• 한국해양학회지
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• v.24 no.2
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• pp.69-78
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• 1989

Cultivated pearls, composed of aragonite crystals, show two distinctive layers: nacreous and conchiolin organic layers. Each aragonite crystal is surrounded by organic matrix, which probably consists of amino acids. Nucleus, surrounded by pearl layer, also consists of nacreous crystals, suggesting that there is a close mineralogical and ultrasturctural relationship between pearl and nucleus. Carbon isotopic values of cultivated pearls are within the range of marine carbonate carbon. Oxygen isotopic composition indicates that the temperature for the growth of pearl and pearl oyster ranges from 16.4 to $21.4^{\circ}C$ and from 15.5 to $24.8^{\circ}C$, corresponding to the summer temperature range of the cultivating area. Elemental composition of pearl, pearl oyster, and nucleus shows that there is a difference in chemical composition depending upon the original mineralogy and the chemical composition of water in which shells grow. Especially, a strong relationship exists between pearl and the inner layer of pearl oyster because both are composed of nacreous aragonite and formed in a shallow marine environment.

• Korean Journal of Soil Science and Fertilizer
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• v.45 no.2
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• pp.209-214
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• 2012

This experiment was carried out to investigate the replaceability of chemical fertilizer by SCB liquid fertilizer (SCB) in pear orchard for 5 years. The effects on the mineral content of leaf, fruit quality, yield and soil chemical properties are as follows: The mineral content of leaf showed no difference between the treatments; two SCB liquid fertilizer treatments based on the N (SCB-N) and K (SCB-K) content, and control (chemical fertilizer application). There were no significant differences in yield, titratable acidity and weight of the fruit although the figure of fruit weight was high in SCB-N treatment. Soluble solids content was higher in the SCB treatments than the control. Soil chemical properties such as the content of soil organic matter, available soil phosphate and exchangeable cation were not different, although soil pH was higher in SCB treatments. In conclusion, it is suggest that the use of chemical fertilizer in pear orchard could be replaced by the application of SCB liquid fertilizer because of the same effect on the growth of pear tree and soil chemical properties.

• The Journal of Korean Medicine Ophthalmology and Otolaryngology and Dermatology
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• v.19 no.3 s.31
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• pp.68-74
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• 2006

목적 : 삼나무(Cryptomeria japonica)로부터 얻은 정유의 구성과 구강박테리아에 대한 항균작용을 연구하였다. 방법 : 정유의 화학적조성은 GC 와 GC-MS에 의하여 분석하였고, 정유와 그 주성분에 대한 구강박테리아 15균주의 항균효과를 시험하였다. 결과 : 정유의 95.82%에 해당하는 68복합체를 증명할 수 있었다. 정유의 주요성분은 ${\alpha}-pinene$ (6.07%), sabinene (8.86%), limonene (3.43%), ${\gamma}-cadinol$ (4.28%), ${\beta}-eudesmol$ (3.90%), and 10(15)-cadien-4-ol (7.16%)이었다. 삼나무의 주요성분은 거의 모든 박테리아에 대하여 MICs, 0.025 to 0.05 mg/ml; MBCs, 0.025 to 0.1 mg/ml에서 유의성있는 억제효과를 나타내었고, 주요성분 또한 다양한 성장억제를 나타내었다. 결론 : 삼나무의 정유는 다종의 화학복합체로 이루어져 있으며, 이는 다종의 구강박테리아에 대해 항균작용을 갖고 있다.

• Journal of Korean Society of Environmental Engineers
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• v.28 no.5
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• pp.522-526
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• 2006

To investigate the characteristics of rainwater in Daegu area, parameters such as pH, electrical conductivity, TOC, TIC and TC were analyzed on 34 samples from January to December 2005. Results revealed that higher values were measured in winter than in summer. Furthermore samples that originated from industrial and commercial areas had higher chemical concentrations and conductivity as compared with those from residential and reference areas. Seldom acid-rain occurrence was recorded(27.2%) as compared with non-acid precipitation(72.8%) incidence. Also higher organic carbon fraction(TOC) was detected(72.5%) than inorganic form(TIC)(27.5%) in terms of component ratio with TC. During frequent rainfalls, the concentration of chemicals was decreased to a degree. Conversely, lower rate of rainfall gave out higher chemical values. Thereby the improvement of air qualify in 2005 compare with 2003 report was influenced by the environment authorities' efforts to reduce air pollutions and various factors by the depression of the region's economy.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2006.04a
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• pp.328-332
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• 2006

