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Continued from Page 17<br />

time, it is a slower process and results in<br />

a less dense set of data point. The EM38<br />

is a smaller device that can be carried<br />

by hand. This allows it to be used in<br />

a variety of situations. There are also<br />

researchers that believe that the electromagnetic<br />

is a more reliable measure of<br />

conductivity.<br />

When using either system, GPS<br />

should be used to record the location of<br />

each data point. Dataloggers are used<br />

to record the two different values and<br />

combined with a location from a GPS<br />

receiver. These values can be mapped for<br />

a visualization of soil variability. Georeferencing<br />

of the mS/m is important as<br />

it allows the transfer of the data in text<br />

format and onto a GIS for mapping.<br />

Photo Courtesy of Veris Technologies<br />

It is important to remember that this<br />

value is not in itself a measure of salinity or other common soil characteristic. But<br />

because it is highly correlated to many of these characteristics, it can be used to estimate<br />

or predict many of these characteristics of soil. EC is therefore a measure of soil<br />

spatial variability. Areas with similar EC values also share soil characteristics such as<br />

water, texture, OM (organic matter) and salinity. Any difference in these characteristics<br />

show up on an EC map.<br />

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Higher water content and salinity<br />

allows higher conductivity. Clay particles<br />

are smaller and form tighter bonds than<br />

other types of soil particles, resulting in<br />

higher conductivity. OM decreases the<br />

conductivity. Each of these characteristics<br />

specifically impacts the conductivity<br />

of the soil. The problem is how to<br />

separate and define the level of just one<br />

of these characteristics since they are all<br />

interrelated.<br />

The good news is determining individual<br />

characteristics can be done with<br />

the proper protocol. Three basic uses of<br />

an ECa map include identifying variability;<br />

determining a soil sampling routine;<br />

and determine level of salinity or other<br />

soil characteristic.<br />

Soil Spatial Variability<br />

Precision farming or site specific<br />

management is based on understanding<br />

the variability that is present within a<br />

field and then managing it for economic<br />

efficiencies. A goal in managing variability<br />

is identifying those areas that are<br />

homogenous, i.e. areas that have more<br />

in common than the area around it. ECa<br />

works well to determine these zones<br />

since areas with similar ECa values have<br />

similar texture, organic matter, CEC<br />

(cation exchange capacity) and water<br />

content which means similar production<br />

decision will be applicable.<br />

This is the one application that<br />

requires very little analysis on the part of<br />

the user. The mapped points interpolated<br />

within a GIS (geographic information<br />

system) creates a map showing variability<br />

of the field. Using a GIS reclassification<br />

tool will create three to five zones of<br />

homogenous areas to serve as management<br />

zones.<br />

Determine Spatial Variability<br />

for EC Directed Soil Sampling<br />

Completing a soil sampling using a<br />

grid has been common in precision ag. A<br />

more common technique is using zones<br />

to determine placement of soil samples.<br />

An EC map can be used to determine<br />

the homogenous areas for targeted<br />

sampling. The same management zones<br />

previously discussed, can also be used<br />

to determine where to take soil samples.<br />

Usually a group of samples would be<br />

taken from each zone and aggregated for<br />

a composite sample. The nutrient values<br />

from the samples would be used for fer-<br />

18 West Coast Nut December 2017

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