2020
DOI: 10.1007/s10661-020-08733-0
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Snowmelt periods as hot moments for soil N dynamics: a case study in Maine, USA

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Cited by 6 publications
(3 citation statements)
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“…Hillslopes produce relatively transient VIE features and may often be seen as extensions of other VIEs, such as hillslope seeps co-located with a wetland or the unchannelized swales that contribute to a non-perennial network. In cold regions, snow, ice and permafrost can create an impermeable layer resulting in near-surface soil being inundated for days to weeks during spring thaw (Coles et al 2017, Patel et al 2020. In dry regions, intense precipitation that exceeds the local infiltration capacity can result in water ponding on the surface of hillslopes or overland flow generation down hillslopes, which can be exacerbated by initial hydrophobicity of dry soil (Kirkby et al 2002).…”
Section: Hillslopes With Surface Runoffmentioning
confidence: 99%
“…Hillslopes produce relatively transient VIE features and may often be seen as extensions of other VIEs, such as hillslope seeps co-located with a wetland or the unchannelized swales that contribute to a non-perennial network. In cold regions, snow, ice and permafrost can create an impermeable layer resulting in near-surface soil being inundated for days to weeks during spring thaw (Coles et al 2017, Patel et al 2020. In dry regions, intense precipitation that exceeds the local infiltration capacity can result in water ponding on the surface of hillslopes or overland flow generation down hillslopes, which can be exacerbated by initial hydrophobicity of dry soil (Kirkby et al 2002).…”
Section: Hillslopes With Surface Runoffmentioning
confidence: 99%
“…Dochází k jarnímu tání a z půdy bez vegetačního krytu jsou dusičnany, velmi slabě navázané na sorpční komplex půdy, lehce vymývány do vodních toků(Scheffer a Schachtschabel 2002). Stejné jarní peaky koncentrací dusičnanů popisují iKvítek et al (2009),Kvítek and Doležal (2003),Dinnel a Bratkovich (1993) aPatel et al (2020). Jako kritické podmínky pro koncentrace dusičnanů se tedy jeví orná půda bez vegetačního krytu v kombinaci s vysokými průtoky způsobenými táním či deštěm.…”
unclassified
“…Dochází k jarnímu tání a z půdy bez vegetačního krytu jsou dusičnany, velmi slabě navázané na sorpční komplex půdy, lehce vymývány do vodních toků(Scheffer a Schachtschabel 2002). Stejné jarní peaky koncentrací dusičnanů popisují iKvítek et al (2009),Kvítek and Doležal (2003),Dinnel a Bratkovich (1993) aPatel et al (2020). Jako kritické podmínky pro koncentrace dusičnanů se tedy jeví orná půda bez vegetačního krytu v kombinaci s vysokými průtoky způsobenými táním či deštěm.…”
unclassified