Solute Movement in the Rhizosphere

By P. Tinker, P. Nye. 2000

602 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/a701116e24a5d5e84a0f2336b511f4b6d3fa1a61

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In Plant Science

Citations in the corpus

A dynamic model for the combined effects of N, P and K fertilizers on yield and mineral composition; description and experimental test (2007, methodology): “These and a number of other soil chemical processes can affect nutrient availability (Tinker and Nye 2000).”
Acquisition of phosphorus and nitrogen in the rhizosphere and plant growth promotion by microorganisms (2009, background): “Orthophosphate is rapidly depleted in the immediate vicinity of plant roots, and as such a large concentration gradient occurs across the rhizosphere between bulk soil and the root surface (Gahoonia and Nielsen 1997; Tinker and Nye 2000; Fig.”
Effects of Root Exudates in Microbial Diversity and Activity in Rhizosphere Soils (2008, background): “The role of phosphatases in the rhizosphere remains uncertain (Tinker and Nye 2000).”
Plant species traits and capacity for resource reduction predict yield and abundance under competition in nitrogen‐limited grassland (2006, background): “Journal compilation © 2006 British Ecological Society Blackwell Publishing LtdPlant species traits and capacity for resource reduction predict yield and abundance under competition in nitrogen-limited grassland J. FARGIONE*† and D. TILMAN”
A dynamic root system growth model based on L-Systems (2010, background): “The root system grew in a pot with a bottom radius of 3 cm, a top radius of 5 cm and a height of 10 cm. Model parameters were taken from liter- ature and represent typical values for phosphate uptake from soil by maize (Tinker and Nye 2000; Föhse et al. 1991).”
Plant mechanisms to optimise access to soil phosphorus (2009, background): “Characteristics of roots (Table 1) that assist exploration of soil and P acquisition include: high rootmass ratio (i.e. a large rootmass as a proportion of total plant mass; Tinker and Nye 2000), high root elongation rate (Silberbush and Barber 1983; Wissuwa 2003), high specific root length or ‘SRL’”
Modelling the rhizosphere: a review of methods for ‘upscaling’ to the whole‐plant scale (2006, methodology): “…is the volumetric water content of the soil, u is the Darcy flux of water and D is the diffusion coefficient of nutrient in the pore solution (¼ DLf where DL is the diffusion coefficient in water and f is the diffusion impedance factor; Tinker & Nye 2000), t is time and ds is defined below.”
Mechanisms of plant competition for nutrients, water and light (2013, background): “If we assume that uptake is a linear function of the supply per unit root length over low nutrient supplies (Tinker & Nye 2000), then over this range fðSLÞ ¼ SL AllocR SRL NR½ eqn 3 where AllocR is the relative allocation of acquired nutrients to root biomass, [NR] is the nutrient concentration of…”
Mycorrhizal Fungi Can Dominate Phosphate Supply to Plants Irrespective of Growth Responses1 (2003, background): “…contribution to total P uptake have often assumed that the direct and mycorrhizal uptake pathways act in concert, although it is recognized that uptake directly from soil may decrease as the concentration of P in the soil solution adjacent to the roots becomes depleted (Tinker and Nye, 2000).”
Arbuscular Mycorrhizal Mediated Nutrition in Plants (2009, background): “This can at least partially be attributed to the assumption that AM fungi have little capacity to enhance plant uptake of mobile ions such as NO3− because these ions move rapidly in soil (Tinker and Nye, 2000).”
Trade-Offs in Arbuscular Mycorrhizal Symbiosis: Disease Resistance, Growth Responses and Perspectives for Crop Breeding (2017, positive): “In the ajority of soils, phosphate supply is li ited due to rapid i obilisation by free cations [14].”
Ecophysiological traits associated with the competitive ability of invasive Australian acacias (2011, positive): “Mass flow of nutrients requires adequate soil water to supply transpirational demand and hence operates at the expense of WUE (Barber, 1995; Tinker & Nye, 2000; Raven et al., 2004; Cramer et al., 2009).”
Resource Exchange in the Rhizosphere: Molecular Tools and the Microbial Perspective (2006, background): “This soil structure strongly influences general rhizosphere resource exchange (e.g., Hillel 1998, Tinker & Nye 2000).”