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Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought
oleh: A. Peyton Smith, Ben Bond-Lamberty, Brian W. Benscoter, Malak M. Tfaily, C. Ross Hinkle, Chongxuan Liu, Vanessa L. Bailey
Format: | Article |
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Diterbitkan: | Nature Portfolio 2017-11-01 |
Deskripsi
The impacts of top down (precipitation) and bottom-up (groundwater rise) wetting processes on carbon sequestration are poorly understood. Here, the authors use incubation experiments to show that drought legacy and pore-scale wetting patterns are important factors controlling short-term carbon dynamics.