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The Legacy of a Severe Wildfire on Stream Nitrogen and Carbon in Headwater Catchments

机译:在散水集液中散射氮气和碳的严重野火的遗产

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Large, high-severity wildfires alter the physical and biological conditions that determine how catchments retain and release nutrients and regulate streamwater quality. The short-term water quality impacts of severe wildfire are often dramatic, but the longer-term responses may better reflect terrestrial and aquatic ecosystem recovery. We followed streamwater chemistry for 14years after the largest fire in recorded Colorado history, the 2002 Hayman Fire, to characterize patterns in nitrogen (N) and carbon (C) export. Throughout the post-fire period, stream nitrate and total dissolved N (TDN) remained elevated in 10 burned catchments relative to pre-burn periods and 4 unburned control catchments. Both the extent of fire in a catchment and wildfire severity influenced stream N concentrations. Nitrate was more than an order of magnitude higher in streams draining catchments that burned to a high extent (>60% of their areas) compared to unburned catchments. Unburned catchments retained more than 95% of atmospheric N inputs, but N retention in burned catchments was less than half of N inputs. Unlike N, stream C was elevated in catchments that burned to a lesser extent (30-60% of their areas burned), compared to either unburned or extensively burned catchments. Remotely sensed estimates of upland and riparian vegetation cover suggest that burned forests could require several more decades before forest cover and nutrient demand return to pre-fire levels. The persistent stream N increases we report are below drinking water thresholds, but exceed ecoregional reference concentrations for healthy stream ecosystems and indicate that extensively burned headwater catchments no longer function as strong sinks for atmospheric N. Combined with increasing trends in wildfire severity and elevated N deposition, our findings demonstrate the potential for substantial post-wildfire changes in ecosystem N retention and have implications for nutrient export to downstream waters.
机译:大,高严重程度的野火改变了决定集水器如何保留和释放营养素并调节流水质的物理和生物条件。严重野火的短期水质影响往往是戏剧性的,但长期反应可能更好地反映陆地和水生生态系统恢复。在2002年海曼火灾记录的科罗拉多历史上最大的火灾之后,我们跟随了14年的Streamwater化学,以表征氮气(n)和碳(c)出口的图案。在整个火灾后时期,硝酸盐和总溶解的N(TDN)相对于预燃烧期和4个未燃烧的对照流量仍然升高。集水区和野火严重程度的火灾程度都影响了流N浓度。与未燃烧的流域相比,硝酸盐在流量排出的流域中燃烧到高度(> 60%)的流域的氮酸量高。未燃烧的流域保留超过95%的大气输入,但燃烧的流域的保留不到N个输入的一半。与N不同,流C升高,在较小程度上燃烧到较小程度(燃烧的30-60%),与未燃烧或广泛的燃烧的集水区相比。普通和河岸植被覆盖的远程感官估计表明,森林覆盖和营养需求恢复到火灾水平之前,烧毁的森林可能需要几十年。我们报告的持久性流量增加是饮用水阈值的低于饮用水阈值,但超过健康流生态系统的常态参考浓度,并表明广泛的燃烧的沿着大气压的强水槽不再起作用。结合野火严重程度的增加趋势和升高的次数,我们的研究结果证明了实质性野外野火的潜力,生态系统N保留的变化,并对营养出口导出到下游水域有影响。

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