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IntensIve sIlvIculture - Forest Science Labs - Research Network ...

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(and other measures of overstorey density) just after thinning. In thinned stands, the density of<br />

small trees (intermediate crown class overstorey trees and advanced regeneration) was 159/ha,<br />

significantly greater than in unthinned stands (90/ha), but not significantly different from that of<br />

old-growth (204/ha). The live crown ratio of these trees in thinned stands (66%) was greater than<br />

in unthinned (44%) and old-growth (48%) stands. Cover and stem density of shrubs was variable<br />

in all 3 stand types. There was significantly less tall shrub cover in unthinned stands than in either<br />

thinned or old-growth stands, which did not differ. Thinned stands had the most low shrub cover.<br />

Salal (Gaultheria shallon) and bracken fern (Pteridium aquilinum) cover was greater in thinned<br />

stands than in the other stand types, but there was no difference in sword fern (Polystichum<br />

munitum) and Oregongrape [Berberis nervosa] cover. Leaf area index in thinned stands (6.6) was<br />

not significantly different from that in unthinned (6.8) and old-growth stands (7.1); however,<br />

there was more leaf area in shrubs in the thinned stands. Thinning young Douglas-fir stands will<br />

hasten the development of multistorey stands by recruitment of conifer regeneration in the<br />

understorey as well as by enabling the survival of small overstorey trees and growth of advanced<br />

understorey regeneration. Thinning will also help develop the shrub layer by increasing tall shrub<br />

stem density and cover of some low shrubs.<br />

33. Bailey, V.L., J.L. Smith and H. Bolton, Jr. 2002. Fungal-to-bacterial ratios in soils investigated<br />

for enhanced C sequestration. Soil-Biology-and-Biochemistry 34(7): 997-1007.<br />

Keywords: fertilization<br />

soil properties<br />

Abstract: Fungi and bacteria govern most of the transformations and ensuing long-term<br />

storage of organic C in soils. We assessed the relative contributions of these two groups of<br />

organisms to the microbial biomass and activity of soils from five different ecosystems with<br />

treatments hypothesized to enhance soil C sequestration: (1) desert (an elevation gradient allowed<br />

comparison of soil developed in a cooler, wetter climate with soil developed in a warmer, drier<br />

climate), (2) restored tallgrass prairie (land reverted to native prairie in 1979 and neighbouring<br />

land farmed to row crops for ~100 year), (3,4) two forest types (Douglas fir [Pseudotsuga<br />

menziesii] and loblolly pine [Pinus taeda], unfertilized control and N-fertilized plots), and (5)<br />

agricultural land (conventional- and no-till management systems). The selective inhibition<br />

technique, using captan (fungicide) and oxytetracycline hydrochloride (bactericide), was used to<br />

determine the activities (respiration) of fungi and bacteria in each of these soils and substrateinduced<br />

respiration was used to measure total active soil microbial biomass C. Phospholipid fatty<br />

acid analysis was used to determine the composition of the soil microbial biomass and determine<br />

if the activities and structure of the microbial communities were related. Differences in fungal-tobacterial<br />

(F:B) activities between treatments at a site were greatest at the prairie sites. The<br />

restored prairie had the highest F:B (13.5) and high total C (49.9 g C kg-1 soil); neighbouring soil<br />

farmed to maize had an F:B of 0.85 and total C of 36.0 g C kg-1 soil. Within the pairs of study<br />

soils, those that were tilled had lower fungal activities and stored C than those that were managed<br />

to native or no-till systems. In all pairs of soils, soils that had higher absolute fungal activities<br />

also had more total soil C and when two extreme cases were removed fungal activity was<br />

correlated with total soil C (R2=0.85). Thus, in this small set of diverse soils, increased fungal<br />

activities, more than F:B ratios, were associated with increased soil C. Practices that involved<br />

invasive land management decreased fungal activity and stored soil C compared to similar soils<br />

that were less intrusively managed.<br />

34. Ballard, T.M. 1984. A simple model for predicting stand volume growth response to fertilizer<br />

application. Canadian-Journal-of-<strong>Forest</strong>-<strong>Research</strong> 14(5): 661-665.<br />

17

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