본 연구는 개망초꽃 에센셜 오일의 항산화, 항균 및 항염 효능에 관하여 조사한 것이다. 개망 초꽃 에센셜 오일은 용매추출법으로 추출하였다. 개망초꽃 에센셜 오일의 항산화 효능은 ABTS 라디칼 소거능과 DPPH 라디칼 소거 효능 측정으로 확인하였다. ABTS 라디칼 소거 효과는 500 μg/ml 농도에 서 98.6%, DPPH 라디칼 소거는 48.3%로 좋은 효능을 나타내었다. 항균 활성은 S. aureus와 P. acnes, E. coli 균에 대하여 paper disc법과 최소저해농도(MIC)와 최소사멸농도(MBC)값을 측정하여 확인하였 다. S. aureus 균주에 대해서는 MIC 값과 MBC 값이 모두 0.31 mg/mL 농도에서 우수한 억제 효과를 나타내었다. P. acnes 균에 대해서는 disc법에서 14 mm의 clear zone 형성과 MIC, MBC에서 각각 0.31 mg/mL, 0.63 mg/mL로 좋은 억제 효과를 보였다. 항염 활성에 관련하여 NO 억제 측정에서도 농도 의존적으로 NO의 생성을 억제시킴을 확인하였고, pro-inflammatory cytokine인 TNF-α, IL-6 역시 농도 의존적으로 억제하였다. 이러한 결과로부터 개망초꽃 에센셜오일은 항산화, 항균 및 항염 효 능을 갖는 화장품 원료로서 개발 가능성이 있음을 시사한다.
This study investigated acetic acid fermentation properties and antioxidant activity of vinegar by addition of lemon grass to develop high quality vinegar by using lemongreass. Traditional brown rice wine contained 5% lemongrass powder and had an alcohol content of 7.2%. The wine was fermented by Acetobacter. sp. RIC-V and made into lemongrass vinegar (LV). The pH and total acidity of the LV were 3.13% and 7.21%, respectively. Fructose was detected whereas glucose, sucrose, and maltose were not detected. Among organic acids, acetic acid was highest at 3658.6 mg%; trace amounts of lactic acid, citric acid, malic acid, tartaric acid, and oxalic aicd were detected. Of the 17 free amino acids, glutamic acid, histidine, alanine, and proline were mainly detected. To conduct total polyphenol content and ABTS radical scavenging activity, 3% and 5% lemongrass powder (P3LV, P5LV) and 1%, 2%, and 3% of lemongrass extract (E1LV, E2LV, E3LV) were added to LV, respectively. Total phenolics increased as the added lemongrass powder and extract increased. Total phenolics were 490.9, 559.4, and 895.7 μg gallic acid equivalents/mL in brown rice vinegar, LV, P5LV. ABTS radical scavenging activities were 43.2%, 58.0%, and 91.0% in brown rice vinegar, LV, P5LV, respectively. These results show that lemongrass vinegar has considerable potential as a high quality functional vinegar with antioxidative effects.
This study examined the anti-inflammatory and whitening effects of Amaranth (Amaranthus spp L.) seed extract. Amaranthus spp L. seeds were extracted using 70% ethanol and then fractionated sequentially with n-hexane, dichloromethan, ethyl acetate and butanol. For the study of anti-inflammatory activity in RAW 264.7 cells, EtOAc fraction of Amaranthus spp L. seeds significantly inhibited nitrogen oxide production as well as the protein level of iNOS. Furthermore, EtOAc fraction of Amaranthus spp L. seeds inhibited expression of TNF-α, PGE2 and the protein level of COX-2 in a dose-dependent manner. Inaddition, the tyrosinase inhibitory activities of the Amaranthus spp L. seed 70% ethanol extract and subfractions were also measured to see if these extracts can be used as an ingredient for whitening cosmetics. Tyrosinase is an oxidase that is a rate-limiting enzyme for controlling the production of melanin. Therefore, tyrosinase inhibitors have become increasingly important in cosmetics and medical products with regards to hyperpigmentation. EtOAc fraction of Amaranthus spp L. seeds showed mushroom tyrosinase inhibitory activity in a dose-dependent manner. This activity was more potent than that of a positive control cynandione A. These results suggest that Amaranthus spp L. seeds may be a valuable natural ingredient for the food and cosmetics industries.
