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通过建模和约束水文及生物地球化学控制来估算土壤中滴滴涕的 p,p'-DDT 降解。

Estimation of p,p'-DDT degradation in soil by modeling and constraining hydrological and biogeochemical controls.

机构信息

Research Centre for Toxic Compounds in the Environment (RECETOX), Faculty of Science, Masaryk University, Kamenice 753/5, Brno, 62500, Czech Republic.

Norwegian Institute for Water Research, Oslo, NO-0349, Norway.

出版信息

Environ Pollut. 2018 Aug;239:179-188. doi: 10.1016/j.envpol.2018.04.022. Epub 2018 Apr 11.

DOI:10.1016/j.envpol.2018.04.022
PMID:29655064
Abstract

Despite not being used for decades in most countries, DDT remains ubiquitous in soils due to its persistence and intense past usage. Because of this it is still a pollutant of high global concern. Assessing long term dissipation of DDT from this reservoir is fundamental to understand future environmental and human exposure. Despite a large research effort, key properties controlling fate in soil (in particular, the degradation half-life (τ)) are far from being fully quantified. This paper describes a case study in a large central European catchment where hundreds of measurements of p,p'-DDT concentrations in air, soil, river water and sediment are available for the last two decades. The goal was to deliver an integrated estimation of τ by constraining a state-of-the-art hydrobiogeochemical-multimedia fate model of the catchment against the full body of empirical data available for this area. The INCA-Contaminants model was used for this scope. Good predictive performance against an (external) dataset of water and sediment concentrations was achieved with partitioning properties taken from the literature and τ estimates obtained from forcing the model against empirical historical data of p,p'-DDT in the catchment multicompartments. This approach allowed estimation of p,p'-DDT degradation in soil after taking adequate consideration of losses due to runoff and volatilization. Estimated τ ranged over 3000-3800 days. Degradation was the most important loss process, accounting on a yearly basis for more than 90% of the total dissipation. The total dissipation flux from the catchment soils was one order of magnitude higher than the total current atmospheric input estimated from atmospheric concentrations, suggesting that the bulk of p,p'-DDT currently being remobilized or lost is essentially that accumulated over two decades ago.

摘要

尽管在大多数国家已经有几十年没有使用滴滴涕了,但由于其持久性和过去大量使用,滴滴涕仍然在土壤中普遍存在。因此,它仍然是一个备受全球关注的污染物。评估滴滴涕从这个储层中长时间消散对于了解未来的环境和人类暴露至关重要。尽管进行了大量的研究,但控制土壤中命运的关键性质(特别是降解半衰期(τ))远未完全量化。本文描述了一个在中欧大型流域的案例研究,在过去二十年中,该流域有数百次空气、土壤、河水和沉积物中 p,p'-滴滴涕浓度的测量。目标是通过约束流域内最先进的水文学、生物地球化学和多介质命运模型,对 τ 进行综合估计,以利用该地区现有的全部经验数据。为此目的,使用了 INCA-污染物模型。该模型对水和沉积物浓度的(外部)数据集具有良好的预测性能,分配性质取自文献,τ 估计值则通过强迫模型根据流域多组分中 p,p'-滴滴涕的经验历史数据进行估计。这种方法允许在充分考虑因径流和挥发造成的损失后,对土壤中的 p,p'-滴滴涕降解进行估计。估计的 τ 值范围在 3000-3800 天之间。降解是最重要的损失过程,每年占总消散量的 90%以上。从流域土壤中总消散通量比从大气浓度估算的当前大气输入高出一个数量级,这表明目前正在重新移动或损失的大部分 p,p'-滴滴涕基本上是过去二十年来积累的。

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