Radial and longitudinal variation in stem diameter increment of lodgepole pine, white spruce, and black spruce: species and crown class differences

1987 ◽  
Vol 17 (10) ◽  
pp. 1223-1227 ◽  
Author(s):  
Merlise A. Clyde ◽  
Stephen J. Titus
Keyword(s):  
Black Spruce ◽  
Lodgepole Pine ◽  
Three Dimensional ◽  
White Spruce ◽  
Maximum Growth ◽  
Maximum Growth Rate ◽  
Stem Diameter ◽  
Longitudinal Variation ◽  
Stem Form ◽  
Diameter Increment

Radial and longitudinal variation in stem diameter increment were examined in lodgepole pine (Pinuscontorta var. latifolia Engelm.), white spruce (Piceaglauca (Moench) Voss), and black spruce (Piceamariana (Mill.) B.S.P.) in Alberta using graphical techniques. Three-dimensional surfaces of diameter increment at various heights and ages differed among the three species and dominant, codominant, and intermediate crown classes within each species. Relative to the maximum growth rate, black spruce and white spruce maintain higher and more constant levels of diameter increment over time than lodgepole pine. Variation among species probably reflects differences in shade tolerance, while differences among crown classes within a species are probably related to shading and wind stress effects. There were more similarities among the diameter increment surfaces for the three crown classes in lodgepole pine than in the two spruces. The stem diameter increment surfaces help explain the development of differences in stem form among the three species.

Influence of phosphorus on growth and biomass distribution of Alaskan taiga tree seedlings

1983 ◽  
Vol 13 (6) ◽  
pp. 1092-1098 ◽  
Author(s):  
F. Stuart Chapin III ◽  
Peter R. Tryon ◽  
Keith Van Cleve
Keyword(s):  
Growth Rate ◽  
Black Spruce ◽  
White Spruce ◽  
Maximum Growth ◽  
Maximum Growth Rate ◽  
Sand Culture ◽  
Tree Seedlings ◽  
Slow Growth Rate ◽  
Phosphate Supply ◽  
High Phosphate

Seedlings of six Alaskan taiga tree species and one tall shrub were grown in sand at three phosphate levels. There was a positive correlation between the growth rate of a species at the high-phosphate level in sand culture and its productivity in the natural environment. Poplar (Populusbalsamifera L.), which had highest growth rate under high phosphate, was most sensitive to reduction in phosphate supply, followed by birch (Betulapapyrifera (Reg.) Fern, and Raup) and aspen (Populustremuloides Michx.), whereas growth of conifers (larch (Larixlaricina (Du Roi) K. Koch), white spruce (Piceaglauca (Moench) Voss), and black spruce (P. mariana (Mill.) B.S.P.)) from late successional sites was slow and unaffected by phosphate supply. Similarly, when birch and white spruce seedlings were transplanted into natural forest stands, the maximum growth rate of birch was greater than that of white spruce, but birch growth was curtailed more by unfavorable conditions than was that of white spruce. We conclude that a slow growth rate reduces nutrient requirement and therefore minimizes nutrient stress on infertile sites, whereas a rapid growth enables nutrient-demanding species to dominate fertile sites.

scholarly journals Cold hardiness of white spruce, black spruce, jack pine, and lodgepole pine needles during dehardening

2017 ◽  
Vol 47 (8) ◽  
pp. 1116-1122 ◽  
Author(s):  
Rongzhou Man ◽  
Pengxin Lu ◽  
Qing-Lai Dang
Keyword(s):  
Picea Glauca ◽  
Pinus Banksiana ◽  
Cold Hardiness ◽  
Black Spruce ◽  
Lodgepole Pine ◽  
White Spruce ◽  
Visual Assessment ◽  
Jack Pine ◽  
Pine Needles ◽  
Late Winter

Conifer winter damage results primarily from loss of cold hardiness during unseasonably warm days in late winter and early spring, and such damage may increase in frequency and severity under a warming climate. In this study, the dehardening dynamics of lodgepole pine (Pinus contorta Dougl. ex. Loud), jack pine (Pinus banksiana Lamb.), white spruce (Picea glauca (Moench) Voss), and black spruce (Picea mariana (Mill.) B.S.P.) were examined in relation to thermal accumulation during artificial dehardening in winter (December) and spring (March) using relative electrolyte leakage and visual assessment of pine needles and spruce shoots. Results indicated that all four species dehardened at a similar rate and to a similar extent, despite considerably different thermal accumulation requirements. Spring dehardening was comparatively faster, with black spruce slightly hardier than the other conifers at the late stage of spring dehardening. The difference, however, was relatively small and did not afford black spruce significant protection during seedling freezing tests prior to budbreak in late March and early May. The dehardening curves and models developed in this study may serve as a tool to predict cold hardiness by temperature and to understand the potential risks of conifer cold injury during warming–freezing events prior to budbreak.

scholarly journals Splitting in Fire-Killed Trees in the Boreal Forest of Alberta

