• 한국광물학회:학술대회논문집
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• 한국광물학회.한국암석학회 2003년도 공동학술발표회 논문집
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• pp.67-67
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• 2003

The chemical compositions and textural relationships of the Nb-Zr oxide minerals including pyrochlore [ideally (Ca,Na)$_2$Nb$_2$O$\sub$6/(OH,F), with up to 24% UO$_2$ and 16% Ta$_2$O$\sub$5/] and baddeleyite [ideally ZrO$_2$, with up to 6% Nb$_2$O$\sub$5/] in the Sokli carbonatite complex, Kola Peninsula, Arctic are described. These two minerals in carbonatites are the major hosts for the HFSEs such as U, Th, Ta, Nb, Zr and Hf and thus are interest both economically and petrologically. The Sokli carbonatite complex (360-370 Ma) in Northern Finland, which forms a part of the Paleozoic Kola Alkaline Province (KAP), is mainly composed of multi-stages of carbonatite and phoscorite associations (P1-C1 P2-C2, P3-C3, D4 and D5) surrounded by altered ultramafic rocks (olivinite and pyroxenite) and cut by numerous small dikes of ultramafic lamprophyre. The Sokli complex contains the highest concentration in niobium and probably in tantalum, which are economically very important to modern steel technology, among the ultramafic-alkaline complexes of the KAP. Pyrochlore and baddeleyite mostly concentrate in the phoscorites. Pyrochlores in the Sokli complex are generally rounded octahedra and cubes in shape, red brown to grey yellow in color, and 0.2 to 5 mm in size. They are found in all calcite carbonatites, phoscorites and dolomite carbonatites, except P1-C1 rocks. These pyrochlores display remarkable zonations which depend on host rock compositions, and have significant compositional variations with evolution of the Sokli complex. The common variation scheme is that (1) early pyrochlore is highly enriched in U and Ta; (2) these elements decrease abruptly in the intermediate stage, while Th and Ce increase, and (3) late stage pyrochlore is low in U, Ta, Th, and Ce, and correspondingly high in Nb. Baddeleyites in the Sokli complex occur in the early P1-C1 and P2-C2 rocks and rarely in P3. They crystallized earlier than pyrochlores, and occasionally show post-magmatic corrosion and replacement. The FeO and TiO$_2$ contents of baddeleyites are much lower than those of the other terrestrial and lunar baddeleyites, whereas Nb$_2$O$\sub$5/ and Ta$_2$O$\sub$5/ contents are the highest among the reported compositions. Ta/Nb and Zr/Nb ratios of pyrochlores and baddeleyites decrease towards later stage facies, which is in accordance with the whole rock compositions. The variation of Ta/Nb and Zr/Nb ratios of pyrochlores and baddeleyites is considered to be a good indicator to trace an evolution of the carbonatite complexes.

• 한국표면공학회지
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• 제48권6호
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• pp.335-342
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• 2015

Recently, the production of oil and gas at the arctic ocean and offshore has been growing. Accordingly, S500 steel with the high tensile strength and excellent toughness has been used and flux cored wire that can be welded to the S500 has been required. In this study, we carried out observation of microstructures, mechanical properties and CTOD (crack tip openning displacement) in the weld zone that GMA (gas metal arc) welded with different component of $TiO_2$ flux core wire (the main components, rutile or Ti-slag) for S500 steel. Weld zone produced with Ti-slag flux cored wire has formed a enough acicular ferrite and shown excellent impact toughness at $-40^{\circ}C$, tensile strength at room temperature and CTOD at $-20^{\circ}C$. As a result, the developed flux cored wire was suitable for S500 steel.

