The human carbon budget: an estimate of the spatial distribution of metabolic carbon consumption and release in the United States
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- West, T.O., Marland, G., Singh, N. et al. Biogeochemistry (2009) 94: 29. doi:10.1007/s10533-009-9306-z
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Carbon dioxide is taken up by agricultural crops and released soon after during the consumption of agricultural commodities. The global net impact of this process on carbon flux to the atmosphere is negligible, but impact on the spatial distribution of carbon dioxide uptake and release across regions and continents is significant. To estimate the consumption and release of carbon by humans over the landscape, we developed a carbon budget for humans in the United States. The budget was derived from food commodity intake data for the US and from algorithms representing the metabolic processing of carbon by humans. Data on consumption, respiration, and waste of carbon by humans were distributed over the US using geospatial population data with a resolution of ~450 × 450 m. The average adult in the US contains about 21 kg C and consumes about 67 kg C year−1 which is balanced by the annual release of about 59 kg C as expired CO2, 7 kg C as feces and urine, and less than 1 kg C as flatus, sweat, and aromatic compounds. In 2000, an estimated 17.2 Tg C were consumed by the US population and 15.2 Tg C were expired to the atmosphere as CO2. Historically, carbon stock in the US human population has increased between 1790 and 2006 from 0.06 Tg to 5.37 Tg. Displacement and release of total harvested carbon per capita in the US is nearly 12% of per capita fossil fuel emissions. Humans are using, storing, and transporting carbon about the Earth’s surface. Inclusion of these carbon dynamics in regional carbon budgets can improve our understanding of carbon sources and sinks.
KeywordsAgriculture Carbon dioxide Food consumption Horizontal carbon transfer Population Respiration
Humans are heterotrophic organisms that ingest carbon in the form of complex carbohydrates and release carbon in the form of carbon dioxide, methane, and a mixture of solid, dissolved, and volatile waste products. As early as 1843 Justus Liebig recognized that humans were heated by the oxidation of carbon compounds and as a result released “carbonic acid” to the atmosphere (Leibig 1843). With a global population now exceeding 6.5 billion people, humans move large amounts of carbon about on the Earth’s surface: growing, transporting, and consuming agricultural and forest products. Movement of carbon for human consumption is particularly evident in developed countries where food is now grown in concentrated cropland regions and transported over sometimes large distances for consumption by humans in metropolitan areas and by animals in pasture and rangeland areas and on farms. These transfers of carbon are significant in our attempt to understand the spatial and temporal distribution of the global cycling of carbon (Ciais 2007; Denning et al. 2005). The objective of the current research is to balance the individual, human, metabolic carbon budget and to estimate the spatial and temporal distribution of carbon releases, particularly of carbon dioxide.
Carbon dioxide is taken from the atmosphere by agricultural crops through the process of photosynthesis. After crops are harvested, CO2 is released back to the atmosphere during the decomposition of crop residues and during the processing and consumption of agricultural commodities by humans and livestock. Released CO2 is taken up again by crops during the following year or during the next crop rotation. This cyclical process is considered to result in no net emission of CO2 to the atmosphere (West and Marland 2002a; EPA 2005; Penman et al. 2003). Carbon dioxide is also released to the atmosphere from the use of fossil fuels in agricultural machinery, the production of agricultural inputs such as fertilizers and insecticides, and during the tillage of agricultural soils (West and Marland 2002b); but our focus here is on the photosynthetic products and the ultimate release of the contained carbon.
While uptake and release of carbon may be approximately balanced for the full Earth and at the temporal scale of a year, the uptake and release of carbon can be very much separated in place and over the course of the year. Ciais et al. (2001) analyzed carbon uptake and release by agricultural products, including imports and exports, at a 1 × 1 degree (latitude/longitude) resolution. Ciais et al. (2001) concluded that the “horizontal displacement is far from negligible and [that] it has a large impact on the spatial (and temporal) distribution of carbon fluxes over large areas of the world…” In an analysis of global agricultural carbon displacement, Ciais (2007) found that CO2 emissions in densely populated regions can be 20% higher when considering CO2 losses from food consumption in addition to fossil-fuel emissions.
In completing a carbon budget for a single US city (Phoenix, Arizona), Koerner and Klopatek (2002) concluded that human activity, including transportation, produced more than 80% of carbon input to the atmosphere. They estimated that 61% of soil CO2 emissions came from agricultural lands and that human respiration alone contributed as much CO2 as five power plants. Koerner and Klopatek (2002) noted, as we have above, that respiration from humans is not a net source of CO2 to the atmosphere, but that humans have a dramatic effect on the carbon balance and the transfer of carbon between regions.
