• Economic and Environmental Geology
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• v.53 no.6
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• pp.781-792
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• 2020

Mine tailings, which are inevitably formed by the development of manganese nodules, manganese crusts, and hydrothermal seafloor deposits, have attracted attention because of their quantity and potential toxicity. However, there is a lack of data on the quantity of mine tailings being generated, their physicochemical properties, and their effects as environmental hazards and on marine ecosystems in general. The importance of treating mine tailings in an environmentally friendly manner has been recognized recently and related reduction/treatment methods are being considered. In the case of deep-sea mineral resource development, if mine tailings cannot be treated aboard a ship, the issue becomes one of the cost of transporting them to land and solving the problem of environmental pollution there. Therefore, the Korea Institute of Ocean Science and Technology conducted research on the harmfulness of mine tailings, their effect on marine ecosystem, the diffusion model of contaminated particles, and candidate purification treatment technologies based on five representative controlling factors: 1) effects of pollution /on the environment, 2) effects of environmental/ biological hazards, 3) diffusion of particles, 4) mineral dressings, and 5) reducing/processing mine tailings. The results of this study can provide a basis for minimizing environmental problems by providing scientific evidences of the environmental effects of mine tailings. In addition, it is also expected that these results could be applied to the treatment of pollutants of different origins and at land-based mining waste sites.

• The Korean Journal of Quaternary Research
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• v.10 no.1
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• pp.53-68
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• 1996

강원도 주문진에서 양양에 이르는 해안평야의 지형형성과 고환경을 신석기유적의 기초조사 연구의 하나로서 연구하였으며 그 결과는 다음과 같다. 1. 제4기 최종빙기의 최성 기에 해당되는 15,000y.B.P. 경에는 연구지역은 해수면의 하강에 따른 연장하천의 개석곡으 로서 아한대의 침엽수림의 육상영역하에 있었다. 2. 15,000y.B.P.경 이후 해수면은 기온의 호 전으로 7,500y.B.P에 이르기까지 서서히 상승하였고 이에 따라 개석곡은 연장하천의 후퇴로 육성에서 얕은 하성으로 바뀌었다. 3 해수면 상승은 7,500y.B.P. 이후 빨라지면서 해진 (transgression)으로 되었고 그결과 개석곡은 4,000y.B.P.경에 이르러 하성에서 내만 또는 익 곡의 기수성으로바뀌게 되었다, 이 기간은 후빙기의 이른바 고온기(hypsithermal period)로 서 낙엽활엽수 시대였고 내만 또는 익곡의 가장자리에서는 수생식물이 생육하는 습지환경으 로 변모되었다. 4. 개석곡을 내만 또는 익곡으로 변모시킨 해진은 1,500yB.P.경까지 이어지 면서 지금의 고도에서 안정되었다. 그 결과 내만 또는 익곡의 만입부에서 사주가형성되면서 내만 또는 익곡은 곳에 따라 담수 또는 기수역의 석호로 변하였고 기후는 이전의 고온시대 와는 달리기온은 조금식 하강하는 한랭기후로 서서히 변모시켰다. 5. 석호는 1,000y.B.P. 경 에 이르는 동안 배후로부터 운반된 하천의 토사와 전면의 풍성사 그리고 무성하게 생육하는 수생식물에 의해 서서히 고석호로 등장되기 시작되었다. 6. 1,000y.B.P. 이후 현재에 이르는 동안 하천의 토사와 풍성사의 퇴적증가로 육화가 가속되면서 본래의 개석곡은 매적곡으로 등장되었고 그 결과 지금의 해안평야가 형성되었다.

