• 제목/요약/키워드: Mean grain size

검색결과 313건 처리시간 0.027초

1998년 하계 여자만의 저질환경 특성 (Characteristics of the Sedimentary Environment in Yoja Bay in the Summer of 1998)

  • 허회권;김도현;안승환;박경원
    • 환경생물
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    • 제18권2호
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    • pp.227-235
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    • 2000
  • As a part of basic investigation to Fishery Purge Project for the Special Administrative in Chollanamdo Province, the sedimentary environmental characteristics of Yoja Bay at 15 stations were studied. The analysis was carried out in July, 1998, through studies of Loss On Ignition (LOI) by depth, Total Sulfide (T-5), Chemical Oxygen Demand (COD) concentrations and Grain-size distribution. The LOI value was found to be 6.20-12.20% (mean of 8.89%), with the neighboring Sunhakri and Haksanri areas showing slightly higher values. These values were similar to the LOI values observed in the Hansan-Koje Bay and Jinju Bay areas on the southern coast of Korea. T-S and COD concentrations were found to be, respectively, 0.060-0.104 mg/gㆍd (mean of 0.052 mg/gㆍd) and 5.53-29.71 mg/gㆍd(mean of 13.24 mg/gㆍd), not exceeding eutrophication limits. T-S concentration was especially high at stations close to the central areas of the bay and inland areas, which caused by organic matter input from the nearby agricultural areas. COD concentration was very high at stations nearby the bay entrance and Doonbyungdo, but the mean value was lower than that of Hansan-Koje Bay. This leads us to believe that the level of pollution in Yoja Bay is not significant. The prevailing sediment composition was mud, consisting of 61.38% silt and 34.87% clay. [Sediments in Yoja Bay, Loss On Ignition, Total Sulfide, Chemical Oxygen Demand, Grain-Size Distribution].

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화순천의 퇴적환경 및 퇴적물과 하천수의 지구화학적 특성 (Sedimentary Environments, Geochemical Characteristics of Sediments and River waters, Hwasun-cheon)

  • 오강호;고영구;김주용;김해경
    • 한국환경과학회지
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    • 제11권9호
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    • pp.881-895
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    • 2002
  • Sediments and river waters form the channel of Hwasun-cheon were studied in sedimentological size and geochemical analyses of metallic elements for the purposes of identification of depositional environments and geochemical characteristics. The sizes of sediments are assigned to pebble to coarse sand in mean size and polymodal in distribution. And the sediments are poorly to very poorly sorted and positively skewed. According to the grain size distributions of the sediments, the Hwasun-cheon belongs to gravel-bed river on the basis of the grain size distribution of the sediments. The behaviors of metallic elements in the sediments mainly depend on not grain size distribution but the geology connected with geomorphological reliefs near the stream. Contamination indices(CI) of Zn, Cu and Pb are 2.83 to 6.96 with average 4.31 in the sediments. Hwasun-cheon is assigned to general stream type in accordance with water quality of physical factors and chemical characteristics by Piper's diagram. Though meaningful values of BOD, T-N, T-P were locally depicted near Masan-ri, Hwasun-eup and Jiseok-cheon areas, artificial metal concentration do not represent in the most area of the stream. Sediments and river water are considered that the relatively more or less high metallic contents in the stream are originated from coal mine and urban area.

가을철 독도 연안에 출현하는 대형저서동물의 종 조성 및 군집 구조 (Species Composition and Community Structure of Macrobenthos during Fall on the Dokdo Coast, Korea)

