Cj. Mikan et Md. Abrams, ALTERED FOREST COMPOSITION AND SOIL PROPERTIES OF HISTORIC CHARCOAL HEARTHS IN SOUTHEASTERN PENNSYLVANIA, Canadian journal of forest research, 25(5), 1995, pp. 687-696
This study related age structure and composition of forests in southea
stern Pennsylvania to edaphic properties caused by the activities of a
local charcoal iron furnace from the late 18th to the late 19th centu
ry. Forests surrounding charcoal hearths were harvested on 20- to 30-y
ear rotations to supply wood for charcoal production in earthmound kil
ns. Charcoal hearths were created by a recurring cycle of disturbance,
including the removal of established vegetation, intense heat, and th
e deposition of charcoal. Thirty-eight hearths of Hopewell Furnace Nat
ional Historic Site were examined to describe differences in vegetatio
n relative to surrounding forests that have developed since the cessat
ion of charcoal production in 1883. Hearth forests were significantly
younger than surrounding forests, with lower tree density and basal ar
ea, decreased sapling and shrub abundance, and higher herbaceous cover
. Compositional differences on charcoal hearths included decreased imp
ortance of several Quercus species and ericaceous shrubs and increased
importance of Liriodendran tulipifera L. Results of this study indica
ted that the initial effect of charcoal production was the prevention
of stump sprouting and a delay in recolonization following disturbance
due to extreme soil physical and chemical properties. Failure of hear
th seedlings to recruit into larger size classes, age-diameter relatio
nships of Liriodendron tulipifera L. trees, and the failure of calcifu
ge species to reestablish similar cover on charcoal hearths suggested
that unfavorable properties of charcoal soils continue to negatively a
ffect long-term productivity. Relative to nonhearth soils, large, sign
ificant differences in soil pH, cation exchange capacity, base saturat
ion, and exchangeable Ca, Mg, and K indicated that continuing inhibiti
on of woody plants on charcoal hearths may be related to alterations i
n soil chemistry that have persisted for 110 years.