• 한국환경과학회지
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• 제14권4호
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• pp.367-371
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• 2005

Soil samples were collected from new-developed wetland soil ecosystem of Tamarix chinesis plantation in Chinese Yellow River Delta in different months of 2003. Soil characteristics, temporal change and spatial distribution of microbial community composition and their relationship with nitrogen turnover and circling were investigated in order to analyze and characterize the role of microbial diversity and functioning in the specific soil ecosystem. The result showed that the total population of microbial community in the studied soil was considerably low, compared with common natural ecosystem. The amount of microorganism followed as the order: bacteria> actinomycetes>fungi. Amount of actinomycetes were higher by far than that of fungi. Microbial population remarkably varied in different months. Microbial population of three species in top horizon was corrected to that in deep horizon. Obvious rhizosphere effect was observed and microbial population was significantly higher in rhizosphere than other soils due to vegetation growth, root exudation, and cumulative dead fine roots. Our results demonstrate that microbial diversity is low, while is dominated by specific community in the wetland ecosystem of Tamarix chinesi.

• 한국물환경학회지
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• 제22권2호
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• pp.209-214
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• 2006

The purpose of this study is to improve the stream water quality by the experimental hybrid constructed wetland system. It consisted of the water layer, sand bed planted reeds, irises and roses, gravel bed, yellow-soil media bed and a flow shifter (FS) which can reverse top and bottom flow in the middle of the wetland. The organic compounds and nitrogen removal efficiencies varied with the seasons, namely temperature change. In summer, the mean efficiencies of COD and TN in the outflow from this wetland system were 63.4 and 48.0% and shown the highest, respectively, whereas, the suspended solids and phosphorus removal efficiencies seemed to be less affected by temperature. As a result of inspecting the decreasing trend of pollutants, nitrification-denitrification in the wetland was the major removal mechanism for nitrogen, the nitrogen reduction was especially enhanced by the application of a FS in the wetland, and phosphorus reduction was mainly occurred as a consequence of adsorption of the yellow-soil media.

• KIEAE Journal
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• 제2권2호
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• pp.45-50
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• 2002

In the last century, mainly our cultures destroyed a lot of ourselves as well as of our natural environment by deterioration, pollution and exploitation. Building activities are for a third responsible for these disasters and they are fully the reason for the growing Sick Building Syndrome. In result, Materials of the building should be derived as much as possible from nature, and walls should be made of yellow soil, or of bricks made from yellow soil The adobe can easily have larger or smaller dimensions, and different thickness as weil, according to the purpose for which they are meant, and the structural load-bearing function they have to fulfill. In spite of the importance of clay, research or experiment of clay has been quite weak. However, in stead of endowing the clay with the value as natural architectural material, we want to evaluate it as an important element of the environment.

• 한국환경보건학회지
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• 제30권5호
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• pp.455-468
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• 2004

The purpose of this paper is to understand the time series and origin of a chemical component and to compare the difference during yellow sand episodes for analysis $PM_{10}$ chemical components in the region of west in Korean Peninsula, 1999-2001. An annual mean concentration of $PM_{10}$ is $29.1\;{\mu}g/m^3$. A monthly mean and standard deviation of $PM_{10}$ concentration are very high in spring but there is no remarkably seasonal variation. Also, water soluble ionic component of $PM_{10}$ be influenced by double more total anion than total cation, be included $NO_{3}^-\;and\;SO_{4}^{2-}$ for the source of acidity and $NH_{4}^+$ to neutralize. Tracer metals of $PM_{10}$ slowly increases caused by emitted for soil and ocean (Fe, Al, Ca, Mg, Na) and Zn, Pb, Cu, Mn for anthropogenic source. According to method of enrichment factor (E.F) and statistics, assuming that the origin of metal component in $PM_{10}$ most of element in the Earth's crust e.g. Mg, Ca, Fe originates soil and Cu, Zn, Cd, Pb derives from anthropogenic sources. The ionic component for $Na^{+}\;Cl^-,\;Mg^{2+}\;and\;Ca^{2+}$ and Mg, Al, Ca, Fe originated by soil component largely increase during yellow sand period and then tracer metal component as Pb, Cd, Zn decrease. According to factor analysis, the first group is ionic component ($Na^+,\;Mg^{2+},\;Ca^{2+}$) and metal component (Na, Fe, Mn and Ni) be influenced by soil. The second group, Mg, Cr also be influenced by soil particle.

