Nitrogen saturation and soil N availability in A high-elevation spruce and FIR forest
A field study was conducted during the summer of 1995 to gain abetter understanding of the causes of nitrate (NO^sub 3^-N)leaching and ongoing changes in soil nitrogen (N) availabilityin high-elevation (1524-2000 m) spruce (Picea rubens) andfir (Abies fraseri) forests of the Great Smoky MountainsNat...
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Published in | Water, air, and soil pollution Vol. 120; no. 3-4; pp. 295 - 313 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Dordrecht
Springer
01.06.2000
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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Summary: | A field study was conducted during the summer of 1995 to gain abetter understanding of the causes of nitrate (NO^sub 3^-N)leaching and ongoing changes in soil nitrogen (N) availabilityin high-elevation (1524-2000 m) spruce (Picea rubens) andfir (Abies fraseri) forests of the Great Smoky MountainsNational Park, Tennessee and North Carolina, U.S.A. Indicatorsof soil N availability (total soil N concentrations,extractable NH^sub 4^-N, extractable NO^sub 3^-N, and C/N ratios)were measured in Oa and A horizons at 33 study plots. Dynamicmeasures included potential net soil N mineralization determinedin 12-week aerobic laboratory incubations at 22 °C.Potential net nitrification in the A horizon was correlated (r =+0.83, P < 0.001) with total soil N concentrations. Mostmeasures of soil N availability did not exhibit significanttrends with elevation, but there were topographic differences.Potential net soil N mineralization and net nitrification in theA horizon were higher in coves than on ridges. Relative amountsof particulate and organomineral soil organic matter influencedpotential net N mineralization and nitrification in the Ahorizon. Calculations indicate that soil N availability andNO^sub 3^-N leaching in high-elevation spruce and fir forests ofthe Great Smoky Mountains National Park will increase inresponse to regional warming.[PUBLICATION ABSTRACT] |
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Bibliography: | ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 DE-AC05-00OR22725 |
ISSN: | 0049-6979 1573-2932 |
DOI: | 10.1023/A:1005270012802 |