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Autor:
G. N. Dowuona, N. K. Amon, James W. Jones, Samuel G.K. Adiku, E. K. Nartey, F. K. Kumaga, T. A. Adjadeh
Publikováno v:
Communications in Soil Science and Plant Analysis. 41:267-276
Soil water content, θ, is a major factor affecting residue decomposition, but simple formulation of this factor is often lacking. We observed that θ significantly (P 30 and C/N < 25, respectively. A θ factor was formulated in terms of the field ca