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Logging Debris Matters: Better Soil, Fewer Invasive Plants
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The logging debris that remains after
timber harvest traditionally has been seen
as a nuisance. It can make subsequent tree
planting more difficult and become fuel
for wildfire. It is commonly piled, burned,
or taken off site. Logging debris, however,
contains significant amounts of carbon
and nitrogen—elements critical to soil
productivity. Its physical presence in the
regenerating forest creates microclimates
that influence a broad range of soil and
plant processes.
Researchers Tim Harrington of the
Pacific Northwest Research Station;
Robert Slesak, a soil scientist with the
Minnesota Forest Resources Council;
and Stephen Schoenholtz, a professor of
forest hydrology and soils at Virginia
Tech, conducted a five-year study at two
sites in Washington and Oregon to see
how retaining logging debris affected
the soil and other growing conditions at
each locale.
They found that keeping logging debris in
place improved soil fertility, especially in
areas with coarse-textured, nutrient-poor
soils. Soil nitrogen and other nutrients
important to tree growth increased, and
soil water availability increased due to the
debris’ mulching effect. The debris cooled
the soil, which slowed the breakdown and
release of soil carbon into the atmosphere.
It also helped prevent invasive species such
as Scotch broom and trailing blackberry
from dominating the sites.
Forest managers are using this information
to help maximize the land’s productivity
while reducing their costs associated with
debris disposal.
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Logging Truck North Carolina
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The Golden-winged warbler needs "young forest" habitat for nesting created by doing a selective harvest that can restore forest health and improve habitat for game species like white-tailed deer, ruffed grouse, and wild turkey.
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Lomte Barhanpurkar 1979.pdf
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Long term climate implications of 2050 emission reduction targets
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A coupled atmosphere-ocean-carbon cycle model is used to examine the long term climate implications of various 2050 greenhouse gas emission reduction targets. All emission targets considered with less than 60% global reduction by 2050 break the 2.0°C threshold warming this century, a number that some have argued represents an upper bound on manageable climate warming. Even when emissions are stabilized at 90% below present levels at 2050, this 2.0°C threshold is eventually broken. Our results suggest that if a 2.0°C warming is to be avoided, direct CO2 capture from the air, together with subsequent sequestration, would eventually have to be introduced in addition to sustained 90% global carbon emissions reductions by 2050.
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Long-Distance Dispersal of Plants
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Long-distance dispersal (LDD) of plants poses challenges to research because it involves rare events driven by complex and highly stochastic processes. The current surge of renewed interest in LDD, motivated by growing recognition of its critical importance for natural populations and communities and for humanity, promises an improved, quantitatively derived understanding of LDD. To gain deep insights into the patterns, mechanisms, causes, and consequences of LDD, we must look beyond the standard dispersal vectors and the mean trend of the distribution of dispersal distances. ‘‘Nonstandard’’ mechanisms such as extreme climatic events and generalized LDD vectors seem to hold the greatest explanatory power for the drastic deviations from the mean trend, deviations that make the nearly impossible LDD a reality.
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Long-term aspen cover change in the western US
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Quaking aspen (Populus tremuloides Michx.) is one of the most important tree species in the western United States due to its role in biodiversity, tourism, and other ecological and aesthetic values. This paper provides an overview of the drivers of long-term aspen cover change in the western US and how these drivers operate on diverse spatial and temporal scales. There has been substantial concern that aspen has been declining in the western US, but trends of aspen persistence vary both geographically and tem- porally. One important goal for future research is to better understand long-term and broad-scale changes in aspen cover across its range. Inferences about aspen dynamics are contingent on the spatial and temporal scales of inquiry, thus differences in scope and design among studies partly explain varia- tion among conclusions. For example, major aspen decline has been noted when the spatial scale of inquiry is relatively small and the temporal scale of inquiry is relatively short. Thus, it is important to consider the scale of research when addressing aspen dynamics.
Successional replacement of aspen by conifer species is most pronounced in systems shaped by long fire intervals and can thus be seen as part of a normal, long-term fluctuation in forest composition. Aspen decline was initially reported primarily at the margins of aspen’s distribution, but may be becoming more ubiquitous due to the direct effects of climate (e.g. drought). In contrast, the indirect effects of recent climate (e.g. forest fires, bark beetle outbreaks, and compounded disturbances) appear to favor aspen and may facilitate expansion of this forest type. Thus, future aspen trends are likely to depend on the net result of the direct and indirect effects of altered climate.
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