Bermudagrass Management in the Southern Piedmont U.S. IV. Soil Surface Nitrogen Pools

The fate of nitrogen (N) applied in forage-based agricultural systems is important for understanding the long-term production and environmental impacts of a particular management strategy. We evaluated the factorial combination of three types of N fertilization (inorganic, crimson clover [Trifolium...

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Main Authors: Alan J. Franzluebbers, John A. Stuedemann
Format: Article
Language:English
Published: Wiley 2001-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1100/tsw.2001.89
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author Alan J. Franzluebbers
John A. Stuedemann
author_facet Alan J. Franzluebbers
John A. Stuedemann
author_sort Alan J. Franzluebbers
collection DOAJ
description The fate of nitrogen (N) applied in forage-based agricultural systems is important for understanding the long-term production and environmental impacts of a particular management strategy. We evaluated the factorial combination of three types of N fertilization (inorganic, crimson clover [Trifolium incarnatum L.] cover crop plus inorganic, and chicken [Gallus gallus] broiler litter pressure and four types of harvest strategy (unharvested forage, low and high cattle [Bos Taurus] grazing pressure, and monthly haying in summer) on surface residue and soil N pools during the first 5 years of ̒Coastal̓ bermudagrass (Cynodon dactylon [L.] Pers.) management. The type of N fertilization used resulted in small changes in soil N pools, except at a depth of 0 to 2 cm, where total soil N was sequestered at a rate 0.2 g ‧ kg–1‧ year–11 greater with inorganic fertilization than with other fertilization strategies. We could account for more of the applied N under grazed systems (76–82%) than under ungrazed systems (35–71%). As a percentage of applied N, 32 and 48% were sequestered as total soil N at a depth of 0 to 6 cm when averaged across fertilization strategies under low and high grazing pressures, respectively, which was equivalent to 6.8 and 10.3 g ‧ m–2 ‧ year–1. Sequestration rates of total soil N under the unharvested-forage and haying strategies were negligible. Most of the increase in total soil N was at a depth of 0 to 2 cm and was due to changes in the particulate organic N (PON) pool. The greater cycling of applied N into the soil organic N pool with grazed compared with ungrazed systems suggests an increase in the long-term fertility of soil.
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spelling doaj-art-1730587a15484afdb10326a8ca4267002025-02-03T05:45:37ZengWileyThe Scientific World Journal1537-744X2001-01-01167368110.1100/tsw.2001.89Bermudagrass Management in the Southern Piedmont U.S. IV. Soil Surface Nitrogen PoolsAlan J. Franzluebbers0John A. Stuedemann1U.S Department of Agriculture-Agricultural Research Service, Natural Resource Conservation Center, Watkinsville, GA 30677-2373, USAU.S Department of Agriculture-Agricultural Research Service, Natural Resource Conservation Center, Watkinsville, GA 30677-2373, USAThe fate of nitrogen (N) applied in forage-based agricultural systems is important for understanding the long-term production and environmental impacts of a particular management strategy. We evaluated the factorial combination of three types of N fertilization (inorganic, crimson clover [Trifolium incarnatum L.] cover crop plus inorganic, and chicken [Gallus gallus] broiler litter pressure and four types of harvest strategy (unharvested forage, low and high cattle [Bos Taurus] grazing pressure, and monthly haying in summer) on surface residue and soil N pools during the first 5 years of ̒Coastal̓ bermudagrass (Cynodon dactylon [L.] Pers.) management. The type of N fertilization used resulted in small changes in soil N pools, except at a depth of 0 to 2 cm, where total soil N was sequestered at a rate 0.2 g ‧ kg–1‧ year–11 greater with inorganic fertilization than with other fertilization strategies. We could account for more of the applied N under grazed systems (76–82%) than under ungrazed systems (35–71%). As a percentage of applied N, 32 and 48% were sequestered as total soil N at a depth of 0 to 6 cm when averaged across fertilization strategies under low and high grazing pressures, respectively, which was equivalent to 6.8 and 10.3 g ‧ m–2 ‧ year–1. Sequestration rates of total soil N under the unharvested-forage and haying strategies were negligible. Most of the increase in total soil N was at a depth of 0 to 2 cm and was due to changes in the particulate organic N (PON) pool. The greater cycling of applied N into the soil organic N pool with grazed compared with ungrazed systems suggests an increase in the long-term fertility of soil.http://dx.doi.org/10.1100/tsw.2001.89
spellingShingle Alan J. Franzluebbers
John A. Stuedemann
Bermudagrass Management in the Southern Piedmont U.S. IV. Soil Surface Nitrogen Pools
The Scientific World Journal
title Bermudagrass Management in the Southern Piedmont U.S. IV. Soil Surface Nitrogen Pools
title_full Bermudagrass Management in the Southern Piedmont U.S. IV. Soil Surface Nitrogen Pools
title_fullStr Bermudagrass Management in the Southern Piedmont U.S. IV. Soil Surface Nitrogen Pools
title_full_unstemmed Bermudagrass Management in the Southern Piedmont U.S. IV. Soil Surface Nitrogen Pools
title_short Bermudagrass Management in the Southern Piedmont U.S. IV. Soil Surface Nitrogen Pools
title_sort bermudagrass management in the southern piedmont u s iv soil surface nitrogen pools
url http://dx.doi.org/10.1100/tsw.2001.89
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