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Elemental composition of aerosols collected in the glacier area on Nyainqêntanglha Range, Tibetan Plateau, during summer monsoon season 总被引:1,自引:0,他引:1
In order to investigate the elemental composition in atmospheric aerosols and its sources in the glacier area over the Tibetan Plateau (TP), seven totally suspended particle samples were collected continuously at the col of the Zhadang glacier (30°28′N,90°39′E,5800 m a.s.l.), Nyainqêntanglha Range, southern TP, from June to October 2006. Twenty-seven elements (Li, Be, B, Na, Mg, Al, K, Ca, Sc, Ti, V, Fe, Mn, Zn, Ga, As, Rb, Sr, Y, Cd, Cs, Ba, Tl, Pb, Bi, Th, U) were analyzed by Inductively Coupled Plasma Mass Spectrometry (ICP-MS). The result indicates that the concentrations of most elements (especially crustal elements) are lower than values at the Nam Co Station during the same period of 2005, and also much lower than other sites in the TP such as Wudaoliang and Waliguan. This suggests that elemental compositions of aerosols in the Zhadang glacier area may represent the background levels of the middle/upper troposphere over the TP. Crustal enrichment factors (EFs) reveal that several elements (e.g. B, Zn, As, Cd, Pb and Bi) may have anthropogenic sources. The southern TP is mainly influenced by the summer Indian monsoon during the sampling period. Backward air mass trajectory analysis suggests that air masses in the region may originate from South Asia. Therefore, anthropogenic pollutants from South Asia may be transported by the summer Indian monsoon to the region which clearly affects the atmospheric environment in the southern TP during the summer monsoon season. 相似文献
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据英国《新科学家》杂志报道,地球发展史已经证实,地球每10万年就要进入一个冰河时期,虽然这是人类居住的这个星球最剧烈的气候变化,但迄今为止没有任何人能够解释清楚引起这一无情周期的原因到底是什么。最近美国科学家对此提出了一个全新的观点,认为地球每10万年进入一个冰河周期实际上是由于太阳磁活动的波动起伏。关于地球进入冰河周期的原因,传统的解释就是被称为米兰柯维奇周期的理论。这一理论认为,地球重大气候的变化与地球轴心的方向和倾斜度以及地球轨道离心率的缓慢周期性变化有关。就是说,地球轨道对来自太阳的能量有多少能到达地球表面,会起着改变的作用。这一改变。是导致地球冰河周期形成的主要原因。但 相似文献
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