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Progressive Crop Consultant July/August 2019

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Iron Deficiency<br />

in Fruit and Nut <strong>Crop</strong>s in California<br />

BY MOHAMMAD YAGHMOUR, | Area Orchard Systems Advisor, Kern County<br />

PHOEBE GORDON, | Area Orchard Systems Advisor, Merced County<br />

Micronutrients play a very<br />

important role in fruit and<br />

nut tree growth and development.<br />

Iron (Fe), which is an immobile<br />

micronutrient in the plant, is associated<br />

with chloroplasts and plays a role<br />

in chlorophyll synthesis. While Fe is<br />

considered the fourth most abundant<br />

element in the Earth’s crust, approximately<br />

five percent by weight, iron<br />

deficiency is a worldwide problem, and<br />

a common micronutrient deficiency in<br />

fruit and nut crops (Figure. 1) though it<br />

is uncommon in California.<br />

Many orchards in the Central Valley<br />

are on semi-arid soils in areas where<br />

the evapotranspiration exceeds<br />

precipitation. Arid and semi-arid soils<br />

can also be found in the southwestern<br />

USA and the Mediterranean areas. In<br />

this article we will be focusing more<br />

on calcareous soils with free calcium<br />

carbonate (CaCO3) and soil solution pH<br />

in the alkaline range (i.e. above 7.5).<br />

Before we get into the specifics of iron<br />

in the soil solution, we’ll give a brief<br />

Photo courtsey of Mohammad Yaghmour.<br />

Figure 1. Advanced iron deficiency on almond tree in Kern County. Interveinal<br />

chlorosis are a typical symptoms of iron deficiency.<br />

26 <strong>Progressive</strong> <strong>Crop</strong> <strong>Consultant</strong> <strong>July</strong> /<strong>August</strong> <strong>2019</strong><br />

description of pH. It indicates the<br />

concentration of H+ ions (protons)<br />

in a solution. Soils with low pH have<br />

more H+ ions than soils with a high<br />

pH. Because the equation is actually a<br />

logarithm (Equation 1), the amount of<br />

H+ ions does not increase linearly as<br />

pH decreases, it increases by a factor of<br />

10. Thus, water with a pH of 5 has 10<br />

times the amount of H+ protons than<br />

water with a pH of 6. Therefore, it is<br />

progressively harder to correct soil pH<br />

the farther it is from 7.<br />

pH = -log[H+]<br />

Equation 1: equation for conversion of<br />

the concentration of H+ ions in solution<br />

to pH. Since the equation is logarithmic,<br />

there is a 10x difference between<br />

consecutive values.<br />

Soil pH is important as the different<br />

soil minerals that contain and release<br />

iron (Fe) into the soil-water solution<br />

decrease in solubility as pH increases,<br />

which results in only a tiny fraction<br />

of the total Fe that is in the soil to<br />

be available. In general, iron is more<br />

soluble and more available as pH<br />

decreases (acidic<br />

soils). Plants<br />

absorb some iron<br />

by diffusion at the<br />

root tips from the<br />

soil solution, and<br />

iron deficiency<br />

in California is<br />

mainly due to<br />

plants’ inability<br />

to take up iron<br />

due to soil factors<br />

such as poor soil<br />

aeriation and/or<br />

high concentration<br />

of HCO3- in the<br />

soil.<br />

Under low iron availability in the<br />

soil, the ability of trees and plants to<br />

mobilize iron immediately around<br />

the root is due to differences in genes<br />

between species. Scientists have<br />

categorized plants either as “Strategy<br />

I’ or ‘Strategy II’ based on their ability<br />

to mobilize Fe in the soil and make it<br />

available for uptake. Strategy I plants<br />

include all plants except grasses and<br />

include fruit and nut trees, while<br />

Strategy II plants comprise grasses such<br />

as wheat and corn. Under Fe deficient<br />

soil conditions, Strategy I plants excrete<br />

H + into the soil, which acidifies it and<br />

makes iron more available for uptake.<br />

In poorly aerated calcareous or<br />

saturated soils, carbon dioxide will<br />

become trapped in the soil due to poor<br />

gas exchange with the atmosphere.<br />

This will cause the production and<br />

accumulation of bicarbonates as a<br />

result of the interaction between CO2<br />

and calcium carbonates in the soil.<br />

Bicarbonates react with the H+ released<br />

by roots and interfere with their ability<br />

to increase iron availability.<br />

Symptoms of Iron Deficiency<br />

The development of Fe deficiency<br />

symptoms is most prominent on<br />

young, newly developing leaves<br />

(Figure 2, see page 28) because this<br />

element is immobile in the plant.<br />

The symptoms are characterized by<br />

interveinal chlorosis, (Figure 3, see<br />

page 28). Under severe conditions,<br />

leaves have a white coloration due to<br />

the disappearance of chlorophyll, and<br />

leaves can turn necrotic and abscise.<br />

Leaf chlorosis due to iron deficiency<br />

reduces photosynthesis and will result<br />

in reduced fruit yields and fruit quality.<br />

These attributes are only for iron<br />

deficient plants; overfertilizing with iron<br />

will not increase these functions in the<br />

Continued on Page 28

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