Leonardite
More details: leonardite-ua.com
| The content of HUMIC and FULVIC acids in NATURAL sources (%) |
| Leonardite |
65-85 |
| Black peat |
10-40 |
| Sapropel |
10-20 |
| Brown coal |
10-30 |
| Humus |
5-15 |
| Compost |
2-5 |
| Soils |
1-5 |
| Sludge |
1-5 |
| Coal |
0-1 |
- 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.
- The decomposition of concentrated organic HUMIC
AND FULVIC acids is a lengthy process taking millions
of years in the natural environment.
