Water use and yield of winter wheat in Northern India as affected by timing of last irrigation

Summary Standard local practice in Northern India is to continue irrigation of winter wheat crop almost up to harvest, based on the farmer's belief that this treatment increases grain weight and yield. The effect of an early cut-off of irrigation on the water use was studied in a three-year experiment on a deep, sandy-loam soil.Wheat, sown during the second or third week of November, received its first irrigation four weeks later. Subsequently treatments included irrigations of 7.5 cm water depth applied after 10 cm of cumulative pan evaporation minus rainfall had elapsed since the previous irrigation up till mid-April; irrigations of 7.5 cm up till mid-February and thereafter irrigation equal to 75 and 100% soil-water deficit in the 0–180 cm profile around March 10 with no later irrigation; and a similar treatment with one additional irrigation after making up the water deficit.Least irrigation water was used from the treatment in which 75% water deficit was restored around March 10 and no further irrigation was applied. This treatment increased the average extraction of profile water by 4 cm compared to treatments in which irrigation was continued until mid-April. Profile water depletion was inversely related to the amount of irrigation. Grain weight and yields from the various treatments harvested in the last week of April were unaffected by the treatments.The authors are grateful to the ICAR for financing this research     

Effect of tillage and mode of straw mulch application on soil erosion in the submontaneous tract of Punjab, India

The submontaneous tract of Punjab comprising 10% of the state, is prone to soil erosion by water. Soils of the area are coarse in texture, low in organic matter and poor in fertility. High intensity rains during the monsoon season result in fertile topsoil removal. There is an urgent need to control soil erosion in this region so as to improve soil productivity. A field study was conducted to estimate the effect of tillage and different modes of mulch application on soil erosion losses. Treatments comprised two levels of tillage, viz. minimum (T_m) and conventional (T_c) in the main plots and five modes of straw mulch application, viz. mulch spread over whole plot (M_w), mulch spread on lower one-third of plot (M_1/3), mulch applied in strips (M_s), vertical mulching (M_v) and unmulched control (M_o), in subplots in a replicated split plot design. Rate of mulch application was 6 t ha⁻¹ in all modes. Compared with M_o, M_w reduced runoff by 33%. Runoff and soil loss were 5 and 40% higher under T_c than under T_m. Though other modes of straw mulch application (M_1/3, M_s and M_v) controlled soil loss better than M_o, their effectiveness was less than M_w. T_m was more effective in conserving soil moisture than T_c. Compared with M_o, M_w had 3–7% higher soil moisture content in the 0–30 cm soil depth under T_m. Minimum soil temperature of the surface layer was 1.4–2.4 °C lower under M_w than under M_o. Straw mulching reduced maximum soil temperature and helped in conserving soil moisture. Minimum tillage coupled with M_w was highly effective in reducing soil erosion losses, decreasing soil temperature and increasing moisture content by providing maximum surface cover.     

Yield,water use and root distribution of wheat as affected by pre-sowing and post-sowing irrigation

Irrigation water is a limited resource, and therefore irrigation practices must be rationalized for high water-use efficiency. Little is known about the influence of stored water in deep soils on the water needs and the post-sowing irrigation requirements of crops. A 3-year field experiment was conducted to determine the effects of combinations of light and heavy pre-sowing irrigations with two post-sowing irrigation regimes on yield, root growth, water use and water-use efficiency of wheat on a deep alluvial sandy loam soil. Post-sowing treatments consisted of (i) five 75-mm irrigations at five growth stages, and (ii) irrigations based on pan evaporation, i.e. at IW/PAN-E ratio of 0.75 (75 mm of irrigation water were provided as soon as the open-pan evaporation minus rainfall since previous irrigation was 100 mm).The latter regime required 175 mm less water than that with irrigation at growth stages. Profile water utilization was inversely related to post-sowing irrigation water. Where pre-sowing irrigation was light, post-sowing irrigations based on pan evaporation yielded significantly less than those based on growth stages. With heavy pre-sowing irrigation, irrigation based on the pan evaporation yielded as much as five irrigations at growth stages. The former decreased the mean water application by 153 mm and increased the water-use efficiency by 26%. Irrigation based on pan evaporation stimulated greater utilization of stored water by increasing the rooting density in deeper layers.It is indicated that for higher water-use efficiency and yield, wheat should be sown after a heavy pre-sowing irrigation, and post-sowing irrigation should be based on 0.75 pan evaporation.     

