Published: Vol 5, Iss 23, Dec 5, 2015 DOI: 10.21769/BioProtoc.1676 Views: 7610
Reviewed by: Tie LiuAnonymous reviewer(s)
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Abstract
Plant survival depends on the ability of root systems to establish themselves in locations where water and nutrients are available for uptake and translocation (Hawes et al., 2003). Rhizosphere influences crop productivity by mediating efficient nutrient transformation, acquisition, and use (Shen et al., 2013). Rhizosphere acidification is a central mechanism for plant mineral nutrition since it contributes to nutrient solubility and the proton motive force (pmf). This pmf is generated by the plasma membrane H+-ATPases (Miller and Smith, 1996; Forde, 2000) in root epidermal and cortical cells, and is coupled to active nutrient acquisition (e.g., N, K, P). Roots are able to acidify the rhizosphere by up to two pH units compared to the surrounding bulk soil mainly through the release of protons, but also bicarbonate, organic acids and CO2. Here we present an easy and inexpensive protocol to quantify protons released to the media by the root system-a method successfully used in our recently published work (Pizzio et al., 2015).
Keywords: RootMaterials and Reagents
Equipment
Procedure
Representative data
Figure 1. Protons released from the roots during day and night hours by Col-0 (empty bars) and transgenic plants overexpressing the type I H+-PPase AVP1 (AVP1-1; Pizzio et al., 2015) (black bars) plants grown in liquid media (mean ± SE; n= 6 pools of 10 plants per line, per time of day, per trial; two independent trials)
Recipes
Acknowledgments
RAG, GAP, and KR were supported by the National Science Foundation (grant no. IOS-1122148). This protocol was adapted from Pizzio et al. (2015).
References
Article Information
Copyright
© 2015 The Authors; exclusive licensee Bio-protocol LLC.
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Category
Plant Science > Plant physiology > Plant growth
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