• Title/Summary/Keyword: Sea mud

검색결과 259건 처리시간 0.028초

한국 서해안 곰소만 조간대의 제 4기 층서와 해수면 변화 (Late Quaternary stratigraphy and sea-level change in the tidal flat of Gomso Bay, West Coast of Korea)

  • 장진호;박용안
    • 한국해양학회지:바다
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    • 제1권2호
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    • pp.59-72
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    • 1996
  • 한반도 서해안 곰소만 조간대의 제 4기 층서는 최소한 2개의 부정합면을 경계로 하여 하부로부터 기반암, 선현세 산화대층(혹은 풍화토), 현세 조간대층의 순서로 배열된다. 선현세의 산화대층은 황갈색의 반고화된 이질 퇴적층으로서 식물 뿌리와 식물 조각들이 산재하고, 수평 및 수직 방향의 미세한 틈(crack)들이 존재하며, 해양성 패각과 미고생물 화석은 전혀 존재하지 않는다. 이 산화대층은 12,000년 B.P.이전의 아빙기(stadial) 시기에 해안 육지의 지형적 저지(소분지)에서 퇴적된 것으로 추정된다. 현세의 조간대층은 하부의 이질 퇴적상(상부 조간대층) 과 상부의 사질 퇴적상(중부 및 하부 조간대층)으로 구성된 상향조립의 해침층 (transgressive succession)으로서 현세의 해수면 상승을 반영한다. 해수면 지시에 적합한 물질의 $^{14}$ C-연령과 심도(depth)의 상관관계에 기초하여 현세의 해수 면 변화를 추적한 결과, 한반도 서해의 해수면(relative sea-level 혹은 local sea- level)은 현재의 평균 해수면을 기준으로 7,000년 B.P.에 6.5 m 아래, 4,000년 B.P. 에 3 m 아래, 그리고 2,000년 B.P.에는 2.5 m 아래에 위치하였고, 현세 동안 큰 범위의 상승 및 하강 변화를 보인 증거는 찾을 수 없었다.

해상 실험에 의한 침하식 해삼 양성 기구의 생물학적 성능 평가 (Biological performance evaluation of tubular subsurface cage system for sea cucumber, Apostichopus japonicus, grow-out by in-situ tests)

  • 오무환;권인영;김태호
    • 수산해양기술연구
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    • 제50권2호
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    • pp.202-213
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    • 2014
  • The sea cucumber, Apostichopus japonicus, is becoming an important aquaculture species in China, Japan and Korea. The purpose of this study is to evaluate the biological performance of a tubular type of subsurface cage for sea cucumber grow-out by in-situ tests. The cage structure was constructed of PP (polypropylene) frames and PP tubes (${\phi}130mm{\times}24pieces$). A set of tests were conducted at a depth of 15 m near Seosaeng, Ulsan, Korea for 295 days (23 July, 2012 to 13 May, 2013). A total of 155 sea cucumbers were used and fed a mixed diet containing mud, mineral, wheat, fish meal, etc (3% of their body weight). At the end of the experiments, sea cucumber showed a higher survival rate in feed shelter (77.14%) rather than no feed shelter (64.71%). The specific growth rate (SGR) of sea cucumbers in feed condition (0.04% $day^{-1}$) was higher than that of no feed culture animals (-0.49% $day^{-1}$) during total experimental periods. The result was able to find a no significance difference in survival rate but a significance difference in SGR under feed and no feed treatments.

First Report of Mud Shrimp Austinogebia wuhsienweni (Crustacea: Decapoda: Upogebiidae) from Korean Waters

  • Lee, Kyu Hyun;Song, Jae Hee;Ahn, Hyun Mi;Ko, Hyun Sook
    • Animal Systematics, Evolution and Diversity
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    • 제30권4호
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    • pp.334-338
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    • 2014
  • Specimens of Austinogebia wuhsienweni (Yu, 1931) previously recorded from China to Japan were collected at a manila clam farm of 0.5 m depth in Hongseong, Yellow Sea. They were briefly described and illustrations included color photographs, since this was the first record of this rare species from Korean waters. Three species of Upogebiidae are known from Korean waters: Upogebia major (De Haan, 1839), U. issaeffi (Balss, 1913), and A. wuhsienweni (Yu, 1931). They are similar to each other, however, the presence of the ventral spines of the rostrum, a proximal knob on the lateral margin of the uropodal endopod, and a longitudinal carina on the inner surface of the palm of the male first pereiopod can easily distinguish the present species from the two species of Upogebia.

아산만일대(牙山灣一帶) 해저퇴적물(海底堆積物)에 대(對)하여 (Bottom sediments of the Asan bay, west coast of Korea)

  • 김승우;장정해;박용안
    • 자원환경지질
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    • 제11권2호
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    • pp.81-88
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    • 1978
  • Nearly 300 bottom sediments and 20 box-cores were sampled from the Asan bay. The central portion of the Asan bay is covered by sand, slightly gravelly sand and gravelly muddy sand. Between the central and marginal zones gravelly mud and slightly gravelly sandy mud are characteristically distributed. The gravel population in the sediments seems to be originated from the rocky bottom on the area near the bay because the gravel is angular and composed of the schist and gneiss. The quartz/feldspar ratio is about 3/2. It is considered to be that the amount of feldspar in this bay is much higher than that of any other areas in the Yellow Sea. This is considerd to be comparatively short distance of transport ion of these sediment from the provenance.

