The Cationic

It is important to point out that silage suffers while in the carcava-silo processes involved where MOS that to her you can see they are in the soil, is being created a microbial flora, and this part of the floor that was previously a part lifeless, with the activity of the MOS again revitalized. These microorganisms being a ferriferous red soil leachate, which is about hard limestone, has a horizon ABC, manifested a leaching of clay’s faith with accumulation in B, presents coating clay in the faces of the aggregates, the cationic exchange capacity is low, 5-5.5 pH and the concentration of organic matter of 2-3% This MO content makes the MOS increase in population since they are heterotrophic and need a carbonated chain to feed themselves. Due to its ferralitizacion process characterized by an intense alternation of minerals, elimination of alkaline bases, fused silica and clays; due to this process as soil microorganisms loses its alkaline base been developed achieving very well that they stay later on the floor, and activate the microbial flora in the same. The MOS more developed are fungi, including yeasts that produce lactic acid and alcoholic fermentation, example: C6H12O6 2CH3-CH2OH + 2CO2 these are natural yeasts that live on the surface of the fruit. So then explains how to implement this experience, which allows to reduce the soil erosion and diversify the cattle feed in the dry season to explain all the requirements to produce silage for livestock silage quality is therefore the conservation of fresh forage in constructions called silos 3. To begin producing silage it is necessary to take into account these measures first, which we will go in the mediated advancing work explaining more clearly. Steps to take to make a good silage: content of water in plants when making the cut. The degree of humidity between 65-75%, too tender plants should not be used because there will be danger that the silage becomes acidic and unpleasant to the palate.