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Loftin 2006.pdf
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LEW-MAR
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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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Lomte Jadhav 1980.pdf
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Loncarich, Frank
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Long et al 1984.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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