• 한국식품과학회지
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• 제35권3호
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• pp.447-454
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• 2003

동해안 특산 어종인 까나리어간장을 속성제조하기 위하여 여러 가지 발효촉진제를 첨가하여 제조한 제품의 숙성 중 화학성분 및 생균수 변화를 요약하면 다음과 같다. 총 creatine 량은 오징어내장첨가구는 숙성 2개월째, 나머지 첨가구에서는 3개월째까지 증가하였다가 점차적으로 감소하였다. TBA가는 숙성초기에 급격하게 증가한 다음 일정수준 유지 내지 서서히 감소하였으며, 전 숙성기간에 걸쳐 오징어내장첨가구에서 가장 높았으며 다른 첨가구들 간에는 뚜렷한 차이가 없었다. 유리아미노산 함량은 모든 시료에 있어 glutamic acid, alanine, valine, leucine, 및 lysine 등의 함량이 높았고 숙성기간이 길어질수록 증가하였다. 생균수는 모든 실험구에서 숙성 중 증가하였다가 숙성 후기에 감소하였으며 오징어내장 첨가구가 가장 높은 값을 나타내었다. koji 첨가구가 향기 및 맛에 있어서 가장 우수하였고 그 다음이 오징어내장첨가구이었다. 속성 까나리 어간장을 제조하기 위한 속성 발효제로서 오징어내장 및 koji는 발효기간을 단축시킬 수 있을 뿐 아니라 독특한 맛을 형성하므로 까나리 어간장의 속성제조에 발효촉진제로 사용이 가능하다고 보여 진다.

• Ocean and Polar Research
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• 제24권1호
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• pp.79-86
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• 2002

It was found that 14 coastal habitats in South Korea have comparetively natural vegetation. The habitats were classified into three types - intertidal flats, sand dunes, and estuaries. There were four intertidal flats, five sand dunes and five estuaries. Except for Cynodon dactylon and Tetragonia tetragonoides, all of the main halophytes and sand dune plants were found in the habitats. These two species were mainly distributed on the southern coast. This study identified coastal vegetation, such as pure stands of Suaeda japonica on intertidal flats, mixed halophyte communities around the high-water mark, pure stands of Vitex rotundifolia on stable sand dunes, mixed communities dominated by Carex kobomugi on unstable sand dunes, and pure stands of Phragmites communis in estuaries. The types of coastal vegetation may depend on sediment types, the inundation time of seawater and the stability of sediments.

• 한국수산과학회지
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• 제32권3호
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• pp.345-352
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• 1999

이 연구는 제주도 함덕연안에 분포하는 구멍연잎성게의 생태 및 번식생활사에 관한 연구보고서이다. 시료는 북제주군 함덕에서 SCUBA를 통하여 채집하였으며, 실험실로 옮긴 뒤, 크기 및 생식소에 대한 분석을 수행하였다. 구멍연잎성게의 크기는 각장 80$\~$200mm 이었으며, 각장 140$\~$170mm 의 개체가 주를 이루었다 (N=129). 구멍연잎성게는 세립질 또는 미립질 ($125\~250\mu$m ($2\~3\phi$))의 사질에 주로 분포하였으며, 퇴적물내의 유기물을 섭취하는 퇴적물식자로 확인되었다. 성숙한 암컷의 생식소는 보라색을 띠며, 수컷은 짙은 노란색을 띤다. 암, 수 모두 11$\~$3월 사이 휴지기를 거쳐 6월경에 성숙하며, 주 방란 방정은 7$\~$10월 사이에 이루어진 것으로 추정된다. 암컷의 경우 성숙한 난은 그 직경이 평균 381$\mu$m이었다.

• 한국지형학회지
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• 제23권1호
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• pp.17-33
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• 2016

