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Academic Journals
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From:Hydrology and Earth System Sciences (Vol. 25, Issue 9) Peer-ReviewedThe direct vapor equilibration laser spectrometry (DVE-LS) method has been developed for obtaining matrix-bound water stable isotope data in soils, the critical zone, and bedrock, deriving therefrom subsurface water flow...
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From:Biogeosciences (Vol. 18, Issue 16) Peer-ReviewedDiel variability in stream NO3- concentration represents the sum of all processes affecting NO3- concentration along the flow path. Being able to partition diel NO3- signals into portions related to different biochemical...
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From:Biogeosciences (Vol. 18, Issue 15) Peer-ReviewedWe developed a setup for a fully automated, high-frequency in situ monitoring system of the stable water isotope deuterium and .sup.18 O in soil water and tree xylem. The setup was tested for 12 weeks within an isotopic...
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From:PLoS ONE (Vol. 12, Issue 8) Peer-ReviewedPurpose To investigate in vivo morphological and functional correlates of oxaliplatin-induced peripheral neuropathy (OXA-PNP) by magnetic resonance neurography (MRN). Methods Twenty patients (7 female, 13 male,...
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From:Soil (Vol. 5, Issue 1) Peer-Reviewed
The short-term dynamics of carbon and water fluxes across the soil-plant-atmosphere continuum are still not fully understood. One important constraint is the lack of methodologies that enable simultaneous...
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From:Earth System Science Data (Vol. 12, Issue 1) Peer-ReviewedKnowledge of water and energy fluxes is key for urban planning and design. Nevertheless, hydrological data from urban environments are sparse, and, as a result, many processes are still poorly understood and thus...
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From:Hydrology and Earth System Sciences (Vol. 24, Issue 2) Peer-ReviewedUnderstanding components of the total streamflow is important to assess the ecological functioning of rivers. Binary or two-component separation of streamflow into a quick and a slow (often referred to as baseflow)...
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From:Hydrology and Earth System Sciences (Vol. 23, Issue 7) Peer-Reviewed
The water isotopic composition of throughfall is affected by complex diffusive exchange with ambient water vapour, evaporative enrichment of heavy isotopes, and mixing processes in the tree canopy. All interception...
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From:Hydrology and Earth System Sciences (Vol. 20, Issue 2) Peer-ReviewedSeveral controls are known to affect water quality of stream networks during flow recession periods, such as solute leaching processes, surface water-groundwater interactions as well as biogeochemical in-stream turnover...
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From:Geoscientific Model Development (Vol. 14, Issue 4) Peer-ReviewedWater fluxes at the soil-atmosphere interface are a key piece of information for studying the terrestrial water cycle. However, measuring and modeling water fluxes in the vadose zone poses great challenges. While direct...
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From:Earth System Science Data (Vol. 12, Issue 4) Peer-ReviewedThe stable isotopes of oxygen and hydrogen, .sup.18 O and .sup.2 H, provide information on water flow pathways and hydrologic catchment functioning. Here a data set of time series data on precipitation and streamflow...
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From:Hydrology and Earth System Sciences (Vol. 24, Issue 12) Peer-ReviewedHillslope-stream connectivity controls runoff generation, during events and during baseflow conditions. However, assessing subsurface connectivity is a challenging task, as it occurs in the hidden subsurface domain where...
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From:Biogeosciences (Vol. 15, Issue 7) Peer-ReviewedDiel fluctuations of stream water DOC concentrations are generally explained by a complex interplay of different instream processes. We measured the light absorption spectrum of water and DOC concentrations in situ and...
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From:Hydrology and Earth System Sciences (Vol. 20, Issue 3) Peer-ReviewedClimate change is expected to impact the water cycle and severely affect precipitation patterns across central Europe and in other parts of the world, leading to more frequent and severe droughts. Usually when...
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From:Hydrology and Earth System Sciences (Vol. 23, Issue 11) Peer-ReviewedThe spatial and temporal controls of preferential flow (PF) during infiltration are still not fully understood. As soil moisture sensor networks allow us to capture infiltration responses in high temporal and spatial...
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From:Hydrology and Earth System Sciences (Vol. 22, Issue 1) Peer-ReviewedByline: Sibylle Kathrin Hassler, Markus Weiler, Theresa Blume To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
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From:Proceedings of the International Association of Hydrological Sciences (Vol. 383) Peer-ReviewedPrecipitation deficits and temperature anomalies are often the main cause for low flows and summer streamflow droughts. However, where groundwater is the main contribution to sustain water availability and ecological...
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From:Earth System Science Data (Vol. 12, Issue 1) Peer-ReviewedPluvial or flash floods generated by heavy precipitation events cause large economic damage and loss of life worldwide. As discharge observations from such extreme occurrences are rare, especially on the scale of small...
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From:Biogeosciences (Vol. 18, Issue 3) Peer-ReviewedThe phosphorus (P) concentration of soil solution is of key importance for plant nutrition. During large rainfall events, the P concentration is altered by lateral and vertical subsurface storm flow (SSF) that...
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From:Hydrology and Earth System Sciences (Vol. 24, Issue 6) Peer-ReviewedPreferential flow strongly controls water flow and transport in soils. It is ubiquitous but difficult to characterize and predict. This study addresses the occurrence and the evolution of preferential flow during the...