• Title/Summary/Keyword: 염분도

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Biomass and Species Composition of Phytoplankton and Zooplankton along the Salinity Gradients in the Seomjin River Estuary (섬진강 하구역에서 염분경사에 따른 동${\cdot}$식물플랑크톤의 현존량 및 종조성)

  • Lee, Pyung-Gang;Park, Chul;Moon, Chang-Ho;Park, Mi-Ok;Gwon, Kee-Young
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.6 no.2
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    • pp.93-102
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    • 2001
  • Biomass and species composition of phytoplankton and zooplankton along the salinity gradients in the Seomjin River estuary were investigated in March, July, September and November, 1999. The locations of sampling sites were set based on the surface salinity during each cruise rather than geographic locations. A total of 96 phytoplankton species were identified with 60 diatom species in the study area. The species number of green algae was relatively high in low salinity region while the number of dinoflagellates increased in high salinity areas. Monthly mean of phytoplankton biomass ranged from 183 cells/ml to 833 cells/ml. There was a diatom bloom of Skeletonema costatum in November at the 5-15 psu salinity region and sharp decrease of biomass in very low salinity region occurred in March. During the rainy season in July with the salinity less than 8.1 psu, the green algae dominated in most of the study areas. Chroomonas spp. were highly dominant in March and September and the biomass increased towards the high salinity regions. A total of 83 zooplankton taxa were identified with 72 marine and 11 freshwater taxa. Major group of marine form was copepods with34 taxonomic groups. Most freshwater taxa were aquatic insects. Threshold salinities of freshwater zooplankton appearance were 8.1 psu in July, 4.7 psu in September, and 0.2 psu in November. The number of taxa appeared and abundances of zooplanktons were minimal in the middle of salinity gradients in this estuary.

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The Effects of different food-wastes of household on the feeding rate and growth rate of Eisenia fetida(Annelida: Oligochaeta) population (가정에서 발생한 서로 다른 종류의 음식물 쓰레기가 줄지렁이(Eisenia fetida)개체군의 섭식 및 생장에 미치는 영향)

  • Park, Kwang-Il;Bae, Yoon-Hwan
    • Journal of the Korea Organic Resources Recycling Association
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    • v.21 no.1
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    • pp.85-93
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    • 2013
  • The amount of salted food waste and non-salted food waste from household consisted of 4 family members was surveyed. And the feeding rate and growth rate of Eisenia fetida population upon the different food wastes such as vegetables, grains, fruits and salted food waste were investigated. Total amount of food waste from a household was 3,200g/week. i.e. 0.114kg/day/capita and non-salted food waste was 53.9% of food waste. Salt contents of vegetables, grains, fruits were 0.60, 0.36 and 0.33%, respectively, if they were assumed to have 70% water content. Salt content of salted food waste was 0.78%. Upon the non-salted vegetables and fruits, feeding rate of earthworm was high but growth rate was low. Upon the non-salted grains, feeding rate of earthworm was low but growth rate was high. Upon the food with 70% water content, earthworm could not feed and grow when salt content of food was over 0.6%, and earthworm could feed normally but showed low growth rate when salt content of food was 0.3%. These results indicated that earthworm could stabilize the non-salted food wastes with ease but could hardly stabilize the salted food wastes.

Effects of Water Temperature, Salinity and Irradiance on the Growth of the Toxic Dinoflagellate, Gymnodinium catenatum (Graham) Isolated from Yeosuhae Bay, Korea (여수해만에서 분리한 유독 와편모조류, Gymnodinium catenatum (Graham)의 성장에 미치는 수온, 염분과 광 조건)

