Dynamic modelling of atmospherically-deposited Ni, Cu, Zn, Cd and Pb in Pennine catchments (northern England)

被引:30
|
作者
Tipping, E. [1 ]
Rothwell, J. J. [2 ]
Shotbolt, L. [3 ]
Lawlor, A. J. [1 ]
机构
[1] Lancaster Environm Ctr, Ctr Ecol & Hydrol, Lancaster LA1 4AP, England
[2] Univ Manchester, Sch Environm & Dev, Upland Environm Res Unit, Manchester M13 9PL, Lancs, England
[3] Univ London, Dept Geog, London E1 4NS, England
关键词
Atmospheric deposition; Catchment; Heavy metals; Modelling; Soil organic matter; Weathering; DISSOLVED ORGANIC-CARBON; UPLAND UK CATCHMENT; LONG-TERM CHEMISTRY; HEAVY-METALS; HUMIC SUBSTANCES; PEAK DISTRICT; SOILS; LEAD; ACIDIFICATION; CONTAMINATION;
D O I
10.1016/j.envpol.2009.12.026
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Simulation modelling with CHUM-AM was carried out to investigate the accumulation and release of atmospherically-deposited heavy metals (Ni, Cu, Zn, Cd and Pb) in six moorland catchments, five with organic-rich soils, one with calcareous brown earths, in the Pennine chain of northern England. The model considers two soil layers and a third layer of weathering mineral matter, and operates on a yearly timestep, driven by deposition scenarios covering the period 1400-2010. The principal processes controlling heavy metals are competitive solid-solution partitioning of solutes, chemical interactions in solution, and chemical weathering. Agreement between observed and simulated soil metal pools and surface water concentrations for recent years was generally satisfactory, the results confirming that most contemporary soil metal is from atmospheric pollution. Metals in catchments with organic-rich soils show some mobility, especially under more acid conditions, but the calcareous mineral soils have retained nearly all anthropogenic metal inputs. Complexation by dissolved organic matter and cotransport accounts for up to 80% of the Cu in surface waters. (C) 2010 Elsevier Ltd. All rights reserved.
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页码:1521 / 1529
页数:9
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