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Biogeochemistry of C, N, and P in a Soil Catena of the Shortgrass Steppe
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1985
Year
EngineeringGeomorphologySoil Organic MatterMineralization RateEarth SciencePhysical PropertiesSoil BiochemistryOrganic GeochemistrySoil MorphologyShortgrass SteppeBiogeochemistrySoil ScienceGeographySediment TransportSoil Biogeochemical CyclingSoil EcologySoil ChemistryGeochemistrySoil Catena
Measurements of carbon, nitrogen, and phosphorus content were carried out in the soils of a hillslope of shortgrass steppe. Plant biomass, soil morphology, and soil physical properties were also measured. Soil morphology indicated that the site had undergone several cycles of rapid erosion and deposition. Total mass of C, N, and P increased downslope, following a trend in soil depth, but the summit A horizon had higher C, N, and organic P concentrations than the backslope, reflecting a higher clay content. Laboratory and field incubations showed that N availability increased downslope, while relative N mineralization (N mineralized: total N) decreased. Organic matter content and mineralization rate were closely coupled to physical properties of the soil, which reflect the geomorphic history of the site.