પરિવર્તન (છોડ અવશેષો),

humified's Usage Examples:

Fully humified humus, on the contrary, has a uniformly dark, spongy, and jelly-like appearance.

soil comprises a vegetal material at the summit (35 cm), followed by a humified horizon of 35 to 40 cm, a tertiary horizon and a clayey horizon.

from the genus of Singulisphaera which has been isolated from dystrophic humified water.

which can at least partly be inhibited in the presence of decomposed (humified) organic matter.

Prairie conditions form a thick, dark colored, humified surface horizon or layer that is humus rich (1 to 4% organic C).

are characterized by one or more of the following: an accumulation of humified organic matter, intimately mixed with the mineral fraction, and not displaying.

Then the humified air enters the cooler where nucleation occur.

annelids and arthropods, themselves able to consume and transform raw or humified organic matter.

The drilosphere is generally richer in nitrogen, phosphorus, and humified organic material than the surrounding soil.

Peat is also high in non humified organic matter that needs to be reduced to produce a high quality product.

Humisols consist mainly of humified organic materials and may contain up to 10% fibre by volume.

humid continental, subarctic, oceanic, equatorial H: common O: always, has humified organic matter mixed with minerals A: absent in most boreal podzols E:.

samples where immature, low rank coals with generally very high content of humified organic matter, what indicates prevailing anoxic and fully saturated conditions.