Carbon assimilation and microbial activity in soil
- 1 January 1986
- journal article
- research article
- Published by Wiley in Journal of Plant Nutrition and Soil Science
- Vol. 149 (4) , 457-468
- https://doi.org/10.1002/jpln.19861490409
Abstract
In order to characterise the term microbial „activity”︁ three different microbial populations belonging to a luvisol (I), a phaeozem (II) and a rendzina (III) were used for studying kinetic parameters such as substrate affinity, growth rate, yield and turnover time and the metabolic quotient of basal respiration. Glucose was used as a carbon source. Specific growth rate values (μ) varied between 0.0037 and 0.015 h−1depending on soil type and glucose concentration and were far below the potential μmax. The calculated turnover time was 3–11 days, respectively. The yield coefficient was in the range between 0.37 and 0.53. The maximal uptake rate of glucose–C of soil population (II) was 0.041 g C g−1biomass‐C h−1. The determined affinity constant (Km) was 57 μg C g−1soil. The affinity to glucose was higher for the glucose‐mediated CO2evolution with Kmvalues of 15.2 and 17.5 than for the glucose uptake system itself. The observed qCO2values of the basal respiration at temperature increments from 0 to 45° C were almost identical for the soils (I) and (II). The calulated Q10lay in the range between 1.4 and 2.0.This publication has 17 references indexed in Scilit:
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