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Research Detail

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Dr. Md. Fazlul Hoque
Professor
Department of Soil Science, Patuakhali Science and Technology University, Dumki, Patuakhali-8602, Bangladesh

Maximum P adsorption capacity of the tested coastal soils ranged from 1250 – 1834 µg g-1. Energy of adsorption varied from 0.223 to 1.00 µg ml – 1, P buffering capacity ranged from 139 to 243 and P saturation ranged from 0.27 to 1.59 µmol g-1. Acid (HCl 0.5M) although extracted the highest amount of both native and applied P, showed the poorest relationship with relative dry matter and P uptake by rice. Olsen extractant showed the best correlation between soil test P and dry matter yield but it explained only about 70% of the variability. The critical level for Olsen P was found 5 mg kg – 1 for the coastal soils of Bangladesh. Tidal floodplain soils, on an average of 12 samples, contained 887 mg kg-1 of total P of which only 0.01% remained in solution form, 1.84% in NaHCO3 extractable, 4.24% in NaOH extracted inorganic P fraction, 46.65% in NaOH extracted organic P fraction, 28.19% in acid pool and 18.97% in residual pool. The tested soils showed a large variability in the distribution in native P in different pools. The application of P mainly increased NaHCO3 extractable P and 0.10 N NaOH extractable inorganic P pools. Continuous rice cultivation without P application, in controlled net house condition, decreased the concentration of labile P (solution P and NaHCO3 P), moderately labile P (NaOH Pi and acid) and stable P (organic and residual P) but with the addition of P increased the labile and moderately labile P. Exhaustive rice cropping in pots was done with no application of P (P0) and with 50 mg kg-1 P application (P50) for four crops. The pot experiment facilitated the estimation of labile and stable P pools in coastal soils based on plant P uptake. Estimated labile P ranged from 5 mg kg–1 in Barisal clay soil collected from Dumki, Patuakhali to 55 mg kg–1 in Sara silty clay soils collected from Gournadi, Barisal. Estimated stable P pool varied from 77 mg kg–1 in Jhalokathi clay collected from Dumki, Patuakhali to 848 mg kg–1 in Barisal clay collected from Barisal. About 3% of the stable P in coastal soils was transferred to labile pool, but depending upon soils 23 to 62% of the labile P was absorbed by the growing rice plants. The estimated labile P showed about 93% variability in relative dry matter and 82% variability in P uptake in P0 pots. Estimated stable P pool exhibited about 90% variability in relative dry matter yield and P uptake by rice plant in P0 conditions. The labile P and stable P estimated through plant based approach explained the variability of relative dry matter yield of rice and P uptake better than the soil test approach. Critical level of labile P and stable P was found 37.5 and 600 mg pot–1, respectively, for the coastal soils of Bangladesh. The labile P and stable P as indicator for differentiating soils into sufficient and deficient level of P need calibration through field studies.

  Phosphorus sorption, Desorption, Fractions, Tidal floodplain soils
  Department of Soil Science, Patuakhali Science and Technology University, Dumki, Patuakhali
  00-01-2009
  00-06-2009
  Crop-Soil-Water Management
  Fertilizer
  1. To determine P sorption capacities of tidal flooded soils,
  2. To determine different P fractions in tidal flooded soils,
  3. To evaluate the commonly used phosphorus extraction methods for available P in tidal flooded soils, and
  4. To determine P supplying capacity of tidal flooded soils for rice.

The laboratory experiment conducted at the Department of Soil Science, Patuakhali Science and Technology University, Dumki, Patuakhali during January to June 2009 involves thirteen surface (0-15 cm) soil samples collected from cultivated rice fields in January to March 2007 after T-Aman harvest.  The selected soil sampling sites includes 7 Upazila–Dumki, Kalapara of Patuakhali, Amtali of Borguna, Wuzirpur and Gouranadi of Barisal and Borhanuddin and Lalmohan of Bhola district. The collected soil samples were air-dried and ground to pass a 2-mm sieve and then mixed to form a composite sample.

