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Seasonal Evolution of the Rhizosphere Effect on Major and Trace Elements in Soil Solutions of Norway Spruce (Picea abies Karst) and Beech (Fagus sylvatica) in an Acidic Forest Soil

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Table 1. Bulk soil (B) and rhizosphere (R) solution pH for the different seasons (autumn, winter, and spring), species (beech and Norway spruce), and depths (layer I: 0 - 3 cm, layer II: 3 - 10 cm, and layer III: 10 - 23 cm) (adapted from [26])
Figure 1. Rhizosphere effect for total C and total N under beech (A) and Norway spruce (B) for the three depths (layer I: 0 - 3 cm, layer II: 3 - 10 cm, and layer III: 10 - 23 cm) and the three seasons (autumn, winter, and spring)
Figure 2. Rhizosphere effect for major elements under beech (A) and Norway spruce (B) for the three depths (layer I: 0 - 3 cm, layer II: 3 - 10 cm, and layer III: 10 - 23 cm) and the three seasons (autumn, winter, and spring)
Figure 3. Rhizosphere effect for trace elements under beech (A) and Norway spruce (B) for the two depths (layer I: 0 - 3 cm and layer III: 10 - 23 cm) and the three seasons (autumn, winter, and spring)

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