Carbon dioxide flux

Raich, J. W. and Schlesinger, W. H. (1992). The global carbon dioxide flux in soil respiration and its relationship to vegetation and climate, Tellus, Ser. B, 44,81-99. 

Shikazono, N. and Kashiwagi. H. (1999) Carbon dioxide flux due to hydrothermal venting from back-arc basin and island arc and its influence on global carbon dioxide cycle. 9th Annual V.M. Gohl.schmidt Conference, August 22-27. Harvard, Abstr., p. 272. 

Rochette P, Angers DA, Flanagan LB (1999) Maize residue decomposition measurements using soil surface carbon dioxide fluxes and natural abundance of carbon-13. Soil Sci Am J 63 1385-1396... 

McGilhs WR, Edson IB, Ware ID, Dacey IWH, Hare IE, Fairall CW, Wanninkhof R. 2001. Carbon dioxide flux techniques performed during GasEx-98. Marine Chemistry 75 267-280. 

Haszpra L. Barcza Z. Davis K.J. and Tarczay K. (2005). Long-term tall tower carbon dioxide flux monitoring over an area of mixed vegetation. Agricultural and Forest Meteorology, 132(1-2), 58 -77. 

Magenheimer, J.F., T.R. Moore, T.R., Chmura, G.L., and Daoust, R.J. (1996) Methane and carbon dioxide flux from a macrotidal salt marsh. Bay of Fundy, New Brunswick. Estuaries 19, 139-145. 

Miranda, A. C., H. S. Miranda, J. Lloyd, J. Grace, J. A. McIntyre, P. Meir, P. Riggan, R, Lockwood, and J. Brass. 1996a. Carbon dioxide fluxes over a cerrado sensu stricto in central Brazil. Pages 353-363. in J. H. C. Gash, C. A. Nobre, J. M. Roberts, and R. L. Victoria, editors. Amazonian deforestation and climate. Institute of Hydrology, London. 

McGillis W. R., Edson J. B., Ware J. D., Dacey J. W. H., Hare J. E., Fairall C. W., and Wanninkhof R. (2001b) Carbon dioxide flux techniques performed during GasEx-98. Mar. Chem. 75, 267-280. 

Bousquet P., Peylin P., Ciais P., Le Quere C., Friedlingstein P., and Tans P. P. (2000) Regional changes in carbon dioxide fluxes of land and oceans since 1980. Science 290, 1342-1346. 

The exchange of organic matter with the oceans is small compared with the basic carbon dioxide flux within the system. 

D. E. (1997). Seasonal trends in energy, water, and carbon dioxide fluxes al a norlhern boreal welland./. Geophys. Res. D 102, 29,009-29,020,... 

Decomposition of organic matter is rapid under aerobic conditions, which predominate in the water column and surface soil layers. These decomposition rates typically decrease with soil depth. Carbon dioxide fluxes from soil into the atmosphere increase with lowered water table depth or drained soil conditions. An enhanced rate of soil respiration in response to both drainage and nutrient enrichment has been previously reported for organic soils. For example, the interaction between hydrology and nutrient enrichment is graphically shown for the Everglades soils in Figure 5.46 (DeBusk and Reddy, 2003). 

At low values of the methane flux can be greater than the carbon dioxide flux even though the... 

Calculate the permeate composition, the carbon dioxide recovery, and the carbon dioxide flux. 

In Chapter 18, Matsuyama and Teramoto report the preparation of new types of cation-exchange membranes by grafting acrylic acid and methacrylic acid to substrates, such as microporous polyethylene, polytetrafluoroethylene, and poly[l-(trimethylsilyl)-l-propyne], by use of a plasma graft polymerization technique. Various monoprotonated amines are immobilized by electrostatic forces in the ion-exchange membranes and used as carriers for carbon dioxide. With these membrane systems carbon dioxide/nitrogen selectivities of greater than 4700 are obtained with high carbon dioxide flux. 

Figure 12 Carbon dioxide flux versus bore liquid flowrate.

Figure 15 Effect of polymer solution flowrate on carbon dioxide flux.

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