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Journal ArticleDOI

Fungal and arboreal biomass in a western Oregon Douglas-fir ecosystem: distribution patterns and turnover

Robert Fogel, +1 more
- 01 Jun 1979 - 
- Vol. 9, Iss: 2, pp 245-256
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TLDR
The allocation of biomass and the turnover time of various components were measured from August 1976 to August 1977 in a young, second-growth Douglas-fir stand in the Oregon Coast Range.
Abstract
The allocation of biomass and the turnover time of various components were measured from August 1976 to August 1977 in a young, second-growth Douglas-fir stand in the Oregon Coast Range. Allocation of biomass among the tree components was 14 732 kg foliage ha−1, 30 455 kg branches ha−1, 212 941 kg boles ha−1, 49 289 kg nonmycorrhizal roots ha−1, and 15 015 kg host portion of mycorrhizae ha−1. Biomass allocation of fungal components was 10 009 kg mycorrhizal mantles ha−1, 2785 kg Cenococcumgeophilum sclerotia ha−1, 65 kg sporocarps ha−1, 369 kg litter hyphae ha−1, and 6666 kg soil hyphae ha−1. The forest floor was composed of 6970 kg fine ( 25 mm) litter ha−1. Soil organic matter (<0.494 mm) was 87 600 kg ha−1. Total annual stand throughput was 30 324 kg ha−1, excluding soil organic matter throughput. Of this total, 50.5% was accounted for by fungal throughput, 39.5% by tree throughput, and 10.0% by forest floor throughput.

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Journal ArticleDOI

Mycorrhizas in ecosystems

TL;DR: It is concluded that knowledge of the full range of functions of each mycorrhizal type is essential for an understanding of the distribution and dynamics of the ecosystem in which it predominates.
Journal ArticleDOI

Soil water repellency: its causes, characteristics and hydro-geomorphological significance

TL;DR: Water repellency (hydrophobicity) of soils is a property with major repercussions for plant growth, surface and subsurface hydrology, and for soil erosion as discussed by the authors.

Production, Turnover, and Nutrient Dynamics of Above and below ground Detritus of World Forests

K. A. Vogt
TL;DR: Evergreen forests accumulate higher forest floor masses than deciduous in similar climatic zones, but in needle-leaved forests none of the climatic factors or latitude explains the variation in amount of aboveground litterfall mass or litterfall nitrogen (N) input.
Book ChapterDOI

Production, Turnover, and Nutrient Dynamics of Above- and Belowground Detritus of World Forests

TL;DR: In this paper, the authors measured the root masses of needle-leaved forests and deciduous forests and found that the proportion of total detrital input to forest floor occurring as aboveground litterfall varied from 23 to 80%.
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