Soil evaporation and organic matter turnover in the Sub-Taiga and Forest-Steppe of southwest Siberia.

Statistical model The linear model explained 58% of soil δ 18 O variance based on the mixed model latent scale (R2 marginal) and 66% of the overall (i.e., both fixed and random factors, R2 conditional) variation 45 in soil water δ 18 O data, furthermore, the fine root mass density was highly significant (Table 3 ).

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