4.7 Article

Effect of a Compost and Its Water-Soluble Fractions on Key Enzymes of Nitrogen Metabolism in Maize Seedlings

Journal

JOURNAL OF AGRICULTURAL AND FOOD CHEMISTRY
Volume 57, Issue 23, Pages 11267-11276

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/jf901808s

Keywords

Maize; compost; water-soluble fractions; molecular fractionation; NMR; nitrogen; enzyme activity

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The growing concern on long-term productivity of agroecosystems has emphasized the need to develop management strategies to maintain and protect soil resources, particularly soil organic matter (SOM). Among these, the composting process allows both recycling of the increasing amount of organic waste materials and restoration of the content of organic matter in soil. A sequential chemical fractionation into structurally unbound (SU), weakly bound (WB) and strongly bound (SB) compounds was applied to a bulk compost, and its soluble fractions were extracted in water, either after oxidation of compost suspension with an oxygen flux (TEA), or without oxidation but separated into hydrophilic (HiDOM) and hydrophobic (HoDOM) components. The ratio of hydrophilic over hydrophobic compounds decreased in the order HiDOM > TEA > compost > HoDCM, while TEA and compost showed the largest content of SU and WB components, respectively. Such chemically characterized bulk compost and fractions were tested on maize seedlings grown in sand and in hydroponic conditions, and the effects on plant growth and nitrogen metabolism were measured. The structurally complex bulk compost and the hydrophobic HoDOM fraction negatively affected plant growth, whereas the hydrophilic and less-structured fractions (HiDOM and TEA) showed large positive effects on both growth and enzymatic activities of plants. These results suggest that composted organic matter can become useful to stimulate plant growth if the content of potentially bioavailable hydrophilic and poorly structured components is large. These components may be progressively separated from the compost matrix and contribute to the dynamics of natural organic matter in soil.

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