Soil pH influences nutrient availability, microbial activity, and overall plant health. Most crops thrive in a pH range of 6.0 to 7.0, where essential nutrients are most soluble.
When soil becomes too acidic, growers often apply agricultural lime (calcium carbonate) to neutralize excess hydrogen ions. The amount of lime needed depends on the current pH, the desired pH, the soilβs buffering capacity, and the purity of the lime material.
The lime requirement (L) can be estimated with a simple linear model that incorporates these factors.
What is the purpose of applying agricultural lime to soil?
How do I determine the lime requirement for my soil?
What factors affect the amount of lime needed?
Can I use any type of lime for my soil?
How long does it take for lime to affect soil pH?
What are the signs that my soil needs lime?
How often should I test my soil for pH?
Results are for informational purposes only and do not constitute professional advice.
