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Termites constitute 10% of all animal biomass in
the tropics, and up to 95% of soil insect biomass. They are the
major determinants of soil structure and the biological processes
that underpin soil health. Termites have been shown to have
spectacular effects on soil hydraulic function, leading to
increased rainfall use efficiency and pasture production.
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Right stocking rates equal pasture health
Results from the research so far are showing
that conservative stocking maintains the ability of soils to
capture rainfall.
Under conservative stocking, soil
macro-invertebrates such as termites, earthworms and ants create
large holes in the soil that facilitate the infiltration of
rainwater (macro-pores).
However, under high rates of pasture use,
macro-invertebrate activity declines, reducing soil porosity and
rainfall capture.
This in turn reduces the length of the growing
season for pastures. We have found that simple assessments of
macro-invertebrate activity are good on-ground indicators of the
state of soil health.
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Many indicators of how grazing affects land
condition are based on assessments of the effects of changing
soil health rather than the causes.
But a team from the Tropical Savannas CRC and
CSIRO has gone to the source, by researching processes that
maintain the soil’s ability to capture rainfall.
They’ve found that providing the right
conditions for earthworms, termites and ants will all improve
tropical pastures.
Further, these macro-invertebrates can also
provide an early-warning system for soils on a downward spiral. The
research team, Tracy Dawes-Gromadzki, Garry Cook, Adam Liedloff,
Austin Brandis, explains.
Australia’s tropical savannas are characterised by low
fertility soils, highly variable rainfall and long dry seasons.
The amount of rainfall captured and stored by the soil is the
key driver of plant growth, but this can vary considerably across
the landscape. If the soils capture the first rains of the wet
season effectively, the longest possible growing season for
pastures is ensured.
However, landscapes that don’t capture this rain
effectively will have a longer dry season, which in turn will cause
further declines in soil health and productivity. In contrast to
southern Australia, high intensity storms account for most of the
rainfall in tropical savannas. Therefore we need to maintain high
soil infiltration rates to ensure that as much of this water as
possible is retained in the landscape.
How is soil health important in savannas?
Soil health, like human health, comprises two important aspects.
Firstly, there is the absence of disease and secondly fitness, or
general well being. In north Australian savannas, the fitness of
soils, and in particular their ability to capture and retain
rainfall, is the most important aspect of soil health and the major
factor that can limit plant production.
In contrast, where the physical properties of soils are either
satisfactory or can be cost-effectively manipulated (e.g. by
tillage) such in the cropping lands and sown pastures of southern
Australia, the disease aspect of soil health can become a more
important limitation.”

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Question: How can we tell if a paddock has
high macropore densities and therefore good water infiltration and
soil health?
Search for signs of the presence of
macro-invertebrate activity. Results from the current research show
that termite sheeting (shown above), earthworm casts and ant nests
on the soil surface provide an indication of the levels of
macro-invertebrate activity and the presence of macropores.
Assessment is easy and provides a simple direct measure of soil
health.
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Role of macro-invertebrates
The critical role of termites and earthworms in maintaining
hydrological function of tropical savanna soils is widely
recognised. Soil macro-invertebrates such as termites, earthworms
and ants create large holes in the soil (macro-pores) that
facilitate the infiltration of rainwater.
These macro-invertebrates increase water infiltration,
facilitate gaseous exchange and provide a favourable environment
for root growth. Increased infiltration rates can reduce surface
run-off and soil erosion.
Macro-invertebrate activity also increases litter decomposition,
carbon and nutrient turnover, nutrient storage and soil turnover.
These animals are most active in patches of perennial vegetation,
and help the patches capture and store run-off water. Grazing
animal management can greatly influence the sustainability of these
perennial vegetation patches.
Under conservative stocking, the activity of soil
macro-invertebrates is high, but under high rates of pasture use,
activity declines, leading to reduced soil porosity and reduced
rainfall capture. This in turn reduces the length of the growing
season for pastures. We have found that simple assessments of
macro-invertebrate activity are good on-ground indicators of the
state of soil health.

