T. K. Adhya

Methane emission from flooded rice fields under irrigated conditions

In a study on CH4 emission from flooded rice fields under irrigated conditions, fields planted with rice emitted more methane than unplanted fields. The CH4 efflux in planted plots varied with the rice variety and growth stage and ranged from 4 to 26 mg h-1m-2. During the reproductive stage of the rice plants, CH4 emission was high and the oxidation power of rice roots, in terms of α-naphthylamine oxidation, was very low. The CH4 emission reached a maximum at midday and declined to minimum levels at midnight, irrespective of the rice variety. The peak CH4 emission at midday was associated with higher solar radiation and higher soil/water temperature.

Methane emission from rice fields at Cuttack, India

Methane (CH4) emission from rice fields at Cuttack (State of Orissa, eastern India) has been recorded using an automatic measurement system (closed chamber method) from 1995–1998. Experiments were laid out to test the impact of water regime, organic amendment, inorganic amendment and rice cultivars. Organic amendments in conjunction with chemical N (urea) effected higher CH4 flux over that of chemical N alone. Application of Sesbania, Azolla and compost resulted in 132, 65 and 68 kg CH4 ha−1 in the wet season of 1996 when pure urea application resulted in 42 kg CH4 ha−1. Intermittent irrigation reduced emissions by 15% as compared to continuous flooding in the dry season of 1996. In the wet season of 1995, four cultivars were tested under rainfed conditions resulting in a range of emissions from 20 to 44 kg CH4 ha−1. Application of nitrification inhibitor dicyandiamide (DCD) inhibited while Nimin stimulated CH4 flux from flooded rice compared to that of urea N alone. Wide variation in CH4 production and oxidation potentials was observed in rice soils tested. Methane oxidation decreased with soil depth, fertilizer-N and nitrification inhibitors while organic amendment stimulated it. The results indicate that CH4 emission from the representative rainfed ecosystem at the experimental site averaged to 32 kg CH4 ha−1 yr−1.

Effect of continuous and alternate water regimes on methane efflux from rice under greenhouse conditions

Abstract In a greenhouse study, the effect of moisture regimes (continuously flooded, continuously nonflooded, alternately flooded) on methane efflux from an alluvial soil planted to rice was studied using the closed chamber method. Methane efflux was almost 10 times more pronounced under continuously flooded conditions than under continuously nonflooded conditions. Intermittently flooded regimes (alternately flooded and nonflooded cycles of 40 or 20 days each) emitted distinctly less methane than the continuously flooded system. A significant negative correlation was found between methane emission under different water regimes and rhizosphere redox potential. Extractable Fe2+, readily mineralizable carbon (RMC) and root biomass presented a significant positive correlation with cumulative methane emission. The correlation of methane emission with other plant parameters and microbial biomass was not significant. Our results further suggest the possibility of reduced methane emissions through appropriate water management in a rainfed rice ecosystem.

Methane budget from paddy fields in India

Abstract Results of national methane campaign launched in 1991 to assess methane budget from Indian paddy fields are reported. The campaign involved a number of scientific institutions and universities with National Physical Laboratory at Delhi operating as a nodal agency and covered most of the major rice growing regions of India. Methane emission rates ranged between −0.64 and 84.1 mg −2 h −1 . The methane budget from Indian paddies has been estimated to be around 4.0 TgY −1 with a range between 2.7 to 5.4 TgY −1 .

Diurnal variation in methane efflux at different growth stages of tropical rice

Diurnal variation in CH4 efflux from continuously flooded fields planted to rice (Oryza sativa L. cv. IR-36) was examined at different crop growth stages using a closed chamber method during the wet season. CH4 emission showed a distinct diurnal pattern especially at tillering, panicle initiation and maturity stages of a field-grown rice crop, with maximum emission in the early afternoon (12.00 to 15.00) followed by a decline to a minimum around midnight. Among several variables (ambient temperature, flood water temperature, redox potential, soil pH, and root oxidase activity), a significant negative correlation existed between oxidase activity of the root base and diurnal fluctuations in CH4 efflux at tillering stage. Evidence also suggested that redox status in the rhizosphere region and atmospheric, soil, and water temperatures influenced CH4 emission from rice fields probably by their contrasting effects on CH4 production and oxidation.

Dehydrogenase and invertase activities of flooded soils

The dehydrogenase and invertase activities of three soils were studied under flooded and nonflooded (60% water holding capacity) conditions. Flooding increased (× 1.25 to 2.50) the dehydrogenase activity. In contrast, invertase activity decreased considerably upon flooding. The addition of rice straw increased the invertase activity under both water regimes, but dehydrogenase activity only under flooded conditions.

