Biosolid stockpiles are a significant point source for greenhouse gas emissions

https://doi.org/10.1016/j.jenvman.2014.04.016Get rights and content

Highlights

  • Biosolid stockpiles emit large amounts of greenhouse gas emissions.

  • Nitrous oxide and carbon dioxide were the dominant greenhouse gases emitted.

  • Younger stockpiles had greater emissions indicating decay of labile organic material.

  • Emissions did not show any seasonality, stockpiles likely create their own climate.

  • Managers of biosolids should assess alternate storage and uses for biosolids.

Abstract

The wastewater treatment process generates large amounts of sewage sludge that are dried and then often stored in biosolid stockpiles in treatment plants. Because the biosolids are rich in decomposable organic matter they could be a significant source for greenhouse gas (GHG) emissions, yet there are no direct measurements of GHG from stockpiles. We therefore measured the direct emissions of methane (CH4), nitrous oxide (N2O) and carbon dioxide (CO2) on a monthly basis from three different age classes of biosolid stockpiles at the Western Treatment Plant (WTP), Melbourne, Australia, from December 2009 to November 2011 using manual static chambers. All biosolid stockpiles were a significant point source for CH4 and N2O emissions. The youngest biosolids (<1 year old) had the greatest CH4 and N2O emissions of 60.2 kg of CO2-e per Mg of biosolid per year. Stockpiles that were between 1 and 3 years old emitted less overall GHG (∼29 kg CO2-e Mg−1 yr−1) and the oldest stockpiles emitted the least GHG (∼10 kg CO2-e Mg−1 yr−1). Methane emissions were negligible in all stockpiles but the relative contribution of N2O and CO2 changed with stockpile age. The youngest stockpile emitted two thirds of the GHG emission as N2O, while the 1–3 year old stockpile emitted an equal amount of N2O and CO2 and in the oldest stockpile CO2 emissions dominated. We did not detect any seasonal variability of GHG emissions and did not observe a correlation between GHG flux and environmental variables such as biosolid temperature, moisture content or nitrate and ammonium concentration. We also modeled CH4 emissions based on a first order decay model and the model based estimated annual CH4 emissions were higher as compared to the direct field based estimated annual CH4 emissions. Our results indicate that labile organic material in stockpiles is decomposed over time and that nitrogen decomposition processes lead to significant N2O emissions. Carbon decomposition favors CO2 over CH4 production probably because of aerobic stockpile conditions or CH4 oxidation in the outer stockpile layers. Although the GHG emission rate decreased with biosolid age, managers of biosolid stockpiles should assess alternate storage or uses for biosolids to avoid nutrient losses and GHG emissions.

Introduction

Greenhouse gas (GHG) concentrations of methane (CH4), nitrous oxide (N2O) and carbon dioxide (CO2) have increased in the atmosphere due to direct and indirect human activities (Dalal et al., 2003). The waste and wastewater industry sectors contribute approximately 3% to the global anthropogenic emissions of GHG (IPCC, 2007), which has led to increased public awareness and the need to better estimate or measure GHG emissions from the sector (Ishigaki et al., 2005). The wastewater sector emits CH4, CO2 and N2O directly through nutrient transformations during the wastewater treatment process and degradation of organic matter (Boldrin et al., 2009, Czepiel et al., 1996) and indirectly through fossil fuel consumption for pumping, transport, operations and processing (Monteith et al., 2005). In all wastewater treatment plants large quantities of sewage sludge are produced (Brown et al., 2008). The dried sludge is called biosolids and still contains significant quantities of organic matter, macro-nutrients and trace elements (Bright and Healey, 2003). The quantity of biosolid produced in Australia is around 360,000 dry Mg per year (Pritchard et al., 2010) and in the state of Victoria it is approximately 68,250 dry Mg (AWA, 2013). These biosolids are often stored in large stockpiles for many years within the wastewater treatment site, before they are moved off-site and used as a resource.

