SOIL NEUTRALIZER FROM VOLCANO FOR BETTER GROWINGNow the high price of fertilizer is not problem for smart farmer
The benefit for plant :
- Greener leaf, stronger stem and higher production
- To decrease fertilizer application and improve its effectiveness
- Increase p elements available for plant
- To neutralize soil ph
- Assist to provide microelements
- To eliminate poisons elements for plant
- To improve silicate content of soil
How does FERTILITE works in Agriculture
In regular Urea application, only 29-45 % that could be exploited by plant, the rest is cleaned or steamed. Because of its high Cation Exchange Capacity, using FERTILITE could decrease Urea dosage and improve its effectiveness.
FERTILITE also improve P elements available for plant, by its nature of ion exchange P elements that bounded in soil could be released to make it available for plant. Thereby the usage P fertilizer could be deducted.
Solve the Problem of Silica & Micro Nutrition
Result of research showed that rice field in south east Asia have a problem in silica deficiency, though silica is a useful element and can make satisfied to the human after eating rice. The problems follow also by increasing of Fe, Al, and Mn in soil, which dangerous for plant when the elements are over.
That matters are resulted because of highly intensive application of N,P, and K fertilizer and also use prime seed varieties. By FERTILITE intake will increase the silica content in the soil and poison elements could be neutralized. Even the microelements will more available for plant. Beside that, because the basic substance of FERTILITE is high alkalinity, it has effect for pH neutralizer on soil with low pH.
- Cut down the usual fertilizer dosage at 30 %
- Replace the reduction by our FERTILITE
What is FERTILITE
The story was began in 1756 when Axel Cronstedt, a Swedish mineralogist collected a suite of well-formed crystals from a copper mine in Lapmark, Sweden. In recent years, there are increasing amount of efforts has been directed toward the natural sedimentary rock of volcanic origin, their valuable physical an agricultural technology. The materials are group of hydrated, crystalline alumino-silicates containing exchangeable cation of group IA and IIA elements such as sodium, potassium, magnesium and calcium. They can be represented by the empirical formula:
where n = cation valence, y = 2 or greater., and w = number of water molecules contained in the voids of material
Structurally, the minerals are complex inorganic polymers based on an infinitely extending framework of AlO4 and SiO4 tetrahedra linked to each other by the sharing of oxygen ions. The channels or interconnecting voids of this framework, whic may amount to as much as 50 % of the volume, normally contain the cations and water molecules. However when a material is reversibly dehydrated by heating, the cations become coordinated with the oxygen along the inner surfaces of the cavities while the crystalline structure remains intact. This leaves a porous crystal permeated with cavities interconnected by channels which have diameters ranging between 0.3 and 0.8 Å.