Skip to main content
Log in

Inferring biogenic and anthropogenic carbon dioxide sources across an urban to rural gradient

  • Ecosystem Ecology
  • Published:
Oecologia Aims and scope Submit manuscript

Abstract

We continuously monitored CO2 concentrations at three locations along an urban-to-rural gradient in the Salt Lake Valley, Utah from 2004 to 2006. The results showed a range of CO2 concentrations from daily averages exceeding 500 p.p.m. at the city center to much lower concentrations in a non-urbanized, rural region of the valley. The highest values were measured in the wintertime and under stable atmospheric conditions. At all three sites, we utilized weekly measurements of the C and O isotope composition of CO2 for a 1-year period to evaluate the CO2 sources underlying spatial and temporal variability in CO2 concentrations. The results of an inverse analysis of CO2 sources and the O isotope composition of ecosystem respiration (δ18 O R) showed large contributions (>50%) of natural gas combustion to atmospheric CO2 in the wintertime, particularly at the city center, and large contributions (>60%) of biogenic respiration to atmospheric CO2 during the growing season, particularly at the rural site. δ18 O R was most enriched at the rural site and more isotopically depleted at the urban sites due to the effects of irrigation on ecosystem water pools at the urban sites. The results also suggested differences in the role of leaf versus soil respiration between the two urban sites, with seasonal variation in the contribution of leaf respiration at a residential site and relatively constant contributions of leaf respiration at the city center. These results illustrate that spatial and temporal patterns of urban CO2 concentrations and isotopic composition can be used to infer patterns of energy use by urban residents as well as plant and soil processes in urban areas.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Barbour MM, Cernusak LA, Whitehead D, Griffin KL, Turnbull MH, Tissue DT, Farquhar GD (2005) Nocturnal stomatal conductance and implications for modelling δ18O of leaf-respired CO2 in temperate tree species. Funct Plant Biol 32:1107–1121

    Article  CAS  Google Scholar 

  • Bowling DR, McDowell NG, Bond BJ, Law BE, Ehleringer JR (2002) 13C content of ecosystem respiration is linked to precipitation and vapor pressure deficit. Oecologia 131:113–124

    Article  Google Scholar 

  • Bowling DR, McDowell NG, Welker JM, Bond BJ, Law BE, Ehleringer JR (2003) Oxygen isotope content of CO2 in nocturnal ecosystem respiration 2. Short-term dynamics of foliar and soil component fluxes in an old-growth ponderosa pine forest. Global Biogeochem Cycles 17. doi: 10.1029/2003GB002082

  • Bush SE, Pataki DE, Ehleringer JR (2007) Sources of variation in δ13C of fossil fuel emissions in an urban region. Appl Geochem (in press)

  • Cernusak LA, Pate JS, Farquhar GD (2002) Diurnal variation in the stable isotope composition of water and dry matter in fruiting Lupinus angustifolius under field conditions. Plant Cell Environ 25:898–907

    Article  Google Scholar 

  • Cernusak LA, Farquhar GD, Wong CS, Stuart-Williams H (2004) Measurement and interpretation of the oxygen isotope composition of carbon dioxide respired by leaves in the dark. Plant Phyiol 136:3350–3363

    Article  CAS  Google Scholar 

  • Cernusak LA, Farquhar GD, Pate JS (2005) Environmental and physiological controls over oxygen and carbon isotope composition of Tasmanian blue gum, Eucalyptus globulus. Tree Physiol 25:129–146

    PubMed  CAS  Google Scholar 

  • Clark-Thorne ST, Yapp CJ (2003) Stable carbon isotope constraints on mixing and mass balance of CO2 in an urban atmosphere: Dallas metropolitan area, Texas, USA. Appl Geochem 18:75–95

    Article  CAS  Google Scholar 

  • Craig H, Gordon LI (1965) Deuterium and oxygen 18 variations in the ocean and marine atmosphere. In: Tongiorigi E (ed) Stable isotopes in oceanographic studies and paleotemperatures. Consiglio Nazionale Delle Ricerche Laboratorio di Geologia Nucleare, Pisa, pp 9–130

