Page 104 - Enzymes in Tropical Soils
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92     Enzymes In Tropical Soils


                           of soil microorganisms and macroorganisms were higher with the increase in water
                           content  (Jha  et  al.,  1992;  Salam,  1998a;  Yusnaini  et  al.,  2002).    For  example,
                           Yusnaini et al. (2002) found that earthworms were found more in the rainy season
                           than  those  in  the  dry  season.    Observation  in  coffee  plantation  of  Sumber  Jaya,
                           West  Lampung,  Sumatra,  Indonesia,  showed  that  the  populations  of  earhworms
                           were lower between July and November and began to increase in December and
                           the  highest  was  between  February  and  April  in  the  rainy  season.    It  was  also
                           reported that the populations and activities of soil microorganisms were related to
                           the soil moisture content (Yusnaini et al., 2002).  Salam (1998a) also found that the
                           increase  in  water  content  below  40%  increased  the  rate  of  soil  organic  P
                           decomposition.  Other  workers also reported that forest conversion changes the
                           soil water contents (Klein and Koths, 1980; Baligar et al., 1988) and also the types
                           of  vegetation,  plant  roots,  and  soil  microorganisms  (Duxbury  and  Tate  III,1981;
                           Frankenberger and Dick, 1983; Jha et al., 1992).  Jha et al. (1992) reported that in
                           the  regions  of  Northeast  India,  the  activities  of  soil  enzymes  such  as
                           dehydrogenase, urease, and phosphatase were higher in the regions that have not
                           been degraded than those in the degraded regions.  This phenomenon was related
                           to the lower populations of fungi and bacteria in the degraded regions.




                                                    180
                                                   Activity (mg p-NPP g -1  h -1 )   120
                                                    160
                                                    140

                                                    100
                                                     80
                                                     60
                                                     40
                                                     20
                                                      0
                                                         0 2 6 10 14
                                                            Time (days)


                                      Fig. 6.6.  The time dependence of soil phosphatase activity in
                                            a japanese soil (Adapted from Salam, 1998a)




                           Abdul Kadir Salam - 2014
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