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Continued from Page 29 exuded by microbes bind soil particles ‘<br />

into aggregates and earthworms burrow<br />

through soil, creating channels for<br />

water and air flow. Microbial metabolites<br />

chelate micronutrients, delivering<br />

iron, zinc and other elements to roots<br />

in plant-available forms. Beneficial<br />

fungi extend the crop’s root system,<br />

exchanging water and nutrients for<br />

photosynthate and signaling when to<br />

activate stress defense mechanisms.<br />

Microbial biomass also provides<br />

nutrient storage, releasing plant-available<br />

nitrogen, phosphorus and other<br />

elements as populations turn over.<br />

such as hydrogen, calcium, potassium<br />

and magnesium, and anions, including<br />

hydroxide, nitrate, borate and molybdate.<br />

Binding with organic matter prevents<br />

essential nutrients from leaching<br />

to groundwater or precipitating out of<br />

soil solution with other minerals. Ions<br />

buffer into or out of soil solution to<br />

maintain chemical equilibrium, keeping<br />

pH near neutral and replenishing<br />

nutrient concentrations in response to<br />

plant absorption.<br />

The living fraction of soil organic<br />

matter drive all of the activity contributing<br />

to healthy soil development.<br />

Fungal networks, beneficial bacterial<br />

populations, earthworms and more<br />

contribute to carbon cycling and<br />

organic matter fixation. Micro and macroorganisms<br />

decompose raw organic<br />

matter, returning essential elements to<br />

plant available form. Sticky substances<br />

Highly productive,<br />

carefully managed<br />

orchards might not<br />

show any changes<br />

in yield or crop quality,<br />

but better soil<br />

health may allow<br />

growers to decrease<br />

water and fertilizer<br />

use while maintaining<br />

productivity.<br />

Feed the Soil its Carbon<br />

Microbial activity, nutrient cycling,<br />

and structure development require<br />

carbon. Almonds and other tree crops<br />

feed the microbiome by sending photosynthate<br />

down to the rhizosphere, but<br />

significant improvement in soil quality<br />

requires more biomass. Feeding microbial<br />

populations by growing cover crops<br />

and applying compost or mulch can<br />

help achieve net carbon gain, initiating<br />

the processes that build organic matter<br />

and improving agricultural sustainability.<br />

Soil structure and beneficial microbial<br />

ecology take time to develop.<br />

During the first few years of cover<br />

cropping, the orchard might require<br />

more water and fertilizer to establish a<br />

robust cover crop stand without jeopardizing<br />

the crop’s access to sufficient<br />

moisture and nutrition. Over time,<br />

the investment pays off. Incremental<br />

increases in organic matter ramp up<br />

the soil’s capacity to sustain diverse,<br />

active microbial populations. Increased<br />

microbial activity accelerates humus<br />

formation and the other beneficial<br />

soil characteristics follow. Improved<br />

nutrient availability, soil moisture and<br />

beneficial microbes can improve tree<br />

health, reducing symptoms of micronutrient<br />

deficiency, drought and salinity.<br />

Measurable improvements in water<br />

holding capacity, bulk density and<br />

nutrient availability may take several<br />

years to develop. Soil type, management<br />

practices, weather, water, fertilizer and<br />

many other factors influence organic<br />

matter accumulation and soil health.<br />

While some soils may respond quickly,<br />

others resist organic matter fixation.<br />

Very sandy soils lack the clay particles<br />

that bind and stabilize organic matter,<br />

preventing accumulation. The type of<br />

’<br />

30 West Coast Nut <strong>Dec</strong>ember 2021

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