首页> 外文期刊>Forest Ecology and Management >Field-scale 'clean rain' treatments to two Norway spruce stands within the EXMAN project - effects on soil solution chemistry, foliar nutrition and tree growth.
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Field-scale 'clean rain' treatments to two Norway spruce stands within the EXMAN project - effects on soil solution chemistry, foliar nutrition and tree growth.

机译:在EXMAN项目中,对两个挪威云杉林进行了现场规模的“清洁降雨”处理-对土壤溶液化学,叶面营养和树木生长的影响。

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摘要

Clean rain treatments were performed in spruce (Picea abies) plantation forests at Klosterhede, Denmark, and Solling, Germany, by replacement of ambient throughfall water with artificial throughfall reducing the load of S (as sulfate, by 55-95%), N(as nitrate and ammonium, by 70-90%) and acidity (ca. 90%). The induced strong reductions in SO2-4 input caused corresponding strong reductions in soil solution concentrations at Klosterhede and to a minor extent at Solling. The difference in response tothe reduced input is suggested to be largely a consequence of differences in storage capacity between the two sites. Reduced input of N at Solling caused strong and immediate reduction in the soil solution concentration. At Klosterhede, N concentrationsin the soil solution were already low prior to the treatment and no effects were recorded. The effects on soil acidification reflected by Al and H concentrations were slow and small although a slight improvement in acid neutralizing capacity (ANC) was observed at Klosterhede, mainly caused by a strong reduction in strong acid anions. The input reductions decreased the general ion activity in the soil solution and the accumulation of base cations at both sites were consequently increased. Within the 6 yr of treatment at Klosterhede and the 2 yr at Solling, the effects on the soil solution chemistry were generally moderate. Accordingly, no significant changes in vegetation were observed apart from a water induced increase in growth rate at Klosterhede.
机译:在丹麦Klosterhede和德国Solling的云杉(Picea abies)人工林中进行了干净的雨水处理,方法是用人工通水代替周围通水,以减少S(作为硫酸盐,减少55-95%),N(如硝酸盐和铵盐,含量为70-90%)和酸度(约为90%)。 SO2-4投入的诱导强烈减少导致Klosterhede的土壤溶液浓度相应的强烈降低,而Solling的土壤溶液浓度也有少量降低。建议减少输入响应的差异主要是两个站点之间存储容量差异的结果。 Solling氮输入减少导致土壤溶液浓度立即大量降低。在Klosterhede,土壤溶液中的N浓度在处理之前已经很低,没有记录到任何影响。尽管在Klosterhede观察到酸中和能力(ANC)略有改善,但铝和H浓度对土壤酸化的影响缓慢而很小,这主要是由于强酸阴离子的强烈还原所致。减少的输入量降低了土壤溶液中的总离子活度,因此增加了两个位置的碱性阳离子的积累。在克洛斯特海德(Klosterhede)处理6年和索林(Solling)处理2年内,对土壤溶液化学的影响通常中等。因此,除了水分引起的克洛斯特海德(Klosterhede)生长速率增加以外,没有观察到植被发生明显变化。

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