“…At the process of synthesizing SPF by use of PMS and K 2 CO 3 , K 2 CO 3 decomposed at 800~1000°C into K 2 O and CO 2 , and K 2 O reacted with CaO, SiO 2 , or MgO in PMS to produce the potassium silicate crystalline phases (Ca 1.917 K 0.166 SiO 4 , K 2 MgSiO 4 , K 4 CaSi 3 O 9 ) and amorphous phases. In previous studies, Ca 1.917 K 0.166 SiO 4 and K 2 MgSiO 4 have been found in the synthetic slowrelease K fertilizer: Yamada et al studied the preparation of a slow-release potassium fertilizer using rice husks, dolomite, and potassium carbonate, and Tokunaga et al synthesized a slow-release potassium fertilizer using coal ash and KOH, and both studies found that K 2 MgSiO 4 in the fertilizers was the slow-release characteristic (Yamada et al, 1994;Tokunaga et al, 1991); Shen et al investigated the crystallizability of a slow-release potassium silicate fertilizers, the result showed that the existence of Ca 1.917 K 0.166 SiO 4 and the amorphous phase in the fertilizer was the main cause for the slow-release characteristic of the fertilizer (Shen et al, 2005). The major constituent phases in SPF are the crystalline phases Ca 1.917 K 0.166 SiO 4 , K 2 MgSiO 4 , and K 4 CaSi 3 O 9 and the amorphous phases, which facilitated the release of indissoluble nutrients such as Ca, Si, and Mg from the SPF, but slowed the release of K; as a result, SPF possesses the slow-release characteristic.…”