Diffusive equilibrium in thin films provides evidence of suppression of hyporheic exchange and large-scale nitrate transformation in a groundwater-fed river-Reference-Cited by-同舟云学术

Diffusive equilibrium in thin films provides evidence of suppression of hyporheic exchange and large-scale nitrate transformation in a groundwater-fed river

Published:2014-07-15 Issue:6 Volume:29 Page:1385-1396
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrol. Process.

Author:

Byrne P.¹²,Zhang H.¹,Ullah S.¹³,Binley A.¹,Heathwaite A.L.¹,Heppell C.M.⁴,Lansdown K.⁴⁵,Trimmer M.⁵

Affiliation:

1. Lancaster Environment Centre; Lancaster University; Lancaster LA1 4YQ UK

2. School of Natural Sciences and Psychology; Liverpool John Moores University; Liverpool L3 3AF UK

3. School of Physical and Geographical Sciences; Keele University; Keele ST5 5BG UK

4. School of Geography; Queen Mary University of London; London E1 4NS UK

5. School of Biological and Chemical Sciences; Queen Mary University of London; London E1 4NS UK

Funder

Natural Environment Research Council

Publisher

Wiley

Subject

Water Science and Technology

Reference55 articles.

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3. Temporal variation of hydrological exchange and hyporheic biogeochemistry in a headwater stream during autumn;Argerich;Journal of the North American Benthological Society,2011

4. Revealing the spatial variability of water fluxes at the groundwater-surface water interface;Binley;Water Resources Research,2013

5. Reduction of the hyporheic zone volume due to the stream-aquifer interaction;Boano;Geophysical Research Letters,2008

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