A Brief Soil Micro-Nutrient Overview

James Coover
|
2019
|
United States
Moderate
Extension article/bulletin
Guidance/extension
Corn
Soybean
Boron
Iron
Manganese
Zinc
View source document
year
2019
intervention
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Response
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significance
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Abstract

In well-pH-balanced soils, micronutrient deficiencies in crops are usually rare in our clay soils, but there are some exceptions. Our soils are naturally high in calcium, iron, and magnesium, while the micronutrients of copper, nickel, and molybdenum are needed in such small quantities that deficiencies are unlikely in most soils. Deficiencies in these nutrients in our clay and silt-based soils are normally caused by high or low pH, which makes them unavailable. The nutrients of boron, manganese, chloride, and zinc are a little different, though. There are some places where these nutrients don’t have a naturally high background level, but they aren’t always a concern either. All of the micronutrients have different aspects, reactions, and levels of concern in the soil. (Technically, calcium and magnesium are secondary nutrients, but they are close enough for this discussion.)

Outcomes reported
Soil properties
Soil properties
Yield
Yield response & Application
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Absolute yield increase
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Percent yield increase
Statistical significance
Not reported
Response type
Not reported
Method
Not reported
Rate
Not reported
Timing
Not reported
Soil characterisation
Soil Type
Not reported
Texture Class
Not reported
Soil Order / Classification
Not reported
Soil pH — Mean (range)
Not reported
Organic Matter — Mean (range)
Not reported
Organic Matter Unit
Not reported
Critical thresholds reported
Soil — DTPA Extraction
Nutrient
Critical Level
Unit
Soil Test Method
plant tissue
Nutrient
sufficiency range
Unit
Tissue Type · Growth Stage
|
Economic analysis
Metric
Value
Unit
Currency · Basis · Price Basis

Synthesis
Key insight

None reported

Limitations

None reported

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