“…Below ground traits that influence the acquisition of mineral elements by plants include, (1) root characteristics, such as root elongation rate, lateral root production, specific root length (length/mass quotient), root length density (root length / soil volume), reduced metabolic load of roots (aerenchyma formation) and root hair length and abundance, all of which increase the volume of soil explored by the root system and the surface area for the uptake of mineral elements, (2) the proliferation of roots in discrete patches of soil containing greater concentrations of mineral elements, such as topsoil horizons rich in organic matter, (3) modification of rhizosphere pH and the exudation of low molecular weight organic solutes and/or enzymes, which influence the concentration of mineral elements in the soil solution, (4) high-capacity uptake systems for mineral nutrients, and (5) interactions with microbes either intimately, through mycorrhizal associations or nodulation by rhizobia, or loosely, through the culture of beneficial microbes or exclusion of detrimental microbes in the rhizosphere. None of these below ground traits work in isolation of one another and it is, therefore, important to consider (1) how they interact with one another , (2) how they interact with the environment (Oburger et al 2011;Jin et al 2012), and (3) how they interact with crop management practices (George et al 2011;Nazeri et al 2013).…”