
Study Site
Research is conducted in collaboration with U.S.D.A. Forest Service
managers on the Morehead and Stanton Ranger
Districts of the Daniel Boone
National Forest (DBNF). The DBNF is located in the Cliff Section of the
Cumberland Plateau in eastern Kentucky. The mean annual temperature is
12º C, with mean daily temperatures ranging from 0º C in January to
31º C in July. The forest stands are approximately 70-80 years old. Fire
has not occurred on these sites for at least 25-30 years.
Morehead:
Three study sites are located in Bath
and Menifee counties.
Study areas are 1000-1200 acres (400-500 ha) with treatment areas within
each study area subdivided along ridge systems (300-400 acres; 120-160
ha). The sites range from xeric to sub-xeric oak-hickory forest at the
ridge-tops to sub-mesic forest in the coves.
The dominant oak species
are scarlet oak (Quercus coccinea Muench.), northern red oak
(Q.
rubra L.) chestnut oak (Q. prinus L.), white oak (Q.
alba L.) and black oak
(Q. velutina Lam.). The dominant hickories are pignut hickory
(Carya
glabra Sweet.) and mockernut hickory (C. tomentosa L.
Nutt) with occasional shagbark (C. laciniosa Loud.), shellbark
(C.
ovata Koch.), and bitternut
hickories (C. cordoformis Koch.). Other dominant overstory
trees include yellow poplar (Liriodendron tulipifera L.) and
white ash (Fraxinus
americana L.). The midstory is dominated by red maple (Acer
rubrum L.), sourwood
(Oxydendrum arboretum [L.] DC), black gum (Nyssa
sylvatica Marsh.), sassafras
(Sassafras officinale Nees and Ebermaier) and sugar maple
(Acer
sacchrum Marsh.).
Mean annual precipitation is 109 cm spread throughout the year.
Elevation ranges from 260 to 360 m (850 – 1150 ft) with a variety
of slope aspects. Soils vary in depth and moisture due to the steep unglaciated
topography and are classified as Typic Hapludults, Typic Hapludalfs,
Ultic Hapludalfs, and Typic Dystrochrepts.
Stanton:
These sites are located on a series of non-contiguous ridge-tops
in Powell, Menifee and Wolfe counties. (see pdf map). Treatment areas
are 70-140 acres (20-40 ha). These sites are xeric to sub-xeric oak-pine
forests dominated by scarlet oak and chestnut oak, with some white oak
and black oak. Hard pines, shortleaf (Pinus echinata Mill.)
and pitch (P.
rigida Mill.),
are also found in the dominant canopy position. The midstory is predominantly
composed of red maple and eastern white pine (P.
strobes L.), with
sourwood and blackgum also abundant.
Mean annual precipitation is 130
cm spread evenly throughout the year. The geologic substrate is composed
of shales and siltstones of the Upper and Lower members of the Lee
formation. The soils range from Latham-Shelocta silt loam of the clayey
subgroups Typic and Aquic Hapludults at Klaber Ridge (Avers et al., 1974)
to Alticrest-Ramsey-Rock outcrop complex of the sandy-loam subgroups
Typic and Lithic Dystrochrepts (SCS, 1975; Hayes, 1993) at Pinch-Em-Tight,
and Gilpin silt loam of the clay loam subgroup Typic Hapludult (Hayes,
1993) at Whittleton Ridge. All of these soils are moderately deep and
well-drained.
Last Updated:
April 23, 2008
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