• 환경영향평가
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• 제16권1호
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• pp.69-77
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• 2007

This study has been conducted to assess blackish-water phenomena in Dam reservoir. To searching for the reason, we survey physical changes in reservoir and analyze metal and organic content in particulate materials and water. The blackish-water phenomena in lake A are occurred with turbidity increases in turnover season irregularly. It was reported on 6 Jan. 2005 weakly and the water column mixed with 35~40m depth and water temperature shows $7^{\circ}C$. The turbidity of AD and AM site increased up to 20NTU. Especially, AN site shows 27NTU, such a result makes that Dam manager conclude it to blackish-water phenomena. The results of sequential extraction analysis show that over 80% of Al, Cr and Fe is existed in residual form in sediment. On the other hand, the most part of Mn shows exchangeable and carbonates form, which have a good possibility of release to water column. Mn contents in pore waters of the sediment samples are also found to be ~4 times higher than Fe contents. The metal contents in pore water of different dam sites are in order of AN (Fe: 9.98, Mn: 40.6) > AD(8.33, 37.5) > DD(1.91, 2.55). According to the results of extracted organic materials from sediment, humic substances is occupied with over 85% in total organic carbon including 23~45% of humic acid (HA) and 0.9~8.5% of fulvic acid (FA). However, HA content in pore water is not detectable while FA contents, acid-soluble humic fractions is higher than that of sediment(10~15%). which indicating that FA is a main humic components affecting water color. The color unit per DOC of FA in pore waters of different dam sites are found to be higher in lake A than lake D. From the results, it could be suggested that blackish-water phenomena of lake A are mainly arise from higher concentration of Mn and water soluble organic fractions (e.g., FA) released from sediments as well as the strength of turnover in Dam reservoir.

• Corrosion Science and Technology
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• 제7권6호
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• pp.328-331
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• 2008

Corrosion behaviour of water intake gate steel structures with different protective measures was investigated. Five material alternatives were taken for investigation, including: imported and recycled stainless steel, carbon steel with hot zinc spraying, painting and composite coatings. Results of corrosion rate for carbon steel, SUS 304, hot zinc spray coats in three water systems of Mekong river basin (saline, blackish and fresh) were also presented. Corrosion rate of carbon steel decreased with decreasing salinity in the investigated water environments. Meanwhile, these values for zinc coated steel, behaved by another way. Environmental data for these systems were filed and discussed in relation with corrosion characteristics. Method of Life Cycle Assessment (LCA) was applied in materials selection for water intake gate construction. From point of Life Cycle Cost (LCA) the following ranking was obtained: Zinc sprayed steel < Recycled stainless steel < Composite coated steel < Painting steel < SUS 304 From investigated results, hot zinc spray coating has been applied as protective measure for steel structures of water intake systems in Mekong river basin.

• 동굴
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• 제89호
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• pp.16-23
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• 2008

In the cave, there are three kinds of CO2 gas from the human body and humidity or H2O from the underground water and also light from illumination fixture creating plants by photosynthesis. For this reason, the green plants of moss created and lived on the rock in the cave, but sometimes there would be the dry season to be killed the green mosses and hence, it could be dried and blackish. When the dried mosses were taken off from the surface of the rock like as laminated dried one, the moss lamination could be taken off together with the skin of the formated stalactite in the cave. Therefore, cave environment should be changed and degenerated. So it is useful and necessary to get selective wave lighting to have photosynthesis in the cave or not to have it in there by using of the LED lamps.

• 생태와환경
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• 제46권4호
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• pp.499-506
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• 2013

