• Title/Summary/Keyword: 저층퇴적물

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Abundance and Distribution Pattern of the Smelid Bivalve, Theora fragilis A. Adams in chinhae Bay, Korea (진해만에서 아기반투명조개 Theora fragilis ( Mollusca : Bivalvia ) 의 분포)

  • 임현식;홍재상;제종길
    • The Korean Journal of Malacology
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    • v.11 no.1
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    • pp.21-34
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    • 1995
  • 1987년 6월부터 1990년 5월까지 진해만의 저서동물 군집에서 우점하는 아기반투명조개(Theora fragilis A. Adams)에 대한 개체군 생태학적 연구를 수행하였다. 조사결과, 이 종의 주된 분포 구역은 진해만의 입구 정점이었으나 겨울철에는 내만의 안쪽으로 확장되었다. 이 종은 여름철과 겨울철의 2회에 걸쳐 치패의 착저가 관찰되었으나 주 착저시기는 여름철이었다. 진해만 입구의 정점에서는 이러한 대량착저로 인해 그 밀도가 2,116개체/m$^{[-992]}$ 에 달하였다. 그러나 착저한 치패의 초기 감모로 인해 가을철의 밀도는 급격히 낮아졌다. 한편, 이 종의 분포는 퇴적물의 유기물 함량과 깊은 관계를 보여서 3.0-5.0%(평균 4.54$\pm$1.42%), 퇴적물의 평균 입도 8.97($\pm$0.62)$\varphi$사이에서 상대적으로 높은 밀도를 보였다. 그러나 퇴적물의유기물 함량의 증가와 함께 이 종의 밀도가 대체로 증가하지만 5.0% 이상에서는 다시 감소하는 현상을 보였다. 이 종은 여름철 저층수의 빈산소 수괴가 사라진 후에는 다시 진해만의 안 쪽 내만정점에서 높은 밀도를 나타냈다. 따라서 진해만에서의 본 종의 분포는 전반적으로 퇴적물의 유기물 함량. 퇴적물의 입도 조성 및 저층수의 용존 산소량 등에 의해 결정된다고 판단된다.

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Swimming Suitability and Management of Sea Water for Artificial created Swimming in the Southwestern Sea of Korea (한국 서남해역 인공해수욕장의 적합성 판정과 수질관리 방안)

  • Kim, Do-Hee;Chang, Jin-Ho
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.20 no.6
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    • pp.640-645
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    • 2014
  • This study aimed to determine the swimming suitability of sea and to suggest methods to address the problems on sea water color and green plants growing on sediment in the artificial created swimming in the beach of southwestern Korea. Sea water samples were collected from January to December of 2010 and analysis for SS, COD, $NH_4{^+}-N$, TP, MPN, sediment IL, ORP and plants on sediment. The results showed that the sea water under the swimming suitability "level of management" based on the relating high levels of SS and TP, but still suitable for swimming on the basis of MPN. Improving exchange seawater flow, dredging, coating and chemical treatment of polluted sediments in addition to removal of point sources and restriction of non point sources in the study area could improve the sea water quality and swimming suitability of the sea.

Seasonal Variation of Residual Flow and Prospect for Sediment Transport in the Macrotidal Coastal Area (대조차 연안해역의 계절적 잔차류 변화와 퇴적물 이동 예상)

  • Lee, Jong Dae;Yoon, Byung Il;Kim, Jong Wook;Kim, Myung-Seok;Jeong, Jae-Soon;Woo, Seung-Buhm
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.32 no.1
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    • pp.39-47
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    • 2020
  • In order to investigate current characteristics at the Gungpyung beach, which is a macrotidal flat, field measurements were carried out in the summer and winter at the intertidal and the subtidal zones. The distribution of residual current at intertidal flat was dominant in the northward direction in the summer and dominant in the northward and southwestern directions in the winter. The direction and speed of the residual current in the winter are highly correlated with the significant wave height, and the turbidity is also highly correlated with the significant wave height. Therefore, in the winter, high sediment rates are suspended by high waves, and sediments are transporting due to the residual current in the southwest direction. On the other hand, it is expected that the northward residual current is predominant due to the small wave in the summer, and sediment transport does not occur largely due to less suspended sediments. In addition, sediment transport in the southern direction is blocked by the dock, which is the artificial structure, and the erosion occurs in the south side of the dock. The erosion pattern in the macrotidal zone of Yellow sea is dominated by seasonal waves, and blocking of sediments by artificial structure is very important.

