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000134443 0247_ $$2doi$$a10.2136/vzj2013.01.0009
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000134443 037__ $$aFZJ-2013-02642
000134443 082__ $$a550
000134443 1001_ $$0P:(DE-HGF)0$$aSauer, D.$$b0
000134443 245__ $$aSoil Moisture Assessment over an Alpine Hillslope with Significant Soil Heterogeneity
000134443 260__ $$aMadison, Wis.$$bSSSA$$c2013
000134443 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1394525214_18104
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000134443 500__ $$3POF3_Assignment on 2016-02-29
000134443 520__ $$aWe strive to assess soil water content on a well-studied slow-moving hillslope in  Austria. In doing so, we employ time lapse mapping of bulk electrical conductivity using a  geophysical electromagnetic induction system operated at low induction numbers. This  information is complemented by the acquisition of soil samples for gravimetric water content  analysis during one survey campaign. Simple visual soil sample analysis reveals that the  upper material in the survey area is a spatially highly variable mixture of predominately  sandy, silty, clayey and organic materials. Due to this heterogeneity, classical approaches of  mapping soil moisture on the basis of stationary mapping of electrical conductivity variations  are not successful. Also the time-lapse approach does not allow ruling out some of the  ambiguity inherent to the linkage of bulk electrical conductivity to soil water content.  However, indication is found that time-lapse measurements may have supportive capabilities  to identify regions of low precipitation infiltration due to high soil saturation. Furthermore,  the relationship between the mean electrical conductivity averaged over a full vegetation  period and an already available ecological moisture map produced by vegetation analysis is  found to resemble closely the relationship observed between gravimetric soil water content  and electrical conductivity during the time of sample collection except for highly organic  soils. This leads us to the assumption that the relative soil moisture distribution is temporarily  stable except for those areas characterized by highly organic soils
000134443 536__ $$0G:(DE-HGF)POF2-211$$a211 - Global Earth Monitoring: Global Processes and Change (POF2-211)$$cPOF2-211$$fPOF II$$x0
000134443 7001_ $$0P:(DE-HGF)0$$aPopp, S.$$b1
000134443 7001_ $$0P:(DE-HGF)0$$aDittfurth, A.$$b2
000134443 7001_ $$0P:(DE-Juel1)136836$$aAltdorff, Daniel$$b3
000134443 7001_ $$0P:(DE-HGF)0$$aDietrich, P.$$b4
000134443 7001_ $$0P:(DE-HGF)0$$aPaasche, H.$$b5
000134443 773__ $$0PERI:(DE-600)2088189-7$$a10.2136/vzj2013.01.0009$$n4$$p $$tVadose zone journal$$v12$$x1539-1663
000134443 8564_ $$uhttps://juser.fz-juelich.de/record/134443/files/FZJ-2013-02642.pdf$$yRestricted$$zPublished final document.
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000134443 909CO $$ooai:juser.fz-juelich.de:134443$$pVDB:Earth_Environment$$pVDB
000134443 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)136836$$aForschungszentrum Jülich GmbH$$b3$$kFZJ
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000134443 9132_ $$0G:(DE-HGF)POF3-259H$$1G:(DE-HGF)POF3-250$$2G:(DE-HGF)POF3-200$$aDE-HGF$$bMarine, Küsten- und Polare Systeme$$lTerrestrische Umwelt$$vAddenda$$x0
000134443 9131_ $$0G:(DE-HGF)POF2-211$$1G:(DE-HGF)POF2-210$$2G:(DE-HGF)POF2-200$$3G:(DE-HGF)POF2$$4G:(DE-HGF)POF$$aDE-HGF$$bErde und Umwelt$$lGeosystem: Erde im Wandel$$vGlobal Earth Monitoring: Global Processes and Change$$x0
000134443 9141_ $$y2013
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000134443 915__ $$0StatID:(DE-HGF)1060$$2StatID$$aDBCoverage$$bCurrent Contents - Agriculture, Biology and Environmental Sciences
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