  • Oh, Seok-Jin;Yoon, Yang-Ho
    • ALGAE
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    • v.19 no.4
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    • pp.293-301
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    • 2004
  • A chain-forming toxic din flagellate, Gymnodinium catenatum (Graham) was known as a paralytic toxin-producer among Gymnodinoid group. In the study, the effects of water temperature, salinity and irradiance on the growth of G. catenatum isolated from Yeosuhae Bay, Korea were investigated. Water temperature range in which G. catenatum showed specific growth rate higher than 0.3 day$^{-1}$ were above about 18${^{\circ}C}$. However, salinity did not have such an effect on growth of G. catenatum. The maximum growth rate (0.5 day$^{-1}$) was obtained at 25${^{\circ}C}$ and 30 psu. The specific growth rate (u) expressed as a polynomial equation as functions of temperature (T; ${^{\circ}C}$) and salinity (S; psu) was $\mu$ = 0.005·T$^2$ - 0.0001164 T$^3$ - 0.063-S + 0.005-S$^2$ - 0.00007608-S$^3$ - 0.003-T-S + 0.00005308-T$^2$-S. Thus, in aspects of water temperature and salinity, the species may be expected to survive in most Korean coastal waters from early summer to autumn. The irradiance-growth curve was described as = 0.16 (I - 10.4)/(1 + 21.8) at 18${^{\circ}C}$ and 30 psu, indicating a half-saturation (Ks) photon flux density (PFD) of 42.6$\mu$mol m$^{-2}s^{-1}$ and compensation PFD (I$_0$) of 10.4$\mu$mol m$^{-2}s^{-1}$. These characteristic responses to irradiance suggest that G. catenatum can reside at the sub-surface.

Survival and Physiological Responses of the Tunicate Halocynthia roretzi to Salinity Changes (염분변화에 따른 멍게 Halocynthia roretzi의 생존과 생리적 반응)

  • Shin, Yun-Kyung;Choi, Nack-Joong;Hur, Young-Baek;Han, Hyoung-Kyun;Park, Jeong-Heum;Kim, Yoon
    • Journal of Aquaculture
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    • v.20 no.4
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    • pp.226-231
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    • 2007
  • We investigated survival and osmolarity, oxygen consumption, amonia extetion and filtration rates associated with physiological responses of the tunicate Halocynthia roretzi salinity changes. Acclimation times for osmolatity in different salinities took $20{\sim}26$ hours in 60% SW (19.8 psu) and $20{\sim}25$ hours in 80% SW (26.4 psu), while their times took $7{\sim}8$ hours in 110% SW (36.3 psu). Accordingly, acclimation times for high salinities were faster than those for low salinities. Survival (%) was more than 80% at salinity over 26.4 psu, and 6 $days-LS_{50}$ was 25.4 psu. physiological responses such as oxygen consumption, amonia excretion and filtration rates of H. roretzi showed more clear reactions in the longer exposure period (four days after exposure) than that in the beginning of the exposure. To sum up the results, the tunicate might be stressed from the beginning of the exposure in low salinity.

Effects of Temperature and Salinity on Hatching Rate of Fertilized Egg in Fleshy Shrimp, Penaeus chinensis (대하(Penaeus chinensis) 수정난의 부화에 미치는 수온과 염분의 영향)

  • HUR Sung Bum;KIM Hyun Jun
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.29 no.1
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    • pp.1-8
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    • 1996
  • The effects of temperature and salinity on hatching rate of fertilized egg were examined to develop the method for the efficient seed production in fleshy shrimp, Penaeus chinensis. At the temperature ranging from $20^{\circ}C\;to\;24^{\circ}C$, the hatching rate increased with temperature and the highest hatching rate $(95.5\%)$ occurred at $24^{\circ}C$. But, with the temperature above $26^{\circ}C$, the hatching rate decreased suddenly, and at $30^{\circ}C$, the egg did not hatch at all. The hatching rate increased with salinity within the range of $20\%_{\circ}\;to\;31\%_{\circ}$ and the highest hatching rate $(95.5\%)$ occurred at $31\%_{\circ}$. However, with the salinity above $31\%_{\circ}$, the rate decreased abruptly, and it was only $25.5\%\;at\;40\%_{\circ}$. The hatching speed of egg was the fastest at $24^{\circ}C$. The hatching rate at $24^{\circ}C$ with the salinity of $31\%_{\circ}\;was\;30.5\%$ within 18hrs of the hatching experiment and it attained to $95.5\%$ within 48hrs of the hatching experiment. At $24^{\circ}C$, the hatching rate with the salinity of $30\~31\%_{\circ}$ is 1,2 times higher than that of egg with the salinity of $33\~35\%_{\circ}$.

