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Research Detail

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P. K. Saha
Senior Scientific Officer
Soil Science Division, BRRI, Gazipur-1701

M. A. Mazid Miah
Chief Scientific Officer and Head
Soil Science Division, BRRI, Gazipur-1701

M. S. Rahman
Senior Scientific officer
Soil Science Division, BRRI, Gazipur-1701

A. Islam
Senior Scientific officer
Soil Science Division, BRRI, Gazipur-1701

A field experiment was carried out at the Bangladesh Rice Research Institute (BRRI) Farm, Gazipur to study the release pattern of NH4+-N from two sources of N viz., prilled urea (PU) and urea super granules (USG) at different N levels under lowland situation. It appeared from the findings that at N0 (with no N fertilizer) plots, NH4+-N concentration increased from 9.03 (initial) to 16.58 mg/kg at 15 days after transplanting (DAT), and then gradually decreased throughout the growing season. At 90 DAT it dropped below the initial value. At 15 DAT the plots, in which PU at different doses (N100-N150) were added, showed a significant positive increase of NH4+-N by 5.31-5.88 mg/kg over N0 plots. However, no significant difference in NH4+-N concentration was observed among N added plots. At 45 DAT, it was observed that the magnitude of release pattern of NH4+-N from USG was slightly higher than that of PU. A tendency of releasing more NH4+-N was observed with the highest doses of PU and USG compared to lower doses at 45 DAT. The amount of released NH4+-N gradually decreased with time depending on the magnitude of the applied N levels. Results indicated that a basal dose of N fertilizer may not be required for the rice crop growing in the Grey-Terrace Soil of Madhupur Tract. Instead, N fertilizer may be used after 15 DAT, when the rice plants are established.

  Release pattern, NH4+-N, Urea super granules, Lowland rice
  Bangladesh Rice Research Institute (BRRI) experimental farm, Gazipur
  01-11-1998
  30-06-1999
  Crop-Soil-Water Management
  Fertilizer

To determining the release pattern of NH4+-N in situ from two sources of N fertilizer prilled urea (PU) and urea super granules (USG) with different N levels under wetland rice cultivation.

The field experiment was conducted at the BRRI farm, Gazipur in the Boro season, 1998-99. Soils of the experimental field is clay loan in texture and slightly acidic in nature having organic carbon 1.18%, total N 0.12%, C:N ratio 9.8, CEC 23 cmol/kg, NH4+-N 9.03 mg/kg and NO3--N 2.64 mg/kg. Field experiment was established with BRRI dhan29 rice variety using two sources of N: PU and USG. The N doses for PU were: 0, 100, 125 and 150 kg/ha and for USG were: 0, 81 and 109 kg/ha. Experiment was laid out in a RCB design with three replications. PU was applied as broadcast in four equal splits: 25% as basal, 25% at 15 days after transplanting (DAT), 25% and 45 DAT and 25% at 90 DAT. All USG was applied one time at 15 DAT in deep placement method when rice plants were established. Initial soil samples (0-20 cm depth) were from 15 spots of each block of the main field prior to fertilizer application. After transplanting, samples (0-20 cm depth) from the three spots of each designated plots were collected to determine in situ N mineralization according to schedule: initial and 1st soil sampling, basal N application and seedling transplanting on 3rd January 1999 (0 DAT); 2nd soil sampling, 1st PU top dressing and USG application on 18th January 1999 (15 DAT); 3rd soil sampling and 2nd PU top dressing on 17th February 1999 (45 DAT); 4th soil sampling and 3rd PU top dressing on 3rd April 1999 (90 DAT). Soil sampling was done before N fertilizer (PU and USG) application. About 200 g composite fresh soils were collected in a plastic bag. Inorganic NH4+-N was determined from the fresh soil samples and considered as the N availability index for submerged soil. At each specified time, after the collection of samples from experimental field, 20 g composite fresh soil was weighed and taken into a 125 ml conical flask and 100 ml of 2M KCl added, capped and shaken for two hours on a reciprocating shaker. Samples were filtered though Whatman No. 42 filter paper. At the same time determination of moisture of soil was done to adjust the results in an oven dry basis. Inorganic NH4+-N was determined by Micro kjeldahl distillation method (Keeney and Nelson, 1982).

  Bangladesh J. Agril. Res. 15 (2): 261-267, June 2008
  
Funding Source:
1.  Government Budget:  
  

Nitrogen fertilization either as PU or USG increased soil N mineralization (NH4+-N) during the growing period of wetland rice. The NH4+-N concentration at N0 plots significantly increased from 9.03 (initial) to 16.58 mg/kg at 15 DAT and then gradually decreased with time throughout the growing period and at 90 DAT, it decreased sharply. Applied N significantly increased the NH4+-N concentration in soil by 5.31-5.88 mg/kg over N0 plots at 15 DAT. However, no significant difference in NH4+-N concentration was observed among N added plots. In the early growth stage, plots receiving low amount of applied N (N100) released slightly more NH4+-N than that of higher N doses plots. At 45 DAT, N fertilized with the highest doses of PU and USG plots released more NH4+-N than did N fertilized with the lower doses plots. Superiority was found with the plots receiving highest doses of USG (N106-N109). Statistically, the difference was at par compared to the plots receiving N100-N150 from PU. The amount of released NH4+-N gradually decreased with time depending on the magnitude of the applied N levels. The release pattern of NH4+-N at 45 DAT was higher from the USG source compared to PU. At 90 DAT, the amount of NH4+-N at the different levels dropped below the initial value.

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