Development of Elongated Uppermost Intemode CMS Lines for Hybrid Rice Breeding in India

Development of cytoplasmic male sterile （CMS） lines with elongated uppermost internode （EUI） trait provides a genetic option to eliminate the use of GA3 in hybrid rice. During the past two decades, extensive work has been carried out on the subject that resulted in identification of several mutants with EUI trait for use in developing cytoplasmic/thermo-sensitive genic male-sterile lines with complete panicle exsertion （Okuno and Kawai, 1978; Rutger and Carnahan, 1981; Shen et al., 1987; Yang et al., 2000; 2002; Gangashetti et al., 2004）. Two recessive genes （eui-1 and eui-2） mapped on chromosome 5 and 10 respectively have so far been reported to control the internode elongation in rice （Librojo and Khush, 1986; Yang et al., 2001; Ma et al., 2004）. Considerable progress has been made in China in exploiting ＇eur gene for development of hybrid rice parental lines （Yang et al., 2000; 2002; Zhang et al., 2002）.     

Selection of soil physical quality indicators in relation to soil erodibility

Soil quality indices based on soil characteristics can be used to assess the sustainability of soil and to assist in soil management decisions. Principal component analysis (PCA) technique was used to identify dominant soil characteristics in relation to soil erodibility in watersheds of submontane Punjab (India). Soil physical and chemical characteristics were evaluated for four locations with four land uses at each location whereas runoff, soil loss and soil erodibility were determined at two locations under natural rainfall conditions and at four locations under simulated rainfall conditions. PCA was performed on 22 physical and chemical soil characteristics, which grouped these soil characteristics into five distinct principal components (PCs). These five PCs namely soil hydraulic factor, density factor, structural factor, sand factor and cation factor, explained 86% variability in data. These PCs also explained 86, 96 and 93% variability under natural rainfall conditions and 75, 76 and 77% variability under simulated rainfall conditions in relation to runoff, soil loss and soil erodibility, respectively. Soil total organic carbon content can be considered as dynamic soil physical quality indicator and can be used to monitor temporal and spatial changes in soil quality.     

Denitrification, N2O and CO2 fluxes in rice-wheat cropping system as affected by crop residues, fertilizer N and legume green manure

