Soil pH

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Last updated 2:33 PM on 11/21/24
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13 Terms

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Definition of soil pH

A measure of the acidity or alkalinity of soil, influencing nutrient availability and microbial activity.

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Optimal pH Range for crops

Most crops thrive at a pH of around 6.5, where nutrient availability is maximized.

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Active Acidity

The acidity present in the soil solution.

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Reserve Acidity

Acidity held on cation exchange sites.

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Total Acidity

The sum of active and reserve acidity.

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Effect of carbonate content on soil pH

Presence of calcium carbonate can increase pH.

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Impact of leaching on soil pH

High rainfall can leach bases, leading to more acidic conditions.

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Contributors to soil acidity

Organic matter decomposition contributes to soil acidity.

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pH preference for blueberries

Blueberries thrive at a pH of 4.0-5.0.

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How to increase soil pH

Achieved by adding lime (calcium carbonate).

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How to decrease soil pH

Accomplished by adding sulfur.

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Buffering Capacity in soil

Refers to the soil's ability to resist rapid pH changes, influenced by cation exchange capacity (CEC) and reserve acidity.

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Importance of understanding soil pH

Crucial for effective soil management and optimizing plant growth.