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. 2012 Apr 4;3:134. doi: 10.3389/fmicb.2012.00134

Figure 5.

Figure 5

X-ray diffraction analyses of clay size fraction from Shovelers Sink soil showing illite–smectite (I/S) as dominant mineral. Small amounts of illite (I), kaolinite (Ka), and quartz (Qz) also exist. The 13.6-Å [I/S (001)] peak in the untreated sample expanded to 15.2 Å by ethylene glycol treatment, and collapsed to 9.9 Å by heat treatment. The 7.2-Å [kaolinite (001)] and 3.6-A [kaolinite (002)] peaks in the untreated sample disappeared by heating at 550°C.