Currently, GHG emissions from waste and wastewater treatment plants are often based on simple emission factors or mathematical models developed from kinetic relationships of mass and energy balances (Yerushalmi et al., 2013). One of the main uncertainties in GHG accounting is associated with the method of calculation, which is frequently not based on, or validated by, direct GHG flux measurements. For example, waste industries use minimum data to predict the GHG emissions based on population, waste generation rate, solid waste composition and methods of solid waste disposal (El-Fadel and Massoud, 2000). Another uncertainty confronting GHG accounting in the wastewater industry is access to long term monitoring of GHG emissions and under a wide range of climatic and management conditions (Cowie et al., 2012, Bogner et al., 2008, Czepiel et al., 1993). Hence, to reduce these uncertainties it is important to obtain reliable long-term data to better understand the magnitude of direct GHG emissions and the variation over seasonal or inter-annual time frames. There are many studies investigating GHG emissions from landfill waste (Bastian et al., 2013, Stanisavljevic et al., 2012, Goldsmith et al., 2012), stockpile composting (Chan et al., 2011, Ahn et al., 2011, Boldrin et al., 2009) and stockpile manure management (Petersen et al., 2013, Wood et al., 2012). However, GHG emissions from stockpiled biosolids have not yet been measured in detail.

The overall objective of this study was therefore to investigate the direct GHG emissions from various ages of biosolids stockpiles at a wastewater treatment plant. The specific objectives were to:

  • (1)

    measure the flux of CH4, CO2 and N2O from different ages of biosolid stockpiles across different seasons and investigate GHG concentrations (CH4, CO2) at two different biosolid stockpile depths,

  • (2)

    investigate the relationship between GHG emissions from biosolid stockpiles and environmental variables,

  • (3)

    calculate the cumulative magnitude of annual CH4, CO2 and N2O fluxes from different aged biosolid stockpiles and compare this against modeled emissions.

Section snippets

Site description and experiment set up

The Western Treatment Plant (WTP) is located 35 km to the south-west Melbourne and services wastewater from a population of about 1.6 million people from the western and northern suburbs of Melbourne (38°1′52″S, 144°34’82″E). Climate in this area is temperate with warm dry summer and cool winters with maximum rainfall occurring during spring. The long-term average rainfall is 542 mm (Stickland et al., 2013) and mean evaporation is generally highest between December and February (Parameswaran,

GHG emissions from different aged biosolid stockpiles

We observed different GHG emissions from the different aged biosolid stockpiles and also different contributions from the GHG. We observed the greatest GHG emissions from the youngest stockpiles and emission decreased with age. Methane emissions were low in all stockpiles and N2O and CO2 dominated emissions, with N2O having the greatest contribution in the youngest stockpile and CO2 the greatest contribution in the oldest stockpile.

In the >3 yo biosolid stockpile, the magnitude of CO2 flux was

GHG emissions from biosolid stockpiles of different age

Our data clearly show that age of the stockpiles is important for the total amount of GHG emissions (CO2-e) and that the contribution of the different GHG species was not equal in the different aged biosolid stockpiles. The youngest stockpile had the greatest GHG emissions and these decreased with stockpile age. We also observed that N2O had the greatest contribution to total GHG emissions in the youngest stockpile and this decreased in favor of CO2 as the stockpiles aged. Methane only played a

Conclusions

Our study evaluated the GHG emission strength of differently aged biosolid stockpiles at a wastewater treatment plant by direct GHG measurements and confirmed that biosolid stockpiles are a significant GHG source. Very young biosolid stockpiles emit large amounts of GHG, mainly in the form of N2O and the GHG emissions source strength decreases as biosolids age and labile organic carbon and nitrogen sources decline. Methane emissions were negligible from biosolid stockpiles, mainly because of

Acknowledgements

The authors would like thank Dr Scott W Laidlaw and Kevin Gillett for assistance with the field based measurements. The study was supported by funding from the Australian Research Council grants LE0882936, LP0883573 and DP120101735 and the Melbourne Water Corporation (LP0883873).

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