• Proceedings of the Korean Quaternary Association Conference
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• 2004.06a
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• pp.49-50
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• 2004

푸른 진주라 불리는 훕스굴호는 러시아 국경에 인접한 몽고 북부의 청정호수로 해발 약 1,645m 지점에 위치한다. 훕스굴호의 길이는 약 136km이고, 폭은 20-40km이며, 최대수심은 약 262m 이다. 이 호수의 물은 세계에서 가장 깨끗한 담수 중 하나로 몽고 지표수원의 약 70%를 공급하고 있다. 훕스굴호는 바이칼 열곡대내에 형성된 일종의 구조호로 약 240만년 내지 400만년전에 형성된 것으로 추정되고 있다. 훕스굴호는 자연공원으로 지정되어 보호되고 있으며, 따라서 호수의 유역은 다행스럽게도 인간활동에 오염되거나 교란되지 않아 다양하고 흥미로운 육상/수성 생물상을 보유하고 있으며, 퇴적물 기록 역시 후기 신생대 동안의 중앙아시아의 지구환경 및 기후변화 연구에 매우 적합하다. 바이칼 시추사업 (Baikal Drilling Project)은 신생대 후기 동안의 중앙아시아의 지구조진화 및 전지구적 기후변화를 규명하기 위해 미국, 러시아, 일본, 독일 등이 참여한 다국가 공동사업이다. 바이칼 시추사업 연구팀은 지난 15년간 많은 노력과 예산을 투자하여 바이칼 호로부터 총 1,600m에 이르는 방대한 양의 퇴적물 코아를 성공적으로 회수하였고, 이 시료를 이용하여 후기 신생대 동안의 중부 유라시아 대륙의 고기후/고환경 진화과정을 성공적으로 규명하였다. 바이칼 시추사업이 성공적으로 진행됨에 따라, 이 사업에 참여했던 러시아와 일본의 과학자들은 바이칼호의 서쪽에 위치한 몽고 북부의 훕스굴에도 많은 관심을 가지게 되었으며, 동시에 바이칼 시추사업의 후속사업으로 훕스굴 시추사업을 새롭게 추진하게 되었다. 한편, 대륙내부에서의 제4기 지구환경 및 기후 변화 과정에 많은 관심을 가지고 연구해 오던 한국지질자원연구원도 2003년에 정식 회원으로 훕스굴 시추사업에 합류하였다. 훕스굴 시추사업 연구팀은 몽고의 지질광물자원연구소 (대표연구기관), 러시아의 지구화학연구소, 일본의 나고야대학교 그리고 한국의 지질자원연구원 등 4개국의 연구기관으로 구성되어 있다. 이들 4개 연구기관은 시추획득 및 기초연구 수행에 필요한 연구비를 현금 혹은 현물 (장비 포함)의 형태로 공동부담하고 있으며, 따라서 획득한 시추코아에 대해서도 각 연구기관이 전 구간에 대해 동일하게 25%의 소유권을 가지고 있다. 훕스굴 시추사업은 2008년까지 수행될 계획이며, 시추작업은 2005년까지 완료될 계획이다. 연구 진행과 관련하여, 공동연구의 명분을 높이고 분석의 효율성을 높이기 위해서 시료채취 및 기초자료 획득은 4개국의 연구원이 모여 공동으로 수행한 후의 결과물을 서로 공유하고, 자세한 전문분야 연구는 각 국의 대표기관이 독립적으로 수행하는 방식을 택하였다. 훕스굴에 대한 제1차 시추작업은 2004년 3월 말에 실시하였다. 시추작업 결과, 약 80m의 시추 코아가 성공적으로 회수되어 현재 러시아 이르쿠츠크 지구화학연구소에 보관중이다. 이 시추코아는 2004년 8월 중순경에 4개국 연구팀원들에 의해 공동으로 기재된 후에 분할될 계획이다. 분할된 시료는 국내로 운반되어 다양한 전문분야별 연구에 이용될 것이다. 한편, 제2차 시추작업은 2004년 12월에서 2005년 2월 사이에 실시될 계획이다. 수백만년에 이르는 장기간에 걸쳐 지구환경변화 기록이 보존되어 있는 훕스굴호에 대한 시추사업은 후기 신생대 동안 유라시아 대륙 중부에서 일어난 지구환경 및 기후변화를 이해함과 동시에 이러한 변화가 육상생태계 및 지표지질환경에 미친 영향을 이해하는데 크게 기여할 것이다.

