“…Growing in soils with low P availability, plants can response to soil in several ways. The influence of mycorrhizae on P acquisition by plants is well known (Marschner, 1990;Rao and Tak, 2002;Wilcox, 1996). Many plant species increase root secretory activities such as exudation of organic acid (Bertin et al, 2003;Jones, 1998), phytase (Yadav and Tarafdar, 2004) and modulate kinetics of phosphate transport across cellular membranes (Raghothama and Karthikeyan, 2005;Rausch and Bucher, 2002;Schachtman et al, 1998) to absorb more P. Furthermore, formation of root clusters (Neumann et al, 2000;Shane et al, 2003;Shane and Lambers, 2006) and other modifications of root morphology are also important strategies for utilizing P. Based on these, different plant species and genotypes possess different rhizosphere characteristics (Rengel and Marschner, 2005), and the P status in rhizosphere is expected to sharply differ from the bulk soil.…”