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PGMS
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Brian Burton Penn State Cooperative Extension Doylestown, PA March-April, 2002 All pavement
and hardscaping installations are critically dependent on the integrity
and stability of base materials below the surface. Any disruption or movement
of the base material or underlying structure will cause deficiencies,
such as rutting, heaving, or displacement of paving surfaces to quickly
appear on the surface. These defects represent a hazard for vehicles,
wheelchair users and pedestrians and can be expensive to repair. A recent
study cited defects directly attributed to tree root growth as the sixth
most common cause of premature sidewalk failure in municipal applications.
For this reason, root barriers, which prevent the growth of opportunistic
tree roots under infrastructure components such as sidewalks and roadways,
have been increasingly recognized as essential components of hardscaping
installations. Over time they have proved to be effective in eliminating
deficiencies in new construction and in retrofitting and repairing existing
installations. SURROUND STYLE PLANTING APPLICATIONS The first
root barriers made their debut in the early 1970s. The first configuration
employed was a surround style barrier. These surround barriers
could be purchased in one-piece, or they were assembled in rolls or panels
which were connected together on-site. Early research
showed that the smooth walls of the surround sound barrier often lead
to circling of the roots. The young tree roots would hit the side of the
barrier and instead of growing in a downward direction they would grow
in a horizontal path. This eventually resulted in a circular root configuration
that could eventually girdle the tree. This kind of root growth
pattern could eventually constrict the vascular system of the tree and
inhibit growth. Root barriers are now available with ribs that encourage
the downward growth of roots. In addition other features, which are now
available, assist in deep watering and continuing oxygen exchange in the
soil. One of the
most crucial factors for the long-term success with root barriers is ensuring
the installation of the top edge of the root barrier above grade. It is
also important to choose a root barrier of sufficient size to accommodate
the growth of the tree as it matures over time. An undersized barrier
will restrict root growth and compromise the trees ability to maintain
a firm anchor in the soil. Additionally, if the root barrier is too small
it will be difficult or impossible to properly backfill between root ball
and barrier. This condition causes air pockets to become filled with water,
creating conditions that can lead to decline of root growth. In general,
barrier installation is more successful if the soil is properly prepared.
Specifically, the soil should be loosened well below the bottom of the
barrier to encourage deep rooting. If hard and compacted in later years
the roots will grow out from the bottom and simply turn upward. As well as proper soil preparation, accommodations for adequate soil moisture below the barrier should also be made at planting time. If adequate moisture levels below the barrier are not maintained the roots tend to grow near the surface where moisture is readily available.
INSTALLATION
LINEAR INSTALLATION
ROOTS, WATER and SOIL Once the
tree is planted attention needs to be directed at roots, water and moisture
movement in the soil. Trees have three primary forms of roots: roots near
the tree base, transport roots and the ephemeral, absorbing roots. These
transport roots carry food to the root tips, as well as water and essential
elements to the leaves. The longer a transport root survives, the bigger
it becomes. Roots grow where soil resources are most plentiful. If that
area is near the soil surface, thats where the roots will grow. The two resources
most important to tree-root growth are oxygen and water. Oxygen is available
only near the soil surface in large air-filled soil pores. Tremendous
competition exists for this oxygen between tree roots and other plant
roots. Because of the ease with which roots pull water from the soil,
roots sense and grow toward areas where plenty of water is available.
The quandary is that water supplies must be located in the same soil areas
where atmospheric oxygen also is available. Soil organisms quickly use
the dissolved oxygen in soil water and,as a result, it is not as readily
available to tree roots as atmospheric soil oxygen. Atmospheric
oxygen is essential to tree life. The aboveground portion of a tree has
no problem finding oxygen in the air for respiration. (Oxygen content
in the atmosphere is about 21 percent.) For roots, however, the plight
of getting enough oxygen is severe. For unconstrained
root growth, the soil atmosphere must contain more than 15 percent oxygen.
As soil-oxygen levels fall below 5 percent, root growth stops. Oxygen
levels of less than 2 percent lead to root decline and death. The three
major problems that cause inadequate soil oxygen are:
All of these
problems lead to an oxygen-limited condition of the soil: an anaerobic
condition. Under anaerobic soil conditions, different types of microorganisms-primarily
bacteria-take over the soil. The anaerobic organisms produce toxins and
consume or infect roots. Several tree root rots thrive at low soil-oxygen
levels. Warmer temperatures
disrupt oxygen use by tree roots. As soil and air temperatures increase,
so does oxygen demand in a tree and in the surrounding soil. For every
18 degrees F increase in temperature, oxygen demand doubles for both tree
roots and other soil organisms. Increasing temperatures cause tree roots
to respire faster, which uses food and oxygen more quickly An additional
example of root-oxygen problems occurs on recreation sites where foot
and vehicle traffic have compacted the soil, collapsing the soil air pores.
To maximize landscape performance, some landscape managers add composted
organic matter and nitrogen to the soil, along with continuous irrigation.
The result is a rich mess of oxygen-demanding microbes fueled by organic
material and nitrogen. WATER MOISTURE
MOVEMENT IN THE SOIL |