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首页> 外文期刊>Hydrology and Earth System Sciences >The influence of riparian evapotranspiration on stream hydrology and nitrogen retention in a subhumid Mediterranean catchment
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The influence of riparian evapotranspiration on stream hydrology and nitrogen retention in a subhumid Mediterranean catchment

机译:河岸蒸散对地中海半湿润地区流水文学和氮素保留的影响

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Riparian evapotranspiration (ET) can influence stream hydrology at catchment scale by promoting the net loss of water from the stream towards the riparian zone (i.e.,?stream hydrological retention). However, the consequences of stream hydrological retention on nitrogen dynamics are not well understood. To fill this gap of knowledge, we investigated changes in riparian ET, stream discharge, and nutrient chemistry in two contiguous reaches (headwater and valley) with contrasted riparian forest size in a small forested Mediterranean catchment. Additionally, riparian groundwater level?(ih/isubgw/sub) was measured at the valley reach. The temporal pattern of riparian ET was similar between reaches, and was positively correlated with ih/isubgw/sub (iρ/i??=??0.60) and negatively correlated with net riparian groundwater inputs (iρ/i??&???0.55). During the vegetative period, stream hydrological retention occurred mostly at the valley reach (59?% of the time), and was accompanied by in-stream nitrate release and ammonium uptake. During the dormant period, when the stream gained water from riparian groundwater, results showed small influences of riparian ET on stream hydrology and nitrogen concentrations. Despite being a small component of annual water budgets (4.5?%), our results highlight that riparian ET drives stream and groundwater hydrology in this Mediterranean catchment and, furthermore, question the potential of the riparian zone as a natural filter of nitrogen loads.
机译:河岸蒸散量(ET)可以通过促进水流向河岸带的净损失(即“溪流水文滞留量”)来影响流域水文学。但是,人们对河流水文滞留对氮动力学的影响尚不十分了解。为了填补这一知识空白,我们调查了两个小河段(上游水源和山谷)的河岸ET,溪流排放和养分化学的变化,在一个地中海小森林流域,河岸森林面积形成了对比。另外,在河谷测得河岸地下水水位?( h gw )。河岸域ET的时间模式在各距离之间相似,并且与 h gw (ρ ?? = 0.60)成正相关,而与与河岸净地下水输入量相关(ρΔθ<0.55)。在营养期内,溪流的水文滞留主要发生在河谷河段(占时间的59%),并伴有溪流中硝酸盐的释放和铵的吸收。在休眠期,当河流从河岸地下水中获取水时,结果表明河岸ET对河流水文和氮浓度的影响较小。尽管仅占年度水预算的一小部分(4.5%),但我们的研究结果突出表明,河岸ET推动了这个地中海流域的河流和地下水水文学,此外,人们质疑河岸带作为天然氮负荷过滤器的潜力。

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