Science. 1974 Jan 18;183(4121):198-200. doi: 10.1126/science.183.4121.198.
The chemical composition of atmospheric particulate material collected at the geographic South Pole indicates that Al, Sc, Th, Sm, V, Mn, Eu, Fe, La, Ce, Co, Cr, Na, K, Mg, and Ca are derived from either crustal weathering or the ocean. The relatively volatile elements Zn, Cu, Sb, Se, Pb, and Br are apparently derived from other sources. Because of their volatility, vapor-phase condensation or a high-temperature dispersion source is suspected for these elements or their compounds.
在南极地理点采集的大气颗粒物的化学成分表明,Al、Sc、Th、Sm、V、Mn、Eu、Fe、La、Ce、Co、Cr、Na、K、Mg 和 Ca 来源于地壳风化或海洋。相对易挥发的元素 Zn、Cu、Sb、Se、Pb 和 Br 显然来自其他来源。由于这些元素及其化合物的挥发性,怀疑它们来自气相冷凝或高温分散源。