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AY-363-W • Four Strategies to Improve Your Field’s Soil Health
Because these factors are oen unique to your location,
soil health can mean dierent things. In other words,
healthy soil in northern Indiana is going to be dierent
from healthy soil in southern Indiana due to the
inherent nature of the soil. Characteristics like these can
inuence the timing and degree of your soil’s response
to the strategies we describe in more detail below.
Key Soil Health Components
What does a healthy soil encompass? Here are some of
the important players in soil health.
Soil aggregates are a fundamental concept in soil
structure. Aggregates are groups of soil particles that
bind to each other more strongly than to other particles.
ey form pores that help soils retain water and air. Soil
aggregates can change quickly. Within a few years of
starting conservation practices (such as implementing
no-till systems and planting cover crops), aggregates can
change in size and stability.
Well-structured soils allow for adequate aeration, water
inltration, and root penetration and growth. Well-
structured soils also resist erosion and compaction. We
oen think of aggregates just as one of soil’s physical
properties, but biological organisms inuence this
structure. Earthworms, mycorrhizal fungi, plant roots,
and organic matter all inuence the ways soils form
aggregates.
When earthworms are present in a system, they create
tunnels. Later, plants can use these tunnels as root
channels, allowing roots and water to penetrate deeper
into the soil prole. Earthworms also leave behind casts,
which are rich in nutrients. Mycorrhizal fungi form
benecial relationships with plants by bringing water
and nutrients, particularly phosphorus, to a plant in
exchange for energy in the form of carbon. ere are
many dierent “good” soil microorganisms that help
break down residue, recycle nutrients, and combat the
“bad” pathogenic microorganisms that might negatively
inuence your cash crop growth.
What you plant can also inuence biological activity
in your soil. Introducing plant diversity into your
system is a natural way to control weeds and pests,
including pathogenic microorganisms. Diversity can
increase nutrient and water use eciency, introduce
dierent root types and residue, and reduce stress on the
cropping system.
Diverse root types and residue may reduce your soil’s
risk of erosion. Some plants decompose faster than
others, so where erosion is a concern, you may want
to consider introducing a plant that decomposes more
slowly and keeps the soil covered longer. Soil microbial
communities thrive on diverse residue produced by
various plants. As you add diverse plants, healthier
soil for agronomic purposes develops. at’s because
dierent plants are able to target a broader range of
soil resources than a monoculture system can target.
Monoculture systems may exhaust certain soil resources
more quickly and require additional inputs to maintain.
Organic matter plays a big role in soil health. Changes
in organic matter content do not occur quickly, and it
may take several years to see an appreciable dierence,
but increasing your soil’s organic matter will improve
its overall health. Organic matter largely contributes
to a soil’s cation exchange capacity (CEC), and organic
matter helps soil hold nutrients and water for plant use.
Soil microbes decompose residue into organic matter
and eventually transform it into mineralizable nutrients
for plant uptake.
The Four Strategies
e four strategies for improving your soil’s health are
not an all-inclusive list. Rather, these strategies provide
a good base to improve overall soil health. Many of the
strategies we discuss are connected and act together to
improve soil health.
1. Practice No-Tillage/Strip-Tillage
Reducing tillage to either no-till or strip-till minimizes
disruptions to soil aggregates by not breaking them up
continuously and forcing the system to restart (Figure
1). Minimal tillage maintains natural aggregates, one
of the key components of soil health, and helps prevent
loose soil particles from washing or blowing away easily.
Residue decomposes more slowly under a reduced
tillage system for several reasons. One reason is that
fewer aggregates are broken up with less intensive tillage,
so less organic matter is exposed to decomposition.
Second, reduced tillage can make soil temperatures
slightly cooler. Lower temperatures help organic
matter accumulate, because the residue is not broken
down as quickly. Reducing tillage can increase soil
organism diversity and activity, another one of the key
components of soil health. Reduced tillage does not
disrupt earthworm burrowing and helps protect the
network created by mycorrhizal fungi that connects
them to their host plant. Leaving residue on the soil
surface also acts as a barrier against raindrops and wind
that could cause erosion.