The source of phosphoric rock is marine sediment from the decomposition of animals and plants on the seabed 50 to 70 million years ago. It mainly contributes phosphorus and calcium in addition to magnesium, molybdenum, potassium, among others.
Phosphate rock has a high reactivity, that is why it delivers its nutrients to the plants gradually when they require it. In this way, it prevents nutrient losses and phosphorus retention in the soil.
Phosphate rock is the best option. It is normal to find phosphorus deficiency in volcanic soil, which limits the productivity of meadows and crops because it is an essential nutrient for the growth and development of plants. In addition, thanks to the contribution of calcium, the pH of the soil improves and lowers the saturation of aluminum.
It is a homogeneous fertilizer, physically it is similar to sand or a kind of fine powder, so it can be applied directly. It can be applied at any time of the year in areas with rainfall over 800 m.m. annual and pH 6.0 down.
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