The present invention claimed herein is directed to a LIQUID PHOSPHATE FERTILIZER SOLUTION FOR AGRONOMIC USE; more particularly, a solution that supplies phosphorus in such a way it can be almost entirely assimilated by the plant from the soil substrate.
More specifically, the present invention provides a fertilizer solution obtained from defluorinated phosphate rock, previously treated in an acidic medium, with the particularity of being almost entirely available and assimilable; when losing its liquid state, it can return to that that state after any rainfall while remaining as a salt in the soil, thus ensuring that the phosphorus is kept soluble in the soil substrate so that it can be entirely assimilated by the plant.
Furthermore, the present invention also refers to the industrial process specifically developed for obtaining said liquid phosphate fertilizer, which results from defluorinated phosphate rock that is previously treated in a medium both acidic and corrosive to phosphorus extraction, the reaction of which mostly depends on the nature of the pre-treated rock as follows:
HnPO4Xm+SO4−2→HnPO4−m+SO4−2+NH4+H2O
wherein, at a density of from 1.25 to 1.30, and pH 1.8 to 2.6, turns out to be almost entirely available to and assimilable by plants.
In case that the pre-treated rock does not contain any nitrogen, it is expected that this should be incorporated into the fertilizer during the manufacture process, by means of a hydroxylation device. This formulation, and subsequent treatment, yields a phosphorus, sulfur and nitrogen complex, with poor reactivity values of residual acidity.
The invention defines a novel combination of media intended to achieve a better result, said invention being unpredictable and surprising even to the skilled artisan. As a consequence, apart from being novel, the constructive and functional conception thereof shows a clear inventive step, duly complying with legal requirements to be considered as a patent of invention.
Chemical analyses have shown the existence of at least thirteen elements in all vegetables. The development of agriculture over time, basically the genetic transformation of all seeds as well as the need to address climate changes have dramatically increased the need to use fertilizers to deal with certain issues ranging from world hunger to biofuel provision, thus forcing a significant increase in harvest yields.
As it is very well known, the elements involved in vegetable fertilization are found in the soil at proportions that must be optimized by human action.
In this sense, the liquid fertilizer of the present invention substantially improves phosphorus quality for agronomic use, said fertilizer being completely solubilized, i.e., in the form that the plants absorb nutrients. This solubility significantly decreases the beta threshold in the formation of chemical compounds. In the soil, it is neutral, neither acidic nor alkaline. This feature reduces the phytotoxicity thereof and provides 12 to 15% more plants grown per hectare.
Phosphorus—Function in Plants
Phosphorus is essential for plant growth, where plants absorb most part of phosphorus as primary orthophosphate ion (H2PO4—) and small amounts of phosphorus as secondary orthophosphate ion (HPO4═).
Soil pH impacts directly on the ratio of these two forms, and indirectly, to a great extent, on the absorption of these two forms of P by the plant. P plays an important role in photosynthesis, respiration, energy storage and transfer, cell growth and division, and other processes in plants. Besides, it promotes rapid root formation and growth.
The highest P concentrations in young plants are found on the tissue of growing points. P improves fruit and grain quality, which is critical for seed formation.
The first sign of phosphorus deficiency is a small plant. The shape of the leaves is distorted and, when deficiency is severe, dead spots are developed on leaves, fruits and stems. The most mature leaves are affected before the younger ones. A purple or reddish color, associated with sugar accumulation, appears frequently in young gramineous plants and in other phosphorus-deficient crops, especially at low temperatures.
Phosphorus deficiency delays maturity of the crop. Gramineous plants grown in deficient soils result in a number of tillers or secondary stems much smaller than those planted in more enriched soils.
Reaction in Soil
Phosphorus is very chemically reactive and, for this reason, it is not present in pure state in nature. It is only found in chemical combinations with other elements. Soil phosphorus comes mostly from meteorization of apatite, a mineral containing both phosphorus and calcium. As apatite breaks down and releases phosphorus, several compounds are formed in the soil, orthophosphate ions being released and absorbed by plants. These orthophosphate ions are present in small amounts in the soil solution.
Soil-soluble phosphorus yields compounds with calcium, iron, aluminum and manganese, or it binds to the reactive surface of certain clay minerals, such as kaolinite, aluminum and iron oxides in tropical red soils and allophanic soils, as well as in aluminum-humus complexes in soils derived from volcanic ashes. These reactions reduce phosphorus availability to plants.
Phosphorus from fertilizers, resulting from acids, react with soil minerals forming crystallization products that are less soluble, said reactions being progressive over time.
Phosphorus scarcely moves in most soils. It generally remains in the site it is applied for fertilization. A very small amount of phosphorus is lost due to lixiviation. Erosion and removal in crops are the only two significant ways of phosphorus loss from the soil.
Up to the present time, the amount of phosphorus comprised by a fertilizer has been expressed as phosphorus pentoxide (P2O5). This is based on international conventions even when there is no fertilizer in the world with (P2O5) and it does not exist as an element in nature. (P2O5) is only found at a certain point during conversion of phosphate rock into phosphoric acid, and no matter whether it exists or not, it offers nothing significant from the agronomic perspective.
All solid phosphate products result from phosphoric acid as raw material, while keeping in part their acidity, so to a certain extent they are phytotoxic to seeds (triple superphosphate is alkaline in soil, though showing phytotoxicity, yet to a lesser degree).
