首页> 外文期刊>Environmental Monitoring and Assessment >Characterizing baseline concentrations, proportions, and processes controlling deposition of river-transported bitumen-associated polycyclic aromatic compounds at a floodplain lake (Slave River Delta, Northwest Territories, Canada)
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Characterizing baseline concentrations, proportions, and processes controlling deposition of river-transported bitumen-associated polycyclic aromatic compounds at a floodplain lake (Slave River Delta, Northwest Territories, Canada)

机译:表征基线浓度,比例和控制洪水泛滥湖(加拿大西北地区奴隶河三角洲)上与河流运输的沥青相关的多环芳族化合物沉积的过程

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摘要

Inadequate knowledge of baseline conditions challenges ability for monitoring programs to detect pollution in rivers, especially where there are natural sources of contaminants. Here, we use paleolimnological data from a flood-prone lake ("SD2", informal name) in the Slave River Delta (SRD, Canada), similar to 500 km downstream of the Alberta oil sands development and the bitumen-rich McMurray Formation to identify baseline concentrations and proportions of "river-transported bitumen-associated indicator polycyclic aromatic compounds" (indicator PACs; Hall et al. 2012) and processes responsible for their deposition. Results show that indicator PACs are deposited in SD2 by Slave "river floodwaters in concentrations that are 45 % lower than those in sediments of BPAD31compounds", a lake upstream in the Athabasca Delta that receives Athabasca River floodwaters. Lower concentrations at SD2 are likely a consequence of sediment retention upstream as well as dilution by sediment influx from the Peace River. In addition, relations with organic matter content reveal that flood events dilute concentrations of indicator PACs in SD2 because the lake receives high-energy floods and the lake sediments are predominantly inorganic. This contrasts with PAD31 where floodwaters increase indicator PAC concentrations in the lake sediments, and concentrations are diluted during low flood influence intervals due to increased deposition of lacustrine organic matter. Results also show no significant differences in concentrations and proportions of indicator PACs between pre-(1967) and post-(1980s and 1990s) oil sands development high flood influence intervals (t = 1.188, P = 0.279, d. f. = 6.136), signifying that they are delivered to the SRD by natural processes. Although we cannot assess potential changes in indicator PACs during the past decade, baseline concentrations and proportions can be used to enhance ongoing monitoring efforts.
机译:对基线条件的了解不足,对监测计划以检测河流中的污染的能力提出了挑战,特别是在有天然污染物源的地方。在这里,我们使用来自奴隶河三角洲(加拿大,SRD)易发洪水湖泊(“ SD2”,非正式名称)的古湖泊学数据,类似于亚伯达省油砂开发和富含沥青的McMurray组的下游500公里确定“河流运输的沥青相关指示剂多环芳族化合物”(指示剂PAC; Hall等人2012)的基线浓度和比例以及造成其沉积的过程。结果表明,指示PAC沉积在SD2中的是“奴隶”河水,其浓度比BPAD31化合物的沉积物低45%。“奴隶河”是在阿萨巴斯卡三角洲上游接收阿萨巴斯卡河洪水的湖泊。 SD2浓度较低可能是上游沉积物滞留以及由于从和平河流入的沉积物而稀释的结果。此外,与有机物含量的关系还表明,洪水事件稀释了SD2中指示剂PAC的浓度,因为该湖泊遭受了高能洪水,并且湖泊沉积物主要是无机物。这与PAD31形成鲜明对比,PAD31的洪水增加了湖泊沉积物中指示性PAC的浓度,而在低洪水影响间隔期间,由于湖相有机质的沉积增加,浓度被稀释。结果还显示,在1967年之前和1980年代和1990年代后(和1980年代和1990年代之后)油砂开发高洪水影响区间之间,指示性PAC的浓度和比例没有显着差异(t = 1.188,P = 0.279,df = 6.136),表明它们通过自然过程传递到SRD。尽管我们无法评估过去十年中指标PAC的潜在变化,但可以使用基线浓度和比例来加强正在进行的监测工作。

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