Soil pH is a key factor in farmland as it controls availability of nutrients, microbial activity and crop productivity. Before delving into what causes soils to become acid or alkaline and the steps to take to treat and correct soil pH, we must first establish what is considered an optimal pH for crop production.
Soil pH is a key factor in farmland as it controls availability of nutrients, microbial activity and crop productivity. Before delving into what causes soils to become acid and the steps to take to treat and correct acidic soil, we must first establish what is considered an optimal pH for crop production.
For most prairie crops, a soil pH range of 6.0 to 8.0 is suitable for optimal growth and development. Soils with pH ranging from 5.6 to 6.0 are considered moderately acid, while strongly acid and very strongly acidic soils have pH ranging from 5.1-5.5 to <5.0, respectively. Crops have difficulty establishing and show a decline in productivity and yield in soils with a pH below 6.0.
Calcium (Ca) is the backbone of every living organism, including plants. Although a plant’s needs for calcium can be as high as its needs for nitrogen and potassium, it is classified as a secondary nutrient. In this post, we examine the importance of calcium and the factors that can limit its availability to plants.
Required by all plants to grow and thrive, calcium (Ca) plays a big part in plant development and fruit quality. Although it’s considered a secondary nutrient, a plant’s need for calcium can be as high as its needs for nitrogen and potassium.
Calcium is essential for the proper functioning of growing points, particularly root tips and nodules. It aids in cell division, forms compounds which strengthen cell walls, supports the function of cell membranes, and helps control enzyme activity and the metabolism of starch.
