“…Generally, Eqn 3 produced soil weathering rates similar in range and magnitude compared to those obtained through more detailed means (see, e.g., Hodson & Langan 1999; Akselsson et al 2004;Ouimet & Duchesne 2005;Mongeon et al 2010, this issue). Nevertheless, and ideally, soil weathering estimates should be derived from actual soil mineral contents and knowledge of reactive soil surfaces, by soil layer (Warfvinge & Sverdrup 1992;Whitfield et al 2006;Whitfield et al 2010, this issue), (iii) refining the atmospheric deposition loads for dry and wet deposition (Boulton et al 2009) within the context of contemplated and actual air pollution abatement policies and targets, (iv) adding a detailed forest inventory component to address BC and N related harvest exports , (v) examining results of standand watershed-based nutrient input/output investigations, especially within the study region (Feller et al 2000;Feller 2005;Feller 2010, this issue), and (vi) dealing with BC and N uptake in a locally systematic fashion, based on, e.g., detailed forest management plans. Systematic investigations pertaining to vegetation-, landform-and topography-induced variations in soil mineralogy, depth, texture, organic matter, pH, CEC, BS, and soil drainage would also be helpful.…”