|
|
||||||||
Inst. of Soils and Water, The Agric. Res. Organization, The Volcani Center, P.O.B. 6, Bet Dagan 50250, Israel.
* Corresponding author.
ABSTRACT
The effect of ash particle size, pH, and Ca(OH)2 presence on the dissolution and adsorption of B by fly ash in aqueous media was studied. Most of the soluble B was found in the small particles of ash. Dissolution of B was independent of the dissolution of Ca from fly ash. Decreasing the pH from 12.5 to 6 increased both the solubility and the extractability of B. A small amount of B was adsorbed by fly ash at pH 7; this was attributed to a ligand exchange mechanism. Sorption of B increased with increasing pH, up to 12, which could not be explained by ligand exchange but rather with coprecipitation with CaCO3.
Key Words: Alkaline fly ash Boron toxicity Coprecipitation boron-CaCO3
Contribution from The Agric. Res. Organization, The Volcani Center.
Received for publication March 26, 1986.
This article has been cited by other articles:
![]() |
R. J. Donahoe Secondary mineral formation in coal combustion byproduct disposal facilities: implications for trace element sequestration Geological Society, London, Special Publications, January 1, 2004; 236(1): 641 - 658. [Abstract] [PDF] |
||||
![]() |
C.J. Warren, L.J. Evans, and R.W. Sheard Release of Some Trace Elements From Sluiced Fly Ash On Acidic Soils With Particular Reference To Boron Waste Management Research, January 1, 1993; 11(1): 3 - 15. [Abstract] [PDF] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Vadose Zone Journal | ||||
| Soil Science Society of America Journal | Journal of Plant Registrations | The Plant Genome | |||