  • Day TA, Gober P, Xiong FS, Wentz EA (2002) Temporal patterns in near-surface CO2 concentrations over contrasting vegetation types in the Phoenix metropolitan area. Agric For Meteorol 110:229–245

    Article  Google Scholar 

  • Ewers BE, Oren R (2000) Analyses of assumptions and errors in the calculation of stomatal conductance from sap flux measurements. Tree Physiol 20:579–589

    PubMed  Google Scholar 

  • Farquhar GD, Cernusak LA (2005) On the isotopic composition of leaf water in the non-steady state. Funct Plant Biol 32:293–303

    Article  CAS  Google Scholar 

  • Farquhar GD, Gan KS (2003) On the progressive enrichment of the oxygen isotopic composition of water along a leaf. Plant Cell Environ 26:1579–1597

    Article  Google Scholar 

  • Farquhar GD, Lloyd J (1993) Carbon and oxygen isotope effects in the exchange of carbon dioxide between plants and the atmosphere. In: Ehleringer JR, Hall AE, Farquhar GD (eds) Stable isotopes and plant carbon–water relations. Academic Press, New York, pp 47–70

    Google Scholar 

  • Farquhar GD, Lloyd J, Taylor JA, Flanagan LB, Syvertsen JP, Hubick KT, Wong SC, Ehleringer JR (1993) Vegetation effects on the isotope composition of oxygen in atmospheric CO2. Nature 363:439–443

    Article  CAS  Google Scholar 

  • Flanagan LB, Comstock JP, Ehleringer JR (1991) Comparison of modeled and observed environmental influences on the stable oxygen and hydrogen isotope composition of leaf water in Phaseolus vulgaris L. Plant Physiol 96:588–596

    PubMed  CAS  Google Scholar 

  • Flanagan LB, Brooks J, Varney GT, Berry SC, Ehleringer JR (1996) Carbon isotope discrimination during photosynthesis and the isotope ratio of respired CO2 in boreal forest ecosystems. Global Biogeochem Cycles 10:629–640

    Article  CAS  Google Scholar 

  • Flanagan LB, Brooks JR, Varney GT, Ehleringer JR (1997) Discrimination against C18O16O during photosynthesis and the oxygen isotope ratio of respired CO2 in boreal forest ecosystems. Global Biogeochem Cycles 11:83–98

    Article  CAS  Google Scholar 

  • Florkowski T, Korus A, Miroslaw J, Necki J, Neubert R, Schimdt M, Zimnoch M (1998) Isotopic composition of CO2 and CH4 in a heavily polluted urban atmosphere and in a remote mountain area (Southern Poland). In: Isotope techniques in the study of environmental change. IAEA, Vienna, pp 37–48

  • Gehre M, Geilmann H, Richter J, Werner RA, Brand WA (2004) Continuous flow 2H/1H and 18O/16O analysis of water samples with dual inlet precision. Rapid Commun Mass Spectrom 18:2650–2660

    Article  PubMed  CAS  Google Scholar 

  • Gelfand AE, Smith AFM (1990) Sampling-based approaches to calculating marginal densities. J Am Stat Assoc 85:398–409

    Article  Google Scholar 

  • Gelman A, Rubin DB (1992) Inference from iterative simulation using multiple sequences. Stat Sci 7:457–511

    Google Scholar 

  • Geman S, Geman D (1984) Stochastic relaxation, Gibbs distributions and the Bayesian restoration of images. IEEE Trans Pattern Anal Mach Intell 6:721–741

    Article  Google Scholar 

  • Gill J (2002) Bayesian methods: a social and behavioral approach. Chapman & Hall, CRC, Boca Raton, Fla.

    Google Scholar 

  • Gillon J, Yakir D (2001) Influence of carbonic anhydrase activity in terrestrial vegetation on the 18O content of atmospheric CO2. Science 291:2584–2587

    Article  PubMed  CAS  Google Scholar 

  • Globalview-CO2 (2005) Cooperative atmospheric data integration project—carbon dioxide. http://www.cmdl.noaa.gov, NOAA CMDL, Boulder, Colo.

