TIMAC PHYSIOLITH ORGANIC CORRECTIVE FERTILIZER BASED ON CALCIUM OXIDE AND MAGNESIUM KG. 25

TIMAC PHYSIOLITH ORGANIC CORRECTIVE FERTILIZER BASED ON CALCIUM OXIDE AND MAGNESIUM KG. 25

• Range: Physiolith
• Typology: Mineral Corrective
• Physical Form: Granular
• PHYSIOLITH EC FERTILIZER
• Calcination substance
• Sea limestone - basic quality

Composition

• Total calcium oxide (CaO) 36%
• Total magnesium oxide (MgO) 1%

• The calcium carbonate of PHYSIOLITH derives entirely from calcium of marine origin. It is a fast-acting corrective, thanks to the microporosity of the individual particles (0.038 mm) and the high carbon solubility value, equal to 66%

• Allowed in organic farming
• Directly from the sea
• PHYSIOLITH is very rich in calcium
• and trace elements: ships from the sea
• specially equipped take it regularly
• Unique and inimitable structure
• Thanks to the slow-release coarse grain, it acts for a long time supplying the soil with calcium. It has a unique porous structure and a large exchange surface.
• Therefore it has great reactivity unlike the carbonates of terrestrial origin which have undergone an active sedimentation (subject to pressure) and which have a compact crystalline structure.
• Consequence on soil fertility
• The saturation of H + ions of the humo-clay complex does not allow the fixation of
• cations (NH4 +, K +) nor that of P2 05 by Ca ++ ions. Increase leaching.
• Furthermore, the reduced microbial activity does not allow a good transformation of the organic substance and in particular that of nitrogen. The absence of an intervention aimed at improving the structure and the pH of the soil leads to a poor exploitation of resources.
• Why use PHYSIOLITH in pre-sowing?
• Problems of acid soils:
• Acid PH slows down the absorption of nutrients by crops
•  Acidity and compaction reduce the activity of microorganisms that transform the organic substance
• in nutrients
• Liquamation and manure cause a temporary acidification of the soil layer explored
• from the roots

1) Calcium of marine origin:

• * Correction of acid and sub acid pH in soils
• * Calcium nutrition in neutral and acidic soils: best Ca / K ratio in forages

2) Porous structure:

• * Improved soil aeration
• * Greater exchange surface for better absorption of nutrients
• * Environment favorable to pedo-fauna

3) Microelements of marine origin:

• * Contribution of micro and trace elements for balanced plant nutrition