The number concentrations and the water soluble ionic concentrations of PM2.5 have measured at Gosan site in Jeju, Korea, from March 2010 to December 2010, to clarify their characteristics. PM2.5 number concentrations vary from 22.57 to 975.65 particles/㎝3 with an average value of 240.41 particles/㎝3, which have been recorded evidently high in spring season as compared with those in other season. And the concentrations in small size ranges are greatly higher than those in large size ranges, so the number concentration in the size range 0.25∼0.45 ㎛ has more than 94% of the total number concentration of PM2.5. The major ionic components in PM2.5 are SO4 2-, NH4 + and NO3 -, which are mainly originated from anthropogenic sources, on the other hand, the concentrations of Cl-, K+, Ca2+ and Mg2+ are recorded relatively lower levels. The concentrations of the major ionic components are very high in spring season, but the concentration levels of the other components are recorded significantly high in winter season. On the other hand, in summer season, the lowest concentration levels are observed for overall components as well as the sum of them. The concentration ratios of nss-SO4 2-/SO4 2- and nss-Ca2+/Ca2+ are 98.1% and 88.9%. And the concentration ratio of SO4 2-/NO3 -(3.64) is greatly higher than the value in urban area due to no large NOx emission sources in the measurement. In addition, the correlation and the factor analysis for the number and the ionic concentrations of PM2.5 are performed to identify their sources. From the Pearson correlation analysis and the factor analysis, it can be suggested that the smaller parts(<0.5 ㎛) of PM2.5 is contributed by anthropogenic sources, but the sources of the remaining larger parts of PM2.5 are not able to be specified sources in this study.
The number concentrations, the mass concentrations and the elemental concentrations of PM10 have measured at Gosan site in Jeju, Korea, from March 2010 to December 2010. And the correlation and the factor analysis for the number, the mass and the elemental concentrations of PM10 are performed to identify their relationships and sources. The average PM10 number concentration is observed 246 particles/㎝3(35.7∼1,017 particles/㎝3) and the average PM10 mass concentration is shown 50.1 ㎍/㎥(16.7∼441.4 ㎍/㎥) during this experimental period. The number concentrations are significantly decreased with increasing particle size, hence the concentrations for the smaller particles less than 2.5 ㎛(PM2.5) are contributed 99.6% to the total PM10 number concentrations. The highest concentration of the 20 elements in PM10 determined in this study is shown by S with a mean value of 1,497 ng/㎥ and the lowest concentration of them is found by Cd with a mean value of 0.57 ng/㎥. The elements in PM10 are evidently classified into two group based on their concentrations: In group 1, including S>Na> Al>Fe>Ca>Mg>K, the elemental mean concentrations are higher than several hundred ng/㎥, on the other hand, the concentrations are lower than several ten ng/㎥ in group 2, including Zn>Mn>Ni>Ti>Cr>Co>Cu>Mo>Sr>Ba>V >Cd. The size-separated number concentrations are shown positively correlated with the mass concentrations in overall size ranges, although their correlation coefficients, which are monotonously increased or decreased with size range, are not high. The concentrations of the elements in group 1 are shown highly correlated with the mass concentrations, but the concentrations in group 2 are shown hardly correlated with the mass concentrations. The elements originated from natural sources have been predominantly related to the mass concentrations while the elements from anthropogenic sources have mainly affected on the number concentrations of PM10.
The aerosol number concentration have measured with an aerodynamic particle sizer spectrometer(APS) at Gosan in Jeju Island, which is known as background area in Korea, from March 2010 to February 2011. The obtained results of asian dust events and non-asian dust period have been compared.
