Soil properties important to the restoration of a Shasta red fir barrens in the Siskiyou Mountains

Citation
Nc. Vance et Ja. Entry, Soil properties important to the restoration of a Shasta red fir barrens in the Siskiyou Mountains, FOREST ECOL, 138(1-3), 2000, pp. 427-434
Citations number
41
Categorie Soggetti
Plant Sciences
Journal title
FOREST ECOLOGY AND MANAGEMENT
ISSN journal
03781127 → ACNP
Volume
138
Issue
1-3
Year of publication
2000
Pages
427 - 434
Database
ISI
SICI code
0378-1127(20001101)138:1-3<427:SPITTR>2.0.ZU;2-D
Abstract
Because of past major disturbances, the highly erodible,granitic soil in a Shasta red fir (Abies magnifica A. Murr. Var. shastensis) barrens located i n McDonald basin on the north side of the Siskiyou Mountains crest is a maj or contributor of sediment to the aquatic system. Soil erosion is accelerat ed where vegetation is sparse and colonization slow, therefore, it is impor tant that native plant cover be restored and the site rehabilitated. We exa mined soil properties that may be associated with vegetation patterns in th e barrens and adjacent Shasta red fir forest and would have application to restoring native plant diversity and cover to the barrens. At a 40 ha study area we investigated plant available nutrients, soil C, microbial biomass, and enzymes involved in organic matter decomposition and nutrient cycling in barrens and forest soils to determine if loss of the organic layer by er osion affected soil chemistry and microbiology. Twelve samples each were co llected from 0 to 10 cm soil depth in forest and barrens and analyzed for C , N, P, K, Ca, Mg, Mn, Fe, Cu, B, Zn, Mo, and Al; microbial biomass, and de hydrogenase, urease, and acid phosphatase activity. Soils supporting forest vegetation contained higher concentrations of C, N, K, Ca, and Mg, indicat ing differences between forest and barrens in important soil chemical prope rties. Ca and Mg were extremely low in the barrens soil suggesting loss of these nutrients by erosion where there is a lack of vegetation cover. Soil organic matter was higher in forest than in barrens soil and was positively correlated with soil N (r(2)=0.78), dehydrogenase (r(2)=0.65) and acid pho sphatase activity (r(2)=0.50). Although microbial biomass was extremely low , dehydrogenase and acid phosphatase activity were sensitive indicators of differences in organic matter and microbial activity between forest and bar rens soil. The study indicates that certain soil chemical and biological pr operties may be useful in monitoring ecological change and helpful in under standing vegetation patterns. Published by Elsevier Science B.V.