• 제목/요약/키워드: low-salinity

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저염분이 바리과 교잡종(Epinephelus fuscoguttatus×E. polyphekadion) 의 성장, 생존 및 스트레스 반응에 미치는 영향 (Effect of Low Salinity on Growth, Survival and Stress Response of Juvenile Hybrid Grouper (Epinephelus fuscoguttatus×E. polyphekadion))

  • 이일영;박중열;임한규
    • 한국수산과학회지
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    • 제53권4호
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    • pp.499-505
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    • 2020
  • We investigated growth, survival and stress response depending on salinity changes in hybrid grouper (Epinephelus fuscoguttatus ♀×E. polyphekadion ♂, BCG) juvenile. Experiment I (Exp I), the hybrids were stocked at 32 psu and reared for 30 days under decreasing salinity at a rate of 5-7 psu per day (25, 20, 15, 10, 5 psu). Experiment II (Exp II), the salinity was decreased from 32 psu to 5 psu during a period of 24, 48 and 72 h. Experiment III (Exp III), acclimatized BCGs were exposed from 5 psu to decreasing salinity at 0, 1, 2, 3, 4 psu. In the Exp I, 90% survival only in the 5 psu. Growth were 5 and 32 psu had significantly low growth than other treatment. In the Exp II 100% survived by the end of the experiment. The plasma cortisol level was highest in the treatment the salinity rapidly dropped, but all the treatment recovered quickly after 24 h of salinity reduction. In the Exp III, the lower the salinity, the faster the mortality occurred in salinity below 5 psu. It is therefore concluded that the BCGs are highly tolerant of low salinity and the salinity tolerance threshold is 5 psu.

미질향상을 위한 간척지 토양 염농도별 적정 질소시비량 (Nitrogen Fertilizer Management for Improving Rice Quality under Different Salinity Conditions in Tidal Reclaimed Area)

  • 최원영;이규성;고종철;박홍규;김상수;김보경;김정곤
    • 한국작물학회지
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    • 제49권3호
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    • pp.194-198
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    • 2004
  • 본 연구는 남서해안 간척지에서 토양 염농도(저염; 0.1%, 중염; 0.3∼0.4%)별로 쌀 품질 향상을 위한 적정 질소 시비량을 구명하기 위하여 시험한 결과를 요약하면 다음과 같다. 1.유추분화기의 초장은 질소 시비량이 많을수록 컸고, 토양염농도간에는 저염 토양에서 켰다. 2. 출수기는 저염 토양에서는 표준비인 N20kg/10a에 비해 N8-N16kg/10a까지는 같았으나 N24kg/10a에서는 1일 늦었고, 중염 토양에서는 N8-N16kg/10a 까지는 1일이 삘랐고 N24kg/10a에서는 같았으며, 토양 염농도간에는 저염 토양에서보다 중염 토양에서 4일 정도 늦었다. 3. 질소시비량이 많을수록 간장이 크고, 포장도복이 심했다. 4. 저염 토양에서 질소시비량이 많을수록 $\textrm{m}^2$ 당 립수는 많았으나 등숙비율이 낮아져 발 수량은 N12kg/10a이상에서는 유의차가 없었으며, N12kg/10a이하에서 현미의 완전미율이 높고 단백질 함량이 낮았다. 5.중염 토양에서는 질소시비량이 많을수록 $\textrm{m}^2$ 당 립수가 많고 등숙비율이 비슷하여 발 수량은 질소시비량이 많을수록 높았으나 N20kg/10a 이상에서는 유의차가 없었고, 현미의 완전미율과 단백질함량은 질소시비량간에 비슷하였다. 따라서 남서해안 간척지에서 쌀 수량 및 미질 등을 고려해 볼 때, 저염 토양에서는 N12kg/10a, 중염 토양에서는 N20kg/10a이 적당할 것으로 생각된다

Southward Intrusion of the East Sea Intermediate Water into the Ulleung Basin: Observations in 1992 and 1993

