REGIONAL SCALE ANALYSIS OF DENITRIFICATION IN NORTH TEMPERATE FOREST SOILS

被引:37
作者
GROFFMAN, PM
TIEDJE, JM
MOKMA, DL
SIMKINS, S
机构
[1] Department of Crop and Soil Sciences, Michigan State University, East Lansing, 48824, MI
关键词
D O I
10.1007/BF02573956
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Large scale analyses of biogeochemical processes are necessary for understanding anthropogenic effects on global climate and environmental quality. Regional scale estimates of denitrification from forest soils in southern lower Michigan USA were produced by stratifying the region into landscape experimental units using soil texture and natural drainage classes, and extrapolating data to larger areas using a geographic information system (GIS). Previous landscape-scale research established relationships between soil texture and drainage and denitrification and quantified annual denitrification N loss in nine soil texture/drainage groups. All forest soils within the region (64 series) were assigned to one of these nine groups based on their texture and drainage characteristics and were assigned an annual denitrification N loss value. A regional estimate of denitrification was produced by multiplying the areal extent of each of the nine soil groups by their annual denitrification N loss value. Loam-textured soils underlie 47% of the regional forest and accounted for 73% of the forest denitrification. Sandy soils were found under 44% of the regional forest but produced only 5% of the regional denitrification. Clay loam soils underlie 9% of the regional forest and produced 22% of the denitrification. Annual denitrification N loss for the region was estimated as 1.4 x 10(7) kg N/yr. We used denitrification enzyme activity (DEA) as a proxy for annual denitrification N loss to determine if the relationship between denitrification and soil texture and natural drainage that we observed at the landscape scale held up at the regional scale. DEA was measured in 22 soils across the region and was strongly related to soil texture and natural drainage (r2 = 0.61), suggesting that extrapolation of data from the landscape to the regional scale was justified.
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页码:45 / 53
页数:9
相关论文
共 36 条
[11]  
Groffman P.M., Tiedje J.M., Denitrification in north temperate forest soils: Spatial and temporal patterns at the landscape and seasonal scales, Soil Biology and Biochemistry, 21, pp. 613-620, (1989)
[12]  
Groffman P.M., Tiedje J.M., Denitrification in north temperature forest soils: Relationships between denitrification and environmental parameters at the landscape scale, Soil Biology and Biochemistry, 21, pp. 621-626, (1989)
[13]  
Hole F.D., An approach to landscape analysis with an emphasis on soils, Geoderma, 21, pp. 1-23, (1978)
[14]  
Jeffers J.N.R., Statistical and mathematical approaches to issues of scales in ecology, Scales and Global Change: Spatial and Temporal Variability in Biospheric and Geospheric Processes, pp. 47-56, (1988)
[15]  
Jenny H., Soil Genesis with Ecological Perspectives, (1980)
[16]  
Keeney D.R., Sources of nitrate to ground water, CRC Critical Reviews in Environmental Control, 16, pp. 257-304, (1987)
[17]  
Lowrance R., Groffman P.M., Impacts of low and high input agriculture on landscape structure and function, American Journal of Alternative Agriculture, 2, pp. 175-183, (1987)
[18]  
Martin K., Parsons L.L., Murray R.E., Smith M.S., Dynamics of soil denitrifier populations: Relationships between enzyme activity, most-probable-number counts, and actual N gas loss, Applied and Environmental Microbiology, 54, pp. 2711-2716, (1988)
[19]  
Matson P.A., Vitousek P.M., Cross-system comparisons of soil nitrogen transformations and nitrous oxide flux in tropical forest ecosystems, Global Biogeochemical Cycles, 1, pp. 163-170, (1987)
[20]  
Matson P.A., Vitousek P.M., Schimel D.S., Regional extrapolation of trace gas flux based on soils and ecosystems, Exchange of Trace Gases Between Terrestrial Ecosystems and the Atmosphere, pp. 119-134, (1989)