Page 67 - Enzymes in Tropical Soils
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Enzymes in Tropical Soils   55


                                The  activities  of  phosphatases  are  among  the  soil  enzymes  greatly  pH
                           dependent.  As pointed out previously (Salam et al., 1998d), choosing the pH value
                           to  measure  the  activities  of  phosphatase  is  based  on  a  curve  indicating  the
                           relationship  between  the  activities  of  phosphatases  and  baffered  pH.
                           Frankenberger  and  Johanson  (1982)  found  that  acid  phosphatase  showed  an
                           optimum pH at pH 6.5 for acid phosphatase and pH 11.0 for alkaline phosphatase.
                           The optimum pH in fact varies with soil types and is determined by various factors,
                           among which is the dominant vegetation affecting the soils.  Salam (1998d) found
                           that the optimum pH for acid phosphatase in West Lampung, Sumatra, Indonesia,
                           shifted  to  higher  pH  due  to  land-use  conversion  from  the  primary  forest  to  the
                           secondary forest and to the cultivated soils.
                                Arylsulfatase activity can be determined by the method previously reported
                                                                          o
                           Salam et al. (1999e). A 1 g of soil sample (0.2 mm and 105 C oven-dry equivalent) is
                           used.  The microbial activity is stopped by the addition of 0.25 ml toluene, followed
                           by a 4 ml  acetate buffer 0.5 M (pH 5.8) and a 1 ml of p-nitrophenol sulfate solution
                           of  0.025M  (ca.  3.5  mg  of  p-nitrophenol  equivalent).    After    gentle  swirling,  the
                                                       0
                           mixture is incubated for 1 h at 30 C.  A 1 ml of 0.5 M CaCl 2  and a 4 ml of 0.5 M
                           NaOH solution are the added.  The concentration of p-nitrophenol in the solution
                           phase  is  determined  with  a  spectrophotometer  at  400  nm  wavelength  after
                           filtering through a Whatman No. 42 paper (Tabatabai, 1982).
                                Urease activity is determined by the amount of urea substrate remaining in
                           the soil system after incubation (Tabatabai, 1982).  A 5 g (oven-dry equivelent) soil
                                                o
                           sample is incubated at 30 C for 5 h after an addition of 5 ml of a urea substrate
                           solution (2 mg urea per ml).  The microbial and enzymatic reactions are stopped
                           after the incubation with the addition of phenylmercuric acetate solution (PMA).
                           Potassium chloride solution is employed for urea extraction.  The amount of the
                           remaing urea in the extract is determined after development of a red color using
                           sulfuric  acid,  phosphoric  acid,  thiosemicarbazide,  and  diacetylmonoxime.    The
                           concentration of urease is determined by measuring the absorbance of a red color
                           at 527nm with a spectrophotometer.
                                Bacause soil temperature affects greatly the activities of soil enzymes, the
                                                                                  o
                           selection of temperature is very important.  The temperature of 37 C will result in
                                                                           o
                           higher activities of soil enzymatic activities than that of 30 C or lower.  However,
                           researchers use various velues of temperature for enzymatic determination.  Some
                                                  o
                                          o
                           researchers use 30 C, not 37 C (Sahrawat, 1980; Salam et al., 1998d).  Tempetarure
                               o
                           of 37 C was used probably to simulate the optimum temperature of animal bodies.
                                                                              o
                           However, in general soils possess temperature lower than 37 C, therefore, other
                                                       o          o
                           researchers use temperature of 30 C and not 37 C
                                                                          Abdul Kadir Salam - 2014
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