| Literature DB >> 26313689 |
Mariana Hassegawa1, Filip Havreljuk2, Rock Ouimet2, David Auty1, David Pothier1, Alexis Achim1.
Abstract
Silvicultural restoration measures have been implemented in the northern hardwoods forests of southern Quebec, Canada, but their financial applicability is often hampered by the depleted state of the resource. To help identify sites most suited for the production of high quality timber, where the potential return on silvicultural investments should be the highest, this study assessed the impact of stand and site characteristics on timber quality in sugar maple (Acer saccharum Marsh.) and yellow birch (Betula alleghaniensis Britt.). For this purpose, lumber value recovery (LVR), an estimate of the summed value of boards contained in a unit volume of round wood, was used as an indicator of timber quality. Predictions of LVR were made for yellow birch and sugar maple trees contained in a network of more than 22000 temporary sample plots across the Province. Next, stand-level variables were selected and models to predict LVR were built using the boosted regression trees method. Finally, the occurrence of spatial clusters was verified by a hotspot analysis. Results showed that in both species LVR was positively correlated with the stand age and structural diversity index, and negatively correlated with the number of merchantable stems. Yellow birch had higher LVR in areas with shallower soils, whereas sugar maple had higher LVR in regions with deeper soils. The hotspot analysis indicated that clusters of high and low LVR exist across the province for both species. Although it remains uncertain to what extent the variability of LVR may result from variations in past management practices or in inherent site quality, we argue that efforts to produce high quality timber should be prioritized in sites where LVR is predicted to be the highest.Entities:
Mesh:
Year: 2015 PMID: 26313689 PMCID: PMC4551735 DOI: 10.1371/journal.pone.0136674
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Fig 1Comparison between LV predicted with parameters from 1976 and the observed LV.
The black dashed line is the reference line, with slope of 1, and the shaded area represents the 95% confidence interval.
Relative prices by NHLA [21] board class.
| Board class | 1976 | 2012 | |
|---|---|---|---|
| Yellow birch | Sugar maple | ||
| FAS | 1.44 | 1.81 | 1.65 |
| 1C | 1.00 | 1.00 | 1.00 |
| 2C | 0.71 | 0.70 | 0.69 |
| 3C | 0.43 | 0.25 | 0.37 |
a Averaged values from 2008 to 2012
Parameter estimates and associated standard errors (SE) for QI and V predictive models.
| Model | Parameter | Estimates | SE |
|---|---|---|---|
|
| β0 | 0.64 | 0.090 |
| β1 | 1.09 | 0.187 | |
| β2 | 0.60 | 0.064 | |
| β3 | 0.49 | 0.039 | |
| β4 | 0.48 | 0.029 | |
|
| γ0 | -0.01 | 0.001 |
| γ1 | 0.58 | 0.007 |
a QI, quality index;
b V , sawn wood yield of a log.
Fig 2Comparison between LV predicted by the reassessed model and observed values.
The black dashed line is the reference line, with slope of 1, and the shaded area represents the 95% confidence interval.
Fig 3Comparison between predicted and observed LVR for (a) yellow birch and (b) sugar maple.
Fig 4Partial dependence plots for each predictor retained in the final models for (a) yellow birch and (b) sugar maple.
The respective relative importance for each independent variable is in parentheses. Note: Stand age class: JEQ—young even-aged stand, JET—young stratified stand, JIN—young uneven-aged stand, VEQ—old even-aged stand, VET—old stratified stand, VIN—old uneven-aged stand; Ecological types: FC1x —red oak, FE1x —sugar maple—bitternut hickory, FE2x —sugar maple—basswood, FE3x —sugar maple—yellow birch, FE4x —sugar maple—beech—yellow birch, FE5x —sugar maple—hop hornbeam, FE6x —sugar maple—red oak, MJ1x —yellow birch—sugar maple, MS1x —balsam fir—yellow birch, RT1x —hemlock; Surficial deposit: 1A —glacial deposits without specific morphology, 1B —glacial deposits characterized by their morphology, 2 —fluvioglacial deposits, 3 —fluvial deposits, 4 —lacustrine deposits, 5 —marine deposits, 6 —littoral marine deposits, 7 —organic deposits, 8 —slope and weathering deposits, R—rock substrate. A complete description of the ecological types and surficial deposit can be found at Berger and Leboeuf [34].
Fig 5Distribution of LVR for (a) yellow birch and (b) sugar maple, across the province of Quebec.
Comparison between LVR from fitting data (inset figure) and predicted LVR from BRT.