The results show that the entire averaged aerosol number concentration from APS measurement during asian dust events and non-asian dust period are about 341 particles/㎝3 and 240 particles/㎝3, respectively. During asian dust events, the number concentration in small size ranges(≤0.4 ㎛) are similar to non-asian dust period, however, those in large size ranges(≥0.7 ㎛) are very higher than non-asian dust period.
The contributions of the size resolved number concentration(23 channel in 0.25∼10.0 ㎛) to total number concentration in that range are dramatically decreased with increased particle size. The contributions of smaller size ranges(≤0.4 ㎛) during asian dust events are very low compared with non-asian dust period, on the other hand, those of larger size ranges(≥0.4 ㎛) are higher than non-asian dust period.
total aerosol number concentration are depended on the number concentration in range of smaller than 0.58 ㎛ during non-asian dust period and asian dust events. On the other hand, PM10 mass concentration has mainly affected with the number concentration in range of smaller than 1.0 ㎛ during non-asian dust period, however, during asian dust events, the mass concentration has mainly affected with the number concentration in range of 0.65∼3.0 ㎛.
The aerosol number concentration have measured with an aerodynamic particle sizer spectrometer(APS) at Gosan site, which is known as background area in Korea, from January to September 2011. The temporal variation and the size distribution of aerosol number concentration have been investigated.
The entire averaged aerosol number concentration in the size range 0.25∼32.0 ㎛ is about 252 particles/㎝3. The number concentration in small size ranges(≤ 0.5 ㎛) are very higher than those in large size ranges, such as, the number concentration in range of larger than 6.5 ㎛ are almost zero particles/㎝3. The contributions of the number concentration to PM10 and/or PM2.5 are about 34%, 20.1% and 20.4% in the size range 0.25∼0.28 ㎛, 0.28∼0.30 ㎛ and 0.30∼0.35 ㎛, respectively, however, the contributions are below 1% in range of larger than 0.58 ㎛.
The monthly variations in the number concentration in smaller size range(<1.0 ㎛) are evidently different from the variations in range of larger than 1.0 ㎛, but the variations are appeared similar patterns in smaller size range(<1.0 ㎛), also the variations in range of larger than 1.0 ㎛ are similar too. The diurnal variations in the number concentration for smaller particle(<1.0 ㎛) are not much, but the variations for larger particle are very evident.
Size-fractioned aerosol number concentrations are dramatically decreased with increased particle size. The monthly differences in the size-fractioned number concentrations for smaller size range(<0.7 ㎛) are not observed, however, the remarkable monthly differences are observed for larger size than 0.7 ㎛.
The aerosol number concentration have measured with an aerodynamic particle sizer spectrometer(APS) at Gosan site in Jeju, Korea, from March 2010 to March 2011. And then the atmospheric aerosol number concentration, the temporal variation and the size distribution of aerosol number concentration have been investigated.
The aerosol number concentration varies significantly from 748 particles/㎝3 to zero particles/㎝3. The average number concentration in small size ranges are very higher than those in large size ranges. The number concentrations in the size range 0.25∼0.28 ㎛, 0.40∼0.45 ㎛ and 2.0∼2.5 ㎛ are about 84 particles/㎝3, 2 particles/㎝3 and 0.4 particles/㎝3, respectively. The number concentrations in range of larger than 7.5 ㎛ are below 0.001 particles/㎝3.
The seasonal variations in the number concentration for smaller particle(<1.0 ㎛) are not much, but the variations for larger particle are very evident. And strong amplitudes of diurnal variations of entire averaged aerosol number concentration are not observed.
Size-fractioned aerosol number concentrations are dramatically decreased with increased particle size. The size-fractioned aerosol number concentrations in size range 0.8∼4.0 ㎛ during nighttime are evidently higher than during daytime, but similar levels are appeared in other size range. The seasonal differences in the size-fractioned number concentrations for smaller size range(<0.7 ㎛) are not observed, however, the remarkable seasonal differences are observed for larger size than 0.7 ㎛.