Soil pH
(a measure of the acidity or alkalinity of the soil) Soil pH is one of the most important soil properties that affects the availability of nutrients.
- Macronutrients tend to be less available in soils with low pH.
- Micronutrients tend to be less available in soils with high pH.
Lime – can be added to the soil to make it less sour (acid) and also supplies calcium and magnesium for plants to use. Lime also raises the pH to the desired range of 6.0 to 6.5.
In this pH range, nutrients are more readily available to plants, and microbial populations in the soil increase. Microbes convert nitrogen and sulfur to forms that plants can use. Lime also enhances the physical properties of the soil that promote water and air movement.
- It is a good idea to have your soil tested. If you do, you will get a report that explains how much lime and fertilizer your crop needs.