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Increased inorganic nitrogen leaching from a mountain grassland ecosystem following grazing removal: a hangover of past intensive land-use?

机译:放牧后山区草地生态系统中无机氮的淋溶增加:过去土地密集集约化的宿醉?

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Heathlands and grasslands occur in montane regions, naturally or due to anthropogenic land-use. These are typically nutrient-poor but exposure to elevated nitrogen deposition and intensive livestock grazing causes large-scale ecological change. We studied the long-term implications of grazing removal on soil and drainage water biogeochemistry and the implications for nitrogen cycling in 50-year replicated grazing exclosures on a montane grassland exposed to high rates of ambient nitrogen deposition. Evidence of 'ecosystem recovery' represented by successional change from graminoid to shrub-dominance after cessation of grazing was not reflected in the soil biogeochemistry. Cessation of grazing had a negative impact, with increased soil extractable and soil solution nitrate concentrations; an apparent shift towards a more nitrogen-rich, bacterially dominated microbial community; and the acidification of soils and leachate. The increase in nitrate leaching appears to have been counterbalanced by a decrease in dissolved organic nitrogen leaching, approximately maintaining the overall nitrogen balance of the system, whilst apparently altering ecosystem functioning. High rates of organic matter cycling and inorganic nitrogen uptake in grazed grassland may have sustained ecosystem N limitation under elevated nitrogen deposition. Grazing removal caused long-term over-supply of nitrogen from mineralisation of enriched organic matter, exacerbated by continued high nitrogen deposition, exceeding the uptake demand of heath vegetation and resulting in nitrification and nitrate leaching. This disequilibrium between vegetation and soil following grazing removal has implications for restoration after periods of intensive grazing. Grazing may not simply leave a legacy of nutrient enrichment but its cessation may trigger nitrogen saturation and soil and freshwater eutrophication and acidification which counteract the immediate benefits of natural vegetation recovery. Long term, nitrogen saturation of abandoned grasslands is likely to reduce ecosystem resilience to invasion by nitrophilous species, pathogen attack and vulnerability to environmental pressures such as climate change. We conclude that partial and/or phased reduction in grazing levels may permit the more synchronised recovery of soils and vegetation, thereby avoiding imbalances between nitrogen supply and nitrogen demand and detrimental ecological effects.
机译:荒地和草原自然或由于人为土地利用而发生在山地地区。这些通常缺乏营养,但是暴露于高氮沉积和密集的牲畜放牧会导致大规模的生态变化。我们研究了放牧对土壤和排水水生物地球化学的长期影响,以及在暴露于高环境氮沉积率的山地草原上50年重复放牧暴露对氮循环的影响。土壤生物地球化学没有反映以放牧结束后从类粒动物到灌木为主的连续变化为代表的“生态系统恢复”的证据。停止放牧会对土壤产生不利影响,增加了土壤可提取物和土壤溶液中硝酸盐的浓度。向着氮含量更高,以细菌为主的微生物群落的明显转变;以及土壤和渗滤液的酸化。硝酸盐浸出的增加似乎已被溶解有机氮浸出的减少所抵消,大约保持了系统的整体氮平衡,同时显然改变了生态系统的功能。在放牧的草地上,高放牧草地有机物循环和无机氮吸收的速率可能会持续限制生态系统的氮含量。放牧导致长期富集的有机物矿化导致氮长期过量供应,而持续的高氮沉积使情况进一步恶化,超出了健康植被的吸收需求,并导致硝化和硝态氮淋失。放牧后植被与土壤之间的这种不平衡关系到密集放牧一段时间后的恢复。放牧可能不仅会留下营养丰富的遗产,而且停止放牧可能会触发氮饱和以及土壤和淡水富营养化和酸化,抵消了自然植被恢复的直接好处。从长远来看,废弃草原的氮饱和度可能会降低生态系统对亚硝酸盐物种入侵,病原体侵袭以及对环境压力(如气候变化)的脆弱性的抵抗力。我们得出结论,放牧水平的部分和/或阶段性降低可能会使土壤和植被的恢复更加同步,从而避免氮素供应与氮素需求之间的不平衡以及不利的生态影响。

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