The DOI matches its Crossref record; 43 of the 44 references it cites were found in a registry or an index.
Rhizosphere priming effect: Its functional relationships with microbial turnover, evapotranspiration, and C–N budgets
Abstract
Understanding soil organic matter (SOM) decomposition and its interaction with rhizosphere processes is a crucial topic in soil biology and ecology. Using a natural 13C tracer method to separately measure SOM-derived CO2 from root-derived CO2, this study aims to connect the level of rhizosphere-dependent SOM decomposition with the C and N balance of the whole plant-soil system, and to mechanistically link the rhizosphere priming effect to soil microbial turnover and evapotranspiration. Results indicated that the magnitude of the rhizosphere priming effect on SOM decomposition varied widely, from zero to more than 380% of the unplanted control, and was largely influenced by plant species and phenology. Balancing the extra soil C loss from the strong rhizosphere priming effect in the planted treatments with C inputs from rhizodeposits and root biomass, the whole plant-soil system remained with a net carbon gain at the end of the experiment. The increased soil microbial biomass turnover rate and the enhanced evapotranspiration rate in the planted treatments had clear positive relationships with the level of the rhizosphere priming effect. The rhizosphere enhancement of soil carbon mineralization in the planted treatments did not result in a proportional increase in net N mineralization, suggesting a possible de-coupling of C cycling with N cycling in the rhizosphere.
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“the SOC can be highly reduced through the disturbance (e.g., tillage practices)”
From Bioenergy production and environmental impacts (2018) · cites this paper as Cheng 2009
In the citing paper
“However, living roots can decrease (50 %) or increase (380 %) SOC mineralisation rates causing losses equivalent to the root C input to soil, the range depending on plant species and age [103].”
From Carbon Sequestration by Perennial Energy Crops: Is the Jury Still Out? (2015) · cites this paper as [103]
In the citing paper
“In addition, decomposition of old SOM can be affected by root priming [103], which varies with root density along the soil profile and crop C balance [99].”
From Carbon Sequestration by Perennial Energy Crops: Is the Jury Still Out? (2015) · cites this paper as [103]
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Metadata
- Authors
- Cheng, W.
- Affiliations
- University of California, Santa Cruz (US)
- Corresponding author
- Cheng, Weixin
- ORCID
- Cheng, Weixin
- Venue
- Soil Biology and Biochemistry
- Publisher
- Elsevier BV
- Published
- 2009-09
- Volume
- 41
- Issue
- 9
- Pages
- 1795-1801
- ISSN
- 0038-0717 (ISSN-L)
- OpenAlex
- W2070571729
- Semantic Scholar
- b52e8624d495ccd5e3ceb3e1876b9e97daa0c326
- Cited by
- 323
- References
- 44
- Citations by year
- 2026: 6 · 2025: 14 · 2024: 23 · 2023: 12 · 2022: 26 · 2021: 24 · 2020: 21 · 2019: 22 · 2018: 26 · 2017: 17 · 2016: 26 · 2015: 13 · 2014: 25 · 2013: 22 · 2012: 17
- FWCI
- 14.69
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Soil Biology and Biochemistry (publishedVersion)
- Funders
- U.S. Department of Agriculture
- University of California, Davis
- Topics
- Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
- Life Sciences › Agricultural and Biological Sciences › Plant Science › Mycorrhizal Fungi and Plant Interactions
- Life Sciences › Agricultural and Biological Sciences › Plant Science › Plant-Microbe Interactions and Immunity
- Keywords
- rhizosphere priming effect, soil organic matter decomposition, evapotranspiration, carbon-nitrogen balance, soil carbon mineralization, soil nitrogen mineralization, 13C tracer, rhizodeposits, plant-soil interactions, plant species effects, phenology
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