Use of renewable N and C sources such as green manure (GM) and crop residues in rice-wheat cropping systems of South Asia may lead to higher crop productivity and C sequestration. However, information on measurements of gaseous N losses (N₂O+N₂) via denitrification and environmental problems such as N₂O and CO₂ production in rice-wheat cropping systems is not available. An acetylene inhibition-intact soil core technique was employed for direct measurement of denitrification losses, N₂O and CO₂ production, in an irrigated field planted to rice (Oryza sativa L.) and wheat (Triticum aestivum L.) in an annual rotation. The soil was a coarse-textured Tolewal sandy loam soil (Typic Ustochrept) and the site a semi-arid subtropical Punjab region of India. Wheat residue (WR, C:N=94) was incorporated at 6 t ha^-1 and sesbania (Sesbania aculeata L.) was grown as GM crop for 60 days during the pre-rice fallow period. Fresh biomass of GM (C:N.=18) at 20 or 40 t ha^-1 was incorporated into the soil 2 days before transplanting rice. Results of this study reveal that (1) denitrification is a significant N loss process under wetland rice amounting to 33% of the prescribed dose of 120 kg N ha^-1 applied as fertilizer urea-N (FN); (2) integrated management of 6 t WR ha^-1 and 20 t GM ha^-1 supplying 88 kg N ha^-1 and 32 kg FN ha^-1 significantly reduced cumulative gaseous N losses to 51.6 kg N ha^-1 as compared with 58.2 kg N ha^-1 for 120 kg FN ha^-1 alone; (3) application of excessive N and C through applying 40 t GM ha^-1 (176 kg N ha^-1) resulted in the highest gaseous losses of 70 kg N ha^-1; (4) the gaseous N losses under wheat were 0.6% to 2% of the applied 120 kg FN ha^-1 and were eight- to tenfold lower (5-8 kg N ha^-1) than those preceding rice; (5) an interplay between the availability of NO₃^- and organic C largely controlled denitrification and N₂O flux during summer-grown flooded rice whereas temperature and soil aeration status were the primary regulators of the nitrification-denitrification processes and gaseous N losses during winter-grown upland wheat; (6) the irrigated rice-wheat system is a significant source of N₂O as it emits around 15 kg N₂O-N ha^-1 year^-1; (7) incorporation of WR in rice and rice residue (C:N=63) in wheat increased soil respiration, and increased CO₂ production in WR- and GM-amended soils under anaerobic wetland rice coincided with enhanced rates of denitrification; and (8) with adequate soil moisture, most of the decomposable C fraction of added residues was mineralized within one crop-growing season and application of FN and GM further accelerated this process.     

Sugarcane response to irrigation and straw mulch in a subtropical region

In Northern India, insufficient soil moisture and excessively high soil temperatures are reported to restrict growth of crops during the hot, dry months of April–June. A 3-year field experiment was conducted to evaluate the effects of three irrigation schedules based on ratios of 0.50, 0.75 and 1.00 times pan evaporation, and two levels of paddy straw mulch of 0 and 6 tons/ha on yield and quality of sugarcane for a sandy loam. The differential irrigations were restricted to 10–12 weeks before the monsoon season.Both irrigation and straw mulching had favourable effects on plant height and yield. Cane yield increased by an average of 13.8% for the 1.00 over the 0.50 times pan evaporation. Similarly, yield averaged 13.8% higher with mulch than without it. Interestingly, the pan evaporation ratio of 0.50 with mulch gave a higher yield than the ratio 1.00 without mulch. For the same yield, irrigation under mulching averaged 34 cm less than under no mulch. These beneficial effects were attributed to better soil moisture and temperature regimes with mulching. Irrigation and mulching had no effect on the quality of cane juice. These results indicate that straw mulching and early season irrigation to sugarcane based on 1.00 times pan evaporation is a promising practice for increasing sugarcane production in subtropical areas.     

Effect of benzimidazoles on amino acid metabolism in Trichuris globulosa

L-aspartic acid C14, L-alanine C14 and L-leucine C14 uptake by Trichuris globulosa was found to be a non-linear function of time and limiting substrate concentration. The uptake was rapid initially but achieved steady state possibly owing to the saturation of transport loci. Linear transformations of substrate saturation kinetics by Lineweaver-Burk plots of L-aspartic acid C14, L-alanine C14 and L-leucine C14 gave Kt values of 6.8 X 10(3) microM, 3.4 X 10(3) microM and 6.06 X 10(3) microM and Jmax of 0.769 mumoles/mg dry weight/min, 10 mumoles/mg dry weight/min and 0.285 mumoles/mg dry weight/min, respectively. The presence of benzimidazole drugs, thiabendazole and fenbendazole, markedly inhibited the uptake of amino acids at concentrations which did not affect the motility of the parasite. The amino acid transport was also found to be pH and temperature dependent. The uptaken amino acids were readily metabolized into different tissue fractions. Thiabendazole and fenbendazole significantly inhibited the incorporation of the three amino acids into the nematode's total protein fractions and trichloroacetic acid soluble fractions. These drugs also decreased the amount of radiocarbon of 14C-amino acids incorporated into CO2.