• Title/Summary/Keyword: High salinity

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하구(河口)의 해수(海水)의 염도변동(鹽度變動)에 관한 연구(研究) - 군산외항(群山外港)부근을 중심(中心)으로 - (A Study on the Salinity Variation of Salt Water in an Estuary)

  • 이정규
    • 대한토목학회논문집
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    • 제1권1호
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    • pp.1-8
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    • 1981
  • 하구(河口)는 해수(海水)와 담수(淡水)가 만나는 아주 복잡(複雜)한 지점(地點)으로 하구(河口)에서의 염도분포(鹽度分布)에 대한 수리학적(水理學的)인 일반적(一般的)인 해석(解析)은 대단히 어렵기 때문에 본(本) 연구(硏究)에서는 현지관측(現地觀測)을 통(通)하여 염도(鹽度)의 분포특성(分布特性)을 알기 위하여 조차(潮差)가 큰 군산(群山) 외항(外港)부근의 3지점(地點)에서 조석일주기(潮汐一週期)동안 1~1.5시간 간격으로 연속적(連續的)으로 현지관측(現地觀測)을 실시하였으며 분석결과(分析結果) 다음과 같은 몇가지 결론(結論)을 얻었다. 1. 염도(鹽度)와 전기전도도와의 비(比)가 0.5~1.0 사이에 대부분(大部分)이 산만하게 분포(分布)되어 있음이 재확인(再確認)되었다. 2. 염도(鹽度)는 만조시(滿潮時)에 가장 크고 만조(滿潮)에서 간조(干潮)로 됨에 따라 점점 작아져서 간조후(干潮後) 0~2시간(時間) 사이에 가장 작았다. 3. 금강하구(錦江河口)의 밀도류(密度流)는 대체로 강혼합형(强混合型)이었고 유량(流量)이 클 때는 완혼합형(緩混合型)이었다. 4. 연직염도분포(鉛直鹽度分布)에 파고(波高)의 영향은 별(別)로 없었다. 5. 최대연직염도차(最大鉛直鹽度差)는 대체로 10g/l 이하(以下)였으며 최소치(最少値)가 나타나는 시기(時期)는 대조시(大潮時)에는 간조후(干潮後) 0~2시간후(時間後)였고 소조시(小潮時)에는 만조후(滿潮後) 2~3시간(時間) 후(後)에 나타났다.

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Evaluation of Field Application of Soil Conditioner and Planting Chrysanthemum zawadskii on the Roadside Soils Damaged by Deicing Agents

  • Yang, Ji;Lee, Jae-Man;Yoon, Yong-Han;Ju, Jin-Hee
    • 인간식물환경학회지
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    • 제23권6호
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    • pp.625-636
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    • 2020
  • Background and objects: Soil contamination caused by CaCl2 that is used to deice slippery roads in winter is now recognized as one of the major causes of damage of roadside plants. The aim of this study is to identify the salt mitigation effects of planting Chrysanthemum zawadskii and using a soil conditioner. Methods: The study was conducted at the site where Pinus densiflora f. multicaulis was planted on the roadside between Konkuk University Sageori and Danwol Samgeori located in Chungju-si. We classified the soils collected from the field experimental site according to the degree of the damage caused by deicing agents and divided the site into six blocks of three 80 × 80 cm plots replicated by treatment type. Three selected plots were treated with loess-balls on the soil surface (high salinity with loess-balls, medium salinity with loess-balls, low salinity with loess-balls) and three were left as an untreated control (H = high salinity, M = medium salinity, L = low salinity). The soil properties were measured including pH, EC and exchangeable cations as well as the growth of Chrysanthemum zawadskiia. Results: In the results of soil analysis, pH before planting Chrysanthemum zawadskiia was 6.39-6.74 and in September, five months after planting, the acidity was reduced to 5.43-5.89. Electrical conductivity (EC) was measured to be H > M > L with the higher degree of damage by deicing agents. The analysis of deicing exchangeable cations showed that the content of Ca2+ of soils were significantly correlated to deicing exchangeable cations (Ca2+, Na+, Mg2+) in the shoot part of Chrysanthemum zawadskii. The loess-ball treatment showed a lower content of deicing exchangeable cations than the treatment where Chrysanthemum zawadskiia was planted. Conclusion: In this study, the use of a new system made of loess-balls is proposed as a soil conditioner to protect soils from the adverse effects of road deicing salts. These data suggest that treatment of soil conditioners and planting Chrysanthemum zawadskiia are effective in mitigation of salt stress on the soils damaged by deicing agents.

