Evaluation of methane production and macronutrient degradation in the anaerobic co-digestion of algae biomass residue and lipid waste
by Stephen Park
Co-authored with Yebo Li
Published in Bioresource Technology. 2012.111: 42-48.
Algae biomass residue was co-digested with lipid-rich fat, oil, and grease waste (FOG) to evaluate the effect on... more Algae biomass residue was co-digested with lipid-rich fat, oil, and grease waste (FOG) to evaluate the effect on methane yield and macronutrient degradation. Co-digestion of algae biomass residue and FOG, each at 50% of the organic loading, allowed for an increased loading rate up to 3 g VS/L•d, resulting in a specific methane yield of 0.54 L CH4/g VS•d and a volumetric reactor productivity of 1.62 L CH4/L•d. Lipids were the key contributor to methane yields, accounting for 68-83% of the total methane potential. Co-digestion with algae biomass residue fractions of 33%, 50%, and 67% all maintained lipid degradations of at least 60% when the organic loading rate was increased to 3 g VS/L•d, while synergetic effects on carbohydrate and protein degradation were less evident with increased loading.
75 views
Seen by:Emissões: Os impactos mais renegados das hidrelétricas.
Fearnside, P.M. 2011. Emissões: Os impactos mais renegados das hidrelétricas. Contra Corrente, No. 3: 27-30.
Hidrelétricas amazônicas e a política energética
Fearnside, P.M. 2011. Hidrelétricas amazônicas e a política energética –. Globoamazonia. http://g1.globo.com/platb/natureza-philipfearnside
Belo Monte: Globo Amazônia série completa
Fearnside, P.M. 2009-2010. Belo Monte: Globo Amazônia série completa. http://colunas.globoamazonia.com/philipfearnside/
64 views
Seen by:Hydroelectric dams in Brazilian Amazonia: Response to Rosa, Schaeffer & dos Santos.
Fearnside, P.M. 1996. Hydroelectric dams in Brazilian Amazonia: Response to Rosa, Schaeffer & dos Santos. Environmental Conservation 23(2): 105-108. doi:10.1017/S0376892900038467
See Amazon Controversies:
http://philip.inpa.gov.br/publ_livres/AMAZONIAN CONTROVERSIES.htm
Comments by Philip M. Fearnside.18 Oct.1999. [on World Commission on Dams Thematic Review II.2 on greenhouse gas emissions from hydroelectric dams].
Fearnside, P.M. 2000. Comments by Philip M. Fearnside.18 Oct.1999. [on World Commission on Dams Thematic Review II.2 on greenhouse gas emissions from hydroelectric dams]. World Commission on Dams, Capetown, South Africa. pp. 85-88. (www.dams.org/docs/kbase/thematic/ drafts/tr22_part2_finaldraft.pdf)
1 views
Gases estufa e radiação [Response to W. Alexandre].
Fearnside, P.M. 2005. Gases estufa e radiação [Response to W. Alexandre]. Ciência Hoje 36(213): 80.
Metano em hidrelétricas [Response to N. de Ávila].
Fearnside, P.M. 2005. Metano em hidrelétricas [Response to N. de Ávila]. Ciência Hoje 36(213): 80.
Dirty hydros [Response to Graham Faichney]
Fearnside, P.M. 2005. Dirty hydros [Response to Graham Faichney] New Scientist 186(2494): 24 (9 April 2005).
Pareceres dos consultores sobre o Estudo de Impacto Ambiental do Projeto para aproveitamento hidrelétrica de Santo Antônio e Jirau, Rio Madeira-RO. Parecer Técnico sobre ecossistemas. Parte B, Volume 1, Parecer 8
Fearnside, P.M. 2006. Pareceres dos consultores sobre o Estudo de Impacto Ambiental do Projeto para aproveitamento hidrelétrica de Santo Antônio e Jirau, Rio Madeira-RO. Parecer Técnico sobre ecossistemas. Parte B, Volume 1, Parecer 8, pp. 1-15 In: Pareceres Técnicos dos Especialistas Setoriais—Aspectos Físicos/Bióticos. Relatório de Análise do Conteúdo dos Estudos de Impacto Ambiental (EIA) e do Relatório de Impacto Ambiental (RIMA) dos Aproveitamentos Hidrelétricos de Santo Antônio e Jirau no, Rio Madeira, Estado de Rondônia. Ministério Público do Estado de Rondônia, Porto Velho, Rondônia. 2 Vols. http://www.mp.ro.gov.br/web/guest/Interesse-Publico/Hidreletrica-Madei
Dirty hydros [Response to Graham Faichney]
Fearnside, P.M. 2005. Dirty hydros [Response to Graham Faichney] New Scientist 186(2494): 24 (9 April 2005).