Spatial and Temporal Variation of Grain Size of the Surface Sediments in Kwangyang Bay, South Coast of Korea (한반도 남해안 광양만 표층퇴적물 입도의 시ㆍ공간적 변화)

  • 류상옥
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.8 no.3
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    • pp.340-348
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    • 2003
  • Sedimentological investigations on surface and suspended sediments were performed in Kwangyang Bay of the middle South Sea in order to reveal recent changes in depositional environments concerning anthropogenic influence. A variety of coastal developments caused the texture of the surface sediments to become distinctively finer, particularly in the southwestern part of the bay. Accordingly, the westward lining sedimentary facies was somewhat simplified from triple-mode distribution to the dual-mode one by the construction of POSCO. This east-west distribution to the sedimentary facies has recently graded into the north-south distribution by further construction of other industrial complexes including Kwangyang Port. The prominent textural changes in surface sediments are most likely associated with weakening of tidal currents related to the developments which is anticipated to be .still continued. The distribution and flux estimation of suspended sediments suggest a noticeable import of fine particles into the bay predominantly through a northern entrance rather than the southern entrance. The movements of suspended sediments in the water level near the seabed prevailed over those of the mid and surficial levels.

Estimation of the Sediment Pollution in Coast of Gwangyang, Mokpo and Shinan, Korea (광양, 목포, 신안 주변해역 해저퇴적물의 오염도 평가에 관한 연구)

  • Kim, Do-Hee;Um, Hyeon-Ho
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.19 no.4
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    • pp.303-308
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    • 2013
  • We estimated sediment pollution by the analysis of COD and AVS. We also estimated the contents of Cu, Cd, Pb, Zn in sediment of Gwangyang bay, Mokpo inner bay and Shinan Bigum coastal area from 2011 July to 2012 February. In these results of sediment COD and AVS show III level pollution in Mokpo inner bay, however Gwangyang and Shinan Bigum coast show I level pollution. The results of Igeo show over 2 on the contents of Cu and Cd in Gwangyang bay and Mokpo inner bay. It also know that Igeo can more and detail estimate sediment pollution in industrial coastal area. These results show that it is suitable to estimated sediment pollution by COD and AVS with trace metal in industrial and initial polluted coastal area rather than analysis of COD and AVS only in coastal area.

A Study on the Measurement Method for Benthic Nutrient Flux in Freshwater Sediments (담수 퇴적물의 영양염 용출 측정 방법에 관한 고찰)

  • Kim, Kyung Hee;Kim, Sung-Han;Jin, Dal Rae;Huh, In Ae;Hyun, Jung-Ho
    • Journal of Korean Society of Environmental Engineers
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    • v.39 no.5
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    • pp.288-302
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    • 2017
  • Accurate measurement of benthic nutrient fluxes (BNF) is a prerequisite for evaluating the effect of sediments on nutrient cycle in the surface water. The intact sediment cores were collected in July 2015 at the midstream of Nakdong River. We identified pre-incubation time (6, 12, 24 hr), dissolved oxygen concentration (90, 70, 50% saturation), diffusive boundary layer thickness (0, 0.6-0.8, 1.2-1.4 mm), and incubation temperature (10, 17, 20, $25^{\circ}C$) as the most important control factors, and measured the BNF fluctuation with the variation of these factors using the laboratory sediment core incubation method. Since the chemical composition, redox condition, hydrodynamic regimes and microbial activities at the sediment-water interface were changed as a result of the alteration of control factors, sediment core incubation should be conducted under as close to the natural conditions of study site as possible, in order to produce the results similar to actual values. Relative percentage differences between two replicates were below 20% in most control factors, which showed satisfactory precision for strict compliance with the experimental conditions and procedures. In the further studies, we will compare the results of core incubation with those of in situ measurements to confirm the accuracy of the sediment core incubation method.

Sedimentary Processes of Fine-grained Sediment around Intake of Pyongtaek Power Plant, West Coast of Korea (평택화력발전소 취수구 주변 해역에서 세립질퇴적물의 운반양상)

  • 류상옥;장진호;최현용
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.7 no.4
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    • pp.247-256
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    • 2002
  • Distribution of surface and suspended sediments was studied to understand sedimentary processes of finegrained sediment near the cooling water intake of Pyongtaek power plant on the west coast of Korea. The grainsize of surface sediment during the winter was coarser in the opened northern area than sheltered southern area. During the summer, finer sediment was found in the east (landward) than west due under dominantly the influence of tidal current. The concentration of suspended sediments was higher in the winter than summer and in the mid- to deep waters than surface waters. Asymmetry of tidal current induced net landward transport of suspended sediments. Landward transport of suspended sediments was most significant at the beginning of flood time when water level is low. Net suspended sediment fluxes ranged from 3.4$\times$10$^{-3}$ kg.m$^{-2}$ .s$^{-1}$ to 5.7$\times$10$^{-3}$ kg.m$^{-2}$ .s$^{-1}$ This large landward transport of suspended sediments is attributable to combination of enhanced flow induced by intake of cooling water and artificial structures near the water intake.

