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Sensitivity of blanket peat vegetation and hydrochemistry to local disturbances

机译:毛毯泥炭植被和水化学对局部扰动的敏感性

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At the ecosystem scale, peatlands can be extremely resilient to perturbations. Yet, they are very sensitive to local disturbances, especially mechanical perturbations (e.g. trampling). The effects of these disturbances on vegetation, and potential effects on hydrochemical conditions along the peat surface, however, are largely unknown.rnWe used three research tracks (paths researchers use to access their study sites) differing in time of abandonment to investigate the impact of local disturbance (trampling) on the vegetation and its short-term (≤2 year) recovery in a flagship research blanket peatland. Additionally, we examined the effects of local disturbance on fluvial runoff events and the concentrations of dissolved organic carbon (DOC) and paniculate organic carbon (POC) in runoff water.rnLocal disturbance heavily impacted peat vegetation, resulting in large areas of scarred and churned peat Recovery of vascular plants along abandoned tracks was slow, but a functional Sphagnum layer re-established after just one year.rnThe absence of vegetation elicited an increase in the number of runoff events along the tracks, by which POC runoff from the tracks increased. POC concentrations were highest in the surface water from the recently abandoned track, while they were low in the runoff water from the track abandoned longest and the undisturbed control track. We attribute this to the relatively fast recovery of the Sphagnum vegetation. DOC concentrations did not differ significantly either spatially or temporally in surface runoff or soil solution waters. While at an ecosystem scale local disturbances may be negligible in terms of carbon loss, our data points to the need for further research on the potential long-term effects of local disturbance on the vegetation, and significant effects on local scale carbon fluxes. Moreover, the effects of disturbances could be long-lasting and their role on ecosystem processes should not be underestimated.
机译:在生态系统范围内,泥炭地可以非常灵活地抵抗干扰。但是,它们对局部干扰非常敏感,尤其是机械扰动(例如践踏)。但是,这些扰动对植被的影响以及对泥炭表面沿线的水化学条件的潜在影响尚不清楚。我们使用了三个不同的研究轨迹(研究人员用来进入其研究地点的路径),它们的废弃时间不同,以研究旗舰研究性泥炭地对植被的局部干扰(踩踏)及其短期(≤2年)恢复。此外,我们研究了局部扰动对河流径流事件以及径流水中溶解有机碳(DOC)和颗粒状有机碳(POC)浓度的影响。rn局部扰动严重影响泥炭植被,导致大面积的结疤和搅动泥炭沿废弃路线恢复维管束植物的速度很慢,但仅在一年后就重新建立了功能的泥炭藓层。缺少植被导致沿径流事件数量增加,从而增加了径流POC径流量。在最近废弃的轨道中,地表水中的POC浓度最高,而在废弃时间最长且不受干扰的控制轨道中,径流水中的POC浓度较低。我们将其归因于泥炭藓植被的相对较快恢复。在地表径流或土壤溶液水中,DOC浓度在空间或时间上均无显着差异。虽然就生态系统规模而言,就碳损失而言,局部扰动可以忽略不计,但我们的数据表明需要进一步研究局部扰动对植被的潜在长期影响以及对局部尺度碳通量的重大影响。此外,干扰的影响可能是长期的,不应低估其在生态系统过程中的作用。

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