These fertilizers possess different amounts of “assimilable” elemental phosphorus (in accordance with the definition provided by fertilizer manufacturers). This amount of elemental phosphorus, which is known as an “assimilable” amount, often confused with availability, is divided by 4.365 for conversion into P2O5 for mathematical purposes, because we are not aware of any other value or rate.
In order to be used as an agricultural fertilizer, solid phosphorus must be stabilized before being employed as a nutrient for plants.
Invariably, out of 100% elemental phosphorus provided, only 30% is solubilized in water under specific soil buffered conditions. To simulate these conditions at the laboratory, a 1-2% citric acid solution is used. During the first year, dilution may be only 10% while reaching at most 30% during the first four or five subsequent years. The remaining elemental phosphorus, up to 70% of the provided phosphorus, is no longer solubilized and becomes part of the total soil phosphorus.
For many years, it was believed that the release of this phosphorus would continue through cation interchange over the years. This is not true, as shown by the professionals disserting during the latest Congress of Soil held in Mar del Plata, Argentina 2012.
Available phosphorus (30%) becomes part of phosphorus measured by traditional methods such as “Bray Kurtz,” “Olsen,” “Melich,” etc., the same phosphorus from which plants can nurture during the following 30 years.
Nevertheless, as phosphorus is an element with high negative charge and great reactivity, as time goes by, elemental phosphorus will form complexes with other nutrients comprised by the soil which have a high positive charge, such as zinc, copper, boron, manganese, calcium, or it will be retained by some clays.
These complexes can be labile, chemical, or easily broken. When these complexes are chemical, they become absolutely unavailable for an indefinite period of time and they override availability of both nutrients to plants.
That is to say, phosphorus availability in a field is decreased with the passing of time (if not added) regardless the amount that can be exported by harvest or used by the plant.
Phosphate Fertilizers
Phosphate rock is the main material used in the production of all phosphate fertilizers. They are classified according to their manufacture process into acid-treated fertilizers or thermally processed materials.
Sulfuric acid (H2SO4) and phosphoric acid (H3PO4) are used to produce phosphate fertilizers. It is important to point out that, after many years, the common term to define the phosphorus content of a material is “pentoxide”, which does not exist in free form in nature. That is the reason why most commercial products include percentages both as pentoxide (P2O5) and elemental form (P) which is known as “assimilable”. The main commercial sources of phosphorus are mono- and di-ammonium phosphates, and superphosphates.
All these products are acidic in soil, except for triple superphosphate that is alkaline, though having phytotoxicity. Phytotoxicity of liquids is higher, and it ends with soil biodiversity, thus limiting biotechnology progress.
The following are some currently well-known phosphate products intended for agronomic use:
Further Phosphate Fertilizers.
The liquid phosphate fertilizer solution provided by the present invention stands out due to the fact that phosphorus is found in total solution, in the form that plants absorb it as a nutrient, from the very moment it is applied to the soil, and it maintains this state in the solution.
As previously discussed, when analyzing prior art, in well-known fertilizers, elemental phosphorus is soluble up to 30% in water, and under soil buffered conditions.
The solution of the present invention, and the phosphorus obtained thereby, will remain available to plants for the next 30 years, according to the current methods of analysis of phosphorus available in soils, Bray, Bray Kurtz, Melich, Olsen, etc., which do not involve phosphorus immediate availability by plants.
The fertilizer solution of the invention is neutral in soils, neither acidic nor alkaline, so it does not imply any phytotoxicity whatsoever to either seeds or plants, and it can be applied in planting rows together with seeds (none of the current phosphate products can achieve this in the required amounts), leading to 12-15% more plants grown per hectare with the best phosphate product known so far (which must be applied at least 10 cm far from the seeds, either laterally or underneath).
When applied to the rows, maximum doses according to the manufacturer's recommendations should not be exceeded per each soil type, thus avoiding phytotoxicity that results from the inherent salinity of any nutrient. The dose ranges from a maximum of 50 Kg in sand soils to 130 Kg in clay soils.
One of the main concerns with current phosphate fertilizers is that highly reactive phosphorus, having a high negative charge, shows a low beta threshold in the formation of chemical complexes with the positive nutrients comprised by the soil and the components of some clays.
In the fertilizer of the invention the beta threshold has been raised, while achieving—rather than avoiding—a decreased formation of chemical complexes.
In summary, we can establish the advantages of the fertilizer of the invention as follows:
Agronomic Advantages
Application Advantages
Logistic Advantages
Manufacture Process
As per the process for producing the fertilizer of the invention as described above, it is possible to state that it is developed in line with the following operative stages:
Under the above conditions, the whole phosphorus becomes soluble in the soil substrate, and can be assimilated by plants
With a view to obtaining the advantages mentioned above, to which users and skilled artisans may add a number of additional advantages, and for the sake of clarity of the constitutive and functional features of the liquid fertilizer of the present invention, an example of the process for producing the fertilizer (to which end a scheme is attached) is described in
In the scheme identified as
13. “Westfalia” decanter;
In order to obtain the liquid phosphate fertilizer of this invention, the following stages are successively conducted:
Number | Date | Country | Kind |
---|---|---|---|
P12 01 04133 | Nov 2012 | AR | national |