• ALGAE
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• 제39권2호
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• pp.75-96
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• 2024

Rhodomonas (Cryptophyceae) and species assigned to this genus have undergone numerous taxonomic revisions. This also applies to R. marina studied here as it was originally assigned as a species of Cryptomonas and later considered a variation of R. baltica, the type species. Despite being described more than 130 years ago, R. marina still lacks a comprehensive characterization. Light and electron microscopy were employed to delineate a strain from western Greenland. The living cells were 18 ㎛ long and 9 ㎛ wide, elliptical in shape with a pointed to rounded posterior and truncated anterior in lateral view. Two sub-equal flagella emerged from a vestibulum, where also a furrow extended. In transmission electron microscopy, the furrow was associated with a tubular gullet and the pyrenoid embedded in a deeply lobed chloroplast. The chloroplast contained DNA in perforations and was surrounded by starch grains. A tubular nucleomorph was enclosed within the pyrenoid matrix. In scanning electron microscopy, the inner periplast consisted of rectangular plates with rounded edges and posteriorly these were replaced by a sheet-like structure. The water-soluble pigment was Crypto-Phycoerythrin type I (Cr-PE 545). A phylogenetic inference based on SSU rDNA confirmed the identity of strain S18 as a species of Rhodomonas as it clustered with congeners but also Rhinomonas, Storeatula, and Pyrenomonas. These genera formed a monophyletic clade separated from a diverse assemblage of other cryptophyte genera. To further explore the phylogeny of R. marina a concatenated phylogenetic analysis based on the SSU rDNA-ITS1-5.8S rDNA-ITS2-LSU rDNA region was performed but included only closely related species. The secondary structure of nuclear internal transcribed spacer 2 was predicted and compared to similar structures in related species. Using morphological and molecular signatures as diagnostic features the description of R. marina was emended.

• Ocean and Polar Research
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• 제27권3호
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• pp.299-309
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• 2005

The community structure of meiobenthos was studied in the sediment of Kongfjorden, Spitsbergen of Svalbard Island in the Arctic Sea. Samples of meiobenthos were collected in August, 2003. Meiobenthic organisms were collected by SCUBA and van veen grab or acryl sub-corers 34mm in internal diameter, and were taken from upper sediment to a depth of 3cm at each station. A total of 26 meiofaunal groups were found in the sediment of Spitsbergen in Svalbard Island. Nematodes were the most dominant faunal group. Sarcomastigophorans, benthic harpacticoids, and nauplius larvae of crustaceans, were also important components of the meiobenthic community of Kongsfjorden. All of these low faunal groups were comprised of more than 90% of total meiobenthos at every station. The total density of meiobenthos at each station was highest at station MeG 6 $(3,583{\pm}1,137inds./10cm^2)$, and lowest at station $MeG9(28{\pm}1inds./10cm^2)$. Meiobenthos in general showed the highest density in the upper 1cm layer. This may be associated with food and oxygen supply to subsurface. Harpacticoids showed extreme preference at the surface and little presence in layers deeper than 2cm. These animals may be less resistant to oxygen deficiency, and nauplius also showed the same trend. However, in St. MeG 8 and 9, meiobenthos were dense at depths of more than 0-1cm, at especially at depths of 2-3m because of relatively easy penetration of oxygen. Based on the results of cluster analysis, three meiobenthos assemblages were distinguished: one was in the outer and two were in the inner fjord. Station SCU 5 was grouped with the meiobenthos assemblage located in the outer fjord. The outer ford community was characterised by : 1) a relatively low mean number of meiobenthos taxa, 2) a relatively high density of harpacticods and nauplius. One of the inner ford communities (a group of four nation: MeG 2, 3, 8, 9) was in the proximity of the glaciers. Specifically, it was characterised by : 1) a low mean number of meiobenthos taxa, 2) a low density. The other inner ford community was characterised by both a high density and great mean number of meiofaunal taxa.

• 미생물학회지
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• 제52권3호
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• pp.365-374
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• 2016

