Figure 1.
Scanning electron micrograph (SEM) images of the rice husk gasification slag (RS).
Figure 1.
Scanning electron micrograph (SEM) images of the rice husk gasification slag (RS).
Figure 2.
Diffusive movement of the WE-P in the latosolicred soil (a) and fluvo-aquic soil (b) with different RS addition levels. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively. The different lowercase letters indicate the significant differences in the WE-P concentrationamong the different RS addition levels in each soil section (p < 0.05).
Figure 2.
Diffusive movement of the WE-P in the latosolicred soil (a) and fluvo-aquic soil (b) with different RS addition levels. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively. The different lowercase letters indicate the significant differences in the WE-P concentrationamong the different RS addition levels in each soil section (p < 0.05).
Figure 3.
Distribution of the AE-P in the latosolic red soil (a) and fluvo-aquic soil (b) with the different addition levels of RS. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively. The different lowercase letters indicate significant differences in AE-P concentration among the different RS addition levels in each soil section (p < 0.05).
Figure 3.
Distribution of the AE-P in the latosolic red soil (a) and fluvo-aquic soil (b) with the different addition levels of RS. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively. The different lowercase letters indicate significant differences in AE-P concentration among the different RS addition levels in each soil section (p < 0.05).
Figure 4.
Movement of P from fertilizer in the latosolic red soil (a) and fluvo-aquic soil (b) with different RS addition levels. The different percentages indicate the percentage between the P movement in each soil section and the total fertilizer P. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Figure 4.
Movement of P from fertilizer in the latosolic red soil (a) and fluvo-aquic soil (b) with different RS addition levels. The different percentages indicate the percentage between the P movement in each soil section and the total fertilizer P. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Figure 5.
Distribution of Olsen-P in the latosolic red soil (a) and fluvo-aquic soil (b) with the different RS addition levels. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively. The different lowercase letters indicate significant differences in the Olsen-P concentration among the different RS addition levels in each soil section (p< 0.05).
Figure 5.
Distribution of Olsen-P in the latosolic red soil (a) and fluvo-aquic soil (b) with the different RS addition levels. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively. The different lowercase letters indicate significant differences in the Olsen-P concentration among the different RS addition levels in each soil section (p< 0.05).
Figure 6.
Proportions of the various P fractions moved from the total P from the fertilizer in the latosolic red soil (a) and fluvo-aquic soil (b). The values indicate the percentage between the total movements of the P fractions in the 0–30 mm soil section and the total fertilizer P. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Figure 6.
Proportions of the various P fractions moved from the total P from the fertilizer in the latosolic red soil (a) and fluvo-aquic soil (b). The values indicate the percentage between the total movements of the P fractions in the 0–30 mm soil section and the total fertilizer P. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Table 1.
Physiochemical properties of the soils used in this study. Olsen-P, WE-P and AE-P represent available P, water-extractable P and acid-extractable P, respectively.
Table 1.
Physiochemical properties of the soils used in this study. Olsen-P, WE-P and AE-P represent available P, water-extractable P and acid-extractable P, respectively.
Soil Type | Olsen-P (mg·kg−1) | WE-P (mg·kg−1) | AE-P (mg·kg−1) | Organic Matter (%) | pH | Total Ca (g·kg−1) | Total Al (g·kg−1) | Total Fe (g·kg−1) |
---|
Latosolic red soil | 27.91 | 7.91 | 190.00 | 2.73 | 5.45 | 4.38 | 79.66 | 