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함평만의 간석지 해안지형의 변화 (The Changing Process of the Tidal Landforms in Hampyeung Bay, Southwest Korea)

  • 김남신;이민부
    • 한국지형학회지
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    • 제18권4호
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    • pp.223-233
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    • 2011
  • 본 연구는 함평만의 간석지 해안지형의 분포특징과 그 변화과정이다. 함평만은 하천의 유입이 없는 분지형태와 같은 반폐쇄형 만으로, 외해 만 입구는 좁고, 내해로 가면서 넓어지는 형태이다. 이곳의 퇴적물 공급원은 조류와 연안사면에서 이동된 물질이다. 연구지역의 주요 지형요소는 간석지, 갯골, 조간대사주, 해식애, 해안단구 등이다. 간석지형은 입도조성에 따라 뻘 간석지, 사질혼성 간석지로 분류되었다. 뻘 간석지는 갯벌이 간석지와 연속성을 보이며 완만히 이어지는 해안지역에, 그리고 사질혼성 간석지는 해식애와 해안단구 기저 지역에 발달하였다. 일부 해안 지형에서는 신생대 4기 해수면 변동으로 퇴적된 지층이 확인되었다. 10년간 간석지 입도조성 변화 분석에서 모래는 2%, 실트는 6% 증가하였고, 점토는 9% 감소하였다. 오목형 간석지에는 염생식물이 정착해 있다. 염생식물의 분포 면적 변화는 2001년에 2.4km2에서 2009년에는 9.3km2로 약 4배 확대되었다. 같은 시기 염생식물 분포 지역에서 평균입도는 6.5φ에서 4.5φ로 조립화되는 경향을 보였다.

Clay Minerals of the Bottom Sediments on the Northwestern Continental Shelf in the East China Sea

  • Park, Yong-Ahn;Khim, Boo-Keun;Nam, Jung-Man;Youn, Jeung-Su
    • 한국지구과학회지
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    • 제25권1호
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    • pp.1-9
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    • 2004
  • The clay minerals of thirty-four bottom sediments collected from the northwestern continental shelf of the East China Sea have been determined by X-ray diffraction analysis. The clay mineral distribution is mainly controlled by the sediment source and the dominant circulation pattern. The predominant clay mineral in our study area is illite comprising more-than 70% of whole clay fraction. The highest concentration of illite (>72%) is found in the southeastern offshore parts beyond the reach of terrigenous input from the Cheju Island. It means that these illites are largely transported by the Kuroshio Current from the South China Sea. Smectite is highly concentrated in the northwest middle part and in the outer-shelf mud patch. It seems to be due to the high supply of smectite transported from China where the fine-grained sediments are discharged from the modern and ancient Huanghe River. The relatively high abundance of kaolinite is likely derived from the Changjiang River via Taiwan ·Warm Current. In contrast, the large amounts of chlorite and high chlorite/kaolinite ratios occur in the northwestern are, reflecting the transportation by the Huanghai Sea Coastal Current from the southern Yellow Sea.

한국 남서 갯벌지역 짱뚱어 (Boleophthalmus pectinirostris)의 연령과 성장 (Age and Growth of the Blue Spot Mudskipper (Boleophthalmus pectinirostris) in the Mud Flat of Southwestern Korea)

  • 정순재;한경호;김진구;심두생
    • 한국수산과학회지
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    • 제37권1호
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    • pp.44-50
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    • 2004
  • Age and growth of the blue spot mudskipper (Boleophthalmus pectinirostris) were studied using the samples caught in the mud flats of southwestern Korea during April-October, 2001. The value of the marginal index of the second actinost bone was the lowest in July and October and indicated by rings that was analysis of formed teice a year. The relationship between body weigt (BW) and total length (TL) was expressed as BW=0.000005 $TL^{3.12}\;(r^2=0.92)$ for females and BW=0.000476 $TL=^{2.18}\;(r^2=0.62)$ for males. Regression analysis of TL-BW between sexes showed a significant difference (P<0.01). Relationship between total length (TL) and actinost radius (R) were expressed as TL=16.9+33.4 R $(r^2=0.62)$ for females and TL=45.8+26.2 R $(r^2=0.41)$ for males. Growth parameters, $L\infty,t_0$ and K were estimated as 165.2 mm, -0.23, and 1.07 for females and 155.3 mm, -0.35, and 1.39 for males.