  • Harwood KG, Gillon JS, Roberts A, Griffiths H (1999) Determinants of isotopic coupling of CO2 and water vapour within a Quercus petraea forest canopy. Oecologia 119:109–119

    Article  Google Scholar 

  • Hastings WK (1970) Monte Carlo sampling methods using Markov chain and their applications. Biometrika 57:97–109

    Article  Google Scholar 

  • Idso CD, Idso SB, Balling RC (1998) The urban CO2 dome of Phoenix, Arizona. Phys Geogr 19:95–108

    Google Scholar 

  • Idso CD, Idso SB, Balling RC (2001) An intensive 2-week study of an urban CO2 dome in Phoenix, Arizona, USA. Atmos Environ 35:995–1000

    Article  CAS  Google Scholar 

  • Keeling CD (1958) The concentration and isotopic abundances of atmospheric carbon dioxide in rural areas. Geochim Cosmochim Acta 13:322–334

    Article  CAS  Google Scholar 

  • Keeling CD (1961) The concentration and isotopic abundance of carbon dioxide in rural and marine air. Geochim Cosmochim Acta 24:277–298

    Article  CAS  Google Scholar 

  • Koerner B, Klopatek J (2002) Anthropogenic and natural CO2 emission sources in an arid urban environment. Environ Pollut 116:S45–S51

    Article  PubMed  CAS  Google Scholar 

  • Lai C, Ehleringer JR, Bond BJ, Paw UKT (2006a) Contributions of evaporation, isotopic non-steady state transpiration and atmospheric mixing on the δ18O of water vapour in Pacific Northwest coniferous forests. Plant Cell Environ 29:77–94

    Article  Google Scholar 

  • Lai C, Riley WJ, Owensby CE, Ham JM, Schauer AJ, Ehleringer JR (2006b) Seasonal and interannual variations of carbon and oxygen isotopes of respired CO2 in a tallgrass prairie: measurements and modeling results from 3 years with contrasting water availability. J Geophys Res 111. doi: 10.1029/2005JD006436

  • Leonard T, Hsu JSJ (1999) Bayesian methods—an analysis for statistics and interdisciplinary researchers. Cambridge University Press, Cambridge

    Google Scholar 

  • Majoube M (1971) Fractionnement en oxygene 18 et en deuterium entre l’eau et sa vapeur. J Chim Phys 58:1423–1436

    Google Scholar 

  • Miller JB, Yakir D, White JWC, Tans PP (1999) Measurement of 18O/16O in the soil–atmosphere CO2 flux. Global Biogeochem Cycles 13:761–774

    Article  CAS  Google Scholar 

  • Mortazavi B, Chanton JP (2002) Carbon isotopic discrimination and control of nighttime canopy δ18O-CO2 in a pine forest in the southeastern United States. Global Biogeochem Cycles 16. doi: 10.1029/2000GB001390

  • Pataki DE, Bowling DR, Ehleringer JR (2003a) The seasonal cycle of carbon dioxide and its isotopic composition in an urban atmosphere: anthropogenic and biogenic effects. J Geophys Res 108:4735

    Article  CAS  Google Scholar 

  • Pataki DE, Ehleringer JR, Flanagan LB, Yakir D, Bowling D, Still CJ, Buchmann N, Kaplan JO, Berry JA (2003b) The application and interpretation of Keeling plots in terrestrial carbon cycle research. Global Biogeochem Cycles 17(1):1022

    Article  CAS  Google Scholar 

  • Pataki DE, Bush SE, Ehleringer JR (2005a) Stable isotopes as a tool in urban ecology. In: Flanagan LB, Ehleringer JR, Pataki DE (eds) Stable isotopes and biosphere–atmosphere interactions: processes and biological controls. Elsevier, San Diego, Calif., pp 199–216

    Google Scholar 

  • Pataki DE, Tyler BJ, Peterson RE, Nair AP, Steenburgh WJ, Pardyjak ER (2005b) Can carbon dioxide be used as a tracer of urban atmospheric transport? J Geophys Res 110. doi: 10.1029/2004JD005723

  • Pataki DE, Alig RJ, Fung AS, Golubiewski NE, Kennedy CA, McPherson EG, Nowak DJ, Pouyat RV, Romero Lankao P (2006a) Urban ecosystems and the North American carbon cycle. Global Change Biol 12:1–11

