A Change
in the Landscape
When viewed from a satellite, the 64,000 square mile Chesapeake Bay watershed still appears mostly green (Figure 1). Had the same satellite passed over the Bay 400 years ago, it would have revealed a watershed that was more than 90%
forested, mostly with oak and hickory trees, but also pines where soils were poorer. By 1900, however, forest cover in the Bay watershed had shrunk to about a third of its pre-settlement extent, primarily because of massive clearing for crops and pasture. The pattern shifted again between 1900 and 1970, when forest cover expanded as marginal farms were abandoned and foresters began to reforest the watershed. By 1970, forest cover had recovered nicely, and comprised more than 60% of the watershed area of the Bay.
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Figure 1 Click on image for larger version |
More recently, land development has triggered a new cycle of forest clearing, and watershed forest cover has begun declining again. Between 1973 and 1997, forest researchers measured an annual loss of forest cover of about 80,000 acres across the watershed. Today, forest cover in the Chesapeake Bay has declined to about 58% of the total watershed area, with further declines expected
as urban sprawl continues..
Healthy Forests Mean a Healthy Bay
From an ecological standpoint, forest cover is very important to the health of the Bay. For example, although forests now comprise a significant percentage of the land area in the Bay watershed, they only generate four percent of its nutrient load and produce an even lower percentage of other pollutants that can harm the Bay. Forests also help build soils and keep them in place.
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Figure 2 Click on image for larger version |
The most important forests for ensuring the health of the Bay's
waters are the ones that buffer its streams and rivers. Stream-side forests, which comprise about five percent of the watershed,
are also known as riparian forests. These play an essential role in the ecology of running waters.
These riparian buffers filter runoff, absorb flood waters,
store nutrients, stabilize stream banks, cool water, provide food for stream life, and are critical habitats for hundreds of species of wildlife (Figure
2). Regrettably, nearly half of the 100,000 miles of streams and rivers that drain to the Bay lack an adequate forest buffer along their banks. Reforesting these missing buffers is one of the most important and inexpensive strategies
for helping to restore the health of the Bay.
Autumn Leaf Fall in the Watershed
Autumn leaf fall signals three major changes in the watershed. The first is that the “leaf pump” is turned off across the watershed. During the growing season, trees are quite thirsty. For example, an acre of mature forest can take up more than 1,800 gallons of water every day from the soil to drive the photosynthesis process. Consequently, groundwater and stream flows usually drop sharply during the growing season
while trees are busy pumping water from the ground. Even in normal rainfall years, stream flow and groundwater levels drop to their lowest levels of the year by the end of the growing season. Once the leaves drop from the forest, the "pump" is effectively turned off until spring. In most years, the fall and winter are the primary seasons
for replenishing groundwater and stream and river flows.
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Figure
3
Click on image for larger version |
The second major change associated with autumn leaf fall is the movement of leaves into small streams. Streams depend on autumn leaves to supply the energy needed to support stream life throughout the rest of the year. When leaves blow
or flow into streams, they accumulate into “packs” that gradually break down over time,
thanks to colonization by fungi (Figure 3). As the fungi do their work, the
leaf pack mass decreases by about one to two percent each day.
The nutrients produced in the process enter the food chain of the stream.
The fungi on leaf packs are a major food source for many aquatic insects such as
caddis flies, stoneflies and crane flies. These insects shred or collect fine leaf particles, and in turn, are eaten by small fish and other aquatic life. Thus, fallen leaves,
which provide as much as 75% of the energy used in the food chain, really are the base of the food chain in small
streams. At a time of year when growth is dormant elsewhere, the first few months after leaf fall usually triggers the biggest pulse of growth and activity in the small streams of the Chesapeake Bay.
The third major change associated with autumn leaf fall is the shift of carbon from the forest to the forest floor. At
this time of year, a typical acre of mature forest in the watershed will drop between two and three tons of
leaves, twigs and branches. This fresh supply of organic matter is gradually composted throughout the winter and spring and helps drive the forest ecosystem during the next growing season. A single acre of the forest floor can support more than a million earthworms, 40 million mites, 12 million spring tails and countless numbers of bacteria and fungi. These organisms, in turn, help support thousands of salamanders per acre. Indeed, salamanders collectively have more biomass than either birds or small mammals in many eastern forests. Thus, the autumn leaf fall supports most of the forest food chain.
You can also take advantage of the autumn leaf fall in your neighborhood to improve the quality of your soils by composting your leaves in your backyard.
While, leaf waste accounts for about 10% of the annual trash flow in most communities,
this rises to almost 70% in the fall. By composting your leaves, you can create
your own supply of humus and, in the process, help preserve landfill space in your
community.
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