춘계 베링해 알류산 해분의 해양환경 특성 (Characteristics of the Oceanographic Environment in the Aleutian Basin of the Bering Sea during Spring)

  • 최석관;오택윤
    • 한국수산과학회지
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    • 제46권2호
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    • pp.201-215
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    • 2013
  • The characteristics of the oceanographic environment in the Aleutian Basin of the Bering Sea during spring in 1996, 1997, and 1999 were clarified. An investigation of the water properties revealed five basic layers in the Bering Sea during spring: (1) a surface layer of warm and low-salinity water induced by solar heating, (2) a subsurface layer of cold and low-salinity water propagated slowly by heat from the surface layer, (3) a thermocline layer where salinity was constant but temperature sharply decreased, (4) a temperature inversion layer, and (5) a deep layer with a gradual decrease in temperature and increase in salinity toward the bottom. The ranges of water temperature and salinity were $1.8-5.5^{\circ}C$ and 31.81-34.08 in 1996, $1.5-7.2^{\circ}C$ and 31.9-34.06 in 1997, and $0.5-5.6^{\circ}C$ and 32.0-34.11 in 1999, respectively. The water temperature of the surface layer was approximately $1.6^{\circ}C$ higher in 1997 than in 1996 and 1999. The lowest temperature at a depth of 100-150 m was about $1^{\circ}C$ lower in 1999 than in 1996 and 1997. Nutrient levels (nitrate, phosphate, and silicate) contributing to the control of the growth of phytoplankton were higher in the Aleutian Basin than in the eastern continental shelf and Bogoslof Island area. This was closely associated with the phytoplankton distribution. Nutrient concentrations were lowest at a depth of 25 m. The high primary production at that depth was confirmed from the vertical distribution of chlorophyll a. Chlorophyll a levels were above $4.0{\mu}L^{-1}$ in some areas in 1996 and 1999, but below $2.0{\mu}L^{-1}$ in most areas in 1997. Zooplankton density was about three times higher in 1999 than in 1997.

염분과 표준 독성물질(Cu, Cd)이 둥근성게(Strongylocentrotus nudus)의 수정 및 배 발생률에 미치는 영향 (Effects of Salinity and Standard Toxic Metals (Cu, Cd) on Fertilization and Embryo Development Rates in the Sea Urchin (Strongylocentrotus nudus))

  • 황운기;이충원;이승민;안경호;박승윤
    • 한국환경과학회지
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    • 제17권7호
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    • pp.775-781
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    • 2008
  • Effects of salinity and standard toxic metals on fertilization and embryo development rates were investigated in the sea urchin, Strongylocentrotus nudus. Spawning was induced by injecting 1ml of 0.5 M KCl into the coelomic cavity. The fertilization and embryo development rates were below 20% when salinity was 25 psu or lower, but were above 90% when salinity was between 30 and 35 psu. The fertilization and embryo development rates in the control condition (not including Cu and Cd) were greater than 90%, but decreased with a high negative correlation (r) of 0.89 and 0.91 with the increasing of Cu and Cd concentrations, respectively. These results suggest that salinity concentrations for successful fertilization and normal embryogenesis of S. nudus are between 30 and 35 psu, and the biological assays of fertilization and embryo development rates using S. nudus are useful methods for the ecological toxicity test of marine pollution elements.

Variability of Surface Water Properties in the Japan/East Sea on Different Time Scales

