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It is derived from the transformation, in the absence of oxygen and prolonged for tens of centuries, of sphagnum moss and marsh moss.
It is characterized by a low fiber content, a high water absorption and a very low salt content.
Due to its ability to simultaneously hold large quantities of air and water, this peat is ideal for improving all types of soil and for building a long-lasting reserve of humus in the soil.
It is a particularly valuable product, which guarantees oxygenation to the roots and avoids water stagnation, optimal for maintaining a stable substrate structure over time.
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