  • Shin, Chang-Woong;Byun, Sang-Kyung;Kim, Cheol-Soo;Seung, Young-Ho
    • Journal of the korean society of oceanography
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    • 제33권4호
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    • pp.146-156
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    • 1998
  • Hydrographic data retrieved in the southwestern part of the East Sea in 1992-1993 were analyzed to investigate the probability of southward intrusion of the East Sea Intermediate Water (ESIW) into the Ulleung Basin. The ESIW showed the ranges of 1 to 4$^{\circ}$C in potential temperature, 33.80-34.06 psu in salinity, and 26.9-27.3 kg/m$^3$ in potential density (${\sigma}$$_{\theta}$). The mean depth occupied by the ESIW was 170 m, where the characteristic values of the above three were 2.64$^{\circ}$C , 34.02 psu, and 27.13 kg/m$^3$, respectively. One of the most prominent features of the ESIW was that its salinity changed not only seasonally but also interannually. It was low in summer and high in winter. The salinity within the isopycnal layer of 26.9-27.3 kg/m$^3$ was closely related with the potential vorticity (${\rho}$$_{\theta}^{-1}$ f ${\varrho}$${\rho}_{\theta}$/${\varrho}$z), being in direct proportion to the salinity. This implies that the low-salinity water was thicker than the high-salinity water. The flow path of the ESIW was investigated by tracking the low-salinity or the low-potential vorticity water and by referring to acceleration potential. Careful analysis of the flow path proves that the ESIW intrudes from the north between the Korean coast and Ulleung Island into the Ulleung Basin in summer. Existence of the high-potential vorticity water in the Ulleung Basin is associated with the interruption of the inflow of low-salinity water.

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Effects of abiotic stressors on kelp early life-history stages

  • Lind, Alyssa C.;Konar, Brenda
    • ALGAE
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    • 제32권3호
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    • pp.223-233
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    • 2017
  • Kelp forests and the many vital ecosystem services they provide are threatened as the severity of climate change and other anthropogenic stressors continues to mount. Particularly in the North Pacific, sea surface temperature is warming and glacial melt is decreasing salinity. This study explored the resiliency of early life-history stages of these foundation species through a factorial laboratory experiment. The effects of rising sea surface temperature under low salinity conditions on kelp spore settlement and initial gametophyte growth in Eualaria fistulosa, Nereocystis luetkeana, and Saccharina latissima were investigated. Decreased settlement and growth were observed in these species at elevated temperatures and at low salinity. Eualaria fistulosa spores and gametophytes were the most negatively impacted, compared to the more widely distributed N. luetkeana and S. latissima. These results suggest that N. luetkeana and S. latissima could potentially outperform E. fistulosa under projected conditions. However, despite decreased performance among all species, our findings indicate that these species are largely resilient to temperature changes when exposed to a low salinity, even when the temperature changes are immediate and extreme. By exploring how early life-history stages of several key kelp species are impacted by dual stressors, this research enhances our understanding of how kelp forests will respond to projected and extreme changes in temperature when already stressed by low salinity.

The Inflow Path of the East Sea Intermediate Water into the Ulleung Basin in July 2005

  • Shin, Chang-Woong
    • Ocean and Polar Research
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    • 제28권2호
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    • pp.153-161
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    • 2006
  • To investigate inflow path of the East Sea Intermediate Water (ESIW) into the Ulleung Basin, hydrographic data surveyed in July 2005 were analyzed. The ESIW was characterized by the Salinity Minimum Layer (SML) within a depth range of 100 to 360 meters. Averaged potential temperature and salinity of the SML were $1.835^{\circ}C$ and 34.049 psu, respectively. Mean potential density $({\sigma}_{\theta})$ of the SML was 27.221 with a standard deviation of 0.0393. On isopycnal surfaces of 27.14 and 27.18 $({\sigma}_{\theta})$ which correspond to upper layers of the ESIW, the coastal low salinity water was separated from the offshore low salinity water by the relatively warm and saline water which might be affected by the Tsushima Warm Current Water. Relatively cold and fresh water, however, intruded into the Ulleung Basin from the region of Korean coast on isopycnal surfaces of 27.22 and 27.26 which was lower layer of the ESIW. The salinity distribution in the isopycnal layer of $27.14{\sim}27.26$ with acceleration potential on 27.22 up surface also showed clearly that the low salinity water flowed from the coastal area and intruded into the Ulleung Basin. This implies that the ESIW flows ken the north to the south along the east coasts of Korea and spreads into the Ulleung Basin in summer.