고위도에서의 온도 상승은 $0.6^{\circ}C$/10 년으로, 이는 토양 유기 탄소에 대한 미생물의 분해 활성 증가를 유도한다. 게다가, 분해된 토양 유기 탄소는 이산화탄소 또는 메탄 같은 온실가스로 전환, 방출되어 기후 변화를 가속화시킨다. 따라서, 토양 유기 탄소 분해와 관련된 미생물의 다양성 및 기능 이해를 위한 토양 해동 모델 연구가 필요하다. 이러한 연구를 위하여 Alaska Council의 두 깊이의 토양(SPF와 PF라 각각 명명한 30-40와 50-60 cm 깊이의 토양)을 $0^{\circ}C$에서 108일 동안 배양하였다. 환경 모사 실험 동안 pyrosequencing을 수행하였고, metagenome을 분석하여 총 111,804개의 미생물 sequence를 얻었다. 이 중, 574-1,128개의 세균 operational taxonomic unit (OTU)과 30-57개의 고세균 OTU를 확인하였다. 토양 배양에 따라 두 토양 모두에서 Crenarchaeota phyla의 상대적 분포가 증가하였으며, Actinobacteria와 Firmicutes phyla의 분포가 SPF와 PF에서 각각 크게 증가하였다. 추출한 토양 유기 탄소에 대한 무게 측정 및 gel permeation chromatography를 통해, 환경 모사 실험이 진행되는 동안 토양 유기 탄소의 주요 구성 성분인 부식산(humic acids)이 중합화(humification)되는 것을 확인하였다. 결론적으로, 냉대 툰드라 동토의 해동은 Crenarchaeota, Actinobacteria 및 Firmicutes phyla의 증가를 야기시키며, 미생물에 의한 토양 유기 탄소 분해 및 이용을 야기시키는 것으로 예측된다.

• Journal of Microbiology and Biotechnology
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• 제25권11호
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• pp.1880-1893
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• 2015

In this study, Pseudomonas R0-14, which was isolated from Arctic soil samples, showed a clear halo when grown on M9 medium agarose plates containing olive oil-rhodamine B as substrate, suggesting that it expressed putative lipase(s). A putative lipase gene, lipR, was cloned from R0-14 by genome walking and Touchdown PCR. lipR encodes a 562-amino-acid polypeptide showing a typical α/β hydrolase structure with a catalytic triad consisting of Ser₁₅₃-Asp₂₀₂-His₂₆₀ and one α-helical lid (residues 103-113). A phylogenetic analysis revealed that LipR belongs to the lipase subfamily I.3. LipR was successfully expressed in Escherichia coli, purified, and biochemically characterized. Recombinant LipR exhibited its maximum activity towards p-nitrophenyl butyrate at pH 8.5 and 60℃ with a K_m of 0.37 mM and a k_cat of 6.42 s^-1. It retained over 90% of its original activity after incubation at 50℃ for 12 h. In addition, LipR was activated by Ca²⁺, Mg²⁺, Ba²⁺, and Sr²⁺, while strongly inhibited by Cu²⁺, Zn²⁺, Mn²⁺, and ethylenediaminetetraacetic acid. Moreover, it showed a certain tolerance to organic solvents, including acetonitrile, isopropanol, acetone, methanol, and tert-butanol. When algal oil was hydrolyzed by LipR for 24 h, there was an enrichment of n-3 long-chain polyunsaturated fatty acids, including eicosapentaenoic acid (1.22%, 1.65-fold), docosapentaenoic acid (21.24%, 2.04-fold), and docosahexaenoic acid (36.98%, 1.33-fold), and even a certain amount of diacylglycerols was also produced. As a result, LipR has great prospect in industrial applications, especially in food and/or cosmetics applications.

• 환경생물
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• 제35권1호
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• pp.1-5
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• 2017

A native species to the European ocean, the tunicate Ciona intestinalis now appears worldwide, from sub-Arctic to tropical regions. C. intestinalis generally occurs as an opportunistic fouling organism on artificial substrates in harbors or aquaculture. This study focused on estimating the early growth pattern of C. intestinalis under various temperature conditions. Adults were collected from the Guryungpo harbour in November 2016, and their artificially inseminated eggs were used for the study. The growth of the C. intestinalis was investigated at 8 constant temperatures, ranging from $12^{\circ}C$ to $26^{\circ}C$, at 30 psu. Results indicate that the growth of C. intestinalis increased with increasing temperature. The growth was sluggish at $12^{\circ}C$, and decreased at $26^{\circ}C$. The optimal temperature for growth of C. intestinalis was therefore estimated to be between $20^{\circ}C$ and $24^{\circ}C$.

