• Ocean and Polar Research
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• 제36권4호
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• pp.373-381
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• 2014

Korea contract Mn-nodule field in the NE equatorial Pacific is composed of seven sectors with average water depths of 4,513-5,025 m. Of the various factors controlling the properties of Mn-nodule, it seems that water depth is likely connected to the chemical composition and occurrence of nodules. To test whether such an assumption held in each sector, we reviewed previous research data accumulated since 1994 for one of the northern sectors (hereafter KR1) where there are stark contrasts in water depth. High-resolution seabed mapping clearly separates a northern part (KR1N) from a deeper southern part (KR1S), cutting across in the middle of the KR1. In addition, significant volcanic activities forming numerous seamounts are distinctive especially in KR1N. In terms of nodule occurrence, manganese nodules in KR1S are comparatively larger (2-4 cm) with a discoidal shape, while those in KR1N are generally small (<2 cm) with poly-lobate and irregular shapes. Nodules in KR1N also have lower Co, Cu, Mn and Ni, and higher Fe contents. The spatial separation in nodule characteristics might be caused by volcanic activities in KR1N rather than water depth contrast. During the formation of the seamounts in KR1N, rock fragments and volcanic ashes as new nuclei of the nodules would have been continuously generated. As a result, the nodules could not grow larger than 2 cm and display the shapes of a newbie (i.e., irregular and poly-lobate shapes). Moreover, significant Fe supply from volcanic activities probably decreases the Mn/Fe ratio, which may lead to the KR1 nodules being misinterpreted as a hydrogenic in origin compared to other sectors where a high Mn/Fe ratio is present.

• 한국해양환경ㆍ에너지학회지
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• 제18권3호
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• pp.143-156
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• 2015

서태평양에 위치한 해저산 해역($150.2^{\circ}E$, $20^{\circ}N$ 부근)에서 수층 환경의 동적 특성을 파악하고자 수괴 및 용존산소, 무기영양염(질소, 인), 엽록소-a 등과 같은 수층 환경 인자의 거동을 살펴보았다. 2014년 10월에 해저산(OSM14-2)을 중심으로 동-서 및 남-북 방향으로 총 9개의 정점에서 CTD system을 이용하여 물리 화학적 자료를 획득하였다. 수온-염분 도표로부터 연구 해역에서 파악된 수괴는 표층에서 북태평양 열대수와 수온약층수, 중층에서 북태평양 중층수 그리고 저층에서 북태평양 심층수로 구분되었다. 용존산소 농도가 낮은 최소층(평균 $73.26{\mu}M$)은 산소 결핍 환경(dysoxic<$90{\mu}M$)으로 연구 해역 전반에 걸쳐 수심 700~1,200 m 사이에 분포하였다. 아질산염+질산염과 인산염으로 대표되는 무기영양염은 표면혼합층 내에서 빈영양 환경을 보인 후 수심 증가에 따라 점차적으로 증가해 용존산소 최소층에서 최대 농도를 나타냈으며, N:P ratio(13.7) 결과로부터 연구 해역은 식물플랑크톤이 성장하기에 질소 성분이 제한된 환경으로 파악되었다. 해저산을 중심으로 동-서 및 남-북 정점 라인에서 환경 인자의 수직 분포는 서쪽과 남쪽 해역에서 저층수 유입에 의한 영향으로 수심 500 m 부근에서 그리고 수심 2,500 m 이하의 저층 내에서도 서쪽 해역과 남쪽 해역에서 반대 해역과 비교해 환경 인자의 농도가 다르게 분포하였다. Redfield ratio(N:P=16:1)을 이용하여 구해진 Excess N 값은 연구 해역 전반에 걸쳐 음의 값을 보여 질소 제거 기작이 우세한 환경임을 나타냈으며, 서쪽 해역과 남쪽 해역 저층에서 상대적으로 높은 값이 관측되었다. 이러한 결과들은 해저산의 지형적인 특성이 저층 해류 순환에 영향을 미치고 이는 수층 환경 인자들의 거동을 결정하는데 중요하게 작용함을 지시한다.