Samples from newly exposed outcrop of sedimentary layers forming Jeongdongjin coastal terrace in Gangreung area are collected and analyzed to find the sedimentary environment. The site are located at the gentle hillslope of the terrace surface area. The height of the outcrop is about 8m and the altitude of it's highest part is 68~73m MSL. The lowest part of this out crop is the partly consolidated sand layer with gravel veneer within it. It is found that this part is not in-situ weathered sand stone through the OSL method. This sand layer is overlain by the gravel layer with sand matrix. The shapes of the gravels from this part are mainly 'platy', 'elongated', and 'bladed' by the index of Sneed and Folk(1958). In addition, mean roundness is not so high. It is sceptical to regard this part as marine sediments which are continuously exposed to erosional processes. The boundary between the lowest sand layer and gravel layer showing the abrupt change in forming material without any mixture or transitional zone, so gravels are seemed to deposited after some degree of consolidation of the lowest sand layer. In addition, the hight of the boundary between layers are changed by the place, so the surface of the partly consolidated sand layer is not flat and has irregularity on topography when it buried by gravels. Main part of this out crop is the poorly sorted coarse gravel(22.4mm) with sand matrix($1.36{\phi}$) layer with at least 2m thick covering the relatively fine gravels discussed above. Over 20% of particles have 'very platy', 'very elongated' and 'very bladed' shape and only less than 5% of particles have 'compact' shape, So this particles are also very hard to be regard as marine gravels which are abraded by marine processes. It can be concluded that this gravel layer formed by fluvial processes rather than coastal processes base on the form of the clast and sedimentary structure. The gravel layer is covered by fine($3{\sim}4{\phi}$) material layers of psudo-gleization which showing inter-bedding of red and white layers. Chemical composition of matrix and other fine materials should be analyzed in further studies. It is attempted to fine the burial ages of the sediment using OSL method, but failed by the saturation. So it can be assumed that these sediments have be buried over 120ka.

• 한국지구과학회지
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• 제33권1호
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• pp.1-10
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• 2012

서해 경기만 조석사주에서 획득한 고해상도 탄성파 탐사자료와 해상시추코어 분석에 의하면 연구지역의 제 4기 후기에 형성된 퇴적층은 총 4개의 퇴적단위(상부층부터 Unit I에서 Unit IV)로 구성된다. 퇴적단위 I은 조간대 및 조수로-충진 퇴적체로서, 홀로세 고해수면 시기동안 퇴적된 것으로 해석된다. 퇴적단위 II는 천해 퇴적상이 나타나는 외해역과 하천과 연계된 하성 퇴적상이 나타나는 조간대에서 조석사주 근접부로 나누어진다. 퇴적단위 III은 조석작용에 의한 조간대 퇴적환경 및 상부의 풍화된 퇴적층으로 각각 구분되며, 퇴적층은 산소동위원소 시기5동안 퇴적된 것으로 판단된다. 퇴적단위 IV는 조석사주 퇴적층의 최하부층으로 중생대 기반암 또는 산소동위원소 시기 5 이전에 퇴적된 층으로 해석된다.

• ALGAE
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• 제37권4호
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• pp.293-299
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• 2022

To examine the effects of substratum types on the growth of Caulerpa okamurae, sand surface and sand burial experiments were conducted. Five assimilators (erect fronds) per replicate were cultured for 15 d on the surface of three different treatments: fine sand (200 ㎛), coarse sand (600 ㎛), and no sand (control). Also, three stolons and three assimilators were buried by fine grain or coarse grain sands and incubated for 15 d. In both experiments, other culture conditions included 25℃, 30 μmol photons m^-2 s^-1, and 16 : 8 h L : D (light : dark). In both experiments, stolon + assimilator-, assimilator-, and stolon-weights were measured. Relative growth rates (RGRs) of stolon + assimilator weights ranged from 0.43 to 1.95% d^-1 at no sand and fine sand treatment, respectively. RGRs for the weight of stolon + assimilator and new assimilators were significantly greater on the fine- and coarse sand surface than the control. In the burial experiments, RGRs of stolons (4.28% d^-1 at coarse sand and 5.57% d^-1 at fine sand, respectively) were significantly greater than those of assimilators (1.38% d^-1 at fine sand and 1.82% d^-1 at coarse sand, respectively). When stolons were buried, RGRs for assimilators were greater at the fine sand than at the coarse sand treatment. On the other hand, RGRs of buried assimilators for total frond weights and for newly produced stolons were significantly greater at the coarse sands than at the fine sands. In conclusion, C. okamurae grew well with all substrates of sands and showed better growth on fine sands than coarse ones. This result suggests that the growth of stolons and assimilators of C. okamurae is stimulated after stable attachment to the sand substrates by rhizophores. In addition, stolons showed higher growth rates than the assimilators in the sand burial states, indicating that stolons are more tolerant to low light than assimilators of C. okamurae.