  • Ponomarev, Vladimir;Rudykh, Natalya;Dmitrieva, Elena;Ishida, Hajime
    • Ocean and Polar Research
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    • 제31권2호
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    • pp.177-187
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    • 2009
  • This study examined the multi-scale variabilities of sea surface temperature (SST) and salinity in the Japan/East Sea (JES) based on statistical analyses of observational data, with a focus on the northwestern part of the sea. The regionality of JES SST variability was estimated for different frequency ranges on semimonthly (11-17 days), monthly to seasonal (30-90 days), quasi-semiannual (157-220 days), and quasi-biennial (1.5-3 years) time scales using cluster analyses of daily gridded SST data for 1996 to 2007 from the Japan Meteorological Agency (JMA). Several significant peaks and regional cores were found in each frequency range of the SST anomaly (SSTA) oscillations. Quasi-semiannual SSTA oscillations with high amplitude were found in the south-southwestern part of the Japan Basin ($41-43^{\circ}N$) and were amplified in the area adjacent to Peter the Great Bay. Oscillations with periods of 79 and 55 days also prevailed over the southwest Japan Basin between the Yamato Rise and the continental slope. A similar method was applied to classify SST and the annual cycle of surface salinity using Generalized Digital Environmental Model (GDEM) gridded data. The Tatarskii Strait and adjacent area showed the most specific annual cycles and variability in salinity on interannual to interdecadal time scales. The most significant inverse relationship between surface salinity in the Tatarskii Strait and southern JES areas was found on the interdecadal time scale. Linkages of sea water salinity in the Tatarskii Strait with Amur River discharge and wind velocity over Amurskii Liman were also revealed.

낙동강 하구의 염수운동 (Saline Water Movement In The Estuary Of The Nakdong River)

  • 장선덕;유청노;이문옥;이재철
    • 한국해양학회지
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    • 제16권1호
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    • pp.31-37
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    • 1981
  • 우리나라 남동부의 광범한 유역을 따라 흐르는 낙동강은 국내에서 가장 긴 하천의 하나로서 영남지역을 굽이쳐 흐르다가 부산 앞바다를 통하여 대한해협에 유입한다. 이 강의 하구는 유역주민의 생활 및 산업용수원으로서 중요할 뿐만 아니라 최근에는 산업입지 및 자연환경 보전문제로서 논의의 대상이 되고 있다. 낙동강은 하구로부터 약 40km상류까지 상향류를 보이며, 약 60km상류까지 조석의 영향을 받는 감조하천으로서 (유 장 1979), 하구역에는 해수, 하천의 담수 및 양자의 혼합수가 조석의 간만등 여러 가지 요인에 따라 유출되기도 하고 유입되기도 한다.

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Analysis of metabolites in wheat roots in response to salinity stress

  • Kim, Da-Eun;Roy, Swapan Kumar;Kim, Ki-Hyun;Cho, Seong-Woo;Park, Chul-Soo;Lee, Moon-Soon;Woo, Sun-Hee
    • 한국작물학회:학술대회논문집
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    • 한국작물학회 2017년도 9th Asian Crop Science Association conference
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    • pp.200-200
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    • 2017
  • Salinity stress is one of the most important abiotic stresses and severely impairs plant growth and production. Root is the first site for nutrient accumulation like as $Na^+$ in the plant. To investigate the response of wheat root under salinity stress, we executed the characterization of morphology and analysis of metabolites. Wheat seeds cv. Keumgang (Korean cultivar) were grown on the moist filter paper in Petri dish. After 5 days, seedlings were transferred to hydroponic apparatus at 1500 LUX light intensity, at $20^{\circ}C$ with 70% relative humidity in a growth chamber. Seedlings (5-day-old) were exposed to 50mM, 75mM, 100mM NaCl for 5 days. Ten-day-old seedlings were used for morphological characterization and metabolite analysis. Root and leaf length became shorter in high NaCl concentration compared to following NaCl treatment. For confirmation of salt accumulation, wheat roots were stained with $CoroNa^+$ Green AM, and fluoresce, and the image was taken by confocal microscopy. $Na^+$ ion accumulation rate was higher at 100mM compared to the untreated sample. Furthermore, to analyze metabolites in the wheat root, samples were extracted by $D_2O$ solvent, and extracted sample was analyzed by 1H NMR spectroscopy. Fourteen metabolites were identified in wheat roots using NMR spectroscopy. Methanol and ethanol were up-regulated, whereas formate, aspartate, aminobutyrate, acetate and valine were down-regulated under salinity stress on roots of wheat. Fumarate had no change, while glucose, betaine, choline, glutamate and lactate were unevenly affected during salinity stress.

