Fs. Gilliam et al., HERBACEOUS LAYER AND SOIL RESPONSE TO EXPERIMENTAL ACIDIFICATION IN ACENTRAL APPALACHIAN HARDWOOD FOREST, Journal of environmental quality, 23(4), 1994, pp. 835-844
The herbaceous layer (vascular plants less-than-or-equal-to 1 m in hei
ght) is an important component of forest ecosystems and a potentially
sensitive vegetation stratum in response to acid deposition. This stud
y tested several hypotheses concerning soil and herbaceous layer respo
nse to experimental acidification at the Fernow Experimental Forest in
north-central West Virginia. Fifteen circular sample plots (0.04 ha)
were established in each of three watersheds: WS3 (an almost-equal-to
20-yr-old watershed receiving acidification treatment with (NH4)2SO4),
WS4 (>80-yr-old control), and WS7 (almost-equal-to 20-yr-old control)
. The herb layer was sampled intensively in 10 1-m2 subplots within ea
ch sample plot, including determination of species composition, cover,
and random biomass harvests. Harvested plant material was separated b
y species and analyzed for macronutrients, micronutrients, and Al. Soi
l was sampled from harvest subplots and analyzed for texture, pH, orga
nic matter, and macro- and micronutrients. Few differences among water
sheds for virtually all measured soil variables indicated minimal resp
onse of soil fertility to the acidification treatment. The herbaceous
layer was also quite similar among watersheds with respect to cover-bi
omass and species diversity; WS7, however, had almost-equal-to 70% hig
her herb layer cover that both Ws3 and WS4, a result of the predominan
ce of a few high-cover fern species and attributable to the north-faci
ng aspect of WS7 vs. south-facing aspects of WS3/WS4. There was a high
degree of species similarity among watersheds, suggesting no shift in
species composition in response to acidification. There was also mini
mal response of element concentrations to acidification, although Fe a
nd Al exhibited evidence of increased uptake in WS3. We conclude that,
contrary to our expectations, there has been little substantive respo
nse of the soil and herb layer to acidification, but hypothesize that
herbaceous layer species may experience toxicity problems with increas
ed mobility of Al and micronutrients in the future.