Legacies of agriculture and forest regrowth in the nitrogen of old-field soils.
Submitted by mhof on Sun, 11/05/2006 - 1:34am.
Year:
2000
Journal:
Forest Ecology and Management
Volume:
138
Pagination:
233-248
Keywords:
Nitrogen cycling; Biogeochemistry; Forest ecosystems; Agro-ecosystems; Long-term soil-ecosystem experiments
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-®eld 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 ®eld 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-®eld forests in the region.
In old-®eld pine stands (Pinus taeda) at the Calhoun Experimental Forest, 40 years of forest growth accumulated
366 kg haÿ1 of N (CV9.3%) in tree biomass and 740 kg haÿ1 (CV9.7%) in forest ¯oor between planting in 1957 and the
last sampling in 1997. In the four decades, mineral-soil N was diminished by 823 kg haÿ1 (CV39.5%), 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 haÿ1 per year over this period (signi®cant at a probability of <0.07), an accretion attributed mainly
to atmospheric N deposition rather than N2 ®xation. Despite the N accretion and legacy of agricultural fertilization, the 40-
year-old Calhoun forest has grown into a state of acute N de®ciency. Future N research should include support for a network of
long-term ®eld studies which investigates N dynamics in forest ¯oor and logging slash, and estimates N-use and N-retention
ef®ciencies of fertilized pine-forest ecosystems. # 2000 Elsevier Science B.V. All rights reserved.
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