• 한국토양비료학회지
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• 제4권2호
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• pp.187-192
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• 1971

산성암(酸性岩)인 화강암(花崗岩)의 풍화잔적층(風化殘積層)을 모재(母材)로한 전남통(全南統)에 대(對)한 형태(形態), 물리적(物理的), 화학적(化學的) 및 생성(生成)과 분류(分類)에 관(關)하여 조사(調査)한 결과(結果)를 요약(要約)하면 다음과 같다. 1. 형태적특성(形態的特性)에 있어서 표토(表土)는 갈색(褐色) 내지(乃至) 암갈색(暗褐色)의 미사질양토(微砂質壤土) 내지(乃至) 토양(土壤)이나 침식(侵蝕)을 받은 곳에서는 진갈색(眞褐色) 내지(乃至) 황적색(黃赤色)의 미사질식양토(微砂質埴壤土) 또는 식양토(埴壤土)이다. 심토(心土)는 황적색(黃赤色) 내지(乃至) 적색(赤色)의 미사질식양토(微砂質埴壤土) 내지(乃至) 미사질식토(微砂質埴土)로서 구조표면(構造表面)에 엷은 점토막(粘土膜)이 형성(形成)되여 있다. 기층(基層)은 심(甚)하게 풍화(風化)된 화강암(花崗岩)의 잔적모재(殘積母材)이며 토양(土壤)의 깊이는 매우 깊다. 2. 물리적(物理的) 특성(特性)에서 토양입자(土壤粒子)의 분포비율(分布比率)은 표토(表土)에서 심토(心土)로 내려 갈수록 점토(粘土)의 함량(含量)이 증가(增加)되어 심토(心土)의 중앙부분(中央部分)이 34-45% 이며 특(特)히 미사(微砂)의 함량(含量)은 50~60%로서 표토(表土) 및 심토(心土)의 차이(差異)는 별(別)로 없다. 3. 화학적(化學的) 성질(性質)은 유기물(有機物) 함량(含量)이 낮고 토양반응(土壤反應)이 강산성(强酸性)이며 염기포화도(鹽基飽和度)가 낮다. 4. 전남통(全南統)은 온난(溫暖) 습윤(濕潤)한 기후조건하(氣候條件下)에서 생성(生成)되며 분류(分類)에 있어 미농무성(美農務省) 7차시안(次試案)에 의(依)하면 Typic Hapludults, UNESCO/FAO의 분류(分類)에 의(依)하면 Helvic Acrisols에 속(屬)한다.

• 한국식품영양학회지
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• 제18권4호
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• pp.316-324
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• 2005

본 실험의 목적은 콩나물의 생육 특성 및 물리화학적 변화에 ion chip과 황토가 미치는 영향을 알아보았다. 콩나물의 무게와 길이는 4일까지 급격히 생장하였으나, 그 후 완만한 속도로 생장하였다. 총 비타민 C의 함량은 이온수(I.W), 수돗물과 이온수에 황토 $1.0\%$를 첨가한 군(T.W+l.0, I.W+l.0)에서 6일 이후 급격하게 증가하였다. 콩나물에 함유된 미네랄 중 Mg, Ca, K, Fe의 함량이 다른 미네랄보다 높았다. 철의 함량은 이온수에 황토 $1.0\%$를 첨가한 군(I.W+l.0)에서 가장 높게 검출되었다. 이온수로 4일 동안 재배한 콩나물에 함유된 glutamic acid는 수도수에 비해 높게 나타났다. 핵산관련 물질은 UMP, CMP, AMP 및 Hx이 검출되었는데, UMP가 가장 높았다. 유리당은 sucrose, raffinose, stachyose가 검출되었고, sucrose가 그 중에 가장 높은 함량이었다.

