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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.
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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