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Effects of forest thinning on the streamwater chemistry of two forest watersheds in the Bavarian Alps

机译:森林抚育对巴伐利亚阿尔卑斯山两个森林流域河流水化学的影响。

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摘要

Two well-buffered mixed mountain forest watersheds were studied with regard to stream water chemistry and the impact of forest thinning. The areas are located in the Bavarian Alps near Lake Tegernsee, 50 km SW of Munich (Germany). In order to obtaininformation on the influence of disturbances on the stream water chemistry, 40% of the trees were removed in October 1992 from one watershed after 2 yr of monitoring (1990-92), using a crane to avoid soil damage and erosion. The second watershed was used as a reference. The water output at 90degree C V-weirs installed at the foot of the watersheds for the monitoring was characterized, in general, by a strong export of silicate, alkali and alkaline earth cations, and bicarbonate. Acidity and nitrogen accumulated in the watersheds. Both areas were subject to a continuously increasing load of acidity, which was mainly buffered by cation exchange and silicate hydrolysis. This was indicated by continuously decreasing pH values and the dominance of Ca2+ and silicic acid in the stream water. Strong changes in the water chemistry along the flowpath indicate that rainwater will be stored in the system for sometime, and water derived from the headwater areas influences the discharge. During precipitation events the new rainwater replaces pre-event water, stored in soils, which had a longer contact time with the biotic and abiotic soil matrix. Acute effects of the selective harvest are levelled in the stream water by multiple buffer reactions. The discharge of the disturbed watershed was increased by the reduction of interception and transpiration. Increased rates of mineralization and acidity loads caused an increase in ion concentration and solution load in the discharge from the disturbed area. NH4+ showed the strongest effects in comparisons with the reference area and the pre-event period. The changes in the runoff returned to pre-event conditions about one year after the disturbance.
机译:研究了两个缓冲良好的混合山区森林流域,涉及溪流水化学和森林间伐的影响。这些地区位于慕尼黑西南部50公里的蒂根湖(Lake Tegernsee)附近的巴伐利亚阿尔卑斯山(德国)。为了获得有关干扰对溪流水化学影响的信息,1992年10月,在进行了2年的监测(1990-92年)后,使用起重机避免了对土壤的破坏和侵蚀,将40%的树木从一个流域中移除。第二个分水岭被用作参考。一般而言,安装在流域脚下以进行监测的90摄氏度V型水的出水特征是硅酸盐,碱金属和碱土金属阳离子以及碳酸氢盐的大量出口。流域中积累了酸度和氮。两个区域都承受着不断增加的酸性负荷,而酸性负荷​​主要受到阳离子交换和硅酸盐水解的缓冲。这通过连续降低pH值以及溪流水中Ca2 +和硅酸的优势来表明。沿流径的水化学变化很大,表明雨水将在系统中存储一段时间,而源头区域产生的水会影响排放。在降水事件期间,新的雨水代替了存储在土壤中的事件前水,后者与生物和非生物土壤基质的接触时间更长。通过多种缓冲液反应,可以在溪流水中平衡选择性收获的急性影响。通过减少截留和蒸腾作用,增加了受干扰流域的流量。矿化率和酸性负荷的增加导致受干扰区域的排放中离子浓度和溶液负荷的增加。与参考区域和赛前时期相比,NH4 +表现出最强的作用。扰动后大约一年,径流的变化又恢复到事前条件。

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