Cadwalader G Owen, Renshaw Carl E, Jackson Brian P, Magilligan Francis J, Landis Joshua D, Bostick Benjamin C
Department of Earth Sciences, Dartmouth College, 6105 Fairchild Hall, Hanover, New Hampshire 03755, USA.
Geomorphology (Amst). 2011 May 1;128(1-2):85-91. doi: 10.1016/j.geomorph.2010.12.025.
Understanding of the transport mechanisms of contaminated soils and sediment is essential for the sustainable management of contaminated lands. In New England and elsewhere, vast areas of agricultural lands are contaminated by the historical application of lead-arsenate pesticides. Left undisturbed the physical and chemical mobility of As and Pb in these soils is limited due to their strong affinity for adsorption onto solid phases. However, soil disturbance promotes erosion and overland flow during intense rainstorms. Here we investigate the event-scale transport of disturbed As and Pb contaminated soils through measurement of concentrations of As and Pb in suspended sediment and changes in Pb isotopic ratios in overland flow. Investigation of several rain events shows that where land disturbance has occurred, physical transport of silt-sized particles and aggregates is the primary transport vector of As and Pb derived from pesticide-contaminated soil. Although both As and Pb are associated with similarly-sized particles, we find that solid-phase As is more effectively mobilized and transported than Pb. Our results demonstrate that anthropogenic land disturbance of historical lands contaminated with lead-arsenate pesticides may redistribute, through physical transport, significant amounts of As, and lesser amounts of Pb, to riparian and stream sediments, where they are potentially more bioavailable.
了解污染土壤和沉积物的迁移机制对于污染土地的可持续管理至关重要。在新英格兰和其他地区,大量农田因过去使用砷酸铅农药而受到污染。在未受扰动的情况下,由于砷和铅对固相的吸附亲和力很强,它们在这些土壤中的物理和化学迁移能力有限。然而,土壤扰动会在暴雨期间促进侵蚀和地表径流。在此,我们通过测量悬浮沉积物中砷和铅的浓度以及地表径流中铅同位素比值的变化,研究了受扰动的砷和铅污染土壤在事件尺度上的迁移情况。对几次降雨事件的调查表明,在发生土地扰动的地方,粉砂大小的颗粒和团聚体的物理迁移是农药污染土壤中砷和铅的主要迁移载体。尽管砷和铅都与大小相似的颗粒相关,但我们发现固相砷比铅更有效地被活化和迁移。我们的结果表明,历史上受砷酸铅农药污染土地的人为扰动可能通过物理迁移将大量的砷以及少量的铅重新分配到河岸和溪流沉积物中,在那里它们可能具有更高的生物可利用性。