Estimation of protease activity in soils at low temperatures by casein amendment and with substitution of buffer by demineralized water.

The aim of this work was to modify the method of Ladd and Buttler (1972), by substituting Tris-HCl buffer (pH 8.52) with demineralized water (DEMI H(2)O), in order to assess its suitability for measurement of casein-protease activity at pH levels close to those of real soil in H(2)O. Measurements were undertaken over a range of incubation temperatures from 3 to 49 degrees C. Testing was performed on one organic soil and two different mineral soils. The substitution of Tris-HCl buffer by DEMI H(2)O at 49 degrees C decreased casein-protease activity to 67.25% in mineral soil and to 53.76% in organic soil. With decreasing temperature casein-protease activity decreased the most in organic soil, i.e., 0.07% of original its value at 3 degrees C. The incubation period was extended to maximally 336 h at 3 degrees C to totally obtain >10.0% of L-tyrosine equivalents released at optimum or close to optimum temperature and pH conditions. The Q(10) values of casein-protease activity measured after substituting Tris-HCl buffer with DEMI H(2)O were unexpectedly high. Between the temperatures of 3 and 49 degrees C Q(10) ranged from 3.46 to 4.25, whereas between 3 and 25 degrees C Q(10) ranged from 6.78 to 11.08. Therefore, the modified method of Ladd and Buttler (1972) presented can be used for measurement of soil casein-protease activity under pH conditions close to that of real soil pH and at an averaged soil temperatures measured in the field. This modification makes possible an expression of soil casein-protease activity potential - when being combined with measurements of casein-protease activity under optimum or close to optimum temperature and pH conditions, if high concentration of casein is present.