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September/October 2017

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Figure 3 (pg. 26) perfectly illustrates<br />

the insufficiency of using the classic ECe<br />

threshold concept as the main driver for<br />

tree growth and yield decline. The Area<br />

1 tree has almost double the canopy volume<br />

of Area 4, but the average rootzone<br />

ECe from 2014-16 is actually higher<br />

for Area 1 (12.9 dS/m) compared to<br />

Area 4 of the same field with an average<br />

rootzone ECe of 9.0 dS/m. Whoa—that<br />

makes no sense—the tree with less salt<br />

is smaller?! What the lab ECe salinity<br />

does not take into account is the high<br />

pH, bad sodic silty clay structure that<br />

makes Area 4 prone to water-logging.<br />

We used a somewhat novel approach<br />

taking EM38 measurements right at the<br />

single-line drip hose and 30 inches away<br />

from the hose to get a larger snapshot<br />

of the rootzone. We then summed the<br />

resulting four horizontal and vertical<br />

EMa readings for a “summed” conductance.<br />

Doing this we find Area 1 has a<br />

summed EMa of 241 mS/cm and Area 4<br />

was 877 mS/cm—fully 360 percent higher<br />

conductance for Area 4 compared to<br />

Area 1, and higher conductance means<br />

more salt and water logging. Thus, the<br />

EM38 provided a superior integration of<br />

the combined impact of salinity and soil<br />

structure on final tree growth.<br />

hundreds of measurements per hour as<br />

opposed to three to four soil cores—and<br />

it’s integration of excessive water logging<br />

problems.<br />

Blake L Sanden, Farm Advisor<br />

UCCE Kern County<br />

1031 South Mount Vernon Avenue<br />

Bakersfield, CA 93307, USA<br />

(661) 868-6218<br />

blsanden@ucdavis.edu<br />

Louise Ferguson, Pomology Extension<br />

Specialist<br />

Department of Plant Sciences<br />

3045 Wickson Hall<br />

Davis, CA 95616<br />

530-752-0507<br />

lferguson@ucdavis.edu<br />

Craig E. Kallsen, Farm Advisor<br />

UCCE Kern County<br />

1031 South Mount Vernon Avenue<br />

Bakersfield, CA 93307, USA<br />

(661) 868-6221<br />

blsanden@ucdavis.edu<br />

Comments about this article? We want<br />

to hear from you. Feel free to email us at<br />

article@jcsmarketinginc.com<br />

Figure 4 illustrates the three-year<br />

summed yield decline as a function of<br />

rootzone ECe to a depth of five feet. The<br />

trend is highly significant, and similar<br />

to the 10 year field trial preceding this<br />

survey: resulting in a yield reduction<br />

of 144 to 351 lb/ac (three year cumulative<br />

inshell yield) for every unit ECe ><br />

6.5 dS/m. Definitely a lower yield loss<br />

salinity “threshold” then we published<br />

13 years ago, but the scatter under the<br />

curve is large (R2 = 0.107)—indicating<br />

the multiple other factors affecting tree<br />

growth and yield. Figure 5 uses the<br />

“summed” EM38 conductivity (EMa)<br />

as an estimator of yield decline and<br />

improves the R2 to 0.207 (Regressing the<br />

natural log transformed EM38 readings<br />

with the lab ECe rootzone salinity gave<br />

an R2 = 0.695, data not shown.)<br />

Figure 4. Three year cumulative pistachio yield as a function of rootzone salinity.<br />

No Perfect Tool<br />

So there is no perfect tool for<br />

indexing soil and salinity impacts on<br />

pistachio yield, but the use of the EM38<br />

shows promise both in it’s ease of use—<br />

Figure 5. Three year cumulative pistachio yield as a function of EM38 “summed”<br />

EMa readings.<br />

<strong>September</strong>/<strong>October</strong> <strong>2017</strong><br />

www.progressivecrop.com<br />

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