여름철 제주 서부해역의 저염분수로 인한 음속변화와 음파채널 형성 (Acoustic Channel Formation and Sound Speed Variation by Low-salinity Water in the Western Sea of Jeju during Summer)

  • 김주호;복태훈;팽동국;방익찬;이종길
    • 한국음향학회지
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    • 제32권1호
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    • pp.1-13
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    • 2013
  • 일반적으로 해양에서는 염분이 크게 변하지 않기 때문에 염분변화로 인한 음속변화는 무시할 수 있다. 그러나 제주 서부 해역에서는 매년 여름 저염분수의 영향으로 염분이 낮아지는 현상이 발생하여 표층 음속의 변화가 발생한다. 해양자료센터의 자료를 이용하여 제주 서부해역 세 정점에서의 30년(1980~2009) 자료 중 28 psu 이하의 저염분수가 발생한 해와 그렇지 않은 해의 수직분포를 각각 평균하여 음속분포를 구한 후에 수온과 염분에 의한 음속 변화를 분석하였다. 그 결과 저염분수 환경에서 염분에 의한 음속 변화는 표층에서 -5.36 m/s, 수심 10 m에서 -1.35 m/s 인 것으로 나타났다. 또한 표층 음속 감소로 인해 수심 약 5 m까지의 음속 수직 분포가 양(+)의 기울기를 갖게 되어 표층 염분채널이 형성되었으며 벨홉(Bellhop)모델을 이용한 음파전달 모의실험을 통해 이를 확인하였다. 30년간 표층채널 발생 동향을 분석한 결과 혼합층에서 압력에 의해 발생하는 정수채널은 9회, 저염분에 의해 발생하는 염분 채널은 5회로 나타났으며 염분 채널이 발생한 경우는 정수 채널에 비해 음선 임계각이 크게 나타나는 것으로 확인되었다. 또한 2010년 8월 1일 제주 서부해역에 발생하였던 저염분수의 공간적 분포를 측정한 자료에서도 일부 정점에서 염분채널이 형성되었다.

Salt Tolerance of Vigna angularis during Germination and Early Seedling Growth

  • Lee, Hee-Kyung;Hong, Jung-Hee
    • Environmental Sciences Bulletin of The Korean Environmental Sciences Society
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    • 제4권1호
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    • pp.59-69
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    • 2000
  • The present study was undertaken in investigate the response to salinity and effect of plant growth regulators and proline under salinity stress on the germination and seedling growth of Vigna angularis. The protective effect of external Ca2+ on root elongation under saline conditions was also investigated. The seed germination of Vigna angularis decreased with an increase in salinity. The growth regulators GA3 was more effective than kinetin. At a higher salinity, low concentrations of kinetin and high concentrations of GA3 were more effective. The external application of proline and betaine improved germination under saline conditions. At a low salinity proline and betaine alleviated the salinity-induced inhibition of germination, yet at higher NaCl concentrations, proline and betaine were both ineffective. Exposure to salinity during germination was accompanied by an increase in the proline content, thereby suggesting that one compatible solute in the germinating seed would seem to be proline. The inhibition of germination by high NaCl concentrations was relatively more severe in scarified seeds than in intact seeds, indicating that the seed coat acts as a partial barrier to an Na2+ ameliorated the adverse effect of salinity stress.

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급격한 저염분 노출에 따른 참돔 Pagrus major 치어의 단기 행동반응 및 내성 한계에 관한 연구 (Short-term behavioral responses and tolerance limits of red seabream Pagrus major fingerlings following sudden low salinity exposure)

  • 윤성진
    • 환경생물
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    • 제39권4호
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    • pp.495-506
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    • 2021
  • In this study, using a continuous behavior measurement technique, the short-term behavioral responses and tolerance limits of red seabream Pagrus major fingerlings to sudden exposure to low salinity in a controlled environment were observed. The activity of the fingerlings suddenly exposed to 21.4, 17.3, and 9.8 psu increased temporarily at the initial exposure to show irregular swimming behavior, but then recovered a stable activity pattern through rapid salinity adaptation. However, the organisms suddenly exposed to 7.3 and 4.3 psu could not withstand the salinity stress, and their swimming behavior was severely disturbed and all individuals died within 48 hours. The findings suggest that red seabream underwent a temporary salinity stress process at the beginning of the exposure to concentrations of 10.0 psu or higher. At these concentrations, osmotic control was possible within at least 11 hours, so stable metabolic activity was also possible. However, organisms suddenly exposed to concentrations below 5.0 psu exceeded the tolerance to low salinity and the sublethal limit. In red seabream exposed to this concentration range, severe behavioral and metabolic disturbances were observed, and death was observed due to osmotic control failure. In conclusion, a salinity range of 5.0 to 10.0 psu can be predicted to correspond to a concentration range in which the osmotic control ability of the red seabream fingerlings is lost, and sub-lethal reactions occur.

