Furthermore, irrespective of the altitudinal gradient, the values of L, LI, CPI, and CMI exhibited a decreasing trend with increasing expansion degrees of Chimonobambusa utilis .
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Changes in Surface Soil Organic Carbon Fractions and Their Pool Management Indices Along an Altitudinal Gradient in Karst Mountains in Relation to the Expansion Degrees of <i>Chimonobambusa utilis</i>.
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