  • 강수민;이형곤;김상렬;최진우;박찬홍;유옥환
    • Ocean and Polar Research
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    • 제41권2호
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    • pp.47-61
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    • 2019
  • The Dokdo coast is known for its high biodiversity. However, few studies have examined the biodiversity and macrobenthic community on the subtidal soft-bottom. Therefore, we collected macrobenthos (> 1 mm) using a Smith-McIntyre grab ($0.1m^2$) at 15 stations along the Dokdo coast in September 2016. The sediments consisted of badly sorted (1.7) coarse sand with gravel and the mean sediment grain size was $-0.4{\phi}$. In total, 177 macrobenthic species were collected; their mean density was $1,566ind./m^2$. The number of species and density of macrobenthic fauna decreased significantly with the mean grain size. The dominant species were the amphipods Melita denticulata (16.5%) and Melita shimizui (5.5%), polychaete Salvatoria clavata (5.4%), bivalve Glycymeris aspersa (4.4%), and ophiuroid Ophionereis dubia (4.3%). The dominant macrobenthos species on the subtidal soft-bottom differed from the coastal areas of the East Sea, suggesting that the difference in the sediment grain size affected the macrobenthos. Cluster analysis was performed to divide the study area into four groups, and environmental factors which correlated with species composition and distribution in the study area were the combination of the four parameters of salinity, dissolved oxygen, total organic carbon and depth. A future seasonal investigation is needed to understand the species composition and characteristics of the Dokdo macrobenthos.

부유사 입경분포 모의를 위한 간편법 (A simple approach to simulate the size distribution of suspended sediment)

  • 권민혁;변지선;손민우
    • 한국수자원학회논문집
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    • 제57권5호
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    • pp.347-357
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    • 2024
  • 많은 연구에서 비점착성 부유사의 입경분포를 평균입경와 표준편차를 이용해 묘사한다. 그러나 부유사는 크기가 다른 많은 입자의 혼합물로 구성되어 있다. 난류조건에서 부유사의 이동은 크기와 밀도로부터 계산된 침강속도에 영향을 받는다. 따라서 비점착성 부유사의 이동을 이해하려면 입경 분포를 보다 정량적으로 고려하는 것이 중요하다. 본 연구의 목적은 난류조건에서 부유사의 입경분포를 모의할 수 있는 간편한 모형화 방법을 제시하는 것이다. 점착성 유사와 비점착성 유사의 차이에 대한 이해를 바탕으로, 점착성 부유사를 위한 추계학적 응집 모형을 비점착성 유사의 입경분포 모의에 적합하도록 수정하였다. 본 연구에서 제안하는 간편법의 적용성을 살펴보기 위해 선행연구의 실험자료에 적용하여 모의 결과와 비교하였다. 수치 모의의 결과를 통해 본 연구에서 제안한 모형이 실험값에서 나타나는 주요한 특성을 모사할 수 있다는 점을 확인하였다. 이를 바탕으로 유사 이동 모형을 사용하여 부유사 입경분포를 모의하는 접근 방식이 부유사 입경분포의 중요한 특성을 이해하기에 효과적이라는 결론을 얻었다.

Evaluation of translucency of monolithic zirconia and framework zirconia materials

  • Tuncel, Ilkin;Turp, Isil;Usumez, Aslihan
    • The Journal of Advanced Prosthodontics
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    • 제8권3호
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    • pp.181-186
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    • 2016
  • PURPOSE. The opacity of zirconia is an esthetic disadvantage that hinders achieving natural and shade-matched restorations. The aim of this study was to evaluate the translucency of non-colored and colored framework zirconia and monolithic zirconia. MATERIALS AND METHODS. The three groups tested were: non-colored framework zirconia, colored framework zirconia with the A3 shade according to Vita Classic Scale, and monolithic zirconia (n=5). The specimens were fabricated in the dimensions of $15{\times}12{\times}0.5mm$. A spectrophotometer was used to measure the contrast ratio, which is indicative of translucency. Three measurements were made to obtain the contrast ratios of the materials over a white background ($L^*w$) and a black background ($L^*b$). The data were analyzed using the one-way analysis of variance and Tukey HSD tests. One specimen from each group was chosen for scanning electron microscope analysis. The determined areas of the SEM images were divided by the number of grains in order to calculate the mean grain size. RESULTS. Statistically significant differences were observed among all groups (P<.05). Non-colored zirconia had the highest translucency with a contrast ratio of 0.75, while monolithic zirconia had the lowest translucency with a contrast ratio of 0.8. The mean grain sizes of the non-colored, colored, and monolithic zirconia were 233, 256, and 361 nm, respectively. CONCLUSION. The translucency of the zirconia was affected by the coloring procedure and the grain size. Although monolithic zirconia may not be the best esthetic material for the anterior region, it may serve as an alternative in the posterior region for the bilayered zirconia restorations.

