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Figure 3: The Relationship Between (A) Lichen Biomass (Dry Mass G/0.25 M2), (B) Soil Moisture (% Top Layer of Mineral Soil), and (C) Soil Temperature (°C at the Depth of 5 Cm).
doi 10.7717/peerj.7330/fig-3
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Figure 1: Total Organic Carbon (G/Kg) Present in the (A) 0–30 Cm, (B) 0–10 Cm, (C) 10–20 Cm, (D) 20–30 Cm Soil Layer.
Figure 3: Soil C Stock (Mg Ha−1) Between 0–100 Cm Depth in Burned and Unburned Land Management Systems.
Figure 2: Relationship Between the Plant Aboveground Biomass of Phaseolus Calcaltus (G Pot−1) and the Soil pH.
Figure 3: Profile Distribution of Soil pH and C/N.
Figure 3: Correlation Between the Soil pH (A, B, C, D, E, F) and the Plant Nutrient Concentration and Uptake.
Figure 1: Soil Microbial Biomass Under Nitrogen Addition in the NRL (A–B), NL (C–D) and C (E–F) Treatments.
Table 2: Soil C, N, C/N and pH in Surface Layer of Seven Soil Profiles.
Effect of Soil Agitation, Temperature or Moisture on Microbial Biomass Carbon of a Forest and an Arable Soil.
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