Dissolved organic carbon lability increases with water residence time in the alluvial aquifer of a river floodplain ecosystem-Reference-Cited by-同舟云学术

Dissolved organic carbon lability increases with water residence time in the alluvial aquifer of a river floodplain ecosystem

Published:2015-04 Issue:4 Volume:120 Page:693-706
ISSN:2169-8953
Container-title:Journal of Geophysical Research: Biogeosciences
language:en
Short-container-title:J. Geophys. Res. Biogeosci.

Author:

Helton Ashley M.¹,Wright Meredith S.²,Bernhardt Emily S.³,Poole Geoffrey C.⁴⁵,Cory Rose M.⁶,Stanford Jack A.⁷

Affiliation:

1. Department of Natural Resources and the Environment and the Center for Environmental Sciences and Engineering; University of Connecticut; Storrs Connecticut USA

2. J. Craig Venter Institute; La Jolla California USA

3. Biology Department; Duke University; Durham North Carolina USA

4. Department of Land Resources and Environmental Sciences; Montana State University; Bozeman Montana USA

5. Montana Institute on Ecosystems; Montana State University; Bozeman Montana USA

6. Earth and Environmental Sciences; University of Michigan; Ann Arbor Michigan USA

7. Flathead Lake Biological Station, Division of Biological Sciences; University of Montana; Missoula Montana USA

Funder

Gordon and Betty Moore Foundation

EPA Star Fellowship

Odum School of Ecology

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

Reference65 articles.

1. Floodplain biogeochemical mosaics: A multidimensional view of alluvial soils;Appling;J. Geophys. Res. Biogeosci.,2014

2. Acetate retention and metabolism in the hyporheic zone of a mountain stream;Baker;Limnol. Oceanogr.,1999

3. Rethinking hyporheic flow and transient storage to advance understanding of stream-catchment connections;Bencala;Water Resour. Res.,2011

4. The Subsurface Macrofauna

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