Bindler Richard, Korsman Tom, Renberg Ingemar, Högberg Peter
Department of Ecology and Environmental Sciences, Umeå University, SE-901 87 Umeå, Sweden.
Ambio. 2002 Sep;31(6):460-5. doi: 10.1579/0044-7447-31.6.460.
Acid rain has caused extensive surface water acidification in Sweden since the mid-20th century. Sulfur emissions from fossil-fuel burning and metal production were the main sources of acid deposition. In the public consciousness, acid deposition is strongly associated with the industrial period, in particular the last 50 years. However, studies of lake-water pH development and atmospheric pollution, based on analyses of lake sediment deposits, have shown the importance of a long-term perspective. Here, we present a conceptual argument, using the sediment record, that large-scale atmospheric acid deposition has impacted the environment since at least Medieval times. Sulfur sources were the pre-industrial mining and metal industries that produced silver, lead and other metals from sulfide ores. This early excess sulfur deposition in southern Sweden did not cause surface water acidification; on the contrary, it contributed to alkalization, i.e. increased pH and productivity of the lakes. Suggested mechanisms are that the excess sulfur caused enhanced cation exchange in catchment soils, and that it altered iron-phosphorus cycling in the lakes, which released phosphorus and increased lake productivity.
自20世纪中叶以来,酸雨已导致瑞典地表水广泛酸化。化石燃料燃烧和金属生产产生的硫排放是酸性沉降的主要来源。在公众认知中,酸性沉降与工业时期紧密相关,尤其是过去50年。然而,基于湖泊沉积物分析的湖水pH值变化及大气污染研究表明了长期视角的重要性。在此,我们利用沉积物记录提出一个概念性观点,即大规模大气酸性沉降至少自中世纪以来就已对环境产生影响。硫源是工业化前的采矿和金属行业,这些行业从硫化矿石中提炼银、铅和其他金属。瑞典南部早期这种过量的硫沉降并未导致地表水酸化;相反,它促成了碱化,即湖泊的pH值升高和生产力提高。推测的机制是,过量的硫导致集水区土壤中阳离子交换增强,并且它改变了湖泊中铁磷循环,从而释放出磷并提高了湖泊生产力。