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Long term changes in atmospheric N and S throughfall deposition and effects on soil solution chemistry in a Scots pine forest in the Netherlands

机译:荷兰苏格兰松树森林中大气N和S贯穿降雨的长期变化及其对土壤溶液化学的影响

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摘要

In a Scots pine forest the throughfall deposition and the chemical composition of the soil solution was monitored since 1984. (Inter)national legislation measures led to a reduction of the deposition of nitrogen and sulphur. The deposition of sulphur has decreased by approximately 65%. The total mineral-nitrogen deposition has decreased by ca. 25%, which is mainly due to a reduction in ammonium-N deposition (-40%), since nitrate-N deposition has increased (+50%). The nitrogen concentration in the upper mineral soil solution at 10 cm depth has decreased, leading to an improved nutritional balance, which may result in improved tree vitality. In the drainage water at 90 cm depth the fluxes of NO_3~- and SO_4~(2-) have decreased, resulting in a reduced leeching of accompanying base cations, thus preserving nutrients in the ecosystem. It may take still several years, however, before this will meet the prerequisite of a sustainable ecosystem.
机译:自1984年以来,一直在苏格兰松树林中监测贯穿物的沉积和土壤溶液的化学成分。(国际)国家立法措施减少了氮和硫的沉积。硫的沉积减少了约65%。矿物氮的总沉积量减少了约25%,这主要是由于硝酸盐-N沉积增加(+ 50%),从而减少了氮铵沉积(-40%)。 10 cm深度的上部矿质土壤溶液中的氮浓度降低,导致营养平衡改善,这可能会提高树木的活力。在深度为90 cm的排水中,NO_3〜-和SO_4〜(2-)的通量减少,从而减少了伴随的碱性阳离子的沉淀,从而保护了生态系统中的养分。但是,要达到可持续生态系统的先决条件可能还需要几年。

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