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Sunshine Complete Plant Care by Top Tropicals

SUNSHINE™ HumiHum - a natural vitamin for plants

SUNSHINE-HumiHum is an extract of humic acids made from 100% organic raw material - leonardite.

The effect of humic acids on plants can be compared with the effect of vitamins on humans. Even considering normal nutrition intake, with lack of vitamins the human body fails to to efficiently absorb those nutrients.

SUNSHINE-HumiHum - is a natural vitamin compex for plants!

If the soil is saturated with humic acids - the plants receive a sufficient amount of fertilizer from the first shoots up to harvest.
SUNSHINE-HumiHum provides for your fruit trees and edibles:
Significantly (up to 30-50%) increases the amount of chlorophyll in the leaves. Chlorophyll is the only source of organic matter for plants.
Accelerates and improves the distribution of nutrients inside the plant and to the fruits.
The plant spends less energy supplying new shoots and fruits.
Causes root growth and increases the number of root hairs. Due to this, there is a more active consumption of moisture and fertilizer from the soil.
Humic acid in the SUNSHINE-HumiHum beneficial effect on soil:
Improves fertility and soil structure.
Increases the availability of trace elements for plants.
Promotes moisture retention on sandy soils.
Cleans the soil by binding heavy metals.
Humic acids - are part of humus - a fertile layer of soil rich in nutrients for plants. Humic acids do not dissolve in water and therefore are practically inaccessible to plants in natural conditions. If they are converted to potassium or sodium salts, which are water-soluble, their biological benefits will increase significantly. Humic acid salts are called humates, they work as vitamins for plants and saturate plants with essential nutrients. Humic acid is also actively involved in the fight against environmental pollution due to the ability to absorb heavy metal ions.

ELEMENT CONTENT:
Potassium Humate 8% (Consists of humic+fulvic acids 6.6%, K2O 1.4%)

Leonardite

Humic and Fulvic acids are the final break-down constituents of the natural decay of plant and animal materials. Humic matter is formed through the chemical and biological humification of plant and animal matter and through the biological activities of micro-organisms. Humic acids are complex molecules that exist naturally in soils, peats, oceans and fresh waters. The one source of humic acids are the sedimentation layers referred to as Leonardite. These layers were originally deep in the earth’s crust, but over many years have been exhumed to near-surface location. Humic acids are found in high concentration in these layers. Leonardite is organic matter, which has not reached the state of coal and differs from soft brown coal by its high oxidation degree, a result of the process of coal formation, and has no value as fuel. The decomposition of concentrated organic acids is a lengthy process taking millions of years in the natural environment.

Where Does It Come From?

One of the first recognized reserves of Leonardite came from the Dakotas, (named after a Mr. Leonard). These strata were not very deep which allowed for simple mining techniques. Since this early beginning, the term Leonardite has been widely used as a name for all humic and fulvic acid containing mined products. A recent discovery has been made in New Mexico of a concentrated organic acid reserve in Oxidized Lignite. These strata (or deposits) occur naturally very close to the surface. For this reason and over the last several thousand years they have become oxidized. This natural process has concentrated the humic acid content to upward of 70 percent.
Our reserve is one of the world’s top reserves of Leonardite. Our Leonardite, in all characteristics, is not worse than the best American samples, and the content of humates and the ratio of Humic acids to fulvic is better than in any worlds produced Leonardite, in which our clients have repeatedly convinced. Also the level of pH in our Leonardite is closed to be an ideal and by introducing it into acidified soils within three years the acidity is completely restored. These factors allow us to attribute our reserve to the category of unique.

 

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