Controvérsias sobre o efeito estufa. Por que a energia hidrelétrica não é limpa.
Fearnside, P.M. 2008. Controvérsias sobre o efeito estufa. Por que a energia hidrelétrica não é limpa. pp. 270-271 In: I. S. Gorayeb (ed.). Amazônia. Jornal "O Liberal"/VALE, Belém, Pará. 384 pp. ISBN 978-85-61628-00-0 [também publicado no jornal O Liberal 30 Jan. 2008].
See Amazon Controversies:
http://philip.inpa.gov.br/publ_livres/AMAZONIAN CONTROVERSIES.htm
English version:
Fearnside, P.M. 2007. Why hydropower is not clean energy. Scitizen, Paris, France (peer-reviewed website). http://www.scitizen.com/screens/blogPage/viewBlog/sw_viewBlog.php?idTh
http://philip.inpa.gov.br/publ_livres/2007/Why hydro not clean energy-Article as posted.pdf
43 views
Seen by:Methane emissions from hydroelectric dams
Fearnside, P.M. 2011. Methane emissions from hydroelectric dams. Science (E-Letter 28 July 2011), http://www.sciencemag.org/content/331/6013/50.short/reply#sci_el_14254
51 views
Seen by:Isotopic variation complicates analysis of trophic relations within the fish community of Plußsee: a small, deep, stratifying lake
by Chris Harrod
Harrod, C. & Grey, J. (2006). Isotopic variation complicates analysis of trophic relations within the fish community of Plußsee: a small, deep, stratifying lake. Archiv für Hydrobiologie 167, 281-299.
Analysis of carbon and nitrogen stable isotopes has allowed freshwater ecologists to examine lake food webs in... more Analysis of carbon and nitrogen stable isotopes has allowed freshwater ecologists to examine lake food webs in increasing detail. Many such studies have highlighted the existence of separate within-lake pelagic and benthic-littoral food webs but are typically conducted on large (> 10 km2) lakes, whereas the majority of lakes are actually relatively small. We used stable isotope analysis (δ13C & δ15N) to examine trophic interactions between fish and their prey in Plußsee, as an example of a small, stratifying lake, and to determine whether separate pelagic/benthic-littoral food webs could be distinguished in such systems. Our results indicate that the Plußsee food web was complicated, and due to extensive intra-annual isotopic variation in zooplankton (e.g. cladoceran δ13C annual range = 25.6‰), it may be impossible to definitively assign consumers from small, eutrophic stratified lakes to pelagic or benthic-littoral food webs. We present evidence that some components of the Plußsee food web (large bream) may be subsidised by carbon of methanogenic origin.
211 views
Seen by:Letts, M.G. 1998. Modelling Peatland Soil Climate and Methane Flux using the Canadian Land Surface Scheme. M.Sc. thesis. McGill University. 86 p.
A soil climate parameterization is designed for peatland environments in the Canadian Land Surface Scheme (CLASS).... more
A soil climate parameterization is designed for peatland environments in the Canadian Land Surface Scheme (CLASS). Three wetland soil classes account for the variation in the hydraulic characteristics of organic soils. Saturated hydraulic conductivity varies from a median of 1.0 x 10-7 m/s in deeply humidified sapric peat to 2.8 x 10-4 m/s in relatively undecomposed fibric peat. Average pore volume fraction ranges from 0.83 to 0.93. Parameters are derived for the soil moisture characteristic curves of fibric, hemic and sapric peat, using the Campbell (1974) equation employed in CLASS, and the van Genuchten (1980) formulation. Validation of modelled water table depth and peat temperature is performed for a fen in northern Quebec and a bog in north-central Minnesota. The new parameterization results in more realistic simulation than the previous version of CLASS, which was constrained to using mineral soil properties to approximate those of organic soils.
Two approaches are used to model methane emissions from northern peatlands using the new soil climate parameterization in CLASS. In the first module, the multiple regression equation of Dise et al. (1993) is used to simulate daily methane emissions from water table depth and peat temperature. In the process-based module, methane flux is divided into its component parts: plant transport, diffusion and ebullition. Each of these transport mechanisms is determined by methane concentrations, which are calculated from a series of processes related to peat temperature, water table level and rooting depth. The daily methane emissions predicted by the two models are similar and correlate reasonably with observations from a bog in north-central Minnesota.

