Abstract
Coorongite, a torbanite precursor found in South Australia, and algal residues derived from Botryococcus braunii and other algae have been examined by solid-state 13C NMR techniques. The majority of carbon in these materials is present as (CH2)n. However, variable-temperature studies show that a considerable proportion of the alkyl chains have unusual dipolar-dephasing behavior and are more mobile than in rigid solids. It is suggested that these mobile structures contribute to the so-called "guest phases" in coal. The data are also consistent with a vascular and algal model of coal.
Original language | English |
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Pages (from-to) | 668-672 |
Number of pages | 5 |
Journal | Energy and Fuels |
Volume | 2 |
Issue number | 5 |
Publication status | Published - 1988 |