Changes in Sedimentary Phosphorus Burial Following Artificial Eutrophication of Lake 227, Experimental Lakes Area, Ontario, Canada-Reference-Cited by-同舟云学术

Changes in Sedimentary Phosphorus Burial Following Artificial Eutrophication of Lake 227, Experimental Lakes Area, Ontario, Canada

Published:2020-08 Issue:8 Volume:125 Page:
ISSN:2169-8953
Container-title:Journal of Geophysical Research: Biogeosciences
language:en
Short-container-title:J. Geophys. Res. Biogeosci.

Author:

O'Connell D. W.¹²^ORCID,Ansems N.³⁴,Kukkadapu R. K.⁵^ORCID,Jaisi D.⁶^ORCID,Orihel D. M.⁷^ORCID,Cade‐Menun B. J.⁸,Hu Y.⁹^ORCID,Wiklund J.¹⁰^ORCID,Hall R. I.¹⁰^ORCID,Chessell H.²,Behrends T.⁴,Van Cappellen P.²

Affiliation:

1. Department of Civil, Structural and Environmental Engineering Trinity College Dublin Dublin 2 Ireland

2. Water Institute, Ecohydrology Research Group University of Waterloo Waterloo Ontario Canada

3. Soil Geography and Landscape Group Wageningen University Wageningen The Netherlands

4. Department of Earth Sciences, Faculty of Geosciences Utrecht University Utrecht The Netherlands

5. Environmental Molecular Sciences Laboratory Pacific Northwest National Laboratory Richland WA USA

6. Department of Plant and Soil Science University of Delaware Newark DE USA

7. School of Environmental Studies Queen's University Kingston Ontario Canada

8. Swift Current Research and Development Centre Agriculture and Agri‐Food Canada Swift Current Saskatchewan Canada

9. Canadian Light Source Saskatoon Saskatchewan Canada

10. Department of Biology University of Waterloo Waterloo Ontario Canada

Publisher

American Geophysical Union (AGU)

Subject

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

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JG005713

Reference92 articles.

1. Biogenic phosphorus in oligotrophic mountain lake sediments: Differences in composition measured with NMR spectroscopy

2. Sediment Depth Attenuation of Biogenic Phosphorus Compounds Measured by 31P NMR

3. Carbon to phosphorus ratios in sediments: Implications for nutrient cycling

4. The phosphorus composition of a diverse series of Australian sediments

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