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Consideration on Changes of Density Stratification in Saemangeum Reservoir (새만금호 내 밀도 성층 변화 고찰)

  • Oh, Chan-Sung;Choi, Jung-Hoon
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.18 no.2
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    • pp.81-93
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    • 2015
  • The comprehensive master plan in November 2010 on Saemangeum internal development has been released, and there is a need for complementary measures related to in-situ monitoring methods in order to acquire water temperature (T) and salinity (S) data. Thus, these data are monitored and analyzed by Korea Rural Community Corporation continuously. The purposes of current study are to evaluate the distributions of seasonal T and S, sigma-t, and stratification parameter and to compare annual stratification system in 2011 and 2012. To achieve these objectives, monthly vertical changes of T, S, and sigma-t, which are reproduced by a kriging technique, have been analyzed. In summer, the temperature difference between surface and bottom layers varies from 2 to $3^{\circ}C$, and the stratification of T is considerably weak. The stratification of S occurs abruptly within depth of EL. (-)5 to EL. (-)10 m. Therefore, stratification is induced by sudden increasing of water inflow amount due to a localized downpour during the rainy season, and these stratification processes are strongly influenced by inflowing a fresh water from watersheds in estuary environment.

Study on Salinity Distribution Change by the Fresh Water at the Bay in Flood (홍수기 하구로 유입된 담수로 인한 만에서의 염분분포 변화에 관한 연구)

  • Lee, Hyun-Seok;Ishikawa, Tadaharu;Kim, Young-Sung;Chae, Hyo-Sok
    • Journal of Korea Water Resources Association
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    • v.44 no.1
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    • pp.23-30
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    • 2011
  • Any significant inflow of fresh water due to flood or snow melting can rapidly reduce salinity at the bay. In such a case, the habitat environment in the sea near river mouth can be partly destroyed. Therefore, research to understand the salinity distribution quantitatively at the bay for the utilization of natural environment and for the inhabitant conservation must be very important. In this study, the investigation on the relationship between satellite image and turbidity is carried out first, and then the salinity distribution at the bay using the relationship between turbidity and salinity is derived. The main results are as follows. First the reappearance ability of RGB bands respectively of the satellite image is investigated, and then it was confirmed that the combination of band2 and band3 expressed best the movement characteristics of turbid water at the bay is chopped up into 4 small areas. Second the turbidity of river mouth is estimated using the travel time from the upward monitoring station to the river mouth. Finally the satellite image is converted into the salinity distribution by the correlation of salinity and turbidity. It is confirmed that the salinity distributions obtained from above three investigation methods are quite reasonable and clear.

Distributional characteristics of Escherichia coli based on seasonal rainfall variations and extension of freshwater pollutant sources by salinity gradients at Ulsan Bay of Korea facing East Sea (동해 울산만에서 계절적 강우변화와 담수기원 오염원이 염분구배 및 유역별 대장균 분포에 미치는 영향)

