Germination induced changes in bioactive compounds and nutritional components of millets.

The present study was conducted to compare the nutritional quality and the concentration of bioactive compounds in the flours from dehusked and germinated foxtail, barnyard, and little millets. Germinated millet flours showed significantly higher protein content (11.79-33.49%), total free amino acid content (66-334.87%) and protein solubility (13.83-34%), compared to the dehusked millet flours. The total phenols and flavonoids in the flours from the three germinated millets were significantly higher by about 142.36 and 437.20%, respectively, compared to the flours from the dehusked millets. Mineral content was also found to be higher in the flours from germinated millets in comparison to the flours from dehusked millets. The results of this study showed that the flours from the germinated millets have the potential for their application in development of novel products,because of their enhanced nutritional value. The extracts from the germinated millets have the potential for use as functional ingredients in the development of novel processed fruit beverages.

Phosphorus availability to rice (Oriza sativa L.)-wheat (Triticum estivum L.) in a Vertisol after eight years of inorganic and organic fertilizer additions.

Integrated use of inorganic fertilizer N and well decomposed cattle manure (CM) or 30-35 days old Parthenium (Parthenium hysterophorus L.), a weed grown off site as green manure (GM) under repeated applications of fertilizer P and urea N for eight years in a rice (Oriza sativa L.)-wheat (Triticum estivum L.) sequence was studied on transformation of fertilizer P applied to soil at the National Research Center for Weed Science, Jabalpur, India. Based on the results, it appeared that, repeated applications of 52 kg super-phosphate P resulted in a marked increase in Olsen P linearly with time. Conjunctive use of urea fertilizer N with organic manure resulted in a larger increase in Olsen P in the Vertisol. Studies further revealed that the greater accumulation of fertilizer P applied in excess to crop removal occurred in inorganic P in the plots receiving only fertilizer N. However, plots receiving fertilizer N along with organic manures led to P accumulation predominantly in organic forms. The study suggests that these two pools of P acted as a sink when fertilizer P was applied in excess to crop removal and are bio-chemically active. The Olsen P status after 8 cycles of rice-wheat crops revealed that the average amount of fertilizer P required after adjusting for crop uptake to increase Olsen P by 1 mg kg(-1) soil was 7.2 kg Pha(-1) in the plots receiving only fertilizer N. Whereas, application of 5t FYM or 6t GM reduced it to 4.6 kg Pha(-1). The plots receiving manure always maintained a greater concentration of Olsen P. The application of CM or GM with fertilizer N enriched short-term inorganic P as well as long-term organic P fertility. After eight years, larger concentrations of organic P in the subsurface layer (16-30 cm), compared to initial values, indicates downward movement of P in organic forms.

Effects of farmyard manure and phosphorus on zinc transformations and phyto-availability in two alfisols of India.

Laboratory pot experiments were run to study the effects of added zinc (Zn) with and without farmyard manure (FYM) and phosphorus (P) on Zn transformations in two Alfisols, together with Zn uptake by wheat plants grown up to 60 days. In the first experiment the treatments included four levels of Zn (0, 3.75, 7.5 and 15 mgkg(-1) soil) and two levels of FYM (0 and 10 tha(-1)), and in the second experiment five levels of P (0, 20, 40, 80 and 160 mgkg(-1) soil) and one level of Zn (7.5 mgkg(-1) soil). The soils were sequentially fractionated into water-soluble plus exchangeable (CA-Zn), inorganically bound (AAC-Zn), organically bound (PYR-Zn), oxide bound (OX-Zn) and residual (RES-Zn) forms. The effect of added FYM was more evident on the OX-Zn fraction and the percentage utilization of Zn by wheat was the greatest with the addition of FYM alone at the rate of 10 tha(-1) (1.95-2.38%) in comparison to other treatment combinations. Among the levels, application of 7.5 mg Zn kg(-1) soil showed the maximum increase in different fractions of soil Zn and significantly increased the Zn utilization by wheat (0.87-1.17%) as compared to other Zn levels (0.58-0.88%). On an average, about 85% of the added Zn was recovered in different fractions in Zn treated pots. However, the recovery per cent of the added Zn was significantly higher at Zn level 7.5 (95%) mgkg(-1) soil than at 3.75 (87%) and 15 (73%) mg Zn kg(-1) soil levels. Phosphorus additions up to 40 mgkg(-1) soil increased the plant-available Zn in soils whereas at higher P levels plant-available forms decreased with a concominant increase in the inert forms. At 160 mg P kg(-1) soil, the P effect was more pronounced in the shoot than in the root, suggesting that a higher P level inhibits Zn translocation from root to upper plant parts. Path analysis showed that the organically (PYR-Zn) and inorganically bound (AAC-Zn) Zn fractions were the predominant fractions that influenced the Zn availability to plants.