Centre for Ecology and Hydrology, Lancaster Environment Centre, Library Avenue, Bailrigg, Lancaster LA1 4AP, UK.
Environ Pollut. 2010 May;158(5):1521-9. doi: 10.1016/j.envpol.2009.12.026. Epub 2009 Dec 31.
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 co-transport accounts for up to 80% of the Cu in surface waters.
采用 CHUM-AM 进行模拟建模,研究了大气沉降重金属(Ni、Cu、Zn、Cd 和 Pb)在英格兰北部奔宁山脉的六个沼泽流域中的积累和释放情况。这五个流域的土壤富含有机物,一个流域的土壤为石灰质棕色土。该模型考虑了两层土壤和一层风化矿物层,每年运行一次,由 1400 年至 2010 年的沉积情景驱动。控制重金属的主要过程包括溶质的竞争固溶分配、溶液中的化学相互作用以及化学风化。近年来,观察到的和模拟的土壤金属库和地表水浓度之间的一致性通常令人满意,结果证实,大多数当代土壤金属来自大气污染。富含有机物的土壤中的金属具有一定的流动性,特别是在更酸性的条件下,但石灰质矿物土壤几乎保留了所有人为输入的金属。溶解有机物的络合作用和共迁移作用解释了高达 80%的地表水 Cu。