Abstract
Summary. Soil microbial biomass comprises less than
5% of organic matter in soil. However, it performs at least 3 critical
functions in soil and the environment. It is a labile source of carbon,
nitrogen, phosphorus, and sulfur; it is an immediate sink of carbon, nitrogen,
phosphorus and sulfur; and it is an agent of nutrient transformation and
pesticide degradation. In addition, microorganisms form symbiotic associations
with roots, act as biological agents against plant pathogens, contribute
towards soil aggregation, and participate in soil formation.
Critical evaluation of the significance of soil microbial biomass is hampered
by the reliable measurement of microbial biomass, and simultaneous
partitioning of its 3 major functions in soil. For comparative purposes, soil
microbial biomass and its derived indices have been successfully used to
measure early changes induced by land use practices, zero tillage, crop
rotations and other cultural practices, nutrient cycling, land disposal of
sewage sludge, and applications of herbicides and insecticides. However, as a
routine analytical tool, it is limited by the cumbersome and time consuming
measurements, lack of benchmarking values and interpretation, ambiguous
relationship with productivity, and cost-effectiveness.
With increasing demand to monitor soil quality and protection of the
environment, improved and rapid techniques, including molecular biotechniques,
will be required to measure soil microbial biomass for its size of sink,
source and rates of turnover. Eventually, agricultural science will benefit
and utilise soil microbial biomass as an analytical tool to produce abundant,
economical, and clean food and fibre.
Subject
General Agricultural and Biological Sciences