Cultivar variation in methane efflux from tropical rice

Wide variation in CH4 flux was noticed among the ten rice cultivars grown under uniform field conditions. Cumulative CH4 flux ranged from 4.61 g m-2 to 20.25 g m-2. The rice cultivars could be ranked into three groups based on their CH4 flux potential. Rice cultivars could also be arranged based on their peak CH4 emission occurring either at vegetative, reproductive or at both growth stages. Of the several variables studied (root region redox potential, above- and underground biomass, grain and straw yield, duration of the crop, percent area occupied by the air space and root oxidase activity), only oxidase activity of the root tip exhibited a significant (negative) correlation with CH4 flux indicating an indirect effect of root oxidation potential on CH4 flux. Data presented in this study, demonstrate inherent variation in CH4 flux among different rice cultivars that can be used for developing future mitigation options.

Review: Current status and future prospects of associative nitrogen fixation in rice

Biological sources of nutrients are gaining importance over the chemical and organic sources from the standpoint of environmental safety and quality, and sustainable agriculture. The nutrient input for a growing rice crop can largely be met by promoting the activities of physiologically diverse microorganisms in the aerobic, anaerobic and interface zones in the ecologically important flooded soils. Associative bacteria contribute from 10 to 80 kg N per hectare per cropping season depending upon the ecosystem, cultural practices and rice variety grown. In addition to N contribution, these bacterial associations can improve the nutrient transformations and contribute to plant growth-promoting effects. Current improved agronomic and crop production management systems greatly affect the contributions of biological sources to the overall soil nutrient status. Azospirillum and other associative bacterial systems have been intensively researched using various evaluation techniques to understand the diazotrophic rhizocoenosis. Researches clearly indicate that these associations are governed by several soil, water, nutrient, agrochemical, plant genotype and other biological factors. Considerable efforts have been made so far in selecting efficient bacterial strains as inoculants and identifying host genotypes which support maximum nitrogenase activity in addition to other beneficial traits of effective associative relationships. Knowledge gained so far on how the N2-fixing system in rice functions suggests the need for providing optimum management practices to ensure greater contribution from the plant-microbe associations. Holistic approaches integrating technological developments and achievements in biological sciences could lead to crop improvement. Research on extending nitrogen-fixing symbiosis to rice using molecular and genetic approaches is underway, albeit at a slow pace. The need for further fine-tuning and developing management practices, innovative approaches to improve rice-bacterial systems and the strategies to sustain the benefits from associative diazotrophy are discussed.

Effect of hexachlorocyclohexane on metel4ne production and emission from flooded rice soil

Abstract Application of commercial formulation (an isomeric mixture) of hmachlorocyelohexane (HCH) to flooded rise fields planted to cv. Ran at 1 kg active ingredient.ha−1 significantly inhibited mute emission. Negative P oxafed between methane emission from HCH-treated fields and root oxidise activity (in tents of α-naphthylamine oxidised). Under laboratory condaition, the addition of technical grade α-, β-, γ- and δ-isomers (99.1% purity) of HM individually at 20 μg.g−1 soil at flooding, effected a distinct inhibition of methane production. Evidence suggests that the inhibitory effect of all the four isomers on methane production only until 20–25 days after their application was related to their persistence in flooded soil.

Nitrification of ammonium in different components of a flooded rice soil system

Nitrification associated with the various components [subsurface soil from unplanted and planted (rhizosphere) fields, standing water and surface soil from planted and unplanted fields and leaf sheath suspensions] of submerged rice paddies was examined in incubation experiments with solutions inoculated with soil or water samples. Substantial nitrification occurred in all samples, standing water and surface soil samples in particular, during their 40-day incubation with NH4+−N. Almost all the NH4+−N, disappeared during incubation with standing water, was recovered as NOinf3sup-−N. This, compared to 70–80% from all soil samples and only 29% from leaf sheath suspensions. Significant loss of nitrogen, especially from leaf sheath suspensions, is probably due to nitrification-denitrification as evidenced by its complete recovery in the presence of N-Serve. Nitrification potential of the soil and water samples varied with the crop growth stage and was more pronounced at tillering and panicle inititation stages than at other stages. Nitrification potential of samples from green-manure-amended plots was distinctly less than that of samples from control and urea-amended plots. Most probable number (MPN) estimates of ammonium-oxidizing bacteria were always higher in surface soil in both planted and unplanted plots at all stages of crop growth.