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