• Journal of the Korea Organic Resources Recycling Association
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• v.8 no.2
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• pp.102-113
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• 2000

This study was conducted to investigate the expandibility of sludge treatment by earthworm through real scale experiment and the optimum counter-plan for organic sludge treatment. For the purposes, sludge removal efficienciesof night-soil using earthworm and it's behavior according to the transplanting methods of the earthworm on non-cover worm bed or in the green house worm bed were compared. Sludge uptake rates on non-cover worm bed for 6 months were $0.27{\sim}0.33ton/m^2$ and the excrement of earthworm yields $0.15ton/m^2$(44.1~46.7% of raw night soil sludge dosage). These results were not much different from the worm bed in the green house. The average and maximum earthworm density were about $6.5kg/m^2$ and $7kg/m^2$ respectively on the non-cover worm bed. The density of the worm bed was comparatively higher in spring and fall terms but lower in summer. The amount of old earthworm was much plenty than young earthworm on the non-cover worm bed, resulting in reverse distribution type of pyramid. From the experiments on non-cover worm bed(7,000 pyeong)and in the green house worm bed(1,200 pyeong), it was concluded that landfill and transporting cost could be reduced when the earthworm was applied for the night-soil sludge treatment. Profits from the excrement sale of earthworm was 9,600,000 won. Through this study, it was founded that earthworm treatment method for organic sludge are much more environmentally sound than landfill treatment.

• Journal of Plant Biotechnology
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• v.29 no.1
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• pp.41-44
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• 2002

During the phloem development from parenchyma cells in a suspension culture of Streptanthus induced sucrose carrier and glucose carrier disappeared. Sieve element area and sieve pore induced suspension culture of Streptanthus were formed almost at the last period of the synthesis of sieve endoplasmic reticulum (SER) and p-protein. The new synthesized cell wall begann to digeste only after the new cell wall was surrounded by SER. The digested region of the cell wall and the formed region of sieve pore were regular comparatively. The completed sieve pore was an oval form, and the outer portion of sieve pore varied, ca 1.2 ${\mu}{\textrm}{m}$~1.6 ${\mu}{\textrm}{m}$ in longitudinal, 0.8 ${\mu}{\textrm}{m}$~1.3 ${\mu}{\textrm}{m}$ in tangential, and the inner size of sieve pore was irregular form of a star-like shape. The number of sieve pore between sieve cells was ca 2~7 per ${\mu}{\textrm}{m}$$^2$ and the sieve pore wall with callose was 0.05 ${\mu}{\textrm}{m}$~0.07 ${\mu}{\textrm}{m}$ in thickness. The energy for the formation of sieve element area and sieve pore might be supplied by mitochondria near the new cell wall and the role of SER remains to be illucidated.

• Korean Journal of Ichthyology
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• v.9 no.2
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• pp.178-185
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• 1997

From November 1996 to April 1997, the rockfish, Sebastiscus marmoratus (Cuvier et Valenciennes) was reared in laboratory, and observed eggs development and morphology of larvae. The eggs of this species are demersal and adhesive, and their diameter were varied within 0.76 to 0.82 mm. The color of yolk is light yellow in early developmental stage, and then turned to orange before hatching out. The yolk contained numerous tiny oil globules. Hatching began about 33 hours and 30 minutes after insemination at $10.0{\sim}14.5^{\circ}C$ of waters. The newly hatched larvae were elongated in shape and 1.62~1.68 mm in total length (TL) with 7~8+16=23~24 myomeres. The larvae absorbed yolk material and oil globule completely in 14 days after hatching and became postlarvae. The spawning season of adult rockfish may be supposed to be from February to March in the southern sea of Korea.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.33 no.2
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• pp.115-118
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• 2000