    Article  Google Scholar 

  • Pataki DE, Bowling DR, Ehleringer JR, Zobitz JM (2006b) High resolution monitoring of urban carbon dioxide sources. Geophys Res Lett 33:L03813. doi: 03810.01029/02005GL024822

  • Riley WM, Still CJ, Helliker BR, Ribas-Carbo M, Berry JA (2003) 18O composition of CO2 and H2O ecosystem pools and fluxes in a tallgrass prairie: simulations and comparisons to measurements. Global Change Biol 9:1567–1581

    Article  Google Scholar 

  • Schauer AJ, Lai C, Bowling DR, Ehleringer JR (2003) An automated sampler for collection of atmospheric trace gas samples for stable isotope analyses. Agric For Meteorol 118:113–124

    Article  Google Scholar 

  • Schauer AJ, Lott MJ, Cook CS, Ehleringer JR (2005) An automated system for stable isotope and concentration analyses of CO2 from small atmospheric samples. Rapid Commun Mass Spectrom 19:359–362

    Article  PubMed  CAS  Google Scholar 

  • Sternberg LL, Moreira MZ, Martinelli LA, Victoria RL, Barbosa EM, Bonates LCM, Neptad D (1998) The relationship between 18O/16O and 13C/12C ratios of ambient CO2 in two Amazonian tropical forests. Tellus 50B:366–376

    CAS  Google Scholar 

  • Tarantola A (2005) Inverse problem theory and model parameter estimation. SIAM, Philadelphia, Pa.

    Google Scholar 

  • West AG, Patrickson SJ, Ehleringer JR (2006) Water extraction times for plant and soil materials used in stable isotope analysis. Rapid Commun Mass Spectrom 20:1317–1321

    Article  PubMed  CAS  Google Scholar 

  • Xu T, White D, Hui D, Luo Y (2006) Probabilistic inversion of a terrestrial ecosystem model: analysis of uncertainty in parameter estimation and model prediction. Global Biogeochem Cycles 20. doi: 10.1029/2005GB002468

Download references

Acknowledgements

We thank A. Schauer, A. Guercio, S. Bush, and C. Cook for their assistance, the Salt Lake City Corporation and Kennecott Utah Copper Corporation for access to their property, and D. R. Bowling for helpful comments about an earlier version of this manuscript. This research was supported by the US National Science Foundation grant ATM 02157658 and by the US Department of Energy.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to D. E. Pataki.

Additional information

Communicated by Russell Monson.

Appendix

Appendix

An example of the Bayesian inversion input data, constraints, and results is given for the dataset collected on January 21, 2004 at the Residential site. CT, δ13CT, and δ18OT were measured directly and are shown below with the standard deviation in parentheses. CB, δ13CB, and δ18OB were interpolated from NOAA CMDL data as described in the text. The prior constraints are specified below. For δ18OR the constraints were modeled from climatic data and source water measurements as the most depleted expected value for soil respiration and the most enriched expected value for leaf respiration during the sampling period. The unknown values CN, CG, CR, and δ18OR were then estimated by sampling the results from equation (5) with a Metropolis-Hastings algorithm as described in the text. The resulting marginal distributions for about 5000 accepted estimates are shown in Figure 11 and the means and standard deviations are given below.

Input data

CT

429.1 (3.2)

δ13 CT

−11.1 (0.1)

δ18 OT

38.3 (0.1)

Prior constants

CN, CG, CR

>0

CN + CG + CR

CT − CB

δ18 OR

23‰ < δ18 OR < 30‰

Final estimates

CN

30.0 (4.8)

CG

10.3 (4.9)

CR

3.5 (3.1)

δ18 OR

28.5 (0.6)

Rights and permissions

Reprints and permissions

About this article

Cite this article

Pataki, D.E., Xu, T., Luo, Y.Q. et al. Inferring biogenic and anthropogenic carbon dioxide sources across an urban to rural gradient. Oecologia 152, 307–322 (2007). https://doi.org/10.1007/s00442-006-0656-0

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00442-006-0656-0

Keywords

Navigation