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The organic matter of the soil develops primarily from decayed leaves, twigs, branches, roots, and fallen trees, all of which recycle nitrogen, carbon, oxygen, and other important nutrients.
The organic matter of the soil was determined by a method described by Jackson (1958).
An index property such as specific gravity, moisture content and organic matter of the soil was determined according to IS codes.
The rate of microbial transformation of organic matter of the soil was calculated by the total number of microorganisms on the MPA and KAA and mineralization rate [12, 14].
All events increasing the organic matter of the soil, all measures that keep the soil undisturbed and all applications that stabilize pH in a neutral range are important in this respect.
The enrichment of arsenic in soil is primarily due to its co-precipitation not only with or sorption on poorly crystalline Fe oxyhydroxides which precipitate from the irrigation water but also to sorption on other components (including crystalline Fe oxides and hydroxides, clay minerals, and organic matter) of the soil matrix (Bhattacharya et al. 2007).
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This, in turn, increases accumulation of organic matter on the soil surface that may reduce the volume, velocity, and erosive capacity of surface run-off.
The carbon and nitrogen cycles are important natural processes that involve the uptake of nutrients from soil, the return of organic matter to the soil by tissue aging and death, the decomposition of organic matter by soil microbes (during which nutrients or toxins may be cycled within the microbial community), and the release of nutrients into soil for uptake once again.
In fact, soil management practices encourage the addition of organic matter to the soil which has significant effect on soil physical and chemical properties (Weyers and Spokas 2014).
As a matter of fact, the soil used in this experiment had high pH and CCE values and contained a large amount of clay minerals which in turn could immobilize heavy metals in the soil.
The organic matter content of the soil determines its quality (Komatsuzaki and Ohta 2007).
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