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Acidification-induced chemical changes in coniferous forest soils in southern Sweden 1988-1999

机译:1988-1999年瑞典南部针叶林土壤中酸化诱导的化学变化

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Thirty-two Norway spruce [Picea abies (L.) Karst.] and Scots pine (Pinus sylvestris L.) stands in southern Sweden were studied for a period of 12 years to evaluate acidification-induced chemical changes in the soil. Soil, at 20-30 cm depth in the mineral layer, was sampled three times during this period (1988, 1993 and 1999). The results show that pH(BaCl2) in mineral soil decreased by, on average, 0.17 units between 1988 and 1999, accompanied by an increase in aluminium (Al) concentration and a decrease in base saturation in the soil. In 1999, the base saturation was below 5% in 58% of the 32 sites compared with 16% in 1988 and 7% in 1993. Concentrations of calcium (Ca), potassium (K) and magnesium (Mg) are low and decreasing. Based on C/N ratios in humus, 45% of the sites may be subjected to leaching of considerable amounts of nitrate. The results show that the acidification of coniferous forest soils in southern Sweden is continuing, and that the negative effects on the nutrient status in soil are extensive. The results are compared with reference values for productive, long-term sustainably managed boreal coniferous or mixed forest soils and implications for long-term sustainability are discussed. (C) 2003 Elsevier Science Ltd. All rights reserved. [References: 50]
机译:对瑞典南部的32个挪威云杉[Picea abies(L.)Karst。]和苏格兰松(Pinus sylvestris L.)林分进行了长达12年的研究,以评估酸化引起的土壤化学变化。在此期间,对矿物层深度为20-30 cm的土壤进行了3次采样(1988、1993和1999)。结果表明,从1988年到1999年,矿质土壤中的pH(BaCl2)平均降低了0.17个单位,同时土壤中的铝(Al)浓度增加且碱饱和度降低。 1999年,在32个站点中,有58%的站点的基本饱和度低于5%,而1988年为16%,1993年为7%。钙(Ca),钾(K)和镁(Mg)的浓度低且呈下降趋势。基于腐殖质中的C / N比,可能会浸出45%的硝酸盐。结果表明,瑞典南部针叶林土壤的酸化作用仍在继续,对土壤养分状况的负面影响是广泛的。将结果与生产性,长期可持续管理的北方针叶林或混交林土壤的参考值进行比较,并讨论了对长期可持续性的影响。 (C)2003 Elsevier ScienceLtd。保留所有权利。 [参考:50]

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