Release of Oregon White Oak from Overtopping Douglas-fir: Effects on Soil Water and Microclimate

2007 ◽  
Vol 81 (2) ◽  
pp. 112-124 ◽  
Author(s):  
Warren D. Devine ◽  
Constance A. Harrington
2021 ◽  
Vol 498 ◽  
pp. 119543
Author(s):  
Jill J. Beckmann ◽  
Rosemary L. Sherriff ◽  
Lucy P. Kerhoulas ◽  
Jeffrey M. Kane

Forests ◽  
2019 ◽  
Vol 10 (5) ◽  
pp. 381 ◽  
Author(s):  
Ze’ev Gedalof ◽  
Jennifer Franks

Due to a suite of environmental changes, Oregon white oak (Quercus garryana Douglas ex Hook; called Gary oak in Canada) associated ecosystems at many North American sites are being encroached upon by Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco var. menziesii) and other conifer species. Alteration of stand structure and composition is causing substantial changes in the dynamics of these ecosystems, creating an environment in which Oregon white oak is not thriving. In this study we used dendrochronology to investigate the competitive dynamics between Oregon white oak and Douglas-fir in a mixed forest stand on Southern Vancouver Island. Significant species-specific differences in radial growth sensitivity to drought were found between Oregon white oak and Douglas-fir. Oregon white oak trees growing at high densities, or competing with Douglas-fir for moisture were found to be more sensitive to drought and more sensitive to growing conditions during the prior year. The response of Douglas-fir to drought was less variable, possibly due to the relatively low conifer densities at our study site, as well as the species’ ability to root graft, its higher shade tolerance than Oregon white oak, and its rapid growth rates that allow it to achieve a more dominant canopy position. The non-stationary response to climate exhibited by Oregon white oak provides insights into the mechanisms by which Oregon white oak savannas are being converted to coniferous woodland, but also suggest that tree-ring reconstructions of climate need to explicitly address changes in stand dynamics that could influence the growth–climate relationship


2011 ◽  
Vol 85 (2) ◽  
pp. 108-119 ◽  
Author(s):  
Carson B. Sprenger ◽  
Peter W. Dunwiddie

1985 ◽  
Vol 15 (1) ◽  
pp. 185-188 ◽  
Author(s):  
T. M. Ballard ◽  
M. G. Dosskey

Needle water potential in western and mountain hemlock falls as the soil dries, but under our experimental conditions, it remained stable in Douglas-fir. Resistance to water flow from soil to foliage is higher for the hemlocks and increases more steeply as the soil dries. These findings physically account for the observation that water uptake is reduced relatively more for the hemlocks than for Douglas-fir, as soil water potential declines.


IAWA Journal ◽  
1996 ◽  
Vol 17 (4) ◽  
pp. 445-461 ◽  
Author(s):  
Hua Lei ◽  
Michael R. Milota ◽  
Barbara L. Gartner

In order to analyze the variation in wood properties within and between trees of an underutilized tree species, we sampled six Oregon white oak (Quercus garryana Dougl.) trees from an 80-year old mixed stand of Q. garryana and Douglas-fir (Pseudotsuga menziesii [Mirb.] Franco) in the Coast Range of Western Oregon, USA. Fibre length, earlywood vessel diameter, tissue proportions, and specific gravity were measured on samples across the diameter at two heights. Trees had a slight lean (2-12°), so we sampled separately both radii of a diametric strip that ran from the lower to upper side of lean.


Fire Ecology ◽  
2019 ◽  
Vol 15 (1) ◽  
Author(s):  
Deborah G. Nemens ◽  
J. Morgan Varner ◽  
Peter W. Dunwiddie
Keyword(s):  

2019 ◽  
Vol 447 ◽  
pp. 77-86
Author(s):  
Jeffrey M. Kane ◽  
Eamon A. Engber ◽  
John E. McClelland

1985 ◽  
Vol 15 (4) ◽  
pp. 701-707 ◽  
Author(s):  
Susan J. Riha ◽  
Gaylon S. Campbell

A model was developed to estimate water fluxes in Douglas-fir (Pseudotsugamenziesii (Mirb.) Franco) plantations using daily measurements of precipitation and maximum and minimum air temperatures. Soil water flow was modeled using a one-dimensional finite element solution to the Richards equation, with precipitation and root uptake of water included as source and sink terms. Soil hydraulic properties varied as a function of depth. Root uptake of water was based on an analog water uptake model modified to include root resistance and cylindrical flow of water. Potential evapotranspiration was calculated assuming leaf and air temperature did not differ and assuming stomatal conductance was dependent on the vapor density deficit of the air. Model validity was tested by comparing predictions with field measurements of soil water content made in the summer of 1978 at two locations in western Washington. In general, the model predicted the observed drying of the soil. Aspects of the simulated water budget for these Douglas-fir stands considered most significant were (i) the use of soil-stored water for transpiration in the summer, (ii) the net flux of water into the root zone from deeper in the soil during the summer, (iii) the dependence of water reaching the soil in the summer on the intensity of rainfall, (iv) the large percentage of the total transpiration that occurred in spring and fall, and (v) the large amount of water moving out of the soil profile in the winter.


1977 ◽  
Vol 7 (4) ◽  
pp. 595-604 ◽  
Author(s):  
C. S. Tan ◽  
T. A. Black ◽  
J. U. Nnyamah

As part of a 2-year study of the effect of thinning on evapotranspiration in Douglas fir (Pseudotsugamenziesii (Mirb.) Franco), the relationship between stomatal diffusion resistance (rs) and environmental variables were studied. Research was conducted in an unthinned stand (1840 stems ha−1) with negligible undergrowth and a thinned stand (840 stems ha−1) with substantial salal (Gaultheriashallon Pursh) undergrowth. During the daytime rs was mainly related to the soil water potential (ψs) and the vapour pressure deficit (v.p.d.) of the canopy air. Daytime values of rs for Douglas fir ranged from 2 to 60 s cm−1 for values of v.p.d. between 4 and 24 mb (4 and 24 × 102 Pa) and values of ψs between 0 and −12.5 bars (0 and −12.5 × 105 Pa). Although increasing rs was usually associated with decreasing pressure potential of the twig xylem (ψt), increasing rs appeared to be associated with increasing ψt when the v.p.d. was high. Stress history was found to cause a shift in the relationship of rs to ψt, but had little effect on the relationship of rs to v.p.d. and ψs. Daytime values of rs for salal ranged from 2 to 45 s cm−1. This stomatal behaviour suggests that as the soil dried out, salal transpiration accounted for an increasing fraction of the total water loss by the thinned stand.


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