The chalk hyporheic zone: a true ecotone?

Author:

Pacioglu Octavian,Pârvulescu Lucian

Publisher

Springer Science and Business Media LLC

Subject

Aquatic Science

Reference76 articles.

1. Abesser, C., P. Shand, D. Goodd & D. Peach, 2008. The role of alluvial valley deposits in groundwater surface water exchange in a Chalk river. In Abesser, C., T. Wagener & G. Nuetzmann (eds), Groundwater–Surface Water Interaction: Process Understanding, Conceptualization and Modelling. IAHS Press, Wallingford: 11–20.

2. Allen, D. J., W. G. Darling, D. C. Gooddy, D. J. Lapworth, A. J. Newell, A. T. Williams, D. Allen & C. Abesser, 2010. Interaction between groundwater, the hyporheic zone and a Chalk stream: a case study from the River Lambourn, UK. Hydrogeology Journal 18: 1125–1141.

3. Baker, M. A., C. N. Dahm & H. M. Vallet, 2000. Anoxia, Anaerobic Metabolism and Biogeochemistry of Stream Water–Groundwater Interface. lx. Academic Press, London: 259–283.

4. Borges, N., J. Spindler, G. Strauch & M. Rode, 2006. Temporal variation of hyporheic denitrification in a lowland agricultural drainage system. Geophysical Resources Abstract 8: 105–125.

5. Berrie, A. D., 1992. The chalk stream environment. Hydrobiologia 248: 3–9.

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