Abstract
Under arid and semiarid conditions, pedogenic (secondary) carbonates are formed in soil by precipitation of Ca²⁺ from soil parent material with dissolved CO₂ originating from root and rhizomicrobial respiration.
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Gocke, Martina; Pustovoytov, Konstantin; Kuzyakov, Yakov (2011). Carbonate recrystallization in root-free soil and rhizosphere of Triticum aestivum and Lolium perenne estimated by 14C labeling. Biogeochemistry, 103(1-3):209-222.
Under arid and semiarid conditions, pedogenic (secondary) carbonates are formed in soil by precipitation of Ca²⁺ from soil parent material with dissolved CO₂ originating from root and rhizomicrobial respiration.
Item Type: | Journal Article, refereed, original work |
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Communities & Collections: | 07 Faculty of Science > Institute of Geography |
Dewey Decimal Classification: | 910 Geography & travel |
Scopus Subject Areas: | Physical Sciences > Environmental Chemistry
Physical Sciences > Water Science and Technology Physical Sciences > Earth-Surface Processes |
Language: | English |
Date: | 2011 |
Deposited On: | 12 Mar 2015 14:43 |
Last Modified: | 13 Sep 2024 01:35 |
Publisher: | Springer |
ISSN: | 0168-2563 |
OA Status: | Closed |
Publisher DOI: | https://doi.org/10.1007/s10533-010-9456-z |