The Forest Habitat of the University of Kansas Natural History ReservationFitch, Henry S. (Henry Sheldon)
History
The Forest Habitat of the University of Kansas Natural History Reservation
Fitch, Henry S. (Henry Sheldon)
Forest reserves -- Kansas; University of Kansas. Natural History Reservation
Stumps that were otherwise intact often had small central cavities an
inch or more in diameter. For these it was necessary to estimate the
numbers of missing rings in order to obtain a figure for the
approximate total age of the tree at the time it was cut. Many of the
logs and stumps were so much decayed that growth rings were no longer
distinct, and on most there were a few rings that were not clearly
defined. In the majority of instances the time of cutting could not be
determined accurately, but it is known that there was little
tree-cutting after 1934 on most parts of the area. Probably most of
the stumps on the Reservation that were well enough preserved to
provide counts were from 20 to 30 years old. Most of the counts of
growth rings on chestnut oaks were obtained on a hillside adjoining
the Reservation where the trees were cut in the early nineteen
forties.
Width of the annual growth rings reflects rapidity of growth in the
tree and is determined, in part, by the amount of annual rainfall,
especially in this region on the western edge of the deciduous forests
where moisture is the chief limiting factor. Periods of drought or of
unusually heavy rainfall may result in growth rings smaller or larger
than average. Because the trees draw moisture from the deeper soil
layer there is a lag in their response to precipitation, and a single
year that is much wetter or much drier than those preceding or
following it may not stand out clearly in the annual rings. In
individual trees the effect of precipitation is often obscured by the
effects of crowding and shading by competitors, injury or disease.
None of the trees examined for growth rings reflected the annual
precipitation accurately for long periods though some indication of
known drought periods or of series of wet years were usually
discernible.
For 35 black oaks, chestnut oaks, and American elms, growth rings
averaged 3.81 per inch of trunk diameter (according to size of the
tree; 5.1 rings per inch in those trees 9 to 12 inches in diameter,
4.0 in those 13 to 15 inches, 3.6 in those 16 to 24 inches, and 2.8 in
those of more than 24 inches). Data from a few complete counts and
many incomplete counts indicate that in _Gleditsia triacanthos_ growth
is much more rapid, with only 2 to 3 rings per inch of trunk diameter,
whereas in _Juglans nigra_, _Celtis occidentalis_, _Carya ovata_, and
_Fraxinus americana_ growth is much slower, with usually five or more
growth rings per inch of trunk diameter. Individual trees deviate
widely from the average for their species, and those in rich
bottomland soil grow more rapidly than those in shallow soil of
hilltops or those on rocky slopes. If such factors are taken into
account the ages of trees may be estimated from the diameters of their
trunks. In mature trees growth slows; age is likely to be
underestimated rather than overestimated in those of exceptionally
large size.
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