Rhizosphere와 해수에 있어서의 Azotobacter의 분포 (Distribution of Azotobacter in Rhizosphere and Sea)

  • 홍순우;최영길
    • 미생물학회지
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    • 제12권1호
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    • pp.15-24
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    • 1974
  • This experiment has been carried out with a view to elucidating the distribution of Azotobacter and their population size in rhizosphere and sea and designed ro compare the results with some environmental factors. Results of the experiment are summarized as follows: 1) It was observed that the population sizes of Azotobacter were decided upon the moisture content of soil and that the soil pH was one of the most impertant factors influencing the distribution of Azotobacter. 2)Population sizes of Azotobacter in rhizosphere were changed in accordance with the kinds of vegetation on soil: The rhizosphere where bamboo, corn, legume, and oak inhabit showed the largest population size of Azotobacter. On the other hand, rhizosphere of ginseng revealed no Azotobacter. However, the largest population of general fungi were measured at the rhizosphere. 3)Comparing the population sizes of general microbes in rhizosphere with those of non-rhizosphere, the population sizes of microbes in rhizosphere are larger than those of non-rhizosphere. 4)In coastal environments, population sizes of Azotobacter in surface water of sea are similar to those of the soil(mud) of tidal land. But the sizes are generally smaller than those of terrestrial soils.

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서해안에 서식하는 쏙(Upogebia major, de Hann 1841)과 가시이마쏙 (Austinogebia wuhsienweni, Yu 1931) 암컷의 생식 주기 (Annual gametogenic cycles of female mud shrimp Upogebia major (de Haan, 1841) and Austinogebia wuhsienweni(Yu, 1931) on the west coast of Korea)

  • 안현미;강현실;송재희;조재권;황운기;정희도
    • 환경생물
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    • 제41권3호
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    • pp.298-307
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    • 2023
  • 이 연구에서는 우리나라 서해안에 서식하는 쏙 (U. major)과 가시이마쏙(A. wuhsienweni) 암컷의 연중 번식 주기를 조직학적 방법을 이용하여 조사하였다. 채집된 시료는 연령에 따른 성숙 및 번식생태 차이가 있는지 알아보기 위해 두흉갑장(carapace length, CL)을 기준으로 성체와 어린 개체로 구분하여 분석하였다. 두흉갑장 25 mm 미만의 어린 쏙(U. major)의 경우에는 생식소 발달단계가 대부분 연중으로 초기발달기(62~100%)와 후기발달기(10~38%)로 관찰되어 번식에 참여하지 않는 것으로 확인된 반면, 두흉갑장 25 mm 이상의 성체 쏙의 경우에는 뚜렷한 계절적 변화 패턴이 관찰되었다. 성체 쏙의 생식소 발달단계는 11월에서 이듬해 3월까지 초기발달기와 후기발달기가 관찰되고, 완숙기의 성숙난은 4월부터 10월까지 관찰되었다. 두흉갑장 15 mm 이상 가시이마쏙 성체의 경우에는 생식소 내 완숙된 성숙난이 연중 관찰되었으며, 완숙기는 1월부터 6월까지로 관찰되었다. 반면, 두흉갑장 15 mm 이하 어린 가시이마쏙의 경우에는 연중 미성숙 상태를 유지하였다. 우리나라에 서식하는 두 종의 쏙류는 암컷 성체의 생식소 성숙기간이 다른 것으로 조사되었으며, 또한 외포란 시기도 쏙은 월에서 4월, 가시이마쏙은 6월에서 9월로 전혀 다른 성 성숙 주기를 지닌 것으로 확인되었다. 이 연구는 조직학적 방법을 이용한 국내 서식 쏙류의 번식 주기를 최초로 구명한 연구로 쏙류의 생리생태를 이해하는데 중요한 기초자료로 활용될 것으로 기대되며, 패류 양식장 내 쏙류의 구제 방안 도출을 위한 기초자료로 활용될 것으로 기대된다.

어군 및 해저 목표물 탐지를 위한 초음파 신호분석에 관한 연구 (A Study on the ultrasonic signals analysis for scan fish schools and seabed targets)

  • 김재갑;김원중;양화섭;정찬주
    • 경영과정보연구
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    • 제2권
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    • pp.95-106
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    • 1998
  • Color Echo-sounder display signals reflected from underwater objects in eight colors according to the strength of the signal. When the sea bottom is hard due to the presence of rocks, etc, the trailing on the reflection become strong signal and soft to presence of mud, etc the trailing on the reflection become weak signal. Strong signals are displayed in the color range, reddish brown, orange and yellow, in descending order of intensity. Weak signals are displayed in the range blue, light blue, cyan and green, in ascending order of intensity. Image of fish schools at or near the sea bottom vary according to the characteristics of the beam angle setting. When the angle is wide, even fish not near the bottom may be recorded as being on the seabed. A narrow angle should, therefore, be selected when you want to get an accurate recording of fish at or near the sea bottom. The condition of the sea bottom can be determinded more easily when the beam angle is wide and pulse with is long. Though the objects could be verified by the type of reflected signals which have been transformed into digital signals strong middle and weak ones, the experiments have in continue under various condition. Futhermore, the methode of measuring temperature inside the sea ought to be examined.

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