증량제의 특성 중 Sumithion 분제의 주성분 분해에 영향을 미치는 요인을 밝힐 목적으로 시험하여 다음과 같은 결과를 얻었다. 가. 증량제의 특성 중 수분함량, 흡습성, C.E.C. 활성천, 염기총량, 표면적 등이 Sumithion 분제의 주성분 분해에 영향을 미치는 요인이 됨을 알았고, 나. 증량제에 의한 Sumithion의 분해산물은 Dimethyl phosphorothionate와 3-methyl-4-nirophenol 및 이의 유연화함은, n-hexane, ethyl ether 불용, methyl alcohol, ethyl, alcohol가용의 화함물이 있음을 알았다. 다. 증량제의 종류별로는 벤토나이트, 규조로, 카올린, 활석의 순으로 분해율이 높았다. 라. 그리고 증랑제의 Sumithion 분제 주성분 변화에 영향을 미치는 특성 중 수분과 염기가 가장 대표적인 주성분 분해 요인으로 보인다.

Future changes in mineral dust emission are studied using CMIP5 models. These models simulate climatological spatial distribution of dust emission over the observed major sources; Sahara Desert to Arabia and Southwest Asia. Model estimates for the range of global dust emission simulation appear large in the quantity of dust produced and the amplitude of interannual variability. According to the ensemble mean in global annual emissions, projections of four RCPs do not have significant long-term trends in mineral dust aerosol emissions at the end of 21st century. Meanwhile over Northeast Asia, annual emissions are projected to decrease significantly in four RCPs. Reductions appear over the major sources of mineral dust. Seasonally emission reduction in spring is distinct. In April and May, future changes with decreasing emission appear only in RCP4.5 with significance. Aerosol emission amount changes are related to changes in land surface property. We analyze future projection of soil moisture and bare soil area fraction. Regarding the projected decreasing trend in the annual emission amount over Northeast Asia, soil moisture is expected to increase in the emission source region in four RCPs. Relatively, the effect of bare soil area changes over the emission source appears in some models and RCPs.