낙동·고령 중권역의 표층 퇴적물 입도 조성 및 유기물질 분포 특성 변화 (The Distribution Characteristics of Grain Size and Organic Matters of Surface Sediments from the Nakdong-Goryeong Mid-watershed)

  • 김신;안정민;김형근;권헌각;김경훈;신동석;양득석
    • 한국환경과학회지
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    • 제27권6호
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    • pp.411-423
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    • 2018
  • To investigate the distribution characteristics of grain size and organic matter of surface sediments from the Nakdong-Goryeong Mid-watershed, surface sediments were collected and analyzed. The samples were collected from six sited at four different times between May 2013 and May 2014. The were analyzed for grain size, water content, ignition loss, chemical oxygen demand, total organic carbon and total nitrogen. The surface sediments were mainly composed of medium sand (mean 44.7%) and coarse sand (mean 32.8%) and became coarser in May 2014. Fine sediments at the site NG-2 were poorly sorted and positively skewed, and occur in a tributary environment that is relatively low-energy compared with the other sites. The water content at the studied sites (15.3 ~ 34.9%) averaged 20.25%, and ignition loss (0.4 ~ 5.8%) and total nitrogen (274 ~ 2493 mg/kg) averaged 1.33% and, 696 mg/kg, respectively. These values indicated that the sediments were not seriously contaminated when compared with the sediment pollution evaluation standard of the National Institute of Environmental Research. The chemical oxygen demand (mean 0.17%) was at the non-polluted level compared with United States Environmental Protection Agency sediment quality standards. The total organic carbon (mean 0.18%) at all sites except site NG-2 (lowest effect level) was the no effect level of the Ontario sediment quality guidelines. The COD/IL (0.02 ~ 0.20) and C/N (0.73 ~ 6.76) were less than 1 and 10, respectively. Organic matter in the study area produced naturally from aquatic organisms. Results of principal component analysis showed that fine sediments (very fine sand and silt) were significantly affected by organic matters (ignition loss, chemical oxygen demand, total organic carbon and total nitrogen). In addition, the highest organic matters content in the study area occurred at the site with the finest sediments (NG-2).

Electron Scattering at Grain Boundaries in Tungsten Thin Films

  • 최두호;김병준;이승훈;정성훈;김도근
    • 한국진공학회:학술대회논문집
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    • 한국진공학회 2016년도 제50회 동계 정기학술대회 초록집
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    • pp.243.2-243.2
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    • 2016
  • Tungsten (W) is recently gaining attention as a potential candidate to replace Cu in semiconductor metallization due to its expected improvement in material reliability and reduced resistivity size effect. In this study, the impact of electron scattering at grain boundaries in a polycrystalline W thin film was investigated. Two nominally 300 nm-thick films, a (110)-oriented single crystal film and a (110)-textured polycrystalline W film, were prepared onto (11-20) Al2O3 substrate and thermally oxidized Si substrate, respectively in identical fabrication conditions. The lateral grain size for the polycrystalline film was determined to be $119{\pm}7nm$ by TEM-based orientation mapping technique. The film thickness was chosen to significantly exceed the electron mean free path in W (16.1 and 77.7 nm at 293 and 4.2 K, respectively), which allows the impact of surface scattering on film resistivity to be negligible. Then, the difference in the resistivity of the two films can be attributed to grain boundary scattering. quantitative analyses were performed by employing the Mayadas-Shatzkes (MS) model, where the grain boundary reflection coefficient was determined to be $0.42{\pm}0.02$ and $0.40{\pm}0.02$ at 293 K and 4.2 K, respectively.

