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Published online 2 February 2006
Published in Soil Sci Soc Am J 70:367-377 (2006)
DOI: 10.2136/sssaj2005.0105
© 2006 Soil Science Society of America
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Moisture Controls on Trace Gas Fluxes in Semiarid Riparian Soils

Jean E.T. McLaina,* and Dean A. Martensb

a USDA-ARS, U.S. Water Conservation Lab., 4331 East Broadway Rd., Phoenix, AZ 85040
b Dean A. Martens (deceased), USDA-ARS, Southwest Watershed Research Center, 2000 East Allen Rd., Tucson, AZ 85719


Figure 1
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Fig. 1. Soil surface temperature in three vegetation zones on measurement dates during 15-mo monitoring period at the San Pedro Riparian National Conservation Area (SPRNCA).

 

Figure 2
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Fig. 2. Environmental variables measured during monsoon 2003 using data loggers installed in each vegetation zone from May 30 (Julian Day 150) to September 27 (Julian Day 270). Figures show averaged data for mesquite (a and b) and grassland (open and sacaton, c and d) sites. No significant differences ({rho} > 0.05) were found between environmental data collected at two grassland sites.

 

Figure 3
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Fig. 3. Carbon dioxide (a) and nitrous oxide (b) efflux and methane (c) consumption in three SPRNCA vegetation sites on measurement dates during 15-mo monitoring period (July 2002 through September 2003). Symbols are averaged values from 2 or 3 flux collars installed at each site.

 

Figure 4
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Fig. 4. Isotopic composition of carbon dioxide respired from soil surface in three SPRNCA vegetation sites on measurement dates during monsoon and post-monsoon (July through December) 2002. Symbols are averaged values of two carbon dioxide collections per site on each sampling date, plus or minus standard deviation.

 

Figure 5
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Fig. 5. Methane consumption (0–45 cm) in laboratory incubations of open/forb vegetation area soils. Symbols are averaged values of duplicate incubations, plus or minus standard deviation.

 





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