• Title/Summary/Keyword: 득량만

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Study on the Natural Spat Collection of the Pen Shell, Atrina pectinata (키조개, Atrina pectinata의 자연채묘연구)

  • Son, Pal-Won;Ha, Dong-Soo;Lee, Chang-Hun;Jang, Dae-Soo;Kim, Dae-Kweon
    • The Korean Journal of Malacology
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    • v.21 no.2 s.34
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    • pp.113-120
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    • 2005
  • In this experiment of natural Atrina pectinata spat collection, the number of the pen shell spats settled on a collector were 4.2, 6.8, and 2.7 in the first, second, and third year, respectively. The highest number of pen shell spat settled on the collector was observed in August, and the shell length of juvenile pen shells grew up to 42.5 mm six months after setting. The relation between shell length (SL) and days (D) after setting could be expressed as; SL = 0.3854D + 0.8423 ($r^2$ = 0.9764). The spats developed the best in depth of 10-20 m. Spat collectors in mesh size of $1{\times}2mm$ mm were better for spats to survive than the ones in $1{\times}1mm$. The most efficient material as substrate for the settlement of pen shell spat was a polyethylene monofilament in the spat collectors.

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Environmental Characteristics According to the Depth in Deukryang Bay , Culturing Ground of Pen Shell ( Atrina Pectinata ) (수심에 따른 득량만 키조개 어장의 환경특성)

  • 최용규
    • Journal of the Korean Society of Fisheries and Ocean Technology
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    • v.31 no.2
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    • pp.127-141
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    • 1995
  • The distribution of water mass in Deukryang Bay was investigated using observational data obtained on July 12 (spring tide) and 19 (neap tide) in 1994. In characteristics of water mass at the bay the area is divided into three ones by a vertical attenuation coefficient k and a stratification parameter, log sub (10) (H/U super (3)), was H is depth, and U mean velocity in the bay. The contour of k=0.6 has a similar distribution to the isobath of 10m depth in spring tide, and of 5m depth in neap tide, respectively. This indicates that the water mass in the area between the isobath of 5m and 10m depth is changed by tidal periods. The stratification parameter corresponding to k=0.6 was 2.1~2.2. In the shallow water of 5m depth the characteristics of water mass was distributed in temperature of 25.5~31.$0^{\circ}C$ and salinity of 32.8~33.8PSU(Practical Salinity Unit), the temperature was high and the salinity distributed widely. In the deep water of 10m depth it was the temperature of 22.0~29.5$^{\circ}C$ and the salinity of 33.0~33.6PSU, the temperature was low and the salinity distributed narrowly. In the middle depth water of 5m to 10m depth, the temperature of 22.0~30.$0^{\circ}C$ and the salinity of 32.8~33.5PSU, its values showed the middle between the values of the deep area and the values of the shallow area.

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Distribution of Bivalve Larvae in Deukryang Bay (득량만에서 조개류 유생의 분포)

  • Kim, Chul-Won;Kwon, Seung-Bai;Hur, Sung-Bum
    • Journal of Aquaculture
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    • v.19 no.4
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    • pp.288-298
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    • 2006
  • Larval distribution of bivalve from 29 stations in Deukryang Bay was examined from May to November in 1995. The abundance of total larvae increased from May ($3,736\;inds/m^3$) and reached maximum in August ($174,616\;inds/m^3$). But it decreased continuously until November ($2,171\;inds/m^3$). D-shape, early umbone and advanced umbone stage larvae composed of 76%, 18% and 6%, respectively, of total bivalve larvae. Nine larval species of bivalve were identified in this study. The mean abundance of Scapharca subcrenata larvae was $14,030\;inds/m^3$, which was 33.5% of total identified larvae. S. broughtonii (16.2%), Crassostrea gigas (12.5%), Mytilus edulis (10.2%) were also major species in order of their abundance. Considering the monthly larval occurrence in Deukryang Bay, main spawning month of bivalves except M. edulis and M. senhausia was estimated as July. Even though the spatial distribution of bivalve larvae in Deukryang Bay was different by the species, the larvae were generally abundant in the inner and west area of the bay, where was shallower and higher water temperature than the entrance and east area of the bay.

The Effect of Wind (Typhoon), Tide and Solar Radiation for the Water Stratification at Deukryang Bay in Summer , 1992 (하계 득량만의 연직혼합과 관련된 바람 (태풍), 조석, 태양에너지의 영향)

  • Lee, Byung-Gul;Cho, Kyu-Dae;Hong, Chol-Hoon
    • Journal of the Korean Society of Fisheries and Ocean Technology
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    • v.31 no.3
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    • pp.256-263
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    • 1995
  • This paper presents the evidence on the considerably strong stratification - destratification(SD) phenomena during spring - neap tidal cycle in summer of 1992 based on the observed temperature, salinity and density data. To find out the main factors causing SD in the bay, we computed the rate of potential energy balance of the surface heat flux, tidal and wind stirring proposed by Simpson and Hunter (1974) and Simpson and Bowders (1981) using observed data. It was found that the energy of the wind stirring was one - order smaller than those of the heat flux and the tidal stirring. It means that the variation of stratification phenomena in the bay mainly depend on tidal stirring and sea surface heating in summer if there was no exceptionally strong wind event like a typhoon. Finally, we tested the effects of typhoon on the mixing characteristics of the bay using the example of a empirical typhoon model. It was found that when wind speed is larger than 15m/sec in Deukryang Bay, the wind energy was always larger than the average heating energy based on empirical typhoon model test. Particularly, typhoon passed on the left side of the bay, strong wind energy happened, which is almost the same as tidal energy of spring tide.

