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Geomorphology and vegetation drive hydrochemistry changes in two Northeast Greenland streams

机译:格陵兰溪东北两岸的地貌和植被驱动水利改变

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Climate change is causing drastic landscape changes in the Arctic, but how these changes modify stream biogeochemistry is not clear yet. We examined how catchment properties influence stream nitrogen (N) and dissolved organic carbon concentrations (DOC) in a high-Arctic environment. We sampled two contrasting headwater streams (10-15 stations over 4.8 and 6.8 km, respectively) in Northeast Greenland (74 degrees N). We characterized the geomorphology (i.e., bedrock, solifluction and alluvial types) and the vegetation (i.e., barren, fell field, grassland and tundra types) cover of each subcatchment area draining into each sampling station and collected water samples for hydrochemistry characterization. The two sampled streams differed in geomorphology and vegetation cover in the catchment. Aucellaelv catchment was mostly covered by a 'bedrock' geomorphology (71%) and 'fellfield' vegetation (51%), whereas K AE erelv was mostly covered by 'alluvial' geomorphology (65%) and 'grassland' and 'tundra' vegetation (42% and 41% respectively). Hydrochemistry also differed between the two study streams, with higher concentrations of inorganic N forms in Aucellaelv and lower DOC concentrations, compared to K AE relv. The results from the linear mixed model selection showed that vegetation and geomorphology had contrasting effects on stream hydrochemistry. Subcatchments with higher solifluction sheets and limited vegetation had higher nitrate concentrations but lower DOC concentrations. Interestingly, we also found high variability on the production and removal of nitrate across subcatchments. These results indicate landscape controls to nutrient and organic matter exports via flow paths, soil organic matter stocks and nutrient retention via terrestrial vegetation. Moreover, the results suggest that climate change induced alterations to vegetation cover and soil physical disturbance in high-Arctic catchments will affect stream hydrochemistry, with potential effects in stream productivity, trophic relations as well as change of solute export to downstream coastal areas.
机译:气候变化导致北极的剧烈景观变化,但这些变化如何修改流生物态化尚未清楚。我们检查了集水区如何影响流氮(n)并在高北极环境中溶解的有机碳浓度(DOC)。我们在格陵兰岛东北部(分别为4.8和6.8公里以上的10-15站)进行了取样(10-15站)(74℃)。我们的特征在于地貌(即,基岩,肌肉和发生类型)和植被(即,贫瘠,下降的场,草地,草地和苔原型)覆盖每个取样站,并收集水样用于水化学表征。两种采样的流在集水区内的地貌和植被覆盖物中不同。 Aucellaelv集水区主要由'基岩'地貌(71%)和'颈椎'植被(51%)覆盖,而K ae Erelv主要被“alluvial”地貌(65%)和'草原'和'苔原'植被覆盖(分别为42%和41%)。与K AE Relv相比,水化学在两种研究流之间也有不同浓度的无机N形式,并且较低的DOC浓度。线性混合模型选择的结果表明,植被和地貌对流水化学的对比作用。具有较高型血管片和有限植被的亚迁移具有更高的硝酸盐浓度,但较低的DOC浓度。有趣的是,我们还发现了对分割的生产和去除硝酸盐的高度变化。这些结果表明通过陆地植被的流动路径,土壤有机物质储备和营养保留来营养和有机物质出口的景观控制。此外,结果表明,气候变化诱导对高北极流域的植被覆盖和土壤物理扰动的改变将影响流水力化,流水生产率,营养不良关系的潜在影响以及对下游沿海地区的溶质出口变化。

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