Dissolved Organic Matter Chemistry and Transport Along an Arctic Tundra Hillslope

Permafrost thaw is projected to restructure the connectivity of surface and subsurface flow paths, influencing export dynamics of dissolved organic matter (DOM) through Arctic watersheds. Resulting shifts in flow path exchange between both soil horizons (organic‐mineral) and landscape positions (hil...

Ausführliche Beschreibung

Gespeichert in:

Bibliographische Detailangaben
Veröffentlicht in:	Global biogeochemical cycles 2019-01, Vol.33 (1), p.47-62
Hauptverfasser:	Lynch, Laurel M., Machmuller, Megan B., Boot, Claudia M., Covino, Timothy P., Rithner, Christopher D., Cotrufo, M. Francesca, Hoyt, David W., Wallenstein, Matthew D.
Format:	Artikel
Sprache:	eng
Schlagworte:	Analytical methods Arctic carbon cycling Catchment area Catchments Chemical composition Dissolved organic matter Dynamics Flow paths Fluorescence Fluorescence spectroscopy global change biology Headwaters Heterogeneity Magnetic resonance Magnetic resonance spectroscopy Metabolism Microorganisms NMR Nuclear magnetic resonance Organic chemistry Organic matter Organic soils Patchiness Permafrost Physiographic features pore water chemistry preferential flow Soil Soil horizons Spatial heterogeneity Spectroscopy Subsurface flow Surface water Tracers Tundra watershed chemistry Watersheds
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!

Schreiben Sie den ersten Kommentar!