Soil biochemistry is one of the parts of soil science managing the development and decomposition of soil organic matter, biochemical responses of carbon, nitrogen, phosphorus, sulfur, metals and xenobiotics in soils and biochemistry of the plant-root rhizosphere. Soil can be considered as a tissue, containing mineralogical mixes, organic matter, water and air in which biochemical processes occur. These responses administer elemental cycles, decay and amalgamation of humic substances, development of soil structure and behavior of a variety of pollutants. Soil biochemical responses concern fundamentally the organic fraction, in spite of the fact that it is made up of just 5% of the aggregate soil volume. This portion serves as a storage facility of fundamental supplements for plant and microbial development, is a major source of energy for microorganisms, also play an important role in determining soil structure. The biochemical responses related with the organic matter fraction are incredibly influenced by ecological factors for example, oxidation - reduction (redox) reactions, pH, water and temperature.
.Biochemistry and Modern Applications is a peer reviewed Journal, with rapid publication process. The topics like DNA polymerases, Heterochromatin, Ribosome, Non-coding DNA, Cell biology, Metabolism, Nutritional Biochemistry, Medicinal Biochemistry and Hormonal Biochemistry are studied. This is not just limited to above areas. The knowledge related to different biomolecules and their mechanisms can be studied in the journal of Biochemistry and modern applications. This journal provides an open access platform for the young scientists and researchers to share their valuable information regarding the biomolecules and their mechanism.