The soil pH is among the most important soil characteristics for crop production. It affects the soil’s physical, chemical and biological properties and processes, as well as plant growth. The nutrition, growth and yields of most crops decrease where pH is low and increase as pH rises to an optimum level. Therefore, to manage soil pH for the best crop performance, a knowledge of the soil and the crop is most important.
Soil pH is a measure of the acidity and alkalinity in soil. pH levels range from 0 to 14, with 7 being neutral, below 7 acidic and above 7 alkaline. The optimal pH range for most plants is between 5.5 and 7.0; however, many plants have adapted to thrive at pH values outside this range. Because pH levels control many chemical processes that take place in the soil – specifically, plant nutrient availability – it is vital to maintain proper levels for your plants to reach their full yield potential.
As soils become increasingly acidic (decreasing pH), important nutrients like phosphorus, calcium, potassium, magnesium, nitrogen, boron and molybdenum become less available to plants. Other elements, like aluminum and manganese, become more available and may actually become toxic to the plant, resulting in reduced crop yields. Liming to optimum pH not only increases the availability of essential nutrients, but also supplies additional calcium and magnesium, improves soil conditions for microorganisms, increases the effectiveness of triazine herbicides, and improves soil structure.
On the pictures bellow are shown various elements deficiency on corn plant.
In very alkaline soils (increasing pH) phosphorus, nitrogen, iron, copper, zinc and boron are frequently deficient.
Factors affecting soil acidity
Increasing soil pH
Soil pH is increased with liming, the addition of organic residues rich in basic cations and crop rotation. Correcting soil acidity by the use of lime is the foundation of a good soil fertility management program.
Liming materials contain calcium and/or magnesium in the form of calcitic (CaCO3) or dolomitic lime (CaMg(CO3)2), which can be found in form of calcitic limestone, dolomitic limestone, oyster shells, marls, hydrated lime and basic slag.
Decreasing soil pH
Applying ammonium based fertilizers, urea, sulfur/ferrous sulfate, irrigating with acidifying fertilizers, or using acidifying residues (acid moss, pine needles, sawdust) soil pH is decreased.
Accurate record keeping of soil pH in Agrivi system
The most accurate soil pH is provided by laboratory analysis of soil samplings. For each field farmer needs to know its pH level, to proper manage which crop to sow next. Tracking of soil pH is very important due to proper management of crop rotation. If a farmer has acid field, on which he has sown sweet potato, which prefered acid soil, another crop in crop rotation needs to prefer acid soil also. Othewise, farmer will need to raise soil pH level with liming, so the soil become optimum pH for growing of that crop.
This is where Agrivi system helps farmers easy determine whether is a particular field suitable for growing of some crop, based on measured pH of that field. The optimum pH for all agriculture crops are entered into Agrivi base, according to which the system indicates whether the measured pH on field is low, optimal or high for the crop which will be grown on a particular field. Overview of pH value per fields you can find in the Field analytics part.
Intensive farming and tendency to achieve higher yields lead to higher and more frequent need for lime applications, to decrease soil pH.
Maintain optimal soil pH for each crop you grow and use pH analytics of Agrivi farm management system.
Source: Crop Nutrition