“…Liming generally improves the forest nutrition in Ca and Mg (Bonneau et al, 1992;Huettl and Zoettl, 1993) by (i) delivering plant-available Ca and Mg (Wilmot et al, 1996;Moore et al, 2000;Bridgham and Richardson, 2003), and/or (ii) because liming improves humus mineralization (Bridgham and Richardson, 2003;Piatek et al, 2009), which increases the nutrient concentration of soil solution, and/or (iii) because liming raises pH and base saturation and decreases Al toxicity to roots (Cronan et al, 1989;De Wit et al, 2010). The rate and depth of Ca and Mg penetration in soil depends on lime solubility (Hindar, 2005;Westling and Zetterberg, 2007), on climate, and on physical, chemical, and biological soil properties, which are in turn influenced by liming. At the catchment level, the effects of liming on stream water chemistry vary with the proportion of catchment limed (Dalziel et al, 1994;Hindar et al, 2003), soil acidity and buffering capacity (Hindar, 2005;Lofgren et al, 2009), and catchment hydrology (Brahmer, 1994).…”