• 한국해양공학회지
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• 제22권2호
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• pp.42-49
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• 2008

Recently many countries have become interested in the development of cold or arctic regions. The construction of engineered structures in those regions demands an understanding of the deformation characteristics of frozen soil. However, an understanding of frozen soil behavior poses difficult problems owing to the complex interaction between the soil particles and the ice matrix. In this research, a series of laboratory tests was performed to investigate the variations in the unconfined compression strength and split tensile strength of weathered granite soil and mixed soil (standard sand and kaolinite) in 15 degrees below zero environments. In the frozen soil tests, specimens were prepared with various water and clay contents, and then the interrelationships between four factors (water content, clay content, unconfined compression strength, split tensile strength) were analyzed. The test results were summarized as follows; as the water content was increased, the unconfined compressive and split tensile strengths also increased in frozen soil. However as the clay content was increased, the unconfined compressive and split tensile strengths were lowered. In the case of frozen soil that contained little clay content, the strength decreased rapidly in mixed soil (standard sand and kaolinite) when the frozen specimen was broken. On the other hand, in the cases of mixed soil that contained a high clay content and weathered granite soil, the strength decreased relatively slowly.

• 한국구조물진단유지관리공학회 논문집
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• 제17권5호
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• pp.59-66
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• 2013

한중공사에 있어서 일반 콘크리트는 영하의 기온에서 타설할 경우 양호한 경화를 얻을 수 없으며, 저온에서 동해를 방지하고 경화성을 확보하기 위하여 내한방동제를 첨가하여 사용하고 있다. 초속경 콘크리트를 한중공사에 적용할 경우 초기 급속한 발열반응을 통하여 동해를 입기 전에 소요강도를 확보할 수 있을 것으로 판단된다. 최근 연구되고 있는 마그네시아인산염복합체는 초속경성이고 저온에서도 수화반응이 가능한 것으로 보고되고 있어 새로운 극한지용 건설재료로 사용할 수 있을 것이다. 따라서 본 연구에서는 극한지용 건설재료의 개발을 위한 연구로서, 마그네시아인산염복합체를 개발하고 이 복합체를 사용한 모르타르에 대해 온도의 영향을 고려한 재료물성 평가를 실시하여 적정 배합을 제안하였다.

• 한국지반환경공학회 논문집
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• 제17권1호
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• pp.49-54
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• 2016

동토지반을 구성하는 지층 중 표층에 분포하는 활동층은 계절에 따라 동결과 융해를 반복하여 지표면의 동상을 야기한다. 동상 높이는 활동층의 두께에 큰 영향을 받으므로, 동토지반 상부 인프라시설의 안전한 설계 및 시공을 위하여 활동층의 두께 산정은 매우 중요한 부분을 차지한다. 본 연구에서는 경량화된 원위치 관입시험 방법인 동적 콘 관입기를 이용하여 동토지반에서 활동층이 분포하는 심도를 평가하고자 하였다. 동적 콘 관입시험을 적용하기 위한 대상현장으로서 알래스카에 위치한 솔로몬 지역의 동토지반이 선택되었으며, 해당 지역의 두 개소에서 지중온도계측 및 동적 콘 관입시험이 수행되었다. 적용실험 결과 동적 콘 관입시험으로부터 획득된 동적 콘 관입지수는 활동층 및 영구동토층에서 서로 상이한 값을 나타내는바 동적 관입특성에 따른 활동층과 영구동토층의 경계부 심도가 산정되었으며, 경계부 심도에서 아이스 렌즈층으로 판단되는 구간이 감지되었다. 해당 개소에서 획득된 지중온도분포도에서 영상 및 영하 온도의 경계 심도는 본 연구의 동적 콘 관입시험으로부터 획득된 활동층 분포 심도와 부합하는 결과를 보였다. 본 연구에서 적용된 동적 콘 관입기는 대형장비의 접근 및 적용에 한계가 있는 극한지 동토 지역의 활동층 심도평가를 위하여 활용될 수 있을 것이라 기대된다.