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cje ›› 1998, Vol. ›› Issue (2): 1-6,31.

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Dry Mass Loss and Chemical Changes of the Decomposed Fine Roots in three China South Subtropical Forests at Dinghushan

Wen Dazhi1, Wei Ping2, Zhang Youchang2, Kong Guohui1   

  1. 1. South China Institute of Botany, Academia Sinica, Guangzhou 510650;
    2. Dinghushan Arboretum, South China Institute of Botany, Academia Sinica, Zhaoqing 526070
  • Received:1996-09-15 Revised:1997-03-10 Online:1998-04-10

Abstract: The experiments of decomposition of fine roots were carried out in pine forest(PF), pine-broadleaved mixed forest(PBF)and evergreen broadleaved forest(EBF)in the Dinghushan biosphere reserve. Regression analyses showed that the power function of X/X0=e-kt with Adj.r2(0.989- 0.993)very well fitted with the data of dry mass loss against time(year). The theoretical values of annual decomposition rate of roots with diameter≤2mm derived from the equations were 43.44%, 43.97%, 46.91% for PF,PBF and EBF respectively and also fitted very well with the measured values(43.15%, 43.90%, 45.68%). Decay coefficients(K)were 0.570 for PF, 0.579 for PBF and 0.633 for EBF. The decomposition rate of roots with diameter of 2-4mm is lower(38.54%)than that of roots with diameter≤2mm.No significant difference of the decomposition rates was found between the decomposing roots buried in mesh bags of 0.25mm and 1.00mm. At the 170th day, about 95% soluble carbohydrate was leached out. At the 300th day, The released rate ranged 20.2%-57.3% for N, 52.3%-82.5% for P, 68.6%-83.4% for K, 75.9%-79.1% for Mn and 41.7%-79.1% for Zn. The negative values(-14.8% to -70.2% for Ca, 5.2% to -59.6% for Mg)implied that a tendency of accumulation for element Ca and Mg occured during decomposition proceses.

Key words: Tibet, Rhododendron aganniphum var. schizopeplum, timberline, population distribution.