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How much rain soaked in?
High tech electronics and remote
communications are being used to validate our indicators, by
measuring the actual variation in rainfall capture across the
landscape. Four stations are used for the automatic collection of
soil water data. Each station is connected to sophisticated soil
moisture measurement probes.
Three stations communicate with a base station
by radio signals, with all data collected monthly via the CDMA
mobile network. Rainfall and flume data are automatically
collected, with SMS messages sent to researchers when overland flow
occurs to enable the quick collection of sediment samples.
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Automated soil moisture data collection
The Tropical Savannas CRC project, Soil health in
savannas , is examining the effects of stocking rates on soil
health and landscape productivity within the Wambiana Grazing Trial
near Charters Towers, Queensland, which is co-funded by the
Queensland Department of Primary Industries & Fisheries and
Meat and Livestock Australia. Previous research using soil
infiltrometers contributed to understanding the impacts of stock
management on soil–water.
However, the artificial and ‘one-off’ nature of this
method restricts its applicability. This project developed an
automated soil moisture data collection facility which gives a
better method of assessing soil health, by directly measuring daily
changes in soil water throughout the year.
In paddocks of different stocking rates, probes in different
patch types (bare, grass and shrub patches) record the amount of
soil water at four soil depths down to 0.5 metres. Integration with
existing automated rain gauges and run-off flumes is allowing a
full eco-hydrological understanding to be developed.
The project is integrating its understanding of the dynamics of
soil health with measurements of pasture and livestock productivity
and enterprise profitability. This information is also being
incorporated into computer simulations such as the Tropical
Savannas CRC Savanna.au model, to predict the outcomes of different
management decisions on landscape ecohydrology, soil health and
productivity.
Soil health indicators
Many indicators of how grazing affects land condition have been
developed, but they are often based on assessments of the effects
rather than the causes of changing soil health. The ability of
indicators to provide early warning of soil health decline will be
greater if they measure the cause rather than the effect.
For example, vegetative cover alone has been shown to be a poor
indicator of soil-surface properties and water infiltration,
because pasture quality and economic productivity can remain high
over the short term while the ability of soils to capture and
retain resources declines.
Heavy use of pastures can start a process of declining soil
health that will reduce soil water availability and limit pasture
regrowth and further reduce soil health. This negative feedback
means that poor soil health is very difficult to reverse and such
efforts are unlikely to be cost-effective.
By studying the biological processes that maintain the
soil’s ability to capture rainfall, the project has shown
that there is potential for early warning indicators of soil
productivity decline which could be used to prevent degradation
occurring. This project is developing and testing the validity of
soil macro-invertebrates as indicators of soil health. As well as
being the key drivers of nutrient cycling and hydrological
processes in tropical soils, they also have many other attributes
that make them ideal indicators of soil health. They are sensitive
to a range of environmental stresses; easily measured and
quantifiable; their functional role is easily understood; and they
are simple to use, rapid and inexpensive. The assessment of broad
groups of soil macrofauna such as termites, worms and ants can
often permit the evaluation of the sustainability of a system
without the need for taxonomic expertise.

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Above: the percent of rainfall entering the soil
within the different vegetation patch types considered in this
study. As grazing intensity increases, the percentage of rainfall
captured is reduced.
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Results from our work are showing that simple measures of
macro-invertebrate activity, such as the density of macropores in
the soil surface and the proportion of the soil covered by worm
casts and termite sheeting, correlate highly with the amount of
rainfall captured during storms. Recently, in some of our
restoration manipulation studies, the indirect introduction of soil
macrofauna led to a 30% increase in soil–water infiltration
and retention rates during the first rains of the wet season, and a
60% increase in litter decomposition rates.
Manipulation experiments are also under way to examine what
effect the removal of specific soil macrofauna has on soil
ecohydrology and nutrient dynamics.
Conclusion
Benefits from devising and implementing optimal grazing
management that promote sustainable soil health through the
management of vegetation and associated soil macrofauna, will
include improved pasture productivity, drought survival,
biodiversity, soil organic matter levels, improved soil structure
and reductions in sediment, nutrient and water run-off. Most
importantly, improvements in all these factors will strengthen
rural enterprises through maintaining productive landscapes.
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