A decreasing trend in soil organic carbon (SOC) was observed with increased soil depths in all the sites except site-II of the Pinus roxburghii forest, where organic carbon was highest in the top layer (0–20 cm) and lowest in middle depth (20–40 cm).
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Altitudinal variation in soil organic carbon stock in coniferous subtropical and broadleaf temperate forests in Garhwal Himalaya.
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