If you want to process natural soil fertilizer, you must know their characteristics.
Basic organization of humus
Humus can be separated into humin, humic corrosive and fulvic corrosive, and the last two are on the whole alluded to as humic corrosive. Humus is basically made out of C, H, 0, N, S and different components. There are likewise a little measure of components, for example, Ca, Mg, Fe, and Si. The basic creation of different humic substances isn't totally the equivalent. Universally, general humus contains C 55% to 60%. The normal is 58%; containing N 3% to 6%. The normal is 5.6%; its C/N is 10:1 to 12:1. The substance of humic corrosive (HA) and humin (Hu) is about the equivalent, the substance of C and N of humic corrosive is higher than that of fulvic corrosive (FA) (Table 3-13), and the substance of O and S is lower than that of fulvic corrosive. (FA). The C/H of HA is higher than FA, which implies that the level of buildup of HA is higher, the level of oxidation is lower than that of FA, and the sub-atomic structure is more confused than FA.
Physical properties of humus
The capacity of humus in the dirt is firmly identified with its sub-atomic shape and size. The sub-atomic mass of humus shifts with soil compose and humus sythesis, regardless of whether a similar example is estimated by various strategies.
The humus is dim darker by and large, however the shade of various humic substances fluctuates with the sub-atomic mass of various parts or the extent of chromophores, (for example, conjugated twofold bonds, sweet-smelling rings, phenolic gatherings, and so on.). The distinction between the profundities. The shade of fulvic corrosive is lighter, yellow to earthy red; while the shade of humic corrosive is darker, from caramel dark to dark; the shade of jimaluolanic corrosive is lighter than humic corrosive, typically chocolate darker. The optical thickness of humus is generally decidedly connected with the sub-atomic mass and the level of aromatization of the particle.
Synthetic properties of humus
Humic corrosive is insoluble in water. It is acidic, and its monovalent salt shaped with K, Na plasma is solvent in water, and the dissolvability of salts framed with polyvalent base particles of Ca, Mg, Fe, A1 and so forth is somewhat low. At the point when humic corrosive and its salts change in ecological conditions, for example, dry season, solidifying, high temperature and collaboration with the mineral piece of the dirt, it tends to be utilized as a moderately steady dark substance that is insoluble in dry water.
Basic organization of humus
Humus can be separated into humin, humic corrosive and fulvic corrosive, and the last two are on the whole alluded to as humic corrosive. Humus is basically made out of C, H, 0, N, S and different components. There are likewise a little measure of components, for example, Ca, Mg, Fe, and Si. The basic creation of different humic substances isn't totally the equivalent. Universally, general humus contains C 55% to 60%. The normal is 58%; containing N 3% to 6%. The normal is 5.6%; its C/N is 10:1 to 12:1. The substance of humic corrosive (HA) and humin (Hu) is about the equivalent, the substance of C and N of humic corrosive is higher than that of fulvic corrosive (FA) (Table 3-13), and the substance of O and S is lower than that of fulvic corrosive. (FA). The C/H of HA is higher than FA, which implies that the level of buildup of HA is higher, the level of oxidation is lower than that of FA, and the sub-atomic structure is more confused than FA.
Physical properties of humus
The capacity of humus in the dirt is firmly identified with its sub-atomic shape and size. The sub-atomic mass of humus shifts with soil compose and humus sythesis, regardless of whether a similar example is estimated by various strategies.
The humus is dim darker by and large, however the shade of various humic substances fluctuates with the sub-atomic mass of various parts or the extent of chromophores, (for example, conjugated twofold bonds, sweet-smelling rings, phenolic gatherings, and so on.). The distinction between the profundities. The shade of fulvic corrosive is lighter, yellow to earthy red; while the shade of humic corrosive is darker, from caramel dark to dark; the shade of jimaluolanic corrosive is lighter than humic corrosive, typically chocolate darker. The optical thickness of humus is generally decidedly connected with the sub-atomic mass and the level of aromatization of the particle.
Synthetic properties of humus
Humic corrosive is insoluble in water. It is acidic, and its monovalent salt shaped with K, Na plasma is solvent in water, and the dissolvability of salts framed with polyvalent base particles of Ca, Mg, Fe, A1 and so forth is somewhat low. At the point when humic corrosive and its salts change in ecological conditions, for example, dry season, solidifying, high temperature and collaboration with the mineral piece of the dirt, it tends to be utilized as a moderately steady dark substance that is insoluble in dry water.
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