되었다. 무경운 논에서 발생되는 주요 잡초는 사마귀풀, 여뀌바늘, 물달개비 순이었으며 자운영을 피복하지 않을 경우 잡초발생량이 $115.4g\;m^{-2}$으로 벼 생육이 어려워 수량이 경운 처리구 $4.42Mg\;ha^{-1}$보다 66% 감소되었다. 따라서 벼 유기농업을 위해 무경운에 자운영을 피복하고 담수깊이를 10 cm로 40일간 유지하는 것이 가장 효율적인 것으로 나타났다.

국지홍수 심도예측을 위한 새로운 홍수지수의 개발 (Development of a New Flood Index for Local Flood Severity Predictions)

  • 조덕준;손인욱;최현일
    • 한국수자원학회논문집
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    • 제46권1호
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    • pp.47-58
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    • 2013
  • 최근 들어 전 세계적인 기후변화 양상에 따라 짧은 시간에 큰 유출양상을 보이는 국지적 돌발성 홍수의 발생이 증가하는 추세이며 이로 인한 인명 및 재산의 피해가 국내뿐만 아니라 전 세계적으로 발생하고 있다. 이와 같이 소규모 지역의 집중된 강우로 발생하는 국지적 돌발성 홍수는 빠른 수문반응으로 인하여 홍수피해를 예방하기 위한 예 경보 시간이 부족한 것이 특징이다. 국지 홍수로 인한 피해를 막기 위해서는 한계유량을 초과하여 제내지의 피해발생 가능성이 있는 홍수사상에 대한 심도예측이 중요하다. 본 논문의 목적은 소규모 유역에서 발생하는 홍수사상의 심각성 정도를 정량화할 수 있는 새로운 홍수지수(New Flood Index)를 개발하고 새로운 홍수지수와 강우특성과의 회귀분석을 통하여 국지 돌발홍수예측에 적용하고자 하였다. 2개의 시범유역들에 대한 홍수유출수문곡선은 장기간 관측된 연최대치계열 실측 강우자료를 이용하여 강우-유출 모형을 통하여 산정하였다. 새로운 홍수지수 NFI는 2년 빈도 홍수량으로 가정된 한계유량을 초과하는 홍수사상에 대하여, 첨두홍수량비, 상승부경사, 초과홍수지속시간 등 홍수 유출수문곡선의 특성을 이용한 3가지 상대심도계수의 기하학적 평균값으로산정하였다. 분석결과 3시간최대강우가 새로운 홍수지수NFI와 가장높은 상관관계가 있음을 확인하였다. 새로운 홍수지수와 강우특성과의 회귀분석을 통해 얻어진 최적 관계식은 소규모 미계측 유역에서의 국지적 홍수 심도예측을 위한 예비정보의 기초자료로 활용될 수 있을 것으로 기대된다.

낙동강 제방 붕괴에 따른 범람홍수 해석 (Flood Inundation Analysis from Levee Failure in Nakdong River)

  • 전민우;한건연;최규현
    • 한국수자원학회논문집
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    • 제38권4호
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    • pp.259-269
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    • 2005
  • 본 연구에서는 제방의 월류 및 붕괴에 따른 홍수파가 제내지로 전파되는 경우의 물리적인 특성을 고려하여 하천에 대한 홍수류 해석은 Preissmann 기법을 적용하였으며, 제내지에서의 범람해석을 위해 2차원 모형을 적용하여 해석할 수 있도록 구성하였고, 이들 두 모형이 상호 작용할 수 있는 하도-제내지 연결부 수치해석 모형을 개발하였다. 본 모형에서는 잠수효과의 해석을 위한 관련방정식을 도입하여 제내지에서의 수위 상승에 따른 하천으로부터의 월류량을 정확하게 계산할 수 있도록 구성하였다. 본 연구모형을 2002년 9월 낙동강 유역 실제 제방붕괴의 경우에 적용하여 제내지에서의 2차원 범람양상을 유속분포와 범람수심에 대해서 주요 시간대별로 계산하여 도시하였으며 모의결과는 당시의 실측자료 및 홍수범람범위와 잘 일치되는 것으로 나타났다.

