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The Sphagnum Acid Peat is the result of the partial transformation of the sphagnum in the absence of oxygen and prolonged for centuries.
Sphagnum is a moss that grows in areas where rainfall is very high and the meteoric water, devoid of salts, constantly washes away the minerals from the surface of the peat bog, acidifying it.
Its ability to make compact soils permeable and loose ones stable, makes it ideal as an amendment to improve soils intended for gardens or vegetable gardens, facilitating cultivation and cultivation operations.
The addition of peat to the soil increases the content of organic matter necessary to obtain a more stable structure that is favorable to plant growth.
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