Division of Terrestrial Ecosystem Research, Department of Microbiology and
Ecosystem Science, Center of Microbiology and Environmental Systems Science, University of Vienna, Althanstr. 14, 1090 Vienna,
Austria
Division of Terrestrial Ecosystem Research, Department of Microbiology and
Ecosystem Science, Center of Microbiology and Environmental Systems Science, University of Vienna, Althanstr. 14, 1090 Vienna,
Austria
Division of Terrestrial Ecosystem Research, Department of Microbiology and
Ecosystem Science, Center of Microbiology and Environmental Systems Science, University of Vienna, Althanstr. 14, 1090 Vienna,
Austria
Division of Terrestrial Ecosystem Research, Department of Microbiology and
Ecosystem Science, Center of Microbiology and Environmental Systems Science, University of Vienna, Althanstr. 14, 1090 Vienna,
Austria
Judith Prommer
Division of Terrestrial Ecosystem Research, Department of Microbiology and
Ecosystem Science, Center of Microbiology and Environmental Systems Science, University of Vienna, Althanstr. 14, 1090 Vienna,
Austria
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Total article views: 3,360 (including HTML, PDF, and XML)
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2,199
1,062
99
3,360
241
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150
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PDF: 1,062
XML: 99
Total: 3,360
Supplement: 241
BibTeX: 108
EndNote: 150
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Total article views: 667 (including HTML, PDF, and XML)
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301
358
8
667
182
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HTML: 301
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Total: 667
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Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 4,027 (including HTML, PDF, and XML)
Thereof 3,560 with geography defined
and 467 with unknown origin.
Total article views: 3,360 (including HTML, PDF, and XML)
Thereof 3,009 with geography defined
and 351 with unknown origin.
Total article views: 667 (including HTML, PDF, and XML)
Thereof 551 with geography defined
and 116 with unknown origin.
Efforts to understand the global phosphorus (P) cycle are limited by the scarcity of global data on rates of soil P processes, as well as on its environmental controls. Here, we present a novel approach using radiophosphorus labeling of soils, which allows for the measurement of fluxes of abiotic and biotic soil P processes. This approach is also suitable for strongly weathered and P-depleted soils. Biotic processes are corrected for abiotic processes by comparing live and sterile soils.
Efforts to understand the global phosphorus (P) cycle are limited by the scarcity of global data...