태풍 매미(0314호)에 의한 마산만 주변연안역에서의 범람해석 (Inundation Analysis on Coastal Zone around Masan Bay by Typhoon Maemi (No. 0314))

  • 천재영;이광호;김지민;김도삼
    • 한국해양공학회지
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    • 제22권3호
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    • pp.8-17
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    • 2008
  • Wrenching climatic changes due to ecocide and global wanning are producing a natural disaster. Coastal zones have been damaged by typhoons and accompanying storm surges. Severe waves, and destruction of the environment are adding to the severity of coastal disasters. There has been an increased interest in these coastal zone problems, and associated social confusion, after the loss of life and terrible property damage caused by typhoon Maemi. Especially if storm surges coincide with high ticks, the loss of life and property damage due to high waters are even worse. Therefore, it is desirable to accurately forecast not only the timing of storm surges but also the amount water level increase. Such forecasts are very important from the view point of coastal defense. In this study, using a numerical model, storm surge was simulated to examine its fluctuation characteristics for the coastal area behind Masan Bay, Korea. In the numerical model, a moving boundary condition was incorporated to explain wave run-up. Numerically predicted inundation regimes and depths were compared with measurements from a field survey. Comparisons of the numerical results and measured data show a very good correlation. The numerical model adapted in this study is expected to be a useful tool for analysis of storm surges, and for predicting inundation regimes due to coastal flooding by severe water waves.

구조물의 영향을 고려한 GIS기반의 제내지 홍수범람해석 (GIS Based Flood Inundation Analysis in Protected Lowland Considering the Affection of Structure)

  • 최승용;한건연;조완희
    • 한국지리정보학회지
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    • 제12권4호
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    • pp.1-17
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    • 2009
  • 본 연구의 목적은 최근 수년간 발생한 홍수피해 원인의 대부분이 하천 제방의 붕괴와 관계하고 있음을 감안하여 제방의 월류 및 붕괴특성을 고려하여 붕괴유량을 산정하고 이에 따라 발생한 홍수파로 인해 제내지에서의 침수위, 침수시간, 침수범위 등을 예측하고 피해예상 규모를 산정하는데 있다. 붕괴유량 산정을 위해서 DEM, 토지피복도, 토양도 등의 기본 GIS자료를 이용하여 수문매개 변수를 추출하고 유역의 유출량을 산정하였다. 또한 제내지 내의 구조물의 영향을 고려한 홍수범람을 실시하여 제내지에서의 범람 홍수파의 전파특성을 정확히 예측하고 제내지의 시간별 침수구역의 예측, 홍수위험강도의 산정 등을 통하여 수방 및 홍수피해 경감대책 수립의 판단 자료로 활용하고자 한다.

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배수지연을 고려한 논 지구의 범용 침수 모의 기법 개발 (General Inundation Modeling of Paddy Field Districts Considering Drainage Delay)

  • 전상민;이현지;황순호;송정헌;최순군;강문성
    • 한국농공학회논문집
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    • 제61권4호
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    • pp.87-96
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    • 2019
  • The objective of this study was to develop a general inundation modeling technique considering the effect of drainage delay in the paddy field districts. In most studies, farmland inundation simulations have been conducted using previously developed watershed models. However, the water cycle in the paddy fields has a different structure from that of the general watershed, and the effect of the drainage delay should be considered. In this study, the drainage delay algorithm was developed using water balance equation, and the inundation modeling was performed for inundation-prone paddy fields located near Doowol stream. As a result, the depth of inundation was 43.1 cm and 45.2 cm, respectively, due to the 100-year and 200-year frequency rainfall. With the operation of drainage pump ($0.1m^3/s$), inundation depths decreased by 5.8 cm and 6.0 cm, respectively, and inundation time reduced by 20 hours and 21 hours, respectively for the 100-year and 200-year frequency rainfall. The result showed that the general inundation modeling technique developed in this study could reflect the effect of drainage delay due to the rise of external water level and the flooding reduction effect by operation of drainage pump. The results of this study are expected to be useful to establish measures for damage caused by farmland inundation.

금호지구 저습답의 암거배수효과에 관한 연구(I) (Studies on Wet Paddy Field Underdrainage Improvement in the Gum-Ho Area (I))

