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Silicon (Si) is assimilated from soil by rice and is deposited in shoots in inter- and intracellularly, resulting in the formation of silicaceous structures, namely phytoliths. During the precipitation of Si, elements present in xylem/phloem sap, including phosphorus (P), can also be occluded in the phytolith. We examined the release of Si and P from the rice straw derived phytolith to elaborate the desilification mechanism, and the potential effects of phytolith as a nutrient ammendment. Data from batch heating experiments revealed that P trapped in the phytolith structure could be released accompanying with the dissolution of the phytolith. The highest values of soluble Si and P were found in the range of 500–700 °C. The chemical composition, X-ray diffraction, infrared spectra and specific surface area (SSA) data suggested that the presence of occluded organic carbon at <500 °C and crystallization of silica at >700 °C …