The production of cultured coho salmon (Oncorhpchus kisutoh) in Korea has being increased year after year. Smolt being reared in freshwater suffer transferring into seawater and are farmed in cages for fattening. This handling processes including transportation, confinement into cages are unavoidable stress to fish in salmon farming and often end up to mass mortality, This study aimed to investigate the impact of handling process on the stress responses of coho salmon. The indicator of stress was measured by cortisol to be a first response, and for the second response test, glucose, triBlyceride, cholesterol, lactate and electrolyte of $K^+, Na^+, Cl^-$ in serum and the activities of alanine aminotrtnferase (ALT), aspartate aminotransferase(AST) and lactate dehydrogenase (LDH) were analyzed. As a result, the concentration of cortisol, glucose as well as LDH activity were significantly increased, whereas others showed no difference comparing with control group. It obviously demonstrated that handling process made fish stressful.

• 한국해양학회지
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• v.28 no.4
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• pp.272-280
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• 1993

The seasonal variations of water salinity and the concentration of suspended particulate matter (SPM value) have been monitored in the Keum Estuary and its adjacent coastal area. the concentrations of suspended matters show great seasonal variations with low concentrations during summer season and high concentrations during winter season. During the flood season of summer, water salinities are less than 5% in the Keum estuary, and the brackish water (salinity<28%) prevails seaward covering the entire coastal area. The concentrations decreased abruptly to the seaward from higher than 100mg/l in the Keum estuary to less than 5 mg/l in the offshore. These phenomena probably results from the rapid e\deposition of riverine suspended matters within the Keum Estuary. The seasonal variations of suspended matter concentrations in the Keum Estuary and its adjacent coastal area are interpreted as the cyclic (seasonal) sedimentation processes in the west coast of Korea, that is, replenishment and deposition of fine sediments in summer, and resuspension and seaward transport in winter.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.26 no.5
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• pp.465-476
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• 1993

Rockfish, Sebastes inermis is a ovoviviparous fish distributed around the coastal waters of Korea and Japan. Naturally beared larvae obtained from female fish kept in the aquarium were reared for three months in the laboratory. The naturally healed larvae were 6.05mm in average total length(TL) with $8+18{\sim}19=26{\sim}27$ myomeres. Melanophores were distributed on the top of head, around the intestine tube and on the dorsal and ventral margins of the tail, but none on the pectoral fins. The larva(7.1mm in TL) consumed all the yolk and oil globule, in 7 days after bearing, and jaw bones were more rapidly ossified than vertebrae and cranium. In 21 days after bearing, the larvae averaged 8.50mm in TL and the caudal notochord flex $45^{\circ}$. Fin development in S. inermis larvae proceeds in the following sequence: caudal, pectoral, dorsal, anal and ventral fin. Individuals $17.6{\sim}20.8mm$ in TL($65{\sim}69$ days after bearing) are regarded as the juvenile stage. All fins bones was nearly completed in this stage.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.26 no.5
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• pp.458-464
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• 1993

From November 1992 to January 1993, the rockfish, Sebastes inermis was reared in the laboratory, and observed the developmental stage of the eggs and larvae squeezed from the parent fish. On December 4 1992, developing eggs at morula stage were obtained from female parent fishes($17.4{\sim}20.3mm$ in total lenght(TL)). The diameter of eggs ranged from 1.20 to 1.35mm(n=50), and oil globules in white color were found in the eggs. Hatching began about 55 hours after morula stage at the water temperature of $9.2{\sim}12.3^{\circ}C$. The newly hatched larvae measured from 2.90 to 3.35mm in TL with $8+12{\sim}13=20{\sim}21$ myomeres. Total lengths of the larvae will be from 5.75 to 6.15mm in 27 and 30 days after the hatching, respectively. Myomere number was $8+17{\sim}18=26$.