Peat depth as a control on moss water availability under evaporative stress-Reference-Cited by-同舟云学术

Peat depth as a control on moss water availability under evaporative stress

Published:2017-10-03 Issue:23 Volume:31 Page:4107-4121
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Dixon Simon J.¹^ORCID,Kettridge Nicholas¹,Moore Paul A.²^ORCID,Devito Kevin J.³^ORCID,Tilak Amey S.¹,Petrone Richard M.⁴,Mendoza Carl A.⁵^ORCID,Waddington James M.²

Affiliation:

1. School of Geography, Earth and Environmental Sciences; University of Birmingham; Edgbaston Birmingham B15 2TT UK

2. School of Geography and Earth Sciences; McMaster University; Hamilton ON L8S 4K1 Canada

3. Department of Biological Sciences; University of Alberta; Edmonton AB T6G 2E9 Canada

4. Department of Geography and Environmental Management; University of Waterloo; Waterloo ON N2L 3G1 Canada

5. Department of Earth and Atmospheric Science; University of Alberta; Edmonton AB T6G 2E3 Canada

Funder

Natural Sciences and Engineering Research Council of Canada

Canadian Natural Resources Limited

Syncrude Canada Ltd

Publisher

Wiley

Subject

Water Science and Technology

Reference81 articles.

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3. The DigiBog peatland development model 1: Rationale, conceptual model, and hydrological basis;Baird;Ecohydrology,2012

4. Anisotropy and depth-related heterogeneity of hydraulic conductivity in a bog peat. I: Laboratory measurements;Beckwith;Hydrological Processes,2003

5. Transport and thermodynamics constrain belowground carbon turnover in a northern peatland;Beer;Geochimica et Cosmochimica Acta,2007

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