• 생명과학회지
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• 제18권3호
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• pp.329-335
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• 2008

해양성 심층수(KDSW)는 해양심층수(DSW)와 유사한 mineral 조성을 가지고 있어 식품 및 의약분야에서 그 유용성에 대한 관심이 증대되고 있다. 본 연구에서는 KDSW 및 탈염한 Danasoo의 항산화력, 면역활성, 함암 및 당뇨에 대한 효과를 연구하였다. KDSW와 Danasoo의 항산화 활성은 DPPH radical scavenging 활성, SOD-like 활성 및 PCL 법에 의하여 항산화 활성을 조사하였다. KDSW와 Danasoo의 항산화 활성은 첨가된 농도에 의존적으로 증가하였으며, 특히 PCL법에 의한 KDSW와 Danasoo의 항산화능은 85.32과 14.02(nmol of ascorbic acid equivalent/ml)로 높은 항산화 활성을 나타내었다. Macrophage RAW 264.7 cell에서 LPS에 의하여 유도된 NO 활성은 Danasoo (20%)를 첨가에 의하여 약 30%정도의 NO 합성이 저해되었으며, 이 농도에서 세포 독성이 없는 것으로 MTT assay에 의하여 확인하였다. NO는 nitric oxide synthase에 의하여 합성되며, tumor성장 및 angiogenesis에서 중요한 역할을 하는 것으로 밝혀져 있으며, Danasoon (20%)는 위암세포와 폐암세포의 iNOS 발현을 현저히 감소시켰다. STZ에 의하여 유도된 당뇨 쥐의 혈당량은 Danasoo (20%) 식이에 의하여 대조구와 유사한 당뇨효과를 나타내었다. 이러한 결과들은 KDSW가 우수한 biological 활성을 가지고 있으며, 또한 천연 기능성 제품생산을 위한 소재로 사용될 수 있는 높은 가능성올 시사하고 있다.

• Journal of Applied Biological Chemistry
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• 제59권3호
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• pp.233-237
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• 2016

Deep sea water (DSW) contains many inorganic materials and minerals, which are extracted for use in diverse fields. However, before application, safety tests should be performed. In the present study, two DSW-extracted minerals were analyzed: calcium (Ca) and magnesium (Mg). Eye and skin irritation tests of DSW-extracted Ca and Mg were performed according to the guidelines of the Ministry of Food and Drug Safety of Korea. These two types of mineral extracts caused no symptoms of eye and skin irritation when compared to the control. These results suggest that DSW-extracted minerals caused no irritation in the eyes and on the skin, and could be safely applied to these areas.

• 한국자기공명학회논문지
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• 제22권4호
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• pp.82-90
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• 2018

The term "hangover" refers to symptoms such as headache, heartburn, nausea, and dizziness caused by acetaldehyde created through alcohol decomposition in the body after alcohol intake. Many scientists have conducted research on diverse drugs, foods, and medicinal herbs aimed at eliminating hangovers. However, research on metabolism to objectively verify or measure their effects on hangover symptoms has been lacking. Accordingly, in this study, deep sea water minerals were administered orally at varying concentrations to rats that consumed alcohol, and changes in the levels of amino acids in their bodies were measured using nuclear magnetic resonance spectroscopy to gauge the minerals' effects on hangover symptoms. Thus far, biochemical research on hangover cures has been confined to basic research measuring changes in the levels of alcohol dehydrogenase and acetaldehyde dehydrogenase as well as in the concentrations of ethanol, acetaldehyde, and acetate using spectroscopes such as enzyme-linked immunosorbent assay kits or gas chromatography-mass spectrometers. In comparison, this study presents pharmacokinetic research that simultaneously tracked biomaterials including amino acids and organic acids, metabolites associated with hangover, to clarify hangover mechanisms more specifically. In addition, this study examined hangover mechanisms without an external supply of tracked materials not overlapping with alcohol metabolism-related materials, such as external amino acids and sugars.