제주도 서부 해역의 저염수층을 고려한 수중통신 성능 (Performance of Underwater Communication in Low Salinity Layer at the Western Sea of Jeju)

  • 복태훈;김주호;이종현;배진호;팽동국;방익찬;이종길
    • 대한전자공학회논문지TC
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    • 제48권1호
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    • pp.16-24
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    • 2011
  • 해양에서의 음속은 수온, 염분, 압력에 의한 실험식으로 계산되며 해양에서의 평균 염분은 약 34 psu (practical salinity unit)로 수성이나 수평 거리에 따른 변화가 대부분 수 psu 이하이기 때문에 음속에 크게 영향을 마치지 못한다. 그러나 최근 여름철에 중국 양쯔강 범람에 의해서 24 psu 정도의 저염수가 제주 서부 해역으로 유입되는 사례가 발생하고 있으며 이 저염수는 음속에 영향을 미친다. 본 논문에서는 이러한 환경 변화가 수중통신에 미치는 영향을 분석하였다. 즉, 저염수로 인한 음속구조의 변화를 계산하였고, 저염수층 내에서 송수선 수심과 전달거리를 바꿔가며 음파 전달 경로를 모의하여 통신 채널을 추정하였으며, BPSK(Binary phase shift key) 변조방식을 이용하여 비트 오류율을 계산하였다. 동일한 실험 조건하에 저염수가 없는 경우의 성능을 비교하여, 저염수가 통신 성능에 어떠한 영향을 미치는가에 대해 분석하였다. 저염수는 수심 약 20m까지의 표층부에서 음속의 기울기를 양의 기울기로 변화시켜 음과 채널을 형성하였고, 표층부에서 대부분의 송수신 신호의 비트 오류율을 감소시키는 경향을 확인하였다. 본 논문의 저염수에 의한 수중 통신 성능에 미치는 영향을 분석한 결과는 정확한 해양 통신 및 탐지 성능분석을 하기 위해서는 해양환경의 변화를 고려하는 것이 매우 중요하다는 것을 시사한다.

서남부 간척지에서 벼 담수표면산파재배시 토양 염농도별 적정 파종량 (Optimum Seeding Rate in Different to Soil Salinity for Broadcasting on the Rice Flooded Paddy Surface at South-western Reclaimed Saline Land of Korea)

  • 백남현;최원영;고종철;박홍규;남정권;박광근;김상수;김보경;김정곤
    • 한국작물학회지
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    • 제51권spc1호
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    • pp.47-51
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    • 2006
  • 서남부 간척지에서 벼 담수표면산파재배시 토양 염분농도별 적정 파종량을 구명하고자 $2003{\sim}2004$년에 걸쳐 호남 농업 연구소 계화도출장소 시험포장인 문포통(세사양토)의 저영답(토양 염농도 0.1%)과 중염답(토양 염농도 0.3%)에서 서간벼를 공시하여 파종량별 입모수, 생육, 수량 및 백미 외관 품위 등을 검토한 결과를 요약하면 다음과 같다. 1. 입모수는 중염답보다 저염답에서 파종량이 증가할수록 많았다. 2. 간장과 수장은 중염답이 저염답보다 파종량이 증가할 수록 짧았으며, 도복은 토양염농도에 상관없이 파종량이 증가할수록 심했다. 3. 완전미 수량은 저염답에서는 파종량 5 kg/10a까지, 중염답에서는 파종량 7 kg/10a까지는 증가되었으나 그 이상의 파종량에 서는 수량이 증가하지 않았다. 4. 백미의 외관상 품위는 파종량이 증가할수록 저염답보다 중염답에서 완전미율이 낮았다. 5. 따라서 서남부 간척지에서 벼 담수표면산파재배시 입모, 벼 생육, 완전미 수량 및 백미의 외관상 품위 등을 고려할 때 적정 파종량은 저염답은 $5{\sim}7kg/10a$, 중염답은 $7{\sim}9kg/10a$이 적당할 것으로 생각된다.