본 연구는 농경활동이 활발한 만경강 하천부지에서 지하수의 수리지질 및 수리지화학적 특성을 고찰하고 B과 Sr 동위원소를 이용하여 지하수 수질 변화에 영향을 미치는 요인을 알아보고자 하였다. 연구 결과 만경강 하천부지는 지표로부터 실트질 모래층, 자갈모래층, 풍화대로 크게 3등분되며 투수성은 모래자갈층에서 가장 좋고 그 다음으로 풍화대, 실트질 모래층 순이었다. 화학성분 검층과 ${\delta}^{11}B,\;^{87}Sr/^{86}Sr$ 동위원소 분석결과 지하수 조성은 해수와 농업 활동에 의한 영향을 크게 받는 것으로 나타났다. 화학성분 검층 결과 해수 영향은 하천과 도로제방 사이 중간정도 까지인 것으로 사료되었으며 ${\delta}^{11}B$ 분석 결과 자갈모래층과 풍화대 지하수는 해수의 영향을 받는 것이 확인되었다. 본 연구지역 지하수는 지층 특성에 의한 영향으로 천층지하수는 토지이용에 따른 농업활동의 영향을 받으며 지표하 10m 이하의 지하수는 해수의 영향을 받는 것으로 사료되었다.

• Applied Chemistry for Engineering
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• v.22 no.1
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• pp.48-55
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• 2011

It was found that the absorbent mixed with 2-aminoethanol and others has been applied to remove them via chemical neutralization. The absorbent of natural second metabolites was achieved by a removal efficiency of 20~30% by itself depending on treatment conditions, but the complex absorbent mixed with 0.2% amine chemical provides the removal efficiency of over 98%. Optimal removal efficiencies have been examined against two major parameters of the temperature and pH to remove ammonia and hydrogen sulfide gases. The chemical analysis was also performed to analyze the composition of an essential oil by GC-MS. The monoterpenes in an essential oil reacted with odorous compounds by neutralization and their reaction mechanism was partially elucidated.

• Proceedings of the KSEEG Conference
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• 2002.04a
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• pp.454-457
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• 2002

• Journal of the Speleological Society of Korea
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• v.4 no.4
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• pp.13-13
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• 1979

한국에 산재하고 있는 20개의 동굴에서 종유석을 채취하여 이들의 구성성분을 화학분석하였다. 시료는 직경이 10cm 이상의 종유석을 취하여 표피로부터 약 1cm를 제거한 다음 1cm의 두께로 각절하여 분말로 만들어 분석하였다.(중략)

• Journal of Environmental Science International
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• v.12 no.6
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• pp.665-676
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• 2003

To investigate the chemical characteristics of PM$\_$2.5/ in Seoul, Korea, atmospheric particulate matters were collected using a PM$\_$10/ dichotomous sampler including PM$\_$10/ and PM$\_$2.5/ inlet during the period of October 2000 to September 2001. The Inductively Coupled Plasma-Mass Spectromety (ICP-MS), ion Chromatography (IC) methods were used to determine the concentration of both metal and ionic species. A statistical analysis was performed for the heavy metals data set using a principal component analysis (PCA) to derived important factors inherent in the interactions among the variables. The mean concentrations of ambient PM$\_$2.5/ and PM/sub10/ were 24.47 and 45.27 $\mu\textrm{g}$/㎥, respectively. PM$\_$2.5/ masses also showed temporal variations both yearly and seasonally. The ratios of PM$\_$2.5/PM$\_$10/ was 0.54, which similar to the value of 0.60 in North America. Soil-related chemical components (such as Al, Ca, Fe, Si, and Mn) were abundant in PM$\_$10/, while anthropogenic components (such as As, Cd, Cr, V, Zn and Pb) were abundant in PM2s. Total water soluble ions constituted 30∼50 % of PM$\_$2.5/ mass, and sulfate, nitrate and ammonium were main components in water soluble ions. Reactive farms of NH$_4$$\^$+/were considered as NH$_4$NO$_3$ and (NH$_4$)$_2$SO$_4$ during the sampling periods. In the results of PCA for PM$\_$2.5/, we identified three principal components. Major contribution to PM$\_$2.5/ seemed to be soil, oil combustion, unidentified source. Further study, the detailed interpretation of these data will need efforts in order to identify emission sources.

• Korean Journal of Soil Science and Fertilizer
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• v.31 no.3
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• pp.246-252
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• 1998

A survey was conducted to investigate the status of soils involving pH, electrical conductivity, total organic matter content, available phosphate and major exchangeable cations in the paddy soils sampled from 1,168 sites throughout the country. The content of soil chemical properties was lower on the average than the optimum levels for cropping. An average value showed pH 5.6, organic matter $25g\;kg^{-1}$, available phosphate $128mg\;kg^{-1}$, available silicate $72mg\;kg^{-1}$, and exchangeable potassium and the calcium and magnesium were 0.32, 4.0, $1.2cmol^+\;kg^{-1}$, respectively. Soil chemical properties was related with topography except soil pH. A soil pH and organic matter, available phosphate, exchangeable potassium increased with time while exchangeable calcium, magnesium available silicate decreased with time.