2012
DOI: 10.3176/oil.2012.3.07
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The Study of Hydration and Carbonation Reactions and Corresponding Changes in the Physical Properties of Co-Deposited Oil Shale Ash and Semicoke Wastes in a Small-Scale Field Experiment

Abstract: Oil shale ash and semicoke, solid residues from the oil shale industry, are today disposed of separately in landfills which pose a considerable environmental hazard. In the current study, the possibility of codepositing ash and semicoke was investigated in a small-scale field experiment. The purpose of the experiment was to elucidate which mineral changes in the landfilled material occurred and how these changes affected its permeability characteristics. For this purpose five mixtures with different ash-tosemi… Show more

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Cited by 8 publications
(5 citation statements)
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“…In the high temperature range, the pyrolysis reaction of kerogen inside the oil shale is basically completed . But a series of physical and chemical interactions also can happen, which include the dehydration of some crystalline water and decomposition of the residual inorganic minerals, and some fixed carbon undergoes coking carbonization to form shale semicoke. ,, Although the growth of pore volume slows down, the porosity, TNF, and MAF continue to increase because thermal cracking intensifies under high temperature.…”
Section: Results and Discussionmentioning
confidence: 99%
“…In the high temperature range, the pyrolysis reaction of kerogen inside the oil shale is basically completed . But a series of physical and chemical interactions also can happen, which include the dehydration of some crystalline water and decomposition of the residual inorganic minerals, and some fixed carbon undergoes coking carbonization to form shale semicoke. ,, Although the growth of pore volume slows down, the porosity, TNF, and MAF continue to increase because thermal cracking intensifies under high temperature.…”
Section: Results and Discussionmentioning
confidence: 99%
“…In the water-mixed samples, the secondary Ca-Al-sulphate phase (ettringite) and the Ca-Alphase (hydrocalumite) also started to precipitate. Formation of ettringite and hydrocalumite is a characteristic process in the hydrated oil shale ash and semicoke deposits [5,8,[15][16][17]. Sulphate needed for ettringite formation was possibly delivered by the CaS dissolution that disappeared quickly after the beginning of our experiments.…”
Section: Hydration Geopolymerization and The Development Of Compressmentioning
confidence: 99%
“…In parallel with anhydrite dissolution, the precipitation of the Ca-sulphoaluminate hydrate phase, ettringite, is initiated and continues for 6–7 days [ 46 ]. Paaver et al [ 25 ] showed that ettringite composes up to 20% of minerals in hydrated pastes of the activated FA already after seven days, whereas ettringite abundances up to 40% have been reported in oil-shale processing waste deposits [ 47 , 48 , 49 ]. Dissolution of anhydrite, slacking of the lime, and formation of abundant ettringite is also evident in FA-CSA mixtures with OPC and sand ( Figure 2 ).…”
Section: Resultsmentioning
confidence: 99%