• 한국해양공학회지
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• 제21권4호
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• pp.61-65
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• 2007

In this research, we have developed a manufacturing process for seawater salt by horizontal spray drying technique using the deep ocean water and seaweed(sea tangle). Deep ocean water, strong acidic electrolyzed water and strong alkaline electrolyzed water were used as extraction solvent of seaweed. Sodium content in seaweed extract solution by strong alkaline electrolyzed water was 1.63(mg/g), which was 3.5 times lower than of seaweed extract by strong acidic electrolyzed water. Major mineral content(Na, K, Ca) in seawater salt by deep ocean water were higher than strong acidic electrolyzed water and strong alkaline electrolyzed water. On the contrary, Mg contents in seawater salt by deep ocean water were lower than strong acidic electrolyzed water and strong alkaline electrolyzed water. Based on the results of seawater salt production using seaweed, it is possible to make law-salt efficiently.

• Ocean and Polar Research
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• 제36권4호
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• pp.395-405
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• 2014

A 570 cm-long sediment core was retrieved at $9^{\circ}57^{\prime}N$ and $131^{\circ}42^{\prime}W$ in 5,080 m water depth from the northeast equatorial Pacific and its stratigraphy was established with $^{10}Be/^9Be$ and paleomagnetic measurements. Successive AF demagnetization reveals eight geomagnetic field reversals. In the reference geologic time scale, the eight reversal events correspond to an age of about 4.5 Ma. However, $^{10}Be/^9Be$-based age yields 9.5 Ma at a depth of 372 cm. Such a large discrepancy in determined ages is attributed to an extremely low sedimentation rate, 0.4 mm/kyr on average, of the study core and resultant loss or smoothing of geomagnetic fields. The composite age model reveals a wide range in the sedimentation rate - varying from 0.1 to 2.4 mm/kyr. However, the sedimentation rate shows systematic variation depending on sedimentary facies (Unit II and III), which suggests that each lithologic unit has a unique provenance and transport mechanism. At depths of 110-80 cm with a sedimentation rate of about 0.1 mm/kyr, ancient geomagnetic field reversal events of at least a 1.8 Myr time span have not been recorded, which indicates the probable existence of a hiatus in the interval. Such a sedimentary hiatus is observed widely in the deep-sea sediments of the NE equatorial Pacific.

• Ocean and Polar Research
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• 제36권4호
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• pp.407-421
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• 2014

The benthic environmental impact experiment addresses environmental impacts at a specific site related to deep-sea mineral resource development. We have acquired several tens of multi- or box core samples at 31 sites within the Benthic environmental Impact Site (BIS) since 2010, aiming to examine the basic properties of surficial deep-sea sediment as a potential source for deep-water plumes. In this study, we present the geochemical properties such as major elements, rare earth elements (REEs), and heavy metal contents at the BIS. Such proxies vary distinctly according to the Facies association. The lithology of all core sediments in the BIS corresponds to both Association Ib and Association IIIb. The vertical profiles of some major elements ($SiO_2$, $Fe_2O_3$, CaO, $P_2O_5$, MgO, MnO) show noticeable differences between Association Ib and IIIb, while others ($Al_2O_3$, $TiO_2$, $Na_2O$, and $K_2O$) do not vary between Association Ib and IIIb. REEs are also distinctly different for Associations Ib and IIIb; in Association Ib, REY and HREE/LREE are uniform through the sediment section, while they increase downward in Association IIIb like the major elements; below a depth of 8 cm, REY is over 500 ppm. The metal enrichment factor (EF) evaluates the anthropogenic influences of some metals (Cu, Ni, Pb, Zn, and Cd) in marine sediments. In both Associations, the EF for Cu is over 1.5, the EF for Ni and Pb ranges from 0.5 to 1.5, and the EF for Zn and Cd are less than 0.5, indicating Cu is enriched but Zn and Cd are relatively depleted in the BIS. The vertical variations of geochemical properties between Association Ib and IIIb are shown to be clearly different, which seems to be related to the global climate changes such as the shift of Intertropical convergence zone (ITCZ).