  • Lee, Minji;Baek, Seung Ho
    • Journal of the Korea Academia-Industrial cooperation Society
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    • v.18 no.4
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    • pp.632-640
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    • 2017
  • In order to understand the seasonal and geographical characteristics of environmental factors and distribution of Escherichia coli by salinity gradient due to precipitation, we investigated abiotic and biotic factors during four seasons from February 2013 to November 2015. The study area was divided into three different zones based on salinity gradient and geo-oceanographic characteristics. During the study period, water temperature, salinity, Chlorophyll a, and secchi-depth varied in the range of $8.5-26.1^{\circ}C$, 13.5-34.4 psu, $0.4-74.0{\mu}g\;L^{-1}$, and 0.5-10.0 m, respectively. Salinity was low at Zone I, which was influenced by water flux from Tae-hwa River, especially in 2014. Salinity was gradually increased (one-way ANOVA; p < 0.05) toward Zone III located offshore of the bay. The highest colony form of E. coli was detected at Zone I. E. coli maintained a relatively low level at Zone III during all seasons. E. coli was correlated with transparency (r = -0.36; p < 0.05) and salinity (r = -0.53; p < 0.01), implying that those parameters might play important roles in the proliferation of E. coli. These results indicated that E. coli were strongly affected by frequent rain (< 50 mm) around inner stations in Ulsan Bay of Korea.

The role of geophysics in understanding salinisation in Southwestern Queensland (호주 Queensland 남서부 지역의 염분작용 조사)

  • Wilkinson Kate;Chamberlain Tessa;Grundy Mike
    • Geophysics and Geophysical Exploration
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    • v.8 no.1
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    • pp.78-85
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    • 2005
  • This study, combining geophysical and environmental approaches, was undertaken to investigate the causes of secondary salinity in the Goondoola basin, in southwestern Queensland. Airborne radiometric, electromagnetic and ground electromagnetic datasets were acquired, along with data on soils and subsurface materials and groundwater. Relationships established between radiometric, elevation data, and measured material properties allowed us to generate predictive maps of surface materials and recharge potential. Greatest recharge to the groundwater is predicted to occur on the weathered bedrock rises surrounding the basin. Electromagnetic data (airborne, ground, and downhote), used in conjunction with soil and drillhole measurements, were used to quantify regolith salt store and to define the subsurface architecture. Conductivity measurements reflect soil salt distribution. However, deeper in the regolith, where the salt content is relatively constant, the AEM signal is influenced by changes in porosity or material type. This allowed the lateral distribution of bedrock weathering zones to be mapped. Salinisation in this area occurs because of local-andintermediate-scale processes, controlled strongly by regolith architecture. The present surface outbreak is the result of evaporative concentration above shallow saline groundwater, discharging at break of slope. The integration of surficial and subsurface datasets allowed the identification of similar landscape settings that are most at risk of developing salinity with groundwater rise. This information is now being used by local land managers to refine management choices that prevent excess recharge and further salt mobilisation.

A Study of the Salt Rejection from the Surface of Marine Waste using Ultra Fine Bubble (초미세기포를 이용한 해양쓰레기 표면 내 염분제거에 관한 연구)

  • Kim, Bo-Min;Kim, Kwang-Koo;Park, Chan-Gyu
    • Journal of the Korea Academia-Industrial cooperation Society
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    • v.22 no.6
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    • pp.11-18
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    • 2021
  • Nano bubble water is used in various washing processes, including cleaning of solar panels, salt rejection of roads, and cleaning precision parts of machines. High cleaning efficiency and water conservation are obtained by applying nano bubbles during pretreatment of the marine waste cleaning system. This study compared the salt rejection of nano bubble water, and it was revealed that marine waste was produced by wood immersed in 200,000 mg/L NaCl solution. Using tap water and nano bubble water for washing, comparisons of the surface salt concentrations of wood were determined according to the nozzle, orifice diameter, pump speed and washing time. Decreased surface salt concentration was observed on the wood surface with increasing washing time. Water consumption was optimal between 5- and 10-seconds washing time. Increasing orifice diameter of the nozzle reduced the spraying pressure, with consequent increase in the wood surface salt concentration, thereby establishing the importance of orifice diameter of the nozzle. Compared to levels obtained with tap water, salt concentration of the wood surface after washing with nano bubble water was 2.2% lower with sector nozzle, and 30.9% lower with circular nozzle. In the washing experiment using nano bubble water, the salt concentration on the wood surface was about 9.5 mg/L lower when washed with sector nozzle than the circular nozzle.