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154     Enzymes In Tropical Soils


                           matter and total N contents, available P, and CEC.  Land-use conversion in general
                           degraded these soil chemical properties.  For example, the soil CEC of the primary
                                                     -1
                           forest in 1998 was 43,2 cmol c  kg .  The soil CEC of the secondary forest at the time
                                                 -1
                           was lower i.e. 18.5 cmol c  kg , about the value of subsoil CEC of the primary forest.
                           The soil CEC of coffee plantation and cultivated land were about the same, 11.4
                                         -1
                           and 14.4 cmol c  kg , respectively.  These values were much lower than those of the
                           primary and the secondary forests.  The availabilities of micronutrients in the same
                           locations also decreased by land-use conversion, in correlation with the decrease in
                           organic C, total N, and CEC (Salam, 1999).


                             Table 10.2.  Effects of land-use conversion on some soil chemical properties in Bukit
                                               Ringgis, West Lampung, Indonesia*.


                                        Soil   Elev.   pH     Org. C   Tot. N   Av. P   CEC
                                                                         -1
                                       Depth   (m)     (H 2 O   (g kg -  (g kg )   (mg kg -  (cmol c  kg -
                                       (cm)            1:1)     1 )             1 )      1 )
                           Primary     0 – 20   1,550   4.4    60.4    5.5     4.0      43.2
                           Forest     20 – 40          4.8     25.0    2.3     1.5      18.2
                           Secondary   0 – 20   1,400   5.4    41.4    3.4     2.1      18.5
                           Forest     20 – 40          4.9     21.7    2.0     1.5      13.7

                           Coffe       0 – 20   1,120   4.9    28.5    2.3     1.5      11.4
                           Plantations   20 – 40       4.9     10.1    1.2     1.0      12.5
                           Dry Land    0 – 20   1,100   4.4    15.8    1.7     1.5      12.4
                                      20 – 40          4.3     7.5     0.8     0.7       1.2
                           *Adapted from Salam et al. (1998d)

                                The above phenomenon shows obviously that the differences in vegetation
                           may  cause  different  soil  properties.    This  suggestion  is  supported  by  abundant
                           research results.  For example, land-use change of bushes to continuous cassava
                           plantation  in  Gunung  Batin  North  Lampung,  Indonesia,    also  results  in  the
                           significantly decrease in  soil  CEC, organic matter content, and available P  (Table
                           10.3);  also  decrease  the  availabilities  of  micronutrients  (Salam  et  al.,  1997b).
                           Treatment with cover vegetation for more than 3 years significantly affected some
                           soil chemical properties of coffee plantations (Table 10.4).  Paspalum conjugatum
                           or natural vegetation caused higher values of organic C, total N, available P, and


                           Abdul Kadir Salam - 2014
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