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Soil Carbon and Other Quality
Indicators in Managed Northern Forests | |
Plot Design |
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The plot design and vegetation description methods used in this study
follow the Forest
Inventory and Analysis (FIA) protocol, to
allow for comparisons. One plot consisted of:
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The GPS coordinates of
the center of each plot were recorded using
a high-precision GPS. A yellow stake was pounded in the ground at the center of the plot as permanent marker. |
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Plot Design | Measuring Soil Carbon | Calculating Soil CarbonMeasuring Above Ground Carbon | Calculating Above Ground Carbon |
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Measuring Soil Carbon |
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In this
study, three 40
x 60 cm soil pits were excavated at each site, down to a
depth of 40-inch, bedrock, or water. |
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Soil horizons can
be identified after excavating a soil pit. Horizon descriptions can be used to
assign a soil series
to each soil described ("soil series" is the soil
science equivalent of the term "species" used in biology). Soil horizons can be differentiated through a change in color or texture, a change in the abundance of roots, the presence or absence of redoxomorphic features, etc. For example in the picture on the right, an E horizon (grey color) and a Bs horizon (reddish color), can very easily be identified. The amount of carbon can vary strikingly between horizons and it is therefore necessary to sample soils by horizons when quantifying soil carbon. Soil samples were collected from each soil horizon and analyzed in the lab. |
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The forest floor, also
known in soil science as the organic
soil
horizons (Oi, Oe, and Oa in the US taxonomic system), was
collected by
cutting three 15 x 15 cm
squares in the forest floor, at each of the six
soil subplots. Organic soil samples were analyzed in the lab. As the forest floor was collected over a known area, carbon per hectare (or acre) can easily be quantified. ![]() |
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Soil samples were
collected from three soil pits. In order to translate
from percent carbon by weight to carbon per hectare
(or acre), soil bulk
density needs to be know. To measure and calculate bulk density, we used a power auger equipped with a diamond-tipped core. We then collected cores of known depth (usually 10-20 cm) at each of the 6 soil subplots. Cores were collected down to bedrock, water, or 100 cm depth, whichever came first. Soil samples obtained from cores were also analyzed in the lab. |
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The power auger
also allowed us to estimate
soil stoniness.
Stoniness is important because the quantity of rocks in the
soil affects the calculation of carbon per hectare (or acre).
The picture on the right illustrates how the power auger cored through a rock, allowing us to collect both the rock and soil sample. |
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Calculating Soil Carbon | ||
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Plot
Design | Measuring Soil
Carbon | Calculating
Soil Carbon Measuring Above Ground Carbon | Calculating Above Ground Carbon |
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Measuring
Above-Ground Carbon |
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In order to
calculate carbon stored in the aboveground biomass, we
measured tree diameter
(DBH) and height (for trees >2 inches) in
each
of the four vegetation subplots. Trees were also identified by
species. Each vegetation subplot contained a microplot where the percent ground cover occupied by moss, lichen, shrubs, etc. was estimated. Saplings and seedlings were counted in each microplot. To estimate the quantity of carbon stored in down woody material, we measured down trees and branches following the FIA protocol. |
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Calculating Above-Ground Carbon | ||
bm = total aboveground biomass (kg dry mass) DBH = diameter at breast height (cm) Exp = exponential function ln = log base e For more details, see: Jenkins J.C., Chojnacky D.C., Heath L.S., and Birdsey R.A., National-Scale Biomass Estimators for United States Tree Species, Forest Science, Vol 49, No.1, February 2003
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Plot Design
| Measuring
Soil Carbon | Calculating Soil Carbon Measuring Above Ground Carbon | Calculating Above Ground Carbon |