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Properties of Several Fly Ash Materials in Relation to Use as Soil Amendments

S. M. Pathana, L. A. G. Aylmoreb and T. D. Colmer*,a

a School of Plant Biology, Univ. of Western Australia, 35 Stirling Highway, Crawley 6009, Western Australia, Australia
b School of Earth and Geographical Sciences, Faculty of Natural and Agricultural Sciences, Univ. of Western Australia, 35 Stirling Highway, Crawley 6009, Western Australia, Australia



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Fig. 1. Water retention characteristics of selected soil and fly ash samples from locations in Western Australia and Queensland at different (-5, -25, -100, -250, and -1500 KPa) matric potentials. Data given are means of three replicates ± standard errors. Standard errors are not visible when smaller than the size of the symbols.

 


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Fig. 2. Water retention characteristics of (A) Karrakatta sand and (B) Joel sand with Kwinana fly ash (3 yr old, weathered) incorporated at different rates (% w/w) and at different (-5, -25, -100, -250, and -1500 KPa) matric potentials. Data given are means of three replicates ± standard errors. Standard errors are not visible when smaller than the size of the symbols.

 


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Fig. 3. Effect of Kwinana fly ash (3 yr old, weathered) incorporated at different rates (% w/w) with Karrakatta sand and Joel sand on plant-available water (-5 to -1500 KPa matric potentials). Data given are means of three replicates ± standard errors.

 





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