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Natural or anthropogenic? On the origin of atmospheric sulfate deposition in the Andes of southeastern Ecuador

机译:天然或人为?论东南厄瓜多尔andes的大气硫酸盐沉积起源

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摘要

Atmospheric sulfur deposition above certain limits can represent a threat to tropical forests, causing nutrient imbalances and mobilizing toxic elements that impact biodiversity and forest productivity. Atmospheric sources of sulfur deposited by precipitation have been roughly identified in only a few lowland tropical forests. Even scarcer are studies of this type in tropical mountain forests, many of them mega-diversity hotspots and especially vulnerable to acidic deposition. In these places, the topographic complexity and related streamflow conditions affect the origin, type, and intensity of deposition. Furthermore, in regions with a variety of natural and anthropogenic sulfur sources, like active volcanoes and biomass burning, no source emission data has been used for determining the contribution of each source to the deposition. The main goal of the current study is to evaluate sulfate (SO4- deposition by rain and occult precipitation at two topographic locations in a tropical mountain forest of southern Ecuador, and to trace back the deposition to possible emission sources applying back-trajectory modeling. To link upwind natural (volcanic) and anthropogenic (urban/industrial and biomass-burning) sulfur emissions and observed sulfate deposition, we employed state-of-the-art inventory and satellite data, including volcanic passive degassing as well. We conclude that biomass-burning sources generally dominate sulfate deposition at the evaluated sites. Minor sulfate transport occurs during the shifting of the predominant winds to the north and west. Occult precipitation sulfate deposition and likely rain sulfate deposition are mainly linked to biomass-burning emissions from the Amazon lowlands. Volcanic and anthropogenic emissions from the north and west contribute to occult precipitation sulfate deposition at the mountain crest Cerro del Consuelo meteorological station and to rain-deposited sulfate at the upriver mountain pass El Tiro meteorological station.
机译:高于某些限制的大气硫沉积可以代表对热带森林的威胁,导致养分失衡,并调动影响生物多样性和森林生产率的有毒元素。沉淀沉积的大气来源沉积的沉积沉积在少数低地热带森林中粗略鉴定。甚至稀少是对热带山区森林的这种类型的研究,其中许多兆多样性热点,特别容易受到酸性沉积的影响。在这些地方,地形复杂性和相关的流流量条件影响沉积的起源,类型和强度。此外,在具有各种天然和人为硫源的区域中,如活性火山和生物质燃烧,已经使用源发射数据来确定每个来源对沉积的贡献。目前研究的主要目的是评估硫酸盐(SO4沉积在南部厄瓜多尔热带山区的两个地形位置,并追溯到应用背部轨迹建模的可能发射源。到Link Unumwind天然(火山)和人为(城市/工业和生物量燃烧)硫排放和观察到硫酸盐沉积,我们采用了最先进的库存和卫星数据,包括火山被动脱气。我们得出结论生物量 - 燃烧的来源通常在评估的位置占据硫酸盐沉积。在向南和西部的主要风的移位过程中发生轻微的硫酸盐。硫酸沉淀硫酸盐沉积和可能的雨水沉积主要与亚马逊低地的生物质燃烧排放相关。来自北部和西部的火山和人为排放有助于在T处潜气沉淀硫酸盐沉积他山顶Cres Cerro del Consuelo气象站,并在Upriver Mountain Pass El Tiro气象站雨沉积硫酸盐。

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