• 한국식품저장유통학회지
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• 제20권5호
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• pp.636-642
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• 2013

해양 암반 심층수의 두부 응고제로서 활용 가능성을 확인하기 위하여 시판 두부 응고제 3종($MgCl_2$, $CaSO_4$ 및 glucono-${\delta}$-lactone)으로 제조한 두부와 농축하여 8 $^{\circ}Brix$로 농도 조절한 해양 암반 심층수를 두유 L당 20, 25 및 30g씩(SW-20, 25, 30) 첨가하여 제조한 두부의 품질특성을 분석하였다. 두부의 제조 수율은 SW-30에서 유의적으로 높았으며, 순물의 탁도는 해양 암반 심층수를 응고제로 사용한 실험군에서 유의적으로 높았다. 두부의 수분은 72.72~74.86%, pH는 6.09~7.01이었는데, glucono-${\delta}$-lactone을 응고제로 사용한 두부에서 유의적으로 낮았으며, 여타 시료간에는 유의차가 없었다. 두부의 무기물 함량은 응고제에 함유되어 있는 무기물의 영향을 많이 받아 응고제의 주요 무기물이 두부에서도 다량 검출되었으나, 25 mg/kg 미만의 미량 무기질은 응고제의 영향이 적었다. 두부의 명도와 황색도는 해양 암반 심층수로 응고한 실험군간에는 유의차가 없었다. 두부의 물성 중 경도는 시판 응고제를 사용한 두부에 비해 해양 암반 심층수를 사용한 두부에서 유의적으로 낮았다. 관능평가 결과 두부의 응고제는 질감과 맛에 영향을 미쳤는데, 경도가 낮거나 높을 경우 질감에 대한 기호도도 감소하였으며, 응고제로부터 유래한 쓴맛이나 신맛도 관능적 특성을 크게 저해하였다. 이상의 결과를 종합하여 볼 때 해양 암반 심층수는 두부의 이화학적 특성에 있어 시판 응고제로 제조한 두부와 유사한 특성을 나타내었으며, 관능적 특성은 오히려 우수하여 두부 응고제로 활용 가능성이 충분하였다.

• 대한의생명과학회지
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• 제11권3호
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• pp.275-279
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• 2005

High-salted mineral water (Daehan Deep Water, Korea) that is pumped up from below the sedimentary rock layer of Dadaepo, Busan, Korea has a composition similar with that of deep sea water. Under the well-being boom, the mineral water is processed for various uses including washing or oral administration. However, high concentrations of various minerals in the mineral water are suspected to affect on the physiology of human body, especially on blood pressure (BP). Here, we examined the effect of Hot Mineral(R), dried powder of the mineral water, on the change of BP. Sprague­Dawley rats were grouped and orally administered $2.5\%$ Hot Mineral(R) (group M), $2.5\%$ NaCl (group S) or normal water (group C). Excreted urine was collected in metabolic cage for 24 hours. The systolic blood pressure (SBP) of the group S was remarkably increased (P<0.005) compared with that of the group M and the group C, which showed little changes of the SBP during 2 weeks. While average daily sodium intake were 0.32 mg in the group C, 6.64 mg in the group M and 4.07 mg in the group S, average daily sodium excretion were 11.37 mg, 53.70 mg and 7.75 mg, respectively. These results indicate that the sodium excretion in the group M was much higher than the other two groups. In this study, we suppose that the plenty amount of minerals such as calcium, potassium and magnesium in Hot Mineral? have an effect not to increase the SBP and to prompt sodium excretion out of the body. Therefore, these results suggest that oral administration of appropriate amount of Hot Mineral(R) for limited period does not induce increased SBP.