Root-induced changes in the availability of nutrients in the rhizosphere.
By Günter Neumann, Volker Römheld, Y. Waisel, A. Eshel, U. Kafkafi. 2002
260 citations recorded by the source corpus.
Subfields: Plant Science, Soil Science
View Paper: https://www.semanticscholar.org/paper/eb8423ff9ee88e30cca676810de0f7b7817a6d07
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Citations in the corpus
- Rhizoeconomics: Carbon costs of phosphorus acquisition (2005, background): “The spatial localization of exudate production near the root apex, prior to the appearance of large microbial populations, may be one means of reducing such competition (Marschner and Römheld, 1996).”
- Different roles of rhizosphere effect and long-term fertilization in the activity and community structure of ammonia oxidizers in a calcareous fluvo-aquic soil (2013, background): “It is well known that the microenvironments in the rhizosphere differ markedly from those in bulk soil owing to interactions among root exudations, plant absorption and rhizosphere microorganisms (Neumann and Römheld, 2002; Sørensen, 1997).”
- 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): “Total PLFA biomass in the rhizosphere significantly increased in comparison with the bulk soil, which can be attributed to root-induced shifts in microbial activity (Neumann and Römheld, 2002).”
- Plant-driven selection of microbes (2009, background): “Strategy I involves the stimulation of proton extrusion, enhanced exudation of reductants and chelators (carboxylates and phenolics) and an enhanced activity of plasma-membrane-bound Fe-(III)-reductase (Marschner 1991; Marschner and Römheld 1994; Rengel 1999).”
- Influence of enhanced malate dehydrogenase expression by alfalfa on diversity of rhizobacteria and soil nutrient availability (2003, background): “Mobilization of other soil nutrients, such as Fe, Mn, or Zn, has been related to complexation with organic acids contained in root exudates (Dinkekaker et al., 1989; Marschner and Römheld, 2001).”
- The dark septate endophytic fungus Phialocephala fortinii is a potential decomposer of soil organic compounds and a promoter of Asparagus officinalis growth (2017, background): “Although P is abundant in agricultural soils, it is mostly in an insoluble form, and it hence cannot be utilized directly by plants (Neumann and Romheld, 2002; Miller et al., 2010; Moe, 2013).”
- Roots of the Second Green Revolution (2007, background): “2002), associated with metal mobilisation in the rhizosphere via protons, phenolics and organic acids in dicots and with phytosiderophores in cereals (Neumann and Römheld 2002; Rengel 1999, 2002).”
- The role of root exudates and allelochemicals in the rhizosphere (2003, background): “duction and release of root exudates favors the further long-term release of nutrients from the solid phase as nutrients in solution are consumed (Neumann and Romheld, 2002).”
- Fertilizer-induced Changes in Rhizosphere Electrical Conductivity: Relation to Forest Tree Seedling Root System Growth and Function (2005, background): “This effect is further confounded by the influence of fertilizer nutrients on ion exchange between root and soil along with root metabolic processes, which may lead to as much as a 2 – 3 unit change in rhizosphere pH compared to bulk soil (Neumann and Romheld 2001).”
- Stability and dynamics of enzyme activity patterns in the rice rhizosphere: Effects of plant growth and temperature (2017, background): “The spatial distribution of the rhizosphere is a dynamic function of the soil matrix and plant properties, including root development and morphology, microbial colonization, nutrient uptake, root exudation and rhizodeposition (Dazzo and Gantner, 2012; Neumann and Romheld, 2002).”
- Root Development and Nutrient Uptake (2006, background): “The rhizosphere can be defined as the volume of soil influenced by root activity; hence, the physical, chemical and biological characteristics within this zone differ drastically from those of bulk soil (Marschner, 1995; Neumann and Römheld, 2000, 2002).”