| 초록 |
This study aims to identify the characteristics of soil in Mongolia, one of the major Asian dust sources that influence the Korean Peninsula. Soil particle size was analyzed and the result shows that sand (57.5~97.3%) was identified prominently in most regions, followed by silt (2.5~34.7%) and clay (0.0~7.8%). Soil pH of the covered regions were in the range 7.1~10.1, either weak alkaline or strong alkaline. Analysis of ion species in the soil samples exhibited that $Na^+$ ( $91.9 ;mg ;kg^{-1}$ ), $Cl^-$ ( $65.9 ;mg ;kg^{-1}$ ), and $Ca^{2+}$ ( $53.5 ;mg ;kg^{-1}$ ) were detected more in the soil than other species such as ${SO_4}^{2-}$ ( $19.2 ;mg ;kg^{-1}$ ), ${NO_3}^-$ ( $46.6 ;mg ;kg^{-1}$ ), ${NH_4}^+$ ( $3.9 ;mg ;kg^{-1}$ ), $K^+$ ( $22.0 ;mg ;kg^{-1}$ ), and $Mg^{2+}$ ( $10.2 ;mg ;kg^{-1}$ ). As for heavy metal content in the soil, concentrations of soil-borne metals including Fe, Al, Ca, Mg, and K tended to be high, while metals that come from manmade sources Pb, Cd, Cr, V, and Ni were remarkably low. The concentration of organic carbon (OC) was relatively high at $15.9 ;{ mu}g ;mg^{-1}$ , while elemental carbon (EC), directly released in the process of fossil fuel combustion, was not detected at all or found in very small amounts. The result indicates that pollution from manmade sources scarcely occurred. The analysis results from this study may contribute to improving modeling accuracy by providing input data for Asian dust prediction models, and be used as base data for determining the process of physiochemical transformation of Asian dust during long-range transport. |
