ANALYSIS OF ENVIRONMENTAL-FACTORS AFFECTING METHANE PRODUCTION FROM HIGH-SOLIDS ORGANIC WASTE

Citation
Jj. Lay et al., ANALYSIS OF ENVIRONMENTAL-FACTORS AFFECTING METHANE PRODUCTION FROM HIGH-SOLIDS ORGANIC WASTE, Water science and technology, 36(6-7), 1997, pp. 493-500
Citations number
32
Categorie Soggetti
Water Resources","Environmental Sciences","Engineering, Civil
ISSN journal
02731223
Volume
36
Issue
6-7
Year of publication
1997
Pages
493 - 500
Database
ISI
SICI code
0273-1223(1997)36:6-7<493:AOEAMP>2.0.ZU;2-M
Abstract
A simple model developed from the Gompertz equation was used to descri be the cumulative methane production curve in the batch culture. By us ing this model, three key parameters, namely methane production rate, potential and lagphase time, in a cumulative methane production curve were exactly estimated based on the experimental data. The results ind icate that each gram of dry organic waste of a sludge cake, meat, carr ot, rice, potato and cabbage had a methane production potential of 450 , 424, 269, 214, 203 and 96 mL, respectively The methanogenic activity of these digesters decreased with a decrease in the moisture content. The moisture content threshold limit, at which the methanogenic activ ity dropped to zero, was found to be 56.6% for the sludge cake, but gr eater than 80% for meat, carrot and cabbage. In the high-solids sludge digestion, the relative methanogenic activity dropped from 100% to 53 % when the moisture content decreased from 96% to 90%. The rate of met hane production at moisture contents of 90% to 96% functioned in a pH range between 6.6 and 7.8, but optimally at pH 6.8, and the process ma y fail if the pH was lower than 6.1 or higher than 8.3. On the other h and, the methanogenic activity was dependent on the level of ammonium, NH4+, but not free ammonia, NH3, indicating that the NH4+ was the mor e significant factor rather than the NY in affecting the methanogenic activity of a well-acclimatized bacterial system. In the wide pH range of 6.5 to 8.5, the methanogenic activity decreased with the increase in the NH4+; dropped 10% at the NH4+-N concentration of 1670-3720 mg.L -1, 50% at 4090-5550 mg.L-1 and dropped to zero at 5880-6600 mg.L-1. H owever, the lagphase time was dependent on the NH3 level, but not on N H4+, and when NH3-N was higher than 500 mg.L-1, a notable shock was ob served. This suggests that the NH3 level was the more sensitive factor than the NH4+ level for an unacclimatized bacterial system. (C) 1997 IAWQ. Published by Elsevier Science Ltd.