Human activities have increased acid deposition throughout the Ohio River Valley due to the large number of coal-fired power-generating facilities. The long-term effects of chronic acid deposition can include a decrease in soil pH, loss of soil fertility, and a decrease in base saturation—all of which can reduce forest productivity. Dysart Woods, a remnant old-growth, mixed mesophytic forest in eastern Ohio, has experienced a decrease in soil pH from 5.0 in 1971 to 4.6 in 1997, which may be due to chronic acid deposition. The objective of this study was to utilize a long-term study to evaluate how soil quality has changed due to chronic acid deposition. To meet the study objectives, a variety of soil chemical properties (pH, base saturation, C, N, P, etc.) were measured from surface soil within two stands of opposing aspect at Dysart Woods within the unglaciated Allegheny Plateau. Because soil pH correlates strongly with other soil chemical properties, we used pH data from 1971 to estimate how soil quality has changed over time. Mean soil pH from the south-facing stand was 5.0 in 1971, 4.6 in 1997, and 4.3 in 2007. While soil pH was not measured in the north-facing stand in 1971, pH was 4.6 in 1997 and 4.7 in 2007. Using changes in pH to estimate past soil properties, our results suggest that available base cations in the south-facing stand have been reduced from ≈12 to 6 (cmol_c kg^-1), with a 50% reduction in base saturation since 1971. Considering that both stands receive the same amount of acid deposition due to their close proximity to each other, results raise an interesting question: Are unglaciated Allegheny Plateau south-facing soils more susceptible to the effects of acid deposition than north-facing soils?