| Root rots of various kinds,
such as a Phytophthora root rot, or caused by Fusarium, Rhizoctonia, or
Pythium, are generally selected by conditions of high nitrate (the
result of putting on lots of fertilizer all-at-once) and limited oxygen.
Compaction, or a loss of soil aggregate structure, usually limits oxygen
diffusion into the soil. When the spaces in soil are lost through
compaction, oxygen has a hard time diffusing into the soil. This
wouldn't be a problem, except that the bacteria that are left after soil
is compacted (the bigger organisms are crushed, leaving the bacteria and
protozoa) grow and use up the oxygen. If the bacteria use up oxygen
faster than oxygen can diffuse in, oxygen content goes down and carbon
dioxide goes up. This is a condition in which the disease-causing
organisms listed above can grow faster than the beneficial organisms.
Thus, disease is more rampant when the soil is compacted.
There's another factor here as well. All fungi require oxygen to grow
(but root rots require less oxygen concentration than their
competitors). But when the roots aren't getting enough oxygen, they are
stressed and release additional exudates. It may well be that these
exudates are the ones the disease-causing fungi grow fastest on, on top
of all the other conditions selecting for these diseases.
Waterlogged conditions can result in limited oxygen diffusion, so
these disease-causing organisms are able to out-compete the beneficial
organisms when the soil is too wet.
What is the Foodweb Solution? Tie-up the excess nitrate in the
bacteria and fungi. When fertilizer is applied, the excess N will leach
from the soil unless it is retained. What retains nutrients in soil?
Organisms and soil organic matter (SOM). What's SOM - the metabolic
products of bacteria, fungi, microarthropods and earthworms chewing on
plant residues. Microarthropods and earthworms break up plant debris
into littler and littler chunks, an extremely important process that
gives beneficial bacteria and fungi new surface areas to grow on. The
waste products from all these organisms, and the not-yet completely
decomposed plant material, is SOM. The more organisms, the more SOM
accumulates more rapidly. But we need to tie-up the excess fertilizer N
in the bacteria and fungi, and on SOM surfaces. Without nitrate, the
disease-causing fungi will not be able to outcompete and escape the
beneficial organisms.
The second thing is to open up the soil to increase oxygen flow into
the soil. When you plow or rip the soil, or when you "aerate" by pulling
plugs from the greens for example, you get some oxygen back into the
soil. But the soils won't remain "fluffed" unless you get life back into
the soil. You have to let them build the structure in soil. If pesticide
applications killed many of the organisms, you can't build soil
aggregates, and you can't improve oxygen diffusion into the soil. Greens
made with sand and little organic matter have few foods to grow the
bacteria that make the smallest size soil aggregates, and few foods for
fungi that bind the smaller aggregates into visible aggregates. There
are no foods for protozoa, beneficial nematodes or microarthropods that
engineer soil pores. In just a few years, what little organic matter was
present is used up, and the sand compacts like concrete.
To open up the spaces between particles, you need to inoculate the
beneficials, and provide food. Soil structure can begin to come back
within days as the bacteria and fungi grow. But be careful - too rapid
growth of bacteria and even fungi in some cases can suck up all the N,
leading to yellow or dying plants. In these just-beginning to-build
conditions, the bacteria can use up all the oxygen, and result in
anaerobic zones. Balance is critical in the conversion from straight
sand to organic matter plus sand. We have work to do to discover the
optimal way in all different kinds of conditions to move back into a
condition of health. |