As a potential raw material for ceramics manufacture, the effluent fro
m the Devil's Woodyard mud volcano of central Trinidad has been invest
igated. Chemically, the material was found to contain 2% organic matte
r and 54, 18, and 6% SiO2, Al2O3, and FeO3 respectively. Loss on ignit
ion at 1000 degrees C amounted to 13.2% and the soluble sulphate and p
hosphate contents were 0.6 and 0.15% respectively. Mineralogically by
X-ray diffractometry and differential thermal analysis, the high plast
icity effluent was found to be essentially a kaolinitic clay. Some qua
rtz, mica, potash feldspar, and calcite were also detected. Rectangula
r test bars fired at 800-1100 degrees C resulted in the 'black core' p
henomenon and bloating at and above 1000 degrees C. However, bars fire
d for 3 and 4 h at 800-900 degrees C, where no bloating occurred, exhi
bited modulus of rupture and fracture toughness values comparable with
, or superior to, those exhibited by other Trinidad clays fired in exc
ess of 1000 degrees C for 3 h. The associated linear firing shrinkage
was less than 3%.