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@ARTICLE{Wiekenkamp:820893,
author = {Wiekenkamp, I. and Huisman, J. A. and Bogena, Heye and Lin,
H. S. and Vereecken, H.},
title = {{S}patial and temporal occurrence of preferential flow in a
forested headwater catchment},
journal = {Journal of hydrology},
volume = {534},
issn = {0022-1694},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2016-06157},
pages = {139 - 149},
year = {2016},
abstract = {The highly dynamic nature of preferential flow in time and
space makes it challenging to identify and analyze its
occurrence at the catchment scale. Novel analysis methods
using soil moisture sensor response times offer an
opportunity to investigate catchment-wide controls on
preferential flow. The aim of this study was to identify
factors that control preferential flow occurrence based on
3-year soil moisture monitoring using a wireless sensor
network in the Wüstebach catchment, Germany. At 101
locations, the sensor response times at three depths (5, 20,
and 50 cm) were classified into one of four classes: (1)
non-sequential preferential flow, (2) velocity-based
preferential flow, (3) sequential flow, and (4) no response.
A conceptual model, postulating that preferential flow in
the Wüstebach catchment is dominated by differences in soil
type, landscape position, and rainfall input, was proposed
for hypothesis testing. To test the conceptual model, the
classification results were combined with spatial and
event-based data to understand and identify controlling
factors. Spatial parameters consisted of hydrological,
topographical, and soil physical and chemical parameters.
Temporal factors included precipitation characteristics and
antecedent soil moisture conditions. The conceptual model as
proposed could only be partly confirmed. Event-based
occurrence of preferential flow was highly affected by
precipitation amount, with a nearly catchment-wide
preferential response during large storm events. During
intermediate events, preferential flow was controlled by
small-scale heterogeneity, instead of showing catchment-wide
patterns. The effect of antecedent catchment wetness on the
occurrence of preferential flow was generally less profound,
although a clear negative relationship was found for
precipitation events with more than 25 mm. It was found that
spatial occurrence of preferential flow was however governed
by small-scale soil and biological features and local
processes, and showed no obvious relationship with any of
the selected spatial parameters. Overall, the results
demonstrate that sensor response time analysis can offer
innovative insights into the spatial–temporal
interrelationship of preferential flow occurrence.},
cin = {IBG-3},
ddc = {690},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000371940900013},
doi = {10.1016/j.jhydrol.2015.12.050},
url = {https://juser.fz-juelich.de/record/820893},
}