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굴(Crassostrea gigas)의 패각운동을 이용한 생물모니터링시스템 연구 -I. 홀 소자를 이용한 저염분하에서 비정상적인 패각운동 측정 (Bio-Monitoring System Using Shell Valve Movements of Pacific Oyster (Crassostrea gigas) -I. Detecting Abnormal Shell Valve Movements Under Low Salinity Using a Hall Element Sensor)

  • 오석진;이준호;김석윤
    • 한국해양환경ㆍ에너지학회지
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    • 제16권2호
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    • pp.138-142
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    • 2013
  • 저염분에 따른 양식생물의 피해를 줄이기 위한 조기경보 방안으로 염분에 따른 굴(Crassostrea gigas) 패각운동 특성을 홀 소자를 이용하여 측정하는 생물모니터링시스템의 적용 가능성을 조사하였다. 염분농도 27 psu에서 굴의 패각운동은 평균 10-15 mm 정도의 개각상태를 유지하다가, 비교적 빠른 폐각상태를 지시하는 큰 파형이 보였으며, 다시 개각상태로 돌아가나, 그 속도는 폐각상태로 진행되는 속도보다 느리게 나타났다. 20 psu까지 저염분의 농도에서는 27 psu의 패각 운동과 큰 변화가 없었다. 하지만 17 psu 이하의 염분농도부터 이상 패각운동이 지시되었으며, 10 psu에서는 패각운동이 없이 폐각상태를 유지하였다. 이와 같은 생물모니터링시스템을 패류 양식에 활용하여 해양환경의 이상변동을 신속히 감지할 수 있다면, 어업피해를 감소시킬 활동으로 연결될 것으로 기대된다.

간척초기답의 벼생육기간중 염분농도 분석 (Analysis of Salinity during the Growing Period in the Unripened Tidal Reclaimed Paddy Fields)

  • 손재권;구자웅;최진규
    • 농촌계획
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    • 제6권2호
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    • pp.3-11
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    • 2000
  • The high salt concentration of reclaimed tidelands in the beginning of reclamation interferes with the growth of most crops. Although the crops are cultivated in the unripened tidal reclaimed paddy fields after desalinization to be arable, they we apt to be injured from salt by the resalinization through accumulated salts in the root zone during the growing period. In oder to make the reasonable irrigation plan in the unripened tidal reclaimed paddy fields, the preventive water requirements of resalinization as well as leaching requirements have to be included in irrigation water requirements. The critical salinity for the normal growth of crops should be determined to estimate the preventive water requirements of resalinization, and the changes of salinity in soil and water should be analyzed during the growing period, In this study, the growth tests of crops were conducted by soil textures and water management methods in the experimental field with lysimeters, using the samples of good drainage soils and poor drainage soils. And the changes of salinity in soil and water during the growing period, were analyzed to obtain the basic data for determining the critical salinity and making the estimation criteria of the preventive water requirements of resalinization. As the results obtained from analyzing the changes of salinity during the growing period in the unripened tidal reclaimed paddy fields, the exchanging interval of water for the prevention of resalinization was estimated to be within two weeks in good drainage soils and a week in poor drainage soils. And the total exchanging requirements of water for the prevention of resalinization during the growing period was estimated to be over 280mm in good drainage soils and 540mm in poor drainage soils.

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하계 동해에 있어서 대마난류의 북상한계와 변동 (THE NORTHERN BOUNDARY THE TSUSHIMA CURRENT AND ITS FOUCTUATIONS)

  • 홍철훈;조규대
    • 한국해양학회지
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    • 제18권1호
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    • pp.1-9
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    • 1983
  • 1970∼1979년 기간중 하계의 동해에 있어서 대마난류의 북상한계와 연변동을 규명하기 위해서 염분최대를 추적하고, 이값에 대한 deltaT(thermosteric anomaly) 에 관하여 검토했다. 29 N 이북의 동지나해로부터 동해북부해역에 이르기 까지 대마난류의 염분최대치 및 그 층의 낮아지는 경향을 보였으며, 그 층도 얕아졌다. 동해의 대마난류역에서 염분최대가 나타나는 층에 대한 deltaT의 값은 220-260 cl/t 이었다. 240cl/t면상의 34.4 등염선을 지표로하여 조사한 대마난류의 북상한계 는 한국 동해안측에서는 4 N 이남해역으로 한정으며, 동염선은 두가지 형태로 나타났다. 즉 동서방향인한국동해안쪽으로 치우쳐 북상하는 경우와 남남서-북북동 방향인 일본연안쪽으로 북상하는 경우였다.

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