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THE ATMOSPHERIC BIOGEOCHEMISTRY OF SELENIUM.

机译:硒的大气生物地球化学。

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Selenium concentration which one measures in the atmosphere can be influenced by the particulate collection characteristics of the filter employed. It appears that in urban areas perhaps 35 - 55% of atmospheric particulate selenium may pass through cellulose and membrane filters type filters routinely used. A fifteen month record of particulate and vapor phase selenium concentrations has been collected at a semi-urban area in Rhode Island. Mean particulate and vapor phase concentrations during this period were 1.7 and 0.11 ng Se/m('3). Approximately 6% of the selenium was found to be in the vapor phase.; Much lower concentrations of both particulate and vapor phase selenium found above the marine boundary layer suggest that the ocean may be an important source of naturally produced reduced selenium species.; In an effort to evaluate the strength of the marine biosphere flux of selenium into the atmosphere, approximately seven hundred weekly particulate samples from a seven island sampling network in the North Pacific have been analyzed for selenium. Concentrations were found to be more closely related to primary productivity of the surrounding waters rather than to factors such as transport of continental/anthropogenic materials into the atmosphere of open ocean regions. Observed selenium concentrations were combined with literature estimates of primary productivity in ocean surface waters to calculate an ocean to atmosphere flux of approximately 7 x 10('9) g Se/y. It is believed that evasion of naturally produced vapor phase selenium species from the ocean surface and subsequent gas-to-particle conversion may explain much of the anomalous enrichment of particulate selenium observed in the marine atmosphere.; To put this ocean to atmosphere flux estimate into perspective a global budget for atmospheric selenium has been constructed. Perhaps 14 -22 x 10('9) g Se are cycled through the atmosphere annually. Approximately 60% of this flux is natural in origin and both natural and anthropogenic emissions are predominantly vapor phase in nature. Natural fluxes are dominated by the marine biosphere while the combustion of coal accounts for slightly less than half of the total anthropogenic emissions. (Abstract shortened with permission of author.)
机译:一种在大气中测量的硒浓度会受到所用过滤器颗粒收集特性的影响。似乎在城市地区,可能有35-55%的大气微粒硒可以通过常规使用的纤维素和膜过滤器类型的过滤器。在罗得岛的一个半城市地区,已经收集了十五个月的颗粒状和气相硒浓度记录。在此期间,平均颗粒和气相浓度分别为1.7和0.11 ng Se / m('3)。发现约6%的硒处于气相。在海洋边界层以上发现的较低浓度的颗粒硒和气相硒表明,海洋可能是天然产生的还原硒物种的重要来源。为了评估硒海洋生物圈向大气中通量的强度,每周对来自北太平洋七个岛采样网络的大约700个颗粒物样品进行了硒分析。人们发现,其浓度与周围水域的初级生产力密切相关,而不是与诸如将大陆/人为物质运输到开放海洋区域的大气等因素密切相关。将观测到的硒浓度与海洋表层水中初级生产力的文献估计值相结合,以计算出大约7 x 10('9)g Se / y的海洋到大气通量。据信,从海洋表面逃逸出天然产生的气相硒物种并随后发生了气态至颗粒转化,这可能解释了在海洋大气中观察到的大量硒颗粒异常富集。为了将这种海洋对大气通量的估计值纳入考虑范围,已建立了全球大气硒预算。也许每年有14 -22 x 10('9)g Se在大气中循环。大约60%的这种通量是自然产生的,自然和人为排放物在自然界中都主要是气相。自然通量主要由海洋生物圈控制,而煤炭燃烧仅占人为排放总量的一半以下。 (摘要经作者许可缩短。)

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