• 한국수산과학회지
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• 제41권3호
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• pp.170-175
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• 2008

We made sand-lance meat paste containing 0.1-0.5% propolis to improve the quality of the product. The quality characteristics were analyzed by the acid value, peroxide value, volatile basic nitrogen, pH, viable cell count, and sensory evaluation. The fried sand-lance meat paste made with added propolis had a lower acid value, peroxide value, and volatile basic nitrogen content after frying compared to the control prepared with potassium sorbate. The antioxidant and antispoiling effect of propolis on the fried fish meat paste increased with the amount of propolis added. The fried sand-lance meat paste made with 0.2% added propolis was very acceptable. In addition, the bitter taste of the sand-lance meat paste containing 0.2% propolis was blocked by adding 2% sweet amber powder to the paste.

• 한국해양생명과학회지
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• 제3권1호
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• pp.38-43
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• 2018

대형저서동물에서 우점하고 있는 갯지렁이류는 퇴적층의 유기물 섭취를 통하여 저질환경개선에 중요한 역할을 한다. 본 연구에서는 최근 양식기술이 개발된 바위털갯지렁이를 이용하여 갯벌 퇴적층의 유기물 제거효과를 검토하였다. 이를 위하여 입자특성이 다른 세종류의 저질환경(S1: 강사질, S2: 해사질, S3: 니사질)에서 해수 및 퇴적층의 TOC를 측정하였다. 바위털갯지렁이는 세종류의 입자특성에서 모두 유기물 제거효과를 나타내었으며, 입자가 클수록 제거율이 높았다. 유기물 정화능력을 정량적으로 평가한 결과 바위털갯지렁이는 각 저질별로 강사질에서 3.9856 ppm g^-1d^-1, 해사질에서 2.8021 ppm g^-1d^-1, 그리고 니사질에서 28.1142 ppm g^-1d^-1의 제거능력을 나타내었다. 본 연구결과는 바위털갯지렁이가 다양한 저질에서 유기물 제거에 기여하고 있음을 보여 주었다.

• 한국해양학회지
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• 제10권1호
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• pp.1-6
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• 1975

A marine geological investigation of the glass sand deposit in the beach along the west coast of Ahnmyeon Island, South Chung Cheong Province, Korea was carried out to solve the problen of sand material migration, textural properties of the sands and the glass sand reserve for future exploitation. Several bos coring analyses by means of the internal sedimentary structure.i.e., cross- stratification show significantly that most sands are moving and accumulation along the mean vector direction of $N20^{\circ}E-N60^{\circ}$ E in the area investigated. The average mean size of the sand sediments in the area studied ranges from 0.212mm to 0.275mm. The mechanism of sand migration in the area is considered to be interplay between longshore drift and flood tidal current. The sorting value of the sands ranges from 0.24 to 0.50. Therefore, these sand sediments are characteristic to be "well sorted". The average chemical composition of the glass sand in the area is the following: $SiO\_2$:-90.8%, $Al_2O_3$: -2.18%, $Fe_2O_3$:-0.73%, CaO:-1.79. The binocular microscope examination of the sands show that most of the sands are characteristically ice- clear quartz in mineral composition and their count percentage is mostly 92% or 96%.

• Geomechanics and Engineering
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• 제19권4호
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• pp.343-352
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• 2019

For quality control and the economical design of grouted sand, the prior establishment of the unconfined compressive strength (UCS) estimating formula is very important. This study aims to develop an empirical UCS estimating formula for grouted sand based on the physical properties of sands and the UCS of cured pure grout. Four sands with varying particle sizes were grouted with both microfine cement and Ordinary Portland cement. Grouted specimens were prepared at three different relative densities and at three different water-to-cement ratios, and unconfined compression tests were performed. The results demonstrate that UCS of grouted sand can be expressed as the power function of the UCS of cured pure grout: $UCS_{grouted\;sand}/1MPa=A_{soil}{\cdot}(UCS_{pure}/1MPa)^N$. Because the exponent N strongly depends on the combination of pore area and pore size, N is expressed as the function of porosity (n) and specific surface ($S_a$). Additionally, because $S_a$ determines the area of the sand particle that cement particles can adsorb and n determines the number of cementation bondings between sand particles, $A_{soil}$ is also expressed as the function of n and $S_a$. Finally, the direct relationship between $A_{soil}$ and N is also investigated.