Page 91 - Enzymes in Tropical Soils
P. 91

Enzymes in Tropical Soils   79


                                The  presence  of  soil  organic  C  is  closely  related  to  cover  vegetation
                           (Handayani and Prawito, 1998; Handayani, 2001; Salam et al., 2001;  Pujiyanto et
                           al., 2003), therefore, the activity of soil enzymes may correlate with the types of
                           vegetation grown on the soils.  Some workers reported differences in enzymatic
                           activities in soils with different vegetations (Duxbury and Tate III, 1981; Jha et al.,
                           1992;  Salam,  1996;  1997c;  1998d).    Duxbury  and  Tate  III  (1981)  reported  that
                           activity  of  acid  phosphatase  significantly  increased  in  soil  covered  with  grasses.
                           Salam  et  al.  (1998d)  also  reported  that  land-use  conversion  from  primary  and
                           secondary  forest  to  agriculture  lands  drastically  decreased  the  soil  enzymatic
                           activities  Jha et al. (1992) also reported that the activity of phosphatase was higher
                           in undisturbed forest soils compared to those in soils that had been disturbed.  All
                           these data indicate that the activities of soil enzymes are related to the contents of
                           soil organic C controlled by plant covers.
                                Therefore, it is obvious that addition of organic C into the soil system may
                           enhance  the  activities  of  soil  enzymes.    Salam  et  al.  (1998i)  reported  that  an
                           addition of organic C (cassava leaf, alang-alang leaf, chicken dung, or goat dung)
                           into the soil system of Ultisol from Tanjungan, South Lampung, Sumatra, Indonesia,
                           clearly  increased  the  activities  of  acid  and  alkaline  phosphatases  for  incubation
                           times of up to 4 weeks.  However, at incubation time of 16 weeks, addition of the
                           organic matters indeed decreased the enzyme activities in soil.



                           5.4  Relationship between Soil Total N and Enzymatic
                                Activities

                                Some  experimental  facts  show  that  the  populations  and  activities  of  soil
                           microorganisms are positively correlated with total N contents in soils (Salam et al.,
                           1998d;  1999d;  1999e).    The  relationship  is  logical  because  N  element  is  very
                           important for the synthesis of proteins in microorganims.  This relationship drives a
                           linear  relationship  between  the  activities  of  soil  enzymes  and  the  total  soil  N
                           contents because soil microorganisms are the main producers of soil enzymes.  This
                           relationship is depicted previousy in Fig. 5.6.
                                The above linear relationship has been repeatedly reported by some other
                           researchers (Nannipieri et al., 1980; Harrison, 1983; Trasar-Cepeda and Gil-Sotres,
                           1987; Bonmati et al., 1991; Tate III et al., 1991; Martens et al., 1992; Salam, 1996;
                           Salam et al., 1998d; Salam et al., 1999e).  Salam et al. (1998d) reported that the
                           activities  of  soil  enzymes,  including  acid  and  alkaline  phosphatases,  urease,  and


                                                                          Abdul Kadir Salam - 2014
   86   87   88   89   90   91   92   93   94   95   96