• 암석학회지
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• 제27권2호
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• pp.73-84
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• 2018

청송 북부에는 청송 암맥군, 중태산 병반과 갈평지 암주 등의 화성관입체를 산출한다. 청송 암맥군은 다양한 구과를 발달시키는 유문암질 암맥들로 구성된다. 암맥들의 분포는 갈평지 암주를 중심으로 기하학적으로 방사상 패턴을 나타낼 뿐만 아니라, 관입체들의 화학조성은 암맥군의 공급원을 지시한다. 여기서 우리는 3개 관입체로부터 28개의 시료에 대한 조성적 자료를 보고한다. 관입체들은 같은 유문암질 조성이지만, 조성대비에 의하면, 관입체 조성 간에 상당히 중첩된다. 특히 청송 암맥군은 암석 색깔에 의해 몇몇 암맥그룹으로 구분되고 조성 다양성을 나타내지만, 대체로 기타 관입암 조성과 중첩을 나타낸다. 중태산 병반은 청송 암맥군과 비교하면 알칼리, $K_2O$와 $Al_2O_3$이 더 풍부하며 $Fe_2O_3{^t}$, $TiO_2$과 REE가 더 고갈되어 있다. 이와 대조적으로, 갈평지 암주는 화학조성이 더 좁은 범위를 나타내며, 청송 암맥군과 흔히 예리한 조성중첩을 가진다. 이러한 조성대비에 의하면 갈평지 암주는 조성적으로 청송 암맥군의 공급원으로 판단되며 화산작용의 에피소드로 연결된다고 생각된다.

• Asian Journal of Atmospheric Environment
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• 제11권3호
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• pp.165-175
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• 2017

In Japan, the primary carbonaceous particles emitted from motor vehicles and waste incinerators have been reduced due to strict regulations against exhaust gas. However, the relative contribution of carbonaceous particles derived from plants and biomass has been increasing. Accordingly, compositional analysis of carbonaceous particles has become increasingly important to determine the sources and types of particles produced. To reveal the sources of the organic particles contained in particulate matter with diameters of ${\leq}2.5{\mu}m$ ($PM_{2.5}$) and the processes involved in their generation, we analyzed molecular marker compounds (2-methyltetrols, cis-pinonic acid, and levoglucosan) derived from the plants and biomass in the $PM_{2.5}$ collected during daytime- and nighttime-sampling periods in summer (July and August) and autumn (November) in Kazo, which is in the northern area of Saitama prefecture, Japan. We also measured $^{14}C$ carbonaceous concentrations in the same $PM_{2.5}$ samples. The concentrations of 2-methyltetrols were higher in the summer than in the autumn. Because the deciduous period overlaps with this decrease in the levels of 2-methyltetrols, we considered the emission source to broad-leaved trees. In contrast, the emission source of the cis-pinonic acid precursor was considered to be conifers, because its concentration remained almost constant throughout the year. The concentration of levoglucosan was considerably increased in the autumn due to frequent biomass open burning. The ratio of plant-derived carbon to total carbon, obtained by measuring of $^{14}C$, in summer $PM_{2.5}$ sample was higher in the nighttime, and could be influenced by anthropogenic sources during the daytime.