Effects of Bioturbation of the Amphipod Monocorophium uenoi on the Vertical Distribution of Sulphides and Oxygen within Sulphides-Rich Sediments of Lake Sihwa (세가시육질꼬리옆새우(단각류)의 생물교란이 시화호 퇴적물 내 황화합물과 산소 농도의 수직적 분포에 미치는 영향)

  • Koo, Bon Joo;Kwon, Kae Kyeong;Shin, Sang-Ho;Je, Jong-Geel
    • Journal of Wetlands Research
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    • v.8 no.3
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    • pp.79-89
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    • 2006
  • The survival rate and tube number of Monocorophium uenoi, one of the dominant species in Lake Sihwa, was investigated under laboratory condition with salinity gradients (1, 5, 10, 15, 20, 25, 30, 35, 40‰). Another laboratory experiments were conducted to investigate the survival rate of Monocorophium uenoi in sulphide-rich sediment with oxic overlying water, and the effect of amphipod bioturbation on sulphide and oxygen profiles. The survival rate and tube-forming number of the amphipod were high in salinity range of 20 to 30‰. The amphipod survival rate was also high in sulphidic sediment when the water column was oxic. The amphipod bioturbation affected the oxygen and sulphide content in the sediment; oxygen conditions in the upper sediment layers were improved, and simultaneously the concentrations of sulphide were reduced. And their depth was clearly dependent on amphipod density. In Lake Sihwa, previously anoxic bottoms with sulphidic sediment during summer turn oxic with pycnocline disappearance during autumn. Amphipods seem to have the capability to quickly invade such areas, and their tubing of the sediment may play an important role in preparing the sediment for further recolonisation of other macrobenthos.

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Physical and Sedimentological Changes in the Keum Estuary after the Gate-Close of Keum River Weir (하구언 갑문폐쇄 후 금강하구의 물리, 퇴적학적 특성변화)

  • 최진용;최현용
    • 한국해양학회지
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    • v.30 no.4
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    • pp.262-270
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    • 1995
  • A comparative study to understand the changes in physical and sedimentological natures was carried out in the Keum Estuary before and after the gate-close of Keum River weir. After closing of weir-gate maximum tidal current speed decreased about 30∼40% compared with that of the previous gate-opening period. Water masses also represent vertical stratifications both on water salinity and water transparency. The Keum Estuary seems to be changed from the well-mixed type estuary during the gate-opening period to the "partially-mixed type" and/or "salt-wedge type" estuary after the closing of weir-gate. The concentrations of suspended matter range 10∼100 mg/l in surface waters after the gate-close of Keum River Weir, representing about 1/4 to 1/3 decrease than those during the gate-close of Keum River Weir, representing about 1/4 to 1/3 decrease than those during the gate0opening period. Such decrease of suspended mater appears to be due to the decrease in the resuspension of bottom sediments, and also due to the vertical stratification of water masses that prevented the upward diffusion of turbid bottom waters. It is, therefore, expected that the depositional environment of Keum Estuary has been changing into the low energy conditions after the closing of weir gate, resulting in the rapid deposition of fine suspended matters within the Keum Estuary.

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The Spatial and Vertical Variations of Metal Pollution in Sediments after Tidal Power Plant Operation in Shihwa Lake (시화호 조력발전소 가동으로 인한 퇴적물 내 중금속 오염 특성 변화)

  • LEE, JIHYUN;JEONG, HYERYEONG;CHOI, JIN YOUNG;RA, KONGTAE
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.24 no.4
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    • pp.535-547
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    • 2019
  • In this study, the heavy metal analysis in sediments (surface sediments, sediments cores and settling particles) from Shihwa Lake has been carried out to evaluate the changes of metal pollution levels in sediments after the operation of Tidal Power Plant (TPP). The average concentrations of metals in surface sediments sampled in 2015 were 8% (Cd)~31% (Zn, Hg) lower than in 2009 before TPP operation. Results of calculating the pollution load index (PLI) with 8 metals, the PLI value in 2015 showed a 18% decrease compared to 2009. However, Cu, Zn, Pb concentrations of surface sediments in 2015 at the upper region around industrial complex still exceeded the TEL (threshold effect level) values for sediment quality guideline in Korea. After the operation of TPP, the metal contaminated depths were increasing from 15 cm to 30 cm at S6 site and from 8 cm to 20 cm at S7 site, respectively. Our data showed that the mean concentration of heavy metals in core samples decreased but the contaminated depth increased. The average of the total sedimentation flux for particulate matter increased by 3.2 times from 32.5 g/㎡/d in 2009 to 103.5 g/㎡/d in 2015. This showed that the bottom sediments were resuspended by the operation of TPP, resulting in an increase of particulate matter in the water column. These results suggest that the sediments contaminated with heavy metals seem to be resuspended and relocated due to the water current caused by the operation of TPP. Cr, Cu, Zn, Pb and Cd were highly exceeding the TEL values in the upstream region and accumulated more than 40 cm of sediment depth, indicating that heavy metal contamination through industrial activity were still a serious environmental problem of Shihwa Lake. Although the metal pollution of Shihwa Lake has been slightly reduced, the contaminated sediments with heavy metals inside of Shihwa Lake might be discharged to outer sea after the resuspension by TPP operation. It is necessary for the advanced scientific approach and political decision to drastically reduce the heavy metal pollution of the study region.