Phosphorus sorption

Phosphorus sorption isotherm studies followed the procedure of Nair et al. (1984). Briefly, one gram of the soil sample was taken in 25 ml test-tube with various addition of P (0, 1, 3, 6, 12, 18, 24, 30, 37, 43, 55, 68 and 80 ppm) in 20 ml of 0.01M CaCl2 solutions separately. The resultant P content was 0, 20, 60, 120, 240, 360, 480, 600, 740, 860, 1100, 1360 and 1600 mg kg-1. Then the test tubes were shaken for 24 hrs on horizontal shaker with low oscillation. After equilibration, the supernatant was passed through a Whatman # 42 filter paper and the filtrate was analyzed for P following Murphy and Riley (1962) method. The equilibrium P concentration data were interpreted by Langmuir, Freundlich and Temkin Equations.

Calculation of Smax, Adsorption energy and P-buffering capacity

The phosphorus adsorption maximum (Smax) was calculated using the Langmuir adsorption equation (Eq. 1). Smax was calculated by regressing C/(x/m) versus C, where C is the equilibrium solution P concentration and (x/m) is adsorbed P. The reciprocal of the slope of the linear regression is Smax (Olsen and Watanabe, 1957; Syers et al., 1973). The energy of adsorption for phosphorus (binding energy) was also calculated from Langmuir adsorption equation, where k is a constant related to the bonding energy of adsorption. The P-buffering capacity of soils has been calculated from the Temkin equation (Eq. 3), where b is considered the P-buffering capacity.

Phosphorus depletion experiment was performed in pot culture with a test crop of local rice variety Mala. Four rice crops of 6 weeks duration were grown with P0 and P50.

Plant dry weight (g pot-1) was recorded and P uptake (mg pot-1) by rice plant was calculated. Relative dry matter yield (RDMY) of rice was calculated as

--------------------------------------------------(1)

Where

DM0 = dry matter yield without P application

DM50 = dry matter yield with 50 mg kg-1 P application

Relationship of RDMY of rice (1st crop) with soil available P extracted by different extraction methods and different fractions of phosphorus was tested. Critical level of different soil test P (Olsen P, Bray I P, Mehlich II and Mehlich III) for dry matter yield of rice was done by Cate-Nelson (1965) graphical method. Phosphorus concentration (%) in plant and P uptake (mg pot-1) by rice plant was determined at first, second, third and fourth harvest. Relationship between dry matter weight and P content, dry matter weight and P uptake of rice plant at different harvests were established. Different P pools were estimated.

  PhD Thesis
  
Funding Source:
  
  • The extraction of P by HCl (0.5M HCl) was observed to vary significantly in different studied soils.
  • Soil P is distributed in solution, NaHCO3-P, NaOH-Pi, NaOH-Po, acid and residual P fractions.
  • The application of P changed the distribution of P in different pools and most of the applied P was recovered from NaOH-Pi, acid P and NHCO3-P fractions.
  • Phosphorus response in all the crops and in all soils was visible. The second, third and fourth crops showed P deficiency in P0 treatments.
  • Different soil series from a given location showed variable P response. The same soil series in different locations also expressed tremendous variation in P response.
  • Olsen P was found better than other methods (Bray I P, Mehlich II P and Mehlich III P) to explain the relationship between relative dry matter yield and soil test P.
  • From the data points in Cate-Nelson graphs, Olsen method also appeared as the best soil testing procedure for coastal soils of Bangladesh.
  • Dry matter yield and P uptake by rice plant showed poor linear relationship with soil P fractions.
  • Phosphorus uptake expressed strong linear relationship with dry matter yield of rice plant but showed poor linear relationship with soil fraction P test results.  
  • Phosphorus concentration in the rice plant tissue tended to show poor logarithmic relationship with plant dry matter yield.
  • All fractions of soil P were decreased due to exhausted cropping uptake in control pots, while the fertilized pots showed an increase in solution P, NaHCO3-P, NaOH-Pi and acid-P but and decrease in NaOH-Po and residual-P. 
  • Without P application the transfer rate of stable to labile P pool was higher than the transfer rate of labile to stable P pool. On the other hand transfer rate of stable to labile P pool is lower than the transfer rate of labile to stable P pool with P application.
  • Total soil P is decreased in the soils having high transferring capacity of P from stable to labile pool, response of P is not visible and response of P is markable in the soils having low transferring capacity of P from stable to labile pool.
  Thesis
  


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