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Tidal Current in the Western Part of Deukryang Bay in Summer 1992 (1992년 하계 득량만 서부해역의 조류 특성)

  • LEE Jae Chul;RHO Hong-Kil;CHO Kyu-Dae;SHIN Sang-Il;KIM Sang-Woo;KIM Sang-Hyun
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.28 no.1
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    • pp.1-6
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    • 1995
  • A recording current meter was deployed in the shallow western part of Deukryang Bay from 1 July to 7 August 1992 during which the wind was weak. Principal component in NNE-SSW direction parallel to the axis of the bay had $98.7\%$ of the total variance and the orthogonal component of only $1.3\%$. Spectral analysis of the principal component revealed that the semidiurnal component comprised about $91.2\%$ of total energy. Whereas the diurnal and longer components were less than $2.5\%$ the shallow water tide was about $6.3\%$ . Weak mean current of 0,8cm/sec in SSE direction implies that the slow circulation in the bay is counterclockwise having the northward net flow in the deep eastern part.

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Eutrophication of Shellfish Farms in Deukryang and Gamagyang Bays (득량만과 가막양 패류양식장의 부영양화)

  • CHO Chang-Hwan;PARK Kyung-Yang;YANG Han-Serb;HONG Jae-Sang
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.15 no.3
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    • pp.233-240
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    • 1982
  • Some environmental parameters on the shell-fish farms in Deukryang and Gamagyang Bays during summer in 1981 were determined to find an eutrophication level for the conservation of the farm. Chlorophyll-a content in the seawater in the Deukryang Bay in September was $1.0{\sim}5.0{\mu}g/l$ with an average of $2.5{\mu}g/l$ In the superficial bottom muds, contents of COD were 5-10 mg/g, ignition loss $5-9\%$, phaeophytin pigment $2{\sim}5{\mu}g/g$, and sulfide 0.1-0.3 mg/g dry mud in both bays. High contents of both organic matters and sulfide were found in the innermost area of the Deukryang Bay and in the north western part of the Gamagyang Bay. All quantities including chlorphyll-a in the water are little less than or similar to those of Hansan-Geoje Bay, one of the most productive shellfish farms in the southern coastal waters in Korea . Eutrophication on both water and bottom mud was under way like other shellfish farms but pollution indices on the bottom mud calculated from the data of CODs and phaeophytin pigments shelved 6-11, which is much lower than those of Jinhae Bay and of the Hansan-Geoje Bay. This means that the bottom muds are in an early stage of eutrophication, unlike the Jinhae and Hansan-Geoje Bays though the water, similar to the other bays, shows a middle stage of eutrophication.

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Bacteriological Quality of Sea Water in Deukryang Bay, Korea (득량만 해수의 세균학적 수질)

  • CHANG Dong-Suck;JEONG Eun-Tak;YU Hong-Sik;LEE Eun-Woo;LIM Sung-Mee
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.31 no.1
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    • pp.77-81
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    • 1998
  • A bacteriological study of sea water in Deukryang Bay was conducted to evaluate sanitary conditions of the bay and compliance of waters with the recommended bacteriological criteria for the designated area of shellfish cultivation. Sea water samples were collected at the established sampling stations (fig. 1) from May 1995 to November 1996. During the study period, coliform group, fecal coliform, classification of coliform group with IMViC reactions and pathogenic vibrios were analyzed. Coliform group and feral coliform MPN's were ranged from $<\;3.0\~4600/100m{\ell}\;and\;<\;30\~1,100/100m{\ell}$, respectively. The bacteriological criteria of sea water in shellfish growing area should be less than 70 per l00ml of sea water for median value of coliform MPN, and below $10\%$ of the samples which contain over than 230 for coliform MPN or over than 43 for fecal coliform MPN, Most of the waters from 26 sampling stations were complied water coliform criteria recommended for designated shellfish growing area. Then, the ratios of the samples with move than 230/10ml of coliform group MPN and more than 43/100ml of fecal coliform MPN were $7.4\%$ and $8.5\%$, respectively. The bacterial density of the sea water was deeply affected by rainfall amount. For example, coliform bacterial counts of sea watery after 48 hours from 93 mm rainfall were $6\~7$ times higher than those of without rainfall. During the study period, infectious bacteria such as Vibrio cholerae, Salmonella sp. an d Shigella sp. were not detected from the samples, but detection ratios of Vibrio parahaemolyticus and Vibrio vulnificus were $15\~20\%$ in summer months.

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고수온기 가막만 피조개(Scapharca broughtonii) 양식장 환경과 대량폐사

  • 윤호섭;정형택;곽은주;라성주;최상덕
    • Proceedings of the Korean Society of Fisheries Technology Conference
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    • 2001.05a
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    • pp.371-372
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    • 2001
  • 피조개(Scapharca broughtonii)는 우리나라 동해안 북부에서 남해안과 서해안의 내만에 널리 분포하는 고막류 가운데 가장 중요한 산업종으로서 주로 남해안에서 많이 양식하고 있다(강 등, 1980: 김 등, 1982). 또한, 피조개의 자연채묘 및 양식기술이 확립된 이후 주로 강진만, 가막만, 득량만 등에서 양식이 되고 있다. 특히, 가막만에서는 1990년대 이후 피조개 종패가 매년 채묘되고 있으나 중간양성중 대부분이 폐사되거나 탈락되어 종패로서 활용하지 못하고 있다. (중략)

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