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A Throughfall Collection Method Using Mixed Bed Ion Exchange Resin Columns

机译:混合床离子交换树脂柱的通量收集方法

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摘要

Measurement of ionic deposition in throughfall is a widely used method for measuring deposition inputs to the forest floor. Many studies have been published, providing a large database of throughfall deposition inputs to forests. However, throughfall collection and analysis is labor intensive and expensive because of the large number of replicate collectors needed and because sample collection and chemical analyses are required on a stochastic precipitation event-based schedule. Therefore we developed and tested a throughfall collector system using a mixed bed ion exchange resin column. We anticipate that this method will typically require only one to three samplings per year. With this method, bulk deposition and bulk throughfall are collected by a funnel or snow tube and ions are retained as the solution percolates through the resin column. Ions retained by the resin are then extracted in the same column with 2N KCl and analyzed for nitrate and ammonium. Deposition values in throughfall from conventional throughfall solution collectors and colocated ion exchange samplers were not significantly different during consecutive 3- and 4-month exposure periods at a high (Camp Paivika; >35 kg N ha-1 year-1) and a low deposition (Barton Flats; 5–9 kg N ha-1 year-1) site in the San Bernardino Mountains in southern California. N deposition in throughfall under mature pine trees at Camp Paivika after 7 months of exposure was extremely high (87 and 92 kg ha-1 based on the two collector types) compared to Barton Flats (11 and 13 kg ha-1). A large proportion of the N deposited in throughfall at Camp Paivika occurred as fog drip, demonstrating the importance of fog deposition as an input source of N at this site. By comparison, bulk deposition rates in open areas were 5.1 and 5.4 kg ha-1 at Camp Paivika based on the two collector types, and 1.9 and 3.0 kg ha-1 at Barton Flats.
机译:穿透水中离子沉积的测量是一种广泛用于测量林地沉积物输入量的方法。已经发表了许多研究,提供了森林通入沉积物输入的大型数据库。但是,由于需要大量的重复收集器,并且由于需要基于随机降水事件的时间表进行样品收集和化学分析,因此穿透瀑布的收集和分析非常费力且昂贵。因此,我们开发并测试了使用混合床离子交换树脂柱的穿透收集器系统。我们预计这种方法通常每年仅需要进行一到三个采样。使用这种方法,通过漏斗或雪管收集大量沉积物和大量穿透物,并且当溶液渗入树脂柱时,离子得以保留。然后,将树脂保留的离子在同一柱中用2N KCl萃取,并分析硝酸盐和铵盐。在连续的3个月和4个月的高暴露时间(营地Paivika;> 35 kg N ha -1 年)中,常规穿透溶液收集器和并置离子交换采样器的穿透物中的沉积值没有显着差异。 -1 )和圣贝纳迪诺山的低沉积(Barton Flats; 5–9 kg N ha -1 -1 )地点在南加州。与Barton Flats(11和13 kg)相比,暴露7个月后Paivika营地成熟松树下穿透性土壤的N沉积量非常高(基于两种收集器类型分别为87和92 kg ha -1 ) ha -1 )。在Paivika营地,贯穿降雨的大部分N沉积物都是以雾滴形式出现的,这表明雾沉积物是该地点N输入源的重要性。相比之下,基于两个收集器类型,Paivika营地在露天区域的总体沉积率分别为5.1和5.4 kg ha -1 ,而在两个集散地则为1.9和3.0 kg ha -1 巴顿平底鞋。

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