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한반도 동해 남부 대륙붕에 분포하는 탄산질-쇄설성분 혼합 퇴적물에 대한 연구 (Mixed Carbonate-Detrital Sediments on the Southeastern Continental Shelf of Korea)

  • 최진용
    • 한국지구과학회지
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    • 제18권6호
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    • pp.493-499
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    • 1997
  • 한반도 동해 남부 대륙붕에 분포하는 탄산질-쇄설성분 혼합 퇴적물에서 성분별 입도분석을 실시하여, 퇴적 환경 및 퇴적기작을 해석하였다. 쇄설성분은 평균입도가 중립사와 세립사 범위였으며, 분급이 양호한 단빈도 입도분포를 나타내었다. 이들 쇄설 퇴적물은 해수면이 낮았던 지난 빙하기동안 해빈 퇴적환경에서 집적되었으며, 전형적인 잔류퇴적물로 해석된다. 패각류가 우세한 탄산질 성분은 거의 파쇄된 상태이며, 표면이 심하게 풍화되었다. 이들 패각도 빙하기동안 천해환경에서 서식하였던 잔류기원 패각편으로 해석된다. 한편 입도특성은 쇄설성 성분에 비하여 다소 조립하며, 분급도는 불량하였다. 이들 패각편 탄산질 성분은 집적된 이후 지속적인 파쇄 및 분급작용에 의해 입도분포의 특징이 조절된 것으로 해석된다.

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자포니카 다수성 품종 소비벼의 입중과 입형의 유전 (Inheritance of Grain Weight and Size of a High Yielding Japonica cultivar, Sobibyeo)

  • 이승엽;노태환;김보경;이중호
    • 한국작물학회지
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    • 제48권3호
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    • pp.142-146
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    • 2003
  • 자포니카 중대립 소비벼의 입중 및 입형 관련형질의 유전양상을 구명하기 위하여, 2조합의 자포니카 품종간 $\textrm{F}_1$$\textrm{F}_2$를 이용하여 현미 천립중, 현미 길이, 넓이, 두께 등의 유전 및 관련형질간 상관관계를 분석한 결과는 다음과 같다. 1. 장폭비를 제외한 현미 천립중, 현미 길이, 넓이, 두께 등은 익산 429호/소비벼, 익산 430호/소비벼 두 조합의 $\textrm{F}_1$ 에서 모두 양친의 평균치보다 높게 나타났으며, 현미 천립중은 $\textrm{F}_2$ 집단에서 18.4g-32.2g과 19.5g-33.4g 범위로 연속적인 빈도분포를 보였다. 2. 현미 천립중에 대한 광의의 유전력은 두 조합에서 각각 89.00과 89.06으로 높게 추정되었으며, 현미의 길이에 대한 유전력은 각각 97.45와 97.35로 관련형질 중 가장 높게 나타났다. 3. 입중과 입형 관련형질 상호간에는 고도로 유의한 정의 상관관계가 인정되었으며, 현미 천립중은 현미 길이, 넓이, 두께 순으로 고도의 상관관계를 보였다. 따라서 소비벼의 입중 및 입형관련 형질들은 우성으로 작용하는 다수의 유전자가 관여하는 양적형질로 나타났으며, 교배 모본으로 활용할 경우 초기세대에서 선발이 가능하여 육종효율을 높일 수 있을 것으로 기대되었다.

공릉천 감조구간에 나타나는 표층퇴적물의 공간적 분포 특성 (Spatial distribution patterns of the surficial sediments in the tidal river, Gongneungcheon)

  • 최영선
    • 한국지형학회지
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    • 제18권4호
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    • pp.203-212
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    • 2011
  • 감조하천이 발달한 경기도 파주시 탄현면 일대의 공릉천 감조구간을 연구지역으로 하여 표층퇴적물의 공간적 분포 특성을 조사하였다. 연구 결과는 다음과 같다. 첫째, 공릉천 감조구간의 표층퇴적물은 주로 실트로 구성되어 있다. 둘째, 종단축의 경우 겨울과 여름 모두 감조구간의 하류보다 상류에서 평균입도가 세립해지는 경향이 나타났으며, 여름이 겨울보다 평균입도가 작고 분급이 양호한 것으로 나타났다. 감조구간 종단축의 입도 분포를 볼 때 부유물질이 퇴적되는 데에는 조류의 작용, 특히 밀물의 영향을 많이 받는 것으로 보이며 이러한 경향은 겨울에 더 우세한 것으로 판단된다. 셋째, 횡단축의 경우 하도로부터 거리가 멀어질수록 평균입도가 세립해지는 경향이 나타났다. 넷째, 갑문과 같은 인공 시설 역시 유속을 정체시킴으로써 입도 분포에 영향을 미친다고 판단된다.