The chemical and morphological changes of porous hydrated calcium silicate
material (PS) during the dissolution process in paddy soil were investigate
d by using both a scanning electron microscope (SEM) and an energy dispersi
ve X-ray (EDS) analysis. The results showed that original PS consisted of a
gglomerate of various sizes with almost the same elemental composition. The
SEM images at a high magnification showed that the original PS consisted o
f agglomerates of small platelike crystals (less than or equal to 1 mu m) o
f tobermorite [Ca-5(Si6O18-H-2). 4H(2)O]. On the other hand, elemental comp
osition showed that the PS agglomerates in paddy soil altered to Si- and Ca
-rich agglomerates after incubation for 53 d, The morphological differences
between the two types of agglomerates were observed by SEM at a high magni
fication, The Si-rich agglomerates were similar to the original PS in morph
ology, whereas the Ca-rich agglomerate appeared as a large crystal. The X-r
ay diffraction patterns obtained in a previous study suggested the presence
of quartz and calcite in PS after incubation for 53 d (Saigusa et al, 2000
: Soil Sci, Plant Nutr., 46, 89-95), Si- and Ca-rich agglomerates were iden
tified as silica skeletons of PS and calcite, respectively. It was suggeste
d that the silica skeletons of PS remained as a silicon source for rice pla
nts even after the disappearance of tobermorite revealed by the X-ray diffr
actogram.