쿨터카운터(Coulter Counter)를 이용한 극지 눈시료 중 광물성 먼지의 입자크기분포 분석
Particle Size Distribution Analysis of Mineral Dust in Polar Snow Using a Coulter Counter
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Mineral dust in the polar snow plays an important role both in the climate system of the Earth and in global biogeochemical cycles. Analysis of the concentration and the particle size distribution of mineraldust has been carried out in the snow from the Antarctic surface snow and the Greenland snowpit. Among hevarious particle size determination techniques, a Multisizer 3 Coulter Counter in a class 100 clean bench counted all particles between 1.1 and 30.0 μm with a 50 μm aperture tube. The aperture tube size, the concentration of electrolytes and the accuracy of the particle size distribution were determined in this study. The number concentrations from the Antarctic surface snow were 81,843 particles mL−1, but those from the Greenland snowpit were 10,666 particles mL−1. In the volume distribution, the distributions of mineral dust in both the Antarctic surface snow and the Greenland snowpit showed lognormal distribution in the size interval 1.1 to 6.0 μm with the mode, 3.562 and 3.836 μm, respectively. The analysis technique using a coulter counter for mineral dust could be used for reconstructing paleoclimates from polar ice cores.
Abstract
Mineral dust in the polar snow plays an important role both in the climate system of the Earth and in global biogeochemical cycles. Analysis of the concentration and the particle size distribution of mineraldust has been carried out in the snow from the Antarctic surface snow and the Greenland snowpit. Among hevarious particle size determination techniques, a Multisizer 3 Coulter Counter in a class 100 clean bench counted all particles between 1.1 and 30.0 μm with a 50 μm aperture tube. The aperture tube size, the concentration of electrolytes and the accuracy of the particle size distribution were determined in this study. The number concentrations from the Antarctic surface snow were 81,843 particles mL−1, but those from the Greenland snowpit were 10,666 particles mL−1. In the volume distribution, the distributions of mineral dust in both the Antarctic surface snow and the Greenland snowpit showed lognormal distribution in the size interval 1.1 to 6.0 μm with the mode, 3.562 and 3.836 μm, respectively. The analysis technique using a coulter counter for mineral dust could be used for reconstructing paleoclimates from polar ice cores.
참고문헌 (23)
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