Nitrogen budget of a shortgrass prairie ecosystem |
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Authors: | R. G. Woodmansee J. L. Dodd R. A. Bowman F. E. Clark C. E. Dickinson |
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Affiliation: | (1) Natural Resource Ecology Laboratory, Colorado State University, 80523 Fort Collins, CO, USA;(2) Present address: Science and Education Administration-Federal Research, USDA, 80521 Fort Collins, CO, USA;(3) Present address: Agricultural Research Service (now: Science and Education Administration-Federal Research), USDA, 80521 Fort Collins, CO, USA |
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Abstract: | Summary A N budget is presented for a shortgrass prairie ecosystem. The grassland was ungrazed by domestic herbivores. The quantities of N in various plant, animal, microorganism, and soil components of the ecosystem are estimated for the date when aboveground living biomass was at its maximum for the growing season of 1973. Annual transfers of N between the various compartments were also estimated.Of the total N, 99.5% was in organic forms. The relatively inert heteropolycondensate fraction of the organic matter in the soils contained 88.8% of the N. Living organisms contained 4.2% and dead but recognizable organisms or part thereof contained 6.5% of the total N. Belowground animals contained more than 10 times as much N as abovegroud animals, but combined, animals contained less than 0.1% of the total in the system. Living plant material contained 2.5% of the total N. Seventy-two percent of the living plant N was below ground. Microorganisms contained 1.4% of the total N.Total N uptake by plants from soil solution was 2.9 g·m-2·yr-1. Aerial portions of plants were allocated 1.9 N·m-2·yr-1 although apparently 26% of this amount came from internally recycled sources. The heteropolycondensate fraction of the soil contributed 0.7 g N·m-2·yr-1 to mineral forms, but these components of the system were assumed to be in steady state; thus an equal amount of mineral N was allocated back to the source. Mineralization of N from plant residues was sufficient to account for all of the N taken up by plants from soil solution. Soil animals immobilized about 0.4 g N·m-2·yr-1 while the amount shunted to aboveground animals was trivial. |
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