  • 김조웅;김시원
    • 한국농공학회지
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    • 제22권4호
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    • pp.82-95
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    • 1980
  • This paper complies the results of the studies so far made on the subsoil improvement of subsurface drainage systems for wet paddy fields (those were located in the Gum-Ho area in Kyung Buk province) which had poor permeability and a high water table. In general, a drainage problem is an excess of water on the ground surface which can effect the productivity and bearing capacity of the soil. With drain pipe systems, (According to their depths and spacing) it may be possible to correct that problem. The experimentation consisted of three test plots, two of which included drain pipe systems with varing depths and width spacing of the pipes. The third plot (C) was an ordinary plot being exempt of a drain pipe system. In detail, the depth of plot A was 80 cm, and the width spacings began at 2. Om and increased by 2. Om up to 10. 0m. The depth of plot B was 60cm and the width spacing was the same as plot A. These tests were performed to research specific details; such as crop yeild, bearing capacity of the soil, the amount of underdrainage, surface cracks, root distribution, the water table level, the consumptive water depth and the soil moisture content. The test period lasted three years, from 1977 thru 1979. The results obtained were as follows: 1. During the test period, the weather conditions for the area tested were in accordance with the annual average for that area. Furthermore the precipitation factor during the spring cultivation season, the intermediate drainage period and the harvest drainage period was of optimum conditions for controling surface cracks, because of less precipitation than evaporation. 2. The difference in the level of the ground water table in plots A and B was hardly noticable, but the difference in the test plots and the ord. plot was greatly noticable. The test plots (A, B) were 30 to 40cm lower than the ordinary plot. On the whole, the ground water table of the ord. plot always stayed at a level of 15-20cm beneath the surface of the soil, the ground water table of the test plot A showed The difference in the depth of the pipe lower than the test plot B, while the test plots showed a remarkable descending effect. 3. The soil temperature in plot A was slightly core than in plot B with a difference of 0. 47$^{\circ}$C, but plot A was 1. 6$^{\circ}$C higher than the ord. plot during the flooding period, but after drainage the temperature difference climed to 2. 0$^{\circ}$C. 4. During the 3rd test year, the values of the cracks were recorded with the values of 59cm in plot A, 42cm in plot B and 15cm in the ordinary plot. Plots A and B had increased 2.5 times the value of the first year while the ordinary plot had remained the same. 5. The root weight of the rice was measured at a value of 77.2 gr. for plot A, 73.5 gr. for plot B and 65.3 gr. for the ord. plot. Therefore, the root growths in plots A and B were much more energetic than in the ord. plot. 6. The consumptive water depth measured during the 3rd year resulted in the values of 26. 0mm per day for plot A, and 24.9 mm per day for plot B, respectively. Therefore, both plot A and plot B maintained the optimum consumptive water depths, but the ordinary plot only obtained the value of 12.3 mm per day, which clearly showed less than the optimum consumptive water depth which is 20 to 30 mm/day. 7. The soil moisture content is in direct relationship to the ground water level. During drainage, test plot A decreased in its ground water level much more rapidly than the other two plots. Therefore, plot A had a much less soil moisture content. But this decreased water level could be directly effected by the weather conditions. 8. The relationship between the bearing capacity and the soil moisture content were directly inversely proportional. It can be assumed that the occurence of soil creaks is limited by the soil moisture content. Therefore, the greater the progress of the surface creaks resulted in a greater bearing capacity. So, tast plot A with a greater amount of surface cracks than the other test plots resulted in a greater bearing capacity. But, the bearing capacity at the harvest season could be effected by the drainage during the intermediate drainage period and by the weather conditions. 9. Comparing the production of the test plots to the ord. plot; there was an increased value of 840kg for plot A, 755kg for plot B and 695kg for the ord. plot in the rough rice. Therefore, plot A had an increase of 20% over the ordinary plot. The possibility of producing double crops was investigated. The effects on barley production in the test plots showed a value of 367kg per 10 acres, which substantiated the possibility of double crops because that value showed an increased value over the average yearly yield for those uplands. 10. So as a result, it can be recommended that by including a drain pipe system with the optimum conditions of an (80cm centimeter) depth and a (l0m) spacing will have a definite positive effect on the over all production capacity and quality of wetpaddy fields.

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하도준설이 사행하천에 미치는 수리학적 영향 분석 (Analysis of Hydraulic Effect by River Dredging in a Meandering Channel)

  • 김태형;김병현;한건연
    • 한국지리정보학회지
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    • 제18권4호
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    • pp.14-30
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    • 2015
  • 본 논문에서는 하상퇴적이 심한 사행하천에서의 월류로 인한 침수피해와 제방 세굴 및 제방유실에 대한 피해를 저감시키기 위한 구조적 대안으로, 준설이 얻을 수 있는 수리학적 효과를 분석하고자 하였다. 사행사천 구간에서의 수리해석을 위해 2차원 수리해석 모형인 RMA-2 모형을 선정하였고, 준설 전의 현재 단면과 준설 후의 가정 단면을 GIS tool을 이용하여 구현한 후 2차원 유한요소격자를 구성하여 모형을 구동하였다. 준설 전 후에 대해 계산된 수위, 수심, 유속, 그리고 소류력을 현재의 계획홍수위와 비교하였고, 편수위가 발생한 지점에서 최대홍수위를 비교 분석한 결과 계획홍수위 대비 최대 0.58m의 수위저감 효과를 나타내었다. 분석구간 내에 위치한 제방에서의 소류력은 전 구간에 대해 평균 42~67% 가량 감소됨을 확인할 수 있었다. 이와 같은 결과를 통해 하천 사행구간에 위치한 유수의 흐름을 방해하는 하상퇴적물의 준설이 만곡부에 위치한 제방에서의 월류 및 세굴에 대한 위험도를 저감시키고 주변 농경지의 침수피해를 경감시킬 수 있는 적절한 구조적 대책이 될 수 있음을 확인할 수 있었다.