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Trends in soil water composition at a heavily polluted site-effects of decreased s-deposition and variations in precipitation

机译:土壤水组合物在较重污染的位点效应下降的S沉积和降水变化的趋势

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Precipitation, soils and soil water in a forested catchment in western Poland have been studied during the period 1992 - 96 (see also Vogt et al., this conf.). The S-deposition in the area during the study period was 2 - 3g S m{sup}(-2)yr{sup}(-1). In spite of decreasing anthropogenic enussions the S-deposition in the area did not change much during the study period mainly because the first years were exceptionally dry". However, the S-deposition was considerably higher during the previous decade. Based on Soil water sulphate concentration, pH, acid neutralising capacity and the ratio of Al{sup}(3+)/(Ca{sup}(2+) + Mg{sup}(2+)), there is apparently an amelioration in the conditions. A study using inter alia principal component analysis, indicates that this improvement is mainly due to more precipitation in the later part of the study period. Variations in precipitation amount have a pronounced effect on the soil-water chemistry, which makes it difficult to establish trends caused by changes in anthropogenic deposition. Long time series are therefore necessary to establish recovery due to reduced S-emissions.
机译:在1992年至96期间,波兰西部森林集水区中的降水,土壤和土壤水分(参见Vogt等人。)。在研究时期的区域中的S沉积为2-3g S m {sup}( - 2)Yr {sup}( - 1)。尽管人为大脑减少了该地区的S沉积在研究期间没有多大变化,主要是因为第一年特别干燥“。然而,在前十年期间,S沉积在土壤水硫酸盐上相当高。浓缩,pH,酸中和容量和Al {sup}(3 +)/(3 +)/(ca {sup}(2+)+ mg {sup}(2+)的比例显然是一种条件的改善。一个除其他外的主要成分分析中使用的研究表明,这种改进主要是由于研究时期的后部部分的降水量。降水量的变化对土壤 - 水化学有明显的影响,这使得难以建立趋势造成的趋势通过人为沉积的变化。因此,需要长时间序列来建立由于S-排放减少而建立恢复。

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