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Modeling aeolian transport in response to succession, disturbance and future climate: Dynamic long-term risk assessment for contaminant redistribution

机译:建模以响应继任,干扰和未来气候的风沙运输:污染物重新分配的动态长期风险评估

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摘要

Aeolian sediment transport is a fundamental process redistributing sediment, nutrients, and contaminants in dryland ecosystems. Over time frames of centuries or longer, horizontal sediment fluxes and associated rates of contaminant transport are likely to be influenced by succession, disturbances, and changes in climate, yet models of horizontal sediment transport that account for these fundamental factors are lacking, precluding in large part accurate assessment of human health risks associated with persistent soil-bound contaminants. We present a simple model based on empirical measurements of horizontal sediment transport (predominantly saltation) to predict potential contaminant transport rates for recently disturbed sites such as a landfill cover. Omnidirectional transport is estimated within vegetation that changes using a simple Markov model that simulates successional trajectory and considers three types of short-term disturbances (surface fire, crown fire, and drought-induced plant mortality) under current and projected climates. The model results highlight that movement of contaminated soil is sensitive to vegetation dynamics and increases substantially (e.g., > fivefold) when disturbance and/ or future climate are considered. The time-dependent responses in horizontal sediment fluxes and associated contaminant fluxes were sensitive to variability in the timing of disturbance, with longer intervals between disturbance allowing woody plants to become dominant and crown fire and drought abruptly reducing woody plant cover. Our results, which have direct implications for contaminant transport and landfill management in the specific context of our assessment, also have general relevance because they highlight the need to more fully account for vegetation dynamics, disturbance, and changing climate in aeolian process studies.
机译:风沙沉积物运输是在干旱地区生态系统中重新分配沉积物,养分和污染物的基本过程。在几个世纪或更长时间的时间框架内,水平沉积物通量和相关的污染物迁移率可能会受到演替,扰动和气候变化的影响,但缺乏解释这些基本因素的水平沉积物迁移模型,这在很大程度上部分准确评估与持久性土壤结合污染物相关的人类健康风险。我们基于水平沉积物运输(主要是盐分)的经验测量结果提供了一个简单的模型,以预测最近受干扰的地点(如垃圾掩埋场)的潜在污染物运输速度。使用简单的马尔可夫模型估算植被变化中的全向传输,该模型模拟连续轨迹并考虑当前和预计气候下的三种类型的短期扰动(地表火,树冠火和干旱引起的植物死亡)。模型结果突出表明,当考虑扰动和/或未来气候时,受污染土壤的运动对植被动态很敏感,并且会大幅增加(例如,> 5倍)。水平沉积物通量和相关污染物通量中随时间变化的响应对扰动时间的变化很敏感,扰动之间的间隔较长,使木本植物成为优势植物,树冠火和干旱突然减少了木本植物的覆盖。我们的结果在评估的特定背景下直接影响污染物的运输和垃圾填埋管理,因此也具有普遍意义,因为它们强调了在风化过程研究中需要更充分地说明植被动态,干扰和气候变化的原因。

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