해수와 담수가 공존하는 시화호 상류 기수역에서 입자성유기물에 대한 조류의 영향을 평가하기 위하여, 2005년과 2006년 3월부터 11월까지 기수역내 7개 지점을 대상으로 입자성유기탄소 (particulate organic carbon; POC), 식물플랑크톤 색소(chlorophyll a; Chl-a), pheophytin a; Pheo-a)의 시공간적 변동과 상관관계를 분석하였다. 조사기간 동안 POC 농도는 $1.0{\sim}76.6mgL^{-1}$ (평균 $7.4mgL^{-1}$)의 범위로 봄에 높은 계절변화를 보였으며, 염분성층이 강하고 고탁도층이 형성되는 중류부에서 높은 값을 보였다. 살아있는 식물플랑크톤의 현존량의 지표로 이용되는 Chl-a 농도는 $1.3{\sim}942.9{\mu}gL^{-1}$ (평균 $71.0{\mu}gL^{-1}$) 범위로 매우 높은 값을 보였고, 4월에 중류부에 최고치를 보여 POC와 유사한 변동을 보였다. 한편 Pheo-a 농도는 $1.4{\sim}1,545.5{\mu}gL^{-1}$ (평균 $59.9{\mu}gL^{-1}$)의 범위로, total Chl-a의 평균 44.2%로 죽거나 활성을 잃은 식물플랑크톤의 양이 많은 것으로 나타났다. POC 농도는 식물플랑크톤 색소와 강한 양의 상관(Chl-a (r=0.93), total Chl-a (r=0.88), >Pheo-a (r=0.81))을 보였는데, 이는 시화호 기수역에서 식물플랑크톤이 POC의 중요한 기원임을 시사한다. 한편 식물플랑크톤 색소와 POC와의 회귀식으로부터 POC/Chl-a 비(82.9)보다 POC/total Chl-a 비(35.9)가 하구에서 조사된 POC/Chl-a 비(40~60)에 더 유사한 것으로 나타났다. 그러므로 시화호 기수역과 같이 Pheo-a 농도가 높은 수역에서는 조류기원성 POC를 산정하거나 또는 수체의 POC 농도에 대한 식물플랑크톤의 기여도를 평가할 때 Chl-a 농도와 함께 Pheo-a 농도도 함께 고려할 필요가 있다.

• 한국어류학회지
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• 제24권3호
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• pp.230-233
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• 2012

과거 우리나라 남해에 출현하는 것으로 알려졌던 농어목 새다래과의 한국미기록종 흰꼬리타락치(Taractichthys steindachneri)에 대해 제주도를 포함한 남해에서 채집된 2개체(표준체장 224.7~406.5 mm)의 표본을 근거로 형태적 특징을 상세히 기재하였다. 본 종은 양측 배지느러미가 서로 멀리 떨어져 위치하는 점, 미병부 배측에 반월상의 홈이 있는 점, 등지느러미와 뒷지느러미가 길게 신장하는 점, 그리고 체색이 전체적으로 검고 꼬리지느러미 후연이 백색인 점이 특징이다.

• 한국환경과학회지
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• 제24권2호
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• pp.261-266
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• 2015

We have analyzed the external morphology and the environment of the foraging site of Vespertilio sinensis. The external morphology was analyzed by twelve parameters and the environment characteristics of the foraging site was analyzed using GIS 10.1 program. The wing membrane was inserted into the ankle of the hind foot and the wing ratio was 1.42, the middle type between broad-short wing type and long-narrow wing type. The fur color was blackish brown but the guard hair color was whitish. The shape of the ear was a rounded triangle and tragus was a fan shape. This study showed that V. sinensis preferred the deciduous forest of the upper forest zone, where human interference was less. We believed that abundance of insects, depending on water system, was closely related to the use of the foraging site. This result showed that the environment characteristics was very similar to the nature preservation zone including Baekyang valley and Keumsun valley in Naejangsan National Park.

• Nutrition Research and Practice
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• 제12권5호
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• pp.365-370
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• 2018

BACKGROUND/OBJECTIVES Oxidative stress is a major cause of cancer. This study investigated the effects of the ethanol extracts from germinated and non-germinated Keunnunjami rice, a blackish-purple pigmented cultivar with giant embryo, on selected human cancer cell lines and on the antioxidant defense system of mice fed with a high-fat diet. MATERIALS/METHODS: High fat-fed mice were orally administered with either distilled water (HF) or extracts (0.25%, w/w) from brown (B), germinated brown (GB), Keunnunjami (K), and germinated Keunnunjami (GK) rice. RESULTS: In comparison with the brown rice extract, Keunnunjami extract showed higher anticancer effect against cervical and gastric cell lines but lower anticancer activity on liver and colon cancer cells. Mice from the HF group showed significantly higher lipid peroxidation and lower antioxidant enzyme activities than the control group. However, the oxidative stress induced by high-fat diet markedly decreased in B, GB, K, and GK groups as compared with the HF group. CONCLUSIONS: Germination may be an effective method for improving the anticancer and antioxidative properties of Keunnunjami rice and extracts from germinated Keunnunjami rice may serve as a therapeutic agent against cervical and gastric cancers and oxidative damage.

