Rhizosphere Effects on Decomposition
By W. Cheng, Dale W. Johnson, S. Fu. 2003
311 citations recorded by the source corpus.
Subfields: Environmental Engineering, Nature and Landscape Conservation, Soil Science
View Paper: https://www.semanticscholar.org/paper/229d15b1e2cb8635136c6e4e81255232cf7d78a0
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In Environmental Engineering
In Nature and Landscape Conservation
In Soil Science
Citations in the corpus
- Acquisition of phosphorus and nitrogen in the rhizosphere and plant growth promotion by microorganisms (2009, background): “In addition, a rhizosphere ‘priming effect’ has been suggested to be involved in the decomposition of native soil organic matter around roots (Cheng et al. 2003; Kuzyakov 2002).”
- Rhizosphere priming effect: A meta-analysis (2017, unknown): “But results from N fertilization experiments have indicated an inconsistent role of soil N status in regulating RPEs (Liljeroth et al., 1994; Cheng et al., 2003; Hoosbeek et al., 2006; Kumar et al., 2016).”
- Responses of extracellular enzyme activities and microbial community in both the rhizosphere and bulk soil to long-term fertilization practices in a fluvo-aquic soil (2012, background): “Soil samples were collected at the wheat reproductive stage in early May 2010, then rhizosphere effects tend to be most pronounced (Cheng et al., 2003).”
- Arbuscular mycorrhizal hyphae promote priming of native soil organic matter mineralisation (2016, background): “Although stimulatory effects of roots on SOM mineralisation have been frequently reported (e.g. Cheng et al. 2003; Paterson et al. 2008; De Graaff et al. 2009), whether AM hyphae have analogous effects is not clear.”
- Plant inter-species effects on rhizosphere priming of soil organic matter decomposition (2013, unknown): “Since the RPE is plant-species specific (Fu and Cheng, 2002; Cheng et al., 2003), it may also vary with plant inter-species interactions.”
- Does accelerated soil organic matter decomposition in the presence of plants increase plant N availability (2009, unknown): “Plant roots are an important source of labile C (root exudates and other rhizodeposits, Hu ¨ tsch et al., 2002), and several studies have shown that when plants are present, soil organic matter decomposition can increase up to 380% compared to soil incubations lacking plants ( Cheng et al., 2003 ).”