SSSAJ Journal of Natural Resources and Life Sciences Education
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Published in Soil Sci Soc Am J 45:428-432 (1981)
© 1981 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Nitrogen Content and Other Soil Properties Related to Age of Red Alder Stands1

B. T. Bormann and D. S. DeBell2

ABSTRACT

The magnitude and pattern of nitrogen (N) accretion and other changes in soil properties were assessed for red alder stands (Alnus rubra Bong.) 5 to 41 years old growing on the same soil type in the same general area. Regression of soil nitrogen (N) content over stand age revealed that N has accumulated at a nearly constant rate of about 35 kg ha–1 year–1 in the mineral soil (0- to 20-cm depth) beneath alder stands. After an apparently rapid build-up in the first decade, forest floor N increased linearly from 10 to 40 years at a rate of 15 kg ha–1 year–1. Other mineral soil characteristics beneath alder stands differed markedly from those beneath adjacent Douglas-fir stands [Pseudotsuga menziesii (Mirb.) Franco]; organic matter content was 20% higher, and pH and bulk density were much lower. The rate of N accretion and improvement of other soil characteristics suggest opportunities for increasing yields of Douglas-fir grown in mixed or rotational culture with red alder.


NOTES

1 Paper no. 1460 of the Forest Research Lab., School of Forestry, Oregon State Univ., Corvallis, OR 97331.

2 Research Assistant, Dep. of Forest Science, School of Forestry, Oregon State Univ., Corvallis, and Principal Silviculturist, USDA Forestry Sciences Lab., Pacific Northwest Forest & Range Exp. Stn., Olympia, Wash., respectively.

Received for publication April 8, 1980. Accepted for publication October 8, 1980.




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A. Rothe, K. Cromack Jr., S. C. Resh, E. Makineci, and Y. Son
Soil Carbon and Nitrogen Changes Under Douglas-fir With and Without Red Alder
Soil Sci. Soc. Am. J., November 1, 2002; 66(6): 1988 - 1995.
[Abstract] [Full Text] [PDF]




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Copyright © 1981 by the Soil Science Society of America.