• Journal of Microbiology and Biotechnology
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• 제21권4호
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• pp.341-346
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• 2011

To study the effects of salinity-sodicity on bacterial population and enzyme activities, soil samples were collected from the Bay of Yellow Sea, Incheon, South Korea. In the soils nearest to the coastline, pH, electrical conductivity ($EC_e$), sodium adsorption ratio (SAR), and exchangeable sodium percentage (ESP) were greater than the criteria of saline-sodic soil, and soils collected from sites 1.5-2 km away from the coastline were not substantially affected by the intrusion and spray of seawater. Halotolerant bacteria showed similar trends, whereas non-tolerant bacteria and enzymatic activities had opposite trends. Significant positive correlations were found between EC, exchangeable $Na^+$, and pH with SAR and ESP. In contrast, $EC_e$, SAR, ESP, and exchangeable $Na^+$ exhibited significant negative correlations with bacterial populations and enzyme activities. The results of this study indicate that the soil chemical variables related with salinity-sodicity are significantly related with the sampling distance from the coastline and are the key stress factors, which greatly affect microbial and biochemical properties.

• Environmental Analysis Health and Toxicology
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• 제17권4호
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• pp.333-339
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• 2002

Yellow sand (YS) storms were observed about ten times in the Korean peninsula during March and April in 2002. Twenty four hour fine particle (PM$\_$2.5/) samples were collected onto the 47 mm Teflon - coated quartz filters over 9 days during and after the events using the MiniVol Portable Air Sampler at a flow rate of 5 liters per minute. The highest PM$\_$2.5/ concentration measured during the YS period was 289 $\mu\textrm{g}$/㎥, which is 13 times higher than the lowest of the values for the samples collected during the non-yellow sand period. The filter samples were analyzed for inorganic ions using the IC, AAS and Autoanalyzer, and for metals using the ICP-MS. The results showed that the concentrations of some inorganic ions (e.g., Ca$\^$2+/ and SO$_4$$\^$2-/) and metals (e.g., Fe, Mn) of soil origin were elevated during the yellow sand events.

• 원예과학기술지
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• 제28권5호
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• pp.735-742
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• 2010

석회질 비료인 고토석회와 탄산칼슘의 시비수준이 'Melody Yellow' 팬지의 플러그 육묘시 토양화학성 변화와 식물생장에 미치는 영향을 구명하기 위해 본 연구를 수행하였다. 피트모스+버미큘라이트(1:1, v/v) 혼합상토에서 고토 석회는 $3.5g{\cdot}L^{-1}$, 탄산칼슘은 2.5 또는 $3.0g{\cdot}L^{-1}$ 비율로 시비한 처리에서 이상적인 pH 5.6-6.2의 범위에 포함되었다. 탄산칼슘 처리구에서는 토양 pH가 빠른 속도로 상승한 후 안정되어 탄산칼슘이 고토석회에 비해 용해도가 높고 빠르게 토양 pH에 영향을 미치는 것을 알 수 있었다. 상토의 Ca 농도는 두 종류 석회질 비료의 시비수준이 높아질수록 비례적으로 상승하였고, 탄산칼슘이 시용된 모든 처리에서 고토 석회가 시비된 처리들보다 2배 이상 높은 농도로 분석되었다. 토양 Mg 농도는 고토석회 처리구에서 3.5와 $8.0g{\cdot}L^{-1}$ 처리에서 가장 높게 나타났고, 모든 탄산칼슘 처리구에서 대조구보다 낮은 농도로 분석되어 추가로 Mg을 공급해 주어야 함을 알 수 있었다. 탄산칼슘 시용량이 증가됨에 따라 팬지 생체중과 건물중이 증가하는 경향이었으나 초장은 뚜렷한 차이를 나타내지 않았다. 식물조직분석을 통한 무기원소 함량은 Ca과 Mg은 처리간의 약간의 차이를 나타냈지만 대부분의 무기원소에서는 처리구 모두 뚜렷한 차이가 나타나지 않았다.

• 한국의상디자인학회:학술대회논문집
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• 한국의상디자인학회 2004년도 International Conference & Exhibition
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• pp.95-97
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• 2004