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Atmospheric organic and inorganic nitrogen inputs to coastal urban and montane Atlantic Forest sites in southeastern Brazil

机译:向巴西东南部沿海城市和山区大西洋森林地点的大气有机和无机氮输入

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Tropical regions are currently experiencing changes in the quantity and form of nitrogen (N) deposition as a result of urban and industrial emissions. We quantified atmospheric N inputs to two coastal urban and two montane (400 m and 1000 m) Atlantic Forest sites downwind of the Metropolitan Region of Rio de Janeiro (MRRJ), Brazil, from August 2008 to August 2009. Concentrations of total dissolved nitrogen (TDN), dissolved inorganic nitrogen (DIN) and urea were measured in bulk precipitation at all sites, as well as in canopy throughfall in the lower montane forest. Dissolved organic nitrogen (DON) was calculated as the difference between TDN and DIN (NH4+ + NO3- + NO2-). Annual volume-weighted mean bulk concentrations of all N species were higher at the coastal urban than montane forest sites, with DON accounting for 32-56% and 26-32%, respectively, of the TON concentration in bulk precipitation. Bulk deposition of TDN ranged 12.1-17.2 kg N ha(-1) yr(-1) and tended to decrease with increasing distance from the coastal urban region. In the lower montane forest, throughfall TDN flux, 34.3 kg N ha(-1) yr(-1), was over 2-fold higher than bulk TDN deposition, and DON comprised 57% of the total N deposited by throughfall to the forest soil. Urea comprised 27% of DON in throughfall compared to up to 100% in bulk precipitation. Our findings show that DON is an important, yet understudied, component of TDN deposition in tropical forest regions, comprising one-third to greater than one-half of the N deposited in rainfall and throughfall. Further, in this lower montane Atlantic Forest site, throughfall DIN flux was 1.5-3 fold higher than the suggested empirical critical load for humid tropical forests, highlighting the potential for increasing N pollution emitted from the MRRJ to impact N cycling in adjacent ecosystems. (C) 2015 Elsevier B.V. All rights reserved.
机译:由于城市和工业排放,热带地区目前正经历着氮(N)沉积数量和形式的变化。我们对2008年8月至2009年8月巴西里约热内卢都会区(MRRJ)下风的两个沿海城市和两个山地(400 m和1000 m)大西洋森林站点的大气氮输入进行了定量。总溶解氮浓度( TDN,溶解的无机氮(DIN)和尿素在所有地点的整体降水中以及山地下部森林的冠层贯穿降雨中进行了测量。溶解有机氮(DON)计算为TDN和DIN(NH4 + + NO3- + NO2-)之差。在沿海城市,所有N物种的年度体积加权平均容重浓度都高于山地林地,其中DON分别占整体降水中TON浓度的32-56%和26-32%。 TDN的批量沉积范围为12.1-17.2 kg N ha(-1)yr(-1),并且随着与沿海城市地区距离的增加而趋于减少。在较低的山地森林中,贯穿的TDN通量为34.3 kg N ha(-1)yr(-1),比整体TDN沉积高出2倍以上,DON占通入森林的N总量的57%泥。尿素占通量DON的27%,相比之下,散装降水量高达100%。我们的研究结果表明,DON是热带森林地区TDN沉积的重要但未被充分研究的组成部分,占降雨和降雨过程中N沉积的三分之一至一半以上。此外,在山地较低的大西洋森林站点中,贯通的DIN通量比湿热带森林的建议经验临界负荷高1.5至3倍,突显了MRRJ排放的N污染增加而影响相邻生态系统中N循环的潜力。 (C)2015 Elsevier B.V.保留所有权利。

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