2003 ◽  
Vol 20 (4) ◽  
pp. 167-174
Author(s):  
Nobutaka Nakamura ◽  
Paul M. Woodard ◽  
Lars Bach
Keyword(s):  
Boreal Forest ◽  
Boreal Forests ◽  
Black Spruce ◽  
Lodgepole Pine ◽  
White Spruce ◽  
Balsam Fir ◽  
Crown Fire ◽  
In Fire ◽  
Solar Angle

Abstract Tree boles in the boreal forests of Alberta, Canada will split once killed by a stand-replacing crown fire. A total of 1,485 fire-killed trees were sampled, 1 yr after burning, in 23 plots in 14 widely separated stands within a 370,000 ha fire. Sampling occurred in the Upper and Lower Foothills natural subregions. The frequency of splitting varied by species but averaged 41% for all species. The order in the frequency of splitting was balsam fir, black spruce, white spruce and lodgepole pine. The type of splitting (straight, spiral, or multiple) varied by species, as did the position of the split on the tree bole. Aspect or solar angle was not statistically related to the type or occurrence of splitting.

scholarly journals Effects of winter warming on cold hardiness and spring budbreak of four boreal conifers

Botany ◽  
2016 ◽  
Vol 94 (2) ◽  
pp. 117-126 ◽  
Author(s):  
Rongzhou Man ◽  
Steve Colombo ◽  
Pengxin Lu ◽  
Qing-Lai Dang
Keyword(s):  
Picea Glauca ◽  
Pinus Banksiana ◽  
Cold Hardiness ◽  
Black Spruce ◽  
Lodgepole Pine ◽  
Temperature Fluctuations ◽  
White Spruce ◽  
Jack Pine ◽  
Experimental Warming ◽  
Freezing Damage

Compared with the effects of spring frosts on opening buds or newly flushed tissues, winter freezing damage to conifers, owing to temperature fluctuations prior to budbreak, is rare and less known. In this study, changes in cold hardiness (measured based on electrolyte leakage and needle damage) and spring budbreak were assessed to examine the responses of four boreal conifer species — black spruce (Picea mariana (Mill.) B.S.P.), white spruce (Picea glauca) (Moench) Voss), jack pine (Pinus banksiana Lamb.), and lodgepole pine (Pinus contorta Dougl. ex. Loud.) — to different durations of experimental warming (16 °C day to –2 °C night with a 10 h photoperiod, except for night temperatures during November warming (+2 °C)). Seedlings showed increased responses to warming from November to March, while the capacity to regain the cold hardiness lost to warming decreased during the same period. This suggests an increasing vulnerability of conifers to temperature fluctuations and freezing damage with the progress of chilling and dormancy release from fall to spring. Both lodgepole pine and jack pine initiated spring growth earlier and had greater responses to experimental warming in bud phenology than black spruce and white spruce, suggesting a greater potential risk of frost/freezing damage to pine trees in the spring.

Pathogenicity of Polyporustomentosus and P. tomentosus var. circinatus on seedlings of 11 conifer species

1976 ◽  
Vol 6 (2) ◽  
pp. 129-131
Author(s):  
Roy D. Whitney ◽  
Wendy P. Bohaychuk
Keyword(s):  
Ponderosa Pine ◽  
Black Spruce ◽  
Lodgepole Pine ◽  
White Spruce ◽  
Conifer Species ◽  
Laboratory Conditions

Polyporustomentosus Fr. caused significantly higher disease ratings than P. tomentosus var. circinatus Fr. in seedlings of 6 of 11 conifer species under laboratory conditions. Both fungi caused highest disease ratings on seedlings of ponderosa pine (Pinusponderosa Laws.), followed by lodgepole pine (Pinuscontorta Dougl. var. latifolia Engelm.), white spruce (Piceaglauca (Moench) Voss), black spruce (Piceamariana (Mill.) B.S.P.), and tamarack (Larixlaricina (Du Roi) K. Koch).

Effects of seed water content and storage temperature on the germination parameters of white spruce, black spruce and lodgepole pine seed

New Forests ◽  
2008 ◽  
Vol 36 (2) ◽  
pp. 171-185 ◽  
Author(s):  
T. Beardmore ◽  
B. S. P. Wang ◽  
M. Penner ◽  
G. Scheer
Keyword(s):  
Water Content ◽  
Storage Temperature ◽  
Black Spruce ◽  
Lodgepole Pine ◽  
White Spruce ◽  
And Storage ◽  
Germination Parameters ◽  
Seed Water Content

Seedling growth and water use of boreal conifers across different temperatures and near-flooded soil conditions

2011 ◽  
Vol 41 (12) ◽  
pp. 2292-2300 ◽  
Author(s):  
Jane M. Wolken ◽  
Simon M. Landhäusser ◽  
Victor J. Lieffers ◽  
Uldis Silins
Keyword(s):  
Soil Temperature ◽  
Water Use ◽  
Water Table ◽  
Seedling Growth ◽  
Black Spruce ◽  
Lodgepole Pine ◽  
White Spruce ◽  
High Water ◽  
Soil Conditions ◽  
Flooded Soil

