Today, our objectives are to:
Discuss about apparent soil electrical conductivity (ECa) and what it is
Discuss how it is measured
Discuss why it is an important layer in precision ag
Measure of how much electrical current is conducted through a medium, measured in Siemens or milliSiemens/meter (S or mS/m)
Relates to level of ionic charges able to conduct electrical current
Initially developed to measure salt concentration in soil water and relate it back to crop growing suitability (saline/sodic soils)
Soil sample is collected on the field, brought to a laboratory, saturated with water, and its extractant measured for electrical conductivity (ECe) between two electrodes.
Time-consuming and labor-intensive, not feasible for PA applications.
Bulk soil apparent electrical conductivity measures EC of bulk soil (liquid and solid phases).
Three methods exist to measure in-situ bulk soil ECa:
Commercial example: Veris 3100
Different disk distances relate to different soil depths.
Commercial example: Geonics EM38
Fixed depth, no flexibility to change it.
Least scalable among the in-situ methods.
Because it is affected by so many factors, soil ECa data can only be interpreted within the context of a given field, and not used to compare across fields.
As solution salinity (ECe) increases, bulk soil conductivity (ECa) also increases
Different lines are different soils
As soil volumetric water content (\(\theta\)) increases, bulk soil conductivity (ECa = \(\sigma_a\)) increases, modulated by solution salinity (ECe = \(\sigma_w\))
Important when taking EC data, need similar levels of soil moisture across a field for quality EC data
When soil ECa is mostly controlled by texture, it can be used to create texture-based zones.
Important in PA as texture can be correlated with yield limiting factors like water/nutrient availability and CEC.