• Nutritional Sciences
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• 제9권3호
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• pp.190-194
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• 2006

Silajit is a blackish brown pitch-like gummy substance. It is an important Unani and Ayurvedic medicine widely used in the treatment of many diseases and as nutritional supplement It is found in certain mountainous regions of Pakistan, Afghanistan, India, Nepal, Australia and Russia. Silajit samples of Pakistani origin were obtained from different sources and analyzed for their physical characteristics and biochemical & elemental composition. X-ray diffraction studies on Silajit showed that it is an amorphous substance and has no crystalline structure. Also, pH studies of Silajit (2 g/L of water) indicated that it was slightly acidic in nature and ranged from 3.45 to 7.23. Conductivity ranged from 157.7 to 330. Amino acid analysis revealed that Silajit contained lysine and alanine in higher amounts than all other amino acids and ranged from 1456 to 2240 and 68 to $1615{\eta}mole/g$, respectively. Mean concentration of arsenic, mercury, cadmium, lead, copper and zinc was 73.15, 104.92, 0.496, 3.89, 4.04 and 17.23 ppm, respectively. Silajit samples were also analyzed for calcium, potassium and sodium.

• 자원환경지질
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• 제9권4호
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• pp.225-240
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• 1976

This study deals with the flow of bed rock ground water of Banyaweol Formation, which is presently cleared up as a laminar flow. The result obtained may be summarized as the following. 1) The Banyaweol Formation consists mainly of thin-bedded, green to blackish green shale, mudstone, and marl. The marl and mudstone alternatively occur with shale. The marl and mudstone form a aquifer of Banyaweol Formation. In this study, a group of aquifer is in convenience named as a aquifer zone. The aquifer occurs in lenticular form. The aquifer seems to be a type of artesian aquifer because it is covered with aquicludes, but it actually forms a unconfined aquifer because its piezometric surface stays under the lower aquiclude. The lowering of piezometric level is formed because of leakage of the ground water to the lower aquifer undersaturated. 2) The coefficient of permeability of Banyaweol Formation's ground water body (K) is derived by using Dupuit's equation as the following ${\log}K=\frac{CK^2-dK+f}{aK-b}\;\(M=1.365(2H-s)s\\M={\log}1.956s{\sqrt{H}}r\)$ here, $$a=\sum_{1}M_iG_i$$ $$b={\frac{1}{2}log{\sum_{i}}Q_i{^2}$$ $$c=2{\sum_{i}}M_i{^2}$$ $$d=loge{\sum_{i}}M_{i}Q_{i}+2{{\sum_{i}}N_{i}Q_{i}$$ $$f=loge{\sum_{i}}Q_i{^2}N_i$$ If the measured values substituted for the above equation, the coefficient of permeability of the aquifer is 4.1m/day. The coefficient of storge of the aquifer is $2.8{\times}10^{-4}$ if the measured values substituted for Theis's equation. Using the above constants, the filtration velocity of the aquifer is $2.1{\times}1O^{-1}m/day$and the daily flow quantity of the ground water is $847.38m^{3}/day$. 3) In order to understand the time necessary for a circulation of ground water body, the contents of tritum contained in the ground water are measured as 2.3 T.U. at the Korea Atomic Energy Research Institute. Before 1952, the average concentration of tritium per year in groundwater was reported as 10T. u., taking it as the standard, the groundwater of the present study 26.25 years old. Therofore, the groundwater of the Banyaweol Formation is judged as an relatively old groundwater. It is characteristic that the ground water of Banyawol Formation is laminar flow as well as unconfined aquifer and ground water flow of relatively long time. 4) The nature, means of flow, and circulation of Banyaweol Formation's ground water body make it possible set up this ground water body as a ground water system.

• 한국어류학회지
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• 제7권2호
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• pp.114-119
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• 1995

1994년(年) 7월(月) 6일(日) 제주도(濟州道) 한림(翰林)에서 채집(採集)된 양태과(科)의 점양태속(屬) 어류(魚類) 1개체를 조사(調査)한 결과(結果) 지금까지 우리나라에서는 보고(報告)된 적이 없는 Inegocia guttata (Cuvier)로 동정(同定)되었다. 본 종(種)은 형태적(形態的)으로 Cymbacephalus beauforti와 흡사(恰似)하나 측선(側線) 유공린수(有孔鱗數)는 측선린(側線鱗) 위쪽에 비스듬이 배열(配列)되어 있는 후하방(後下方) 종열린수(縱列鱗數)보다 매우 적으며 두부(頭部)에는 비극(鼻棘)이 있고 눈 위에 피판(皮瓣)이 없으며 간새개부의 피판(皮瓣)은 단일형(單一形)이고 가슴지느러미와 배지느러미에는 도형(圖形)의 검은 반점(斑點)이 존재(存在)하는 것 등의 특징(特徵)이 Cymbacephalus beauforti와 잘 구별(區別)되었다. 본(本) 종(種)의 한국명(韓國名)으로는 "악어양태" 라고 잠정적으로 명명(命名)하였다.