Articles | Volume 17, issue 7
Hydrol. Earth Syst. Sci., 17, 2569–2579, 2013
Hydrol. Earth Syst. Sci., 17, 2569–2579, 2013

Research article 09 Jul 2013

Research article | 09 Jul 2013

Gaining and losing stream reaches have opposite hydraulic conductivity distribution patterns

X. Chen et al.

Related subject area

Subject: Groundwater hydrology | Techniques and Approaches: Instruments and observation techniques
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Cited articles

Banzhaf, S., Krein, A., and Scheytt, T.: Investigative approaches to determine exchange processes in the hyporheic zone of a low permeability riverbank, Hydrogeol. J., 19, 591–601,, 2011.
Bouwer, H.: Artificial recharge of groundwater: hydrogeology and engineering, Hydrogeol. J., 10, 121–142, 2002.
Chen, X. H.: Streambed hydraulic conductivity for rivers in south-central Nebraska, J. Am. Water Resour. Assoc., 40, 561–574, 2004.
Chen, X. H.: Hydrologic connections of a stream-aquifer-vegetation zone in south-central Platte River valley, Nebraska, J. Hydrol., 333, 554–568, 2007.
Chen, X. H.: Depth-dependent hydraulic conductivity distribution patterns of a streambed, Hydrol. Process., 25, 278–287,, 2011.