To balance regional carbon budgets it is thus necessary to understand and quantify the location of carbon sources and sinks, and to do this we need to know how humans redistribute carbon around the Earth and in time. The North American Carbon Program is intended to improve estimates of carbon fluxes by improving ground-based and atmospheric-based flux estimates (Denning et al. 2005) and to compare these two estimates for enhanced accuracy (Ogle et al. 2006). The human carbon budget is one component of ground-based estimates.
In this paper, we balance the human carbon budget and estimate the spatial distribution of net carbon release associated with the consumption of agricultural commodities by humans. We focus on the carbon budget, including both CO2 and CH4. Net emissions of CO2 and CH4 are provided in units of carbon and are also, where appropriate, combined in a standard carbon-equivalent (Ceq) unit that is calculated using the 100-year global warming potential of 23 for CH4 (Ramaswamy et al. 2001). Many components of the human carbon budget have not previously been calculated or documented. We document our calculations for carbon intake, expiration, excretion, other bodily releases of carbon, and the spatial distribution of these releases in the methods section of this paper. Additional details on these calculations are provided in the appendix. We use the final estimates to conduct an analysis of the US human carbon budget and report the main components of this budget in the results section.
Methods of carbon accounting
Our focus is on the United States. Methods have been developed for estimating carbon uptake by agricultural crops (Hicke et al. 2004; Hicke and Lobell 2004; Lobell et al. 2002; Prince et al. 2001). These methods can be used to estimate carbon uptake at the county level within the US. Release of this carbon occurs in processing plants, in landfills, and during the consumption of food products by humans and livestock. We focus here on the consumption and release of carbon by humans at a sub-county scale. We seek a mass balance for carbon uptake and release by humans and we consider the stock of carbon in humans. For an individual, the intake and output of carbon should approximately balance over the course of a year. We estimate the intake and output independently and compare the two results. Imbalance in the annual carbon budget, in the form of weight gain, is quantified and discussed.
Consumption of carbon by humans
Carbon consumption per capita was estimated by developing carbon coefficients for food commodities and then analyzing food consumption in the US. A list of food commodities and data on food consumption are available in the food commodity intake database (FCID), available from the National Technical Information Service (EPA 2000). The FCID is a compilation of survey data and includes intake of food commodities by age, sex, and race. Survey data collected for the FCID include 2 days of food intake for ~21,700 individuals, including 11,800 children from birth to 19 years of age. Appendix 1 details the data and assumptions used to arrive at estimates of C intake by humans.
Expiration of carbon by humans
Respiration is the process of inspiring and expiring air. Dry atmospheric air at standard temperature and pressure (STP = 0°C and 760 mm Hg) consists of 78.09% (by volume) N2, 20.95% O2, 0.03% (now approaching 0.04%) CO2, 0.93% Ar, and traces of other gases (Weast 1972). The body uses O2 and generates CO2, thereby expiring air with about 16.5% O2 and 3.5% CO2 (Johnson 1992; Keele et al. 1982; Piiper 1996; Thews 1983; Tuttle and Schottelius 1965). Average minute volume (VE) of air expired is about 6 L, consisting of a tidal volume (VT) of 500 mL per breath at about 12 breaths per minute (Ganong 2001; Johnson 1992; Keele et al. 1982). Mean CO2 released through human respiration at rest is therefore estimated at about 58.6 kg C year−1. This value represents a healthy young adult, and can increase by an order of magnitude during heavy exercise (Piiper 1996).
Excretion and secretion of carbon by humans
In addition to expiring CO2 during the process of respiration, humans also release carbon as excreta, flatus, sweat, and aromatic compounds. Humans excrete, on average, 80–170 g feces and 1,000 g urine per capita per day (Orten and Neuhaus 1982). Carbon in flatus and sweat is a relatively small component of the human carbon budget, but is included here for completeness. Appendix 2 details our estimates of carbon excretion and secretion by humans. Our estimates are that average per capita loss of carbon by humans in the US is 4.62 kg C year−1 in feces, 1.93 kg C year−1 in urine, 0.0815 kg C year−1 in sweat, and 0.0293 kg C year−1 (0.1154 kg Ceq year−1) in flatus.
The treatment of solid or liquid wastes following their exit from the body influences whether the carbon is emitted to the atmosphere as CO2 or CH4. About 25% of domestic wastewater in the US is treated in septic systems (EPA 2005). The remainder of domestic wastewater is treated in central wastewater treatment facilities where the waste is decomposed by either aerobic or anaerobic processes. It has been estimated that 16.25% of wastewater is anaerobically digested (EPA 2005), and this estimate includes treatment in septic systems. As detailed in Appendix 2, our estimate is that total annual carbon release from human waste is 0.53 kg C capita−1 year−1 as CH4 and 6.02 kg C capita−1 year−1 as CO2, with another 0.11 kg C capita−1 year−1 as volatile and inorganic compounds in flatus and perspiration. Considering the global warming potential of CH4, total net Ceq emissions from human waste and subsequent waste treatment is 10.65 kg Ceq capita−1 year−1.
Our analysis of the fate of CO2 from human waste assumes that emissions occur in the same year that carbon is excreted from the body. The majority (75%) of human waste in the United States is processed at wastewater treatment plants, and these treatment plants increase the rate of decomposition in an effort to reduce the chemical oxygen demand of waste effluent. Remaining solid waste is dried and transported to hazardous waste landfills (Jack Graham, Engineer and Assistant Director of Water Quality, Maryville, TN, USA). Emissions of N2O also occur from processing the nitrogenous compounds in human waste at wastewater treatment facilities (Czepiel et al. 1995). In conducting an analysis of N2O emissions from a wastewater treatment plant in Durham, New Hampshire, Czepiel et al. (1995) estimated net per capita N2O emissions of 0.0032 kg N2O per year. The focus here is on the human carbon balance and these compounds are not considered further in spite of the fact that N2O is a greenhouse gas.
Carbon stock of humans
The uptake and loss of carbon by humans represent carbon flows. The total human population is a carbon stock, and this stock changes over time as the total US population increases in number and in mass per person. The human body consists of about 60% water, 15% protein, 6% minerals, and 19% fat (ICRP 1975; Going 1996). Almost all carbon in the body is found in fat, protein, and glycogen, with smaller amounts of carbon in bone mineral and lipids (Heymsfield et al. 1996). As detailed in Appendix 3, our estimate of carbon content in the average human adult is 20.7 kg C per capita. Average carbon content across all ages, ranging from 8 to 27 kg C per capita, is 17.3 kg C per capita.
Geospatial distribution of human respiration
To estimate the release of carbon by humans we need to first estimate how the human population is spatially distributed. LandScan (Dobson et al. 2000, Bhaduri et al. 2007) is a grid-based population dataset that estimates where people are located around the world at a resolution of 30 arcseconds (~1 km × 1 km at the equator). LandScan combines data on population, road networks, digital terrain, schools, prisons, commercial and residential buildings, and nighttime lights with high-resolution satellite imagery to estimate where people are located during the day and during the evening. In our analysis, we use a US version of LandScan for year 2000 that uses block-group population data from the US Census Bureau and that estimates the ambient (i.e., integrated diurnal movements) location of humans at a resolution of 15 arcseconds (~450 m × 450 m). Estimates of carbon intake and release by humans are applied to unique age and sex categories within the block-group demographic data and then distributed within the LandScan model. The model does not distinguish variations that might occur over the course of a year so it does not capture any differences in respiration that might occur due to an annual variation in the level of human activity or of human distribution. Our computation distinguishes between human respiration and the discharge of other waste products but this cannot be captured by LandScan so the assumption is implicit that all of these emissions occur in the same place. LandScan allows for estimates, at the finest scale possible, of the direct release of human carbon into the atmosphere, the approximate location of net Ceq flux from humans (including the treatment of human waste), and the stocks of human carbon in the US.
Results and synthesis
Estimated carbon consumed, released, and stored by the US population
Total release of CO2 and CH4
Estimated carbon stock
(kg C capita−1 year−1)
(kg Ceq capita−1 year−1b
(kg C capita−1)
Figure 6 shows that the densely populated areas of the United States are strong sources of CO2 from human respiration. With average per capita consumption of agricultural carbon at 67 kg C year−1 and average per capita use of fossil-fuel carbon at 5430 kg C year−1 (Marland et al. 2006), emissions from human respiration are 1.2% of those from fossil-fuel use when averaged over the country. The fraction is likely to be somewhat larger in densely populated areas. The fraction is likely to be still larger in urban concentrations of developing countries where there is less automobile traffic. Our estimate includes only the agricultural carbon that humans directly consume and subsequently respire. If we consider total harvested carbon in the US (Ciais et al. 2007) divided by total US population, as is done with the estimate for fossil-fuel consumption per capita, we then compare agricultural carbon use of 627 kg C year−1 with fossil-fuel use of 5430 kg C year−1 and see that the displacement and release of total harvested carbon is nearly 12% of fossil-fuel emissions. Tracking carbon flows in all agricultural commodities would include consumption and use by humans and livestock, processing wastes, textile products, and imports and exports. We have documented the human component of agricultural carbon displacement here.
We thank Maithilee Kunda for her assistance with calculations of human respiration and Aarthy Sabesan for initial analyses on human food consumption. We kindly acknowledge support from the US Department of Energy Global Change Education Program for A. Roddy. This work was supported by the National Oceanic and Atmospheric Association, Human Dimensions of Climate Change Program. Additional resources were provided by the US Department of Energy, Office of Biological and Environmental Research, Carbon Dioxide Information Analysis Center. Oak Ridge National Laboratory is managed by UT-Battelle, LLC, for the US Department of Energy under contract DE-AC05-00OR22725.
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