To test the hypothesis that seedling growth and water use increase with soil temperature and improved soil aeration and vary with species, we evaluated the above- and below-ground growth and water use of seedlings of four northern boreal conifer species: black spruce ( Picea mariana (Mill.) B.S.P.), white spruce ( Picea glauca (Moench) Voss), tamarack ( Larix laricina (Du Roi) K. Koch), and lodgepole pine (Pinus contorta Dougl. ex Loud.) grown under different temperature and near-flooded soil conditions. Seedlings were grown in specialized pots that maintained the water table level at either 15 cm (high water table treatment: very wet) or 30 cm (low water table treatment: moderately wet) below the soil surface, and whole-seedling transpiration was assessed. Soil temperature (5, 10, or 20 °C) was controlled with a water bath surrounding the pots. Although some species were sensitive to the high water table treatment, soil temperature was the driver of seedling growth and water use. We ranked the ability of the seedlings of the species to tolerate the cold soil conditions examined as black spruce > lodgepole pine > tamarack > white spruce. The ranking of the ability to tolerate near-flooded conditions was tamarack and lodgepole pine > black spruce > white spruce.

scholarly journals Growth of Coniferous Seedlings on a Drained and Mounded Peatland in Central Alberta

2000 ◽  
Vol 17 (2) ◽  
pp. 71-79 ◽  
Author(s):  
Sam K. Takyi ◽  
Graham R. Hillman
Keyword(s):  
Picea Glauca ◽  
Pinus Contorta ◽  
Black Spruce ◽  
Lodgepole Pine ◽  
White Spruce ◽  
Diameter Growth ◽  
Larix Laricina ◽  
Growing Seasons ◽  
Collar Diameter ◽  
Survival And Growth

Abstract Artificial reforestation experiments compared survival and growth of five species of coniferous containerized seedlings, and seedling browsing by ungulates on a clearcut, drained, and mounded peatland in the boreal forest. Six to seven growing seasons after planting, 91% of all seedlings had survived. Height and diameter growth in five species were ranked as follows: Siberian latch (Larix sibirica Ledeb.) > lodgepole pine (Pinus contorta var. latifolia Engelm.) > tamarack (Larix laricina [Du Roi] K. Koch) > black spruce (Picea mariana [Mill.] B.S.P.) = white spruce(Picea glauca [Moench] Voss). Overall, tamarack height and diameter growth was twice that of either spruce species. Height and diameter growth of tamarack, black spruce, and white spruce planted in the spring was 65% to 97% greater than that of the more robust seedlings for the same species planted in the fall of the same year. Repeated winter browsing by ungulates did not affect survival and growth of the five species. In an experiment where survival and growth of tamarack and black spruce seedlings planted on the mounds were compared with that of seedlings planted on the flat areas between mounds, there were no differences in survival, height, or root collar diameter growth between the two planting sites. In the event that suitable peatlands are used to augment existing timber supplies, lowering the water table through ditching, combined with mound-planting, is a feasible method of reforesting timber-harvested, boreal wet sites with Siberian latch, lodgepole pine, and white spruce. Tamarack and black spruce, however, survive and grow well on drained peatlands without mound-planting. North. J. Appl. For. 17(2):71-79.

Three-dimensional instabilities of oscillatory equatorial zonal shear flows

2009 ◽  
Vol 623 ◽  
pp. 59-74 ◽  
Author(s):  
ANDREI NATAROV ◽  
KELVIN J. RICHARDS
Keyword(s):  
Growth Rate ◽  
Three Dimensional ◽  
Maximum Growth ◽  
Maximum Growth Rate ◽  
Oscillatory Shear ◽  
Resonant Excitation ◽  
Wave Number ◽  
Zonal Flows ◽  
Vertical Scale ◽  
Zonal Wave Number

In this paper, we investigate the linear stability of oscillating zonal flows on the equatorial β-plane in the presence of fully three-dimensional disturbances. To exclude inflection point effects, we focus on the simplest case of a linear meridional shear with time-mean and oscillating components. For purely oscillatory background flows we find that in addition to resonant excitation of ‘additive’ type that occurs in the zonally invariant case, resonant excitation of ‘difference’ type is also possible. For flows with an oscillatory shear superimposed on an unstable time-mean shear it is shown that while the oscillatory shear has a stabilizing influence on disturbances with a small zonal wave number k, at higher k the effect of the oscillating shear diminishes and can even be destabilizing. Overall, a small oscillatory shear tends to reduce the fastest growth rate in the system and pushes the dominant k to higher values. Calculation of dominant zonal and vertical modes shows that the zonally asymmetric modes dominate a large portion of the parameter space, especially at high time-mean background shear and low oscillatory shear. As a result, the dominant vertical mode can have a somewhat larger vertical scale than in the zonally invariant case. At intermediate values of the time-mean shear the growth rate is relatively flat with respect to the zonal mode number, with maximum growth rate occurring in bands of high and low k. We have uncovered a rich assortment of vertical and zonal modes which are likely to play a role in the nonlinear evolution of equatorial flows.

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