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Correcting Acidic Soil pH
Definition: Acidic soil refers to soil with a pH level below 7.0. Most plants prefer a slightly acidic to neutral pH range of 6.0 to 7.0 for optimal growth. When the soil pH becomes too acidic, it can negatively affect plant health and nutrient availability.Causes of Acidic Soil
Several factors can contribute to the development of acidic soil:- Parent Material: The composition of the underlying rocks and minerals can influence soil pH. Soils derived from granite or sandstone tend to be more acidic.
- Climate: Regions with high rainfall or areas prone to leaching can result in acidic soil due to the leaching of basic nutrients.
- Organic Matter: Decomposing organic matter, such as fallen leaves or pine needles, can release acids into the soil, gradually lowering the pH over time.
- Overuse of Fertilizers: Excessive application of certain fertilizers, particularly those high in ammonium or sulfur, can contribute to soil acidity.
Methods to Correct Acidic Soil pH
There are several effective methods to correct acidic soil pH:It is crucial to monitor the pH levels regularly to ensure the desired pH range is maintained. Additionally, it is recommended to conduct a soil test before applying any amendments to determine the appropriate amount needed for correction.
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