
 
The  increase  of  temperature  from  1000°C  to 
1050°C reduced the density for about 2%. It aligns 
with the previous study by Huda and Astuti (2012), 
showing  that  adding  20°C  heating  temperature 
reduced  the  brick  density.  The  effect  of  adding 
duration  of  calcination  temperature  reduced  the 
density.  
3.1.3  Water Absorption 
The density in every composition and calcination is 
shown in Table 7.  
 Table 7: Water Absorption of fine ALWA 
Water absorption 
(ASTM) (%) 
 
The water absorption value is shown in Table 7 
shows  that  almost  all  of  the  values  meet  the 
requirement (ASTM C 330-04) less than 20%. The 
water absorption value is in the range of 11-20.5%. 
The smallest water absorption occurs at calcination 
temperature of 1050 °C for 6 hours by 11-12.5%. 
The addition of fly ash to water absorption of fine 
ALWA reduces the water absorption of fine ALWA. 
The addition of calcination temperature from 1000°C 
to 1050°C reduces water absorption of fine ALWA. 
The addition of duration of calcination temperature 
reduces water absorption of fine ALWA  
3.2  X-Ray Diffraction Analysis 
Xray diffraction analysis for fine ALWA FA-0-1000-
6,  fine  ALWA  FA-0-1050-6,  fine  ALWA  FA-30-
1050-6, fine ALWA FA-50-1050-6, fine ALWA FA-
0-1050-4, analysis fine ALWA FA-30-1050-4, fine 
ALWA FA-50-1050-4 discribe below.  
The diffraction pattern is shown in figure 6 forms 
scattered  and  peaked.  It  shows  that  in  temperature 
1000°C duration 6 hours, the minerals that appeared 
are quartz (SiO2), anorthite (Al2CaO8Si2), hematite., 
calcite  (CaCO3),  indialite  (Al4Mg2O18Si5)  and 
silimanite (Al2SiO5).  
Xray  diffraction  of  fine  ALWA  100%  Sidoarjo 
mud, with calcination temperature 1050°C for 6 hours 
is shown in figure 7.  
The  diffraction  pattern  presented  in  figure  7 
shows  that  mineral  occure  are  anorthite 
(Al2CaO8Si2),  quartz  (SiO2),  hematite  (Fe2O3), 
Indialite  (Al2Mg2O18Si5),  Calcite  (CaCO3). 
Silimanite has not been detected in this sample. 
Xray  diffraction  of  fine  ALWA  70%  Sidoarjo 
mud-30%  Fly  Ash,  with  calcination  temperature 
1050°C for 6 hours is shown in figure 8. 
The  diffraction  pattern  presented  in  figure  8 
shows that minerals occuref in higher peak are quartz 
(SiO2),  anorthite  (Al2CaO8Si2)  and  hematite 
(Fe2O3). In the short peak, calcite, silimanie, and a 
little indialite can be found. 
Xray  diffraction  of  fine  ALWA  50%  Sidoarjo 
mud-50%  Fly  Ash,  with  calcination  temperature 
1050°C for 6 hours shown in figure 9. 
Xray  diffraction  of  fine  ALWA  100%  Sidoarjo 
mud, with calcination temperature 1050°C for 4 hours 
shown in figure 10. 
The diffraction pattern shown in figure 10 show 
that  mineral  occure  in  higher  peak  are  anorthite 
(Al2CaO8Si2) quartz (SiO2), and hematite (Fe2O3). 
The short peak occur calcite and indialite.  
Xray  diffraction  of  fine  ALWA  70%  Sidoarjo 
mud-30%  Fly  ash,  with  calcination  temperature 
1050°C for 4 hours shown in figure 12. 
The diffraction pattern shown in figure 12 show 
that  mineral  occure  in  higher  peak  are  anorthite 
(Al2CaO8Si2) quartz (SiO2), and hematite (Fe2O3). 
The short peak occur calcite, silimanite and indialite.  
Xray  diffraction  of  fine  ALWA  50%  Sidoarjo 
mud-50%  Fly  ash,  with  calcination  temperature 
1050°C for 4 hours shown in figure 13. 
The diffraction pattern shown in figure 13 show 
that mineral occure in FA-50-1050-4 same with FA-
30-1050-4.  
 
 
 
 
  
 
 
Study of Fine Artificial Lightweight Aggregate (ALWA) from Sidoarjo-Mud and Fly Ash with Different Calcination and Composition
181