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Legacies of agriculture and forest regrowth in the nitrogen of old-field soils

Forest Ecology and Management
Publication Date
DOI: 10.1016/s0378-1127(00)00399-6
  • Nitrogen Cycling
  • Biogeochemistry
  • Forest Ecosystems
  • Agro-Ecosystems
  • Long-Term Soil-Ecosystem Experiments
  • Agricultural Science
  • Biology
  • Ecology


Abstract In the Carolina Piedmont of the USA, agricultural and forest management in the 19th and 20th centuries has greatly altered soil organic nitrogen (N). The objective of this study is to evaluate effects of two centuries of land use on N in upland Piedmont soils that are derived from the region’s most common bedrock, granitic gneiss. Effects of agriculture on total soil N were examined by comparing soils cropped mainly for cotton since about 1800 with soils that remained under hardwood forest without cultivation or fertilization. Effects of forest regrowth on the N of old-field soils were examined in eight permanent plots resampled on seven occasions from 1962 to 1997 at the Calhoun Experimental Forest in South Carolina. Together, the soil-comparative study and the four-decade field experiment illustrate how soil N in the southern Piedmont has been altered by agricultural management during the 19th and 20th centuries. Not only have agricultural harvests removed considerable N from Piedmont soils, but soil organic matter has been enriched in N by agricultural fertilization, a practice that has now contributed greatly to N cycles of many old-field forests in the region. In old-field pine stands ( Pinus taeda) at the Calhoun Experimental Forest, 40 years of forest growth accumulated 366 kg ha −1 of N (CV=9.3%) in tree biomass and 740 kg ha −1 (CV=9.7%) in forest floor between planting in 1957 and the last sampling in 1997. In the four decades, mineral-soil N was diminished by 823 kg ha −1 (CV=39.5%), a reduction in N accompanied by substantial decreases in mineralizable N as well. On the other hand, N accretion in the whole forest ecosystem averaged 5.9 kg ha −1 per year over this period (significant at a probability of <0.07), an accretion attributed mainly to atmospheric N deposition rather than N 2 fixation. Despite the N accretion and legacy of agricultural fertilization, the 40-year-old Calhoun forest has grown into a state of acute N deficiency. Future N research should include support for a network of long-term field studies which investigates N dynamics in forest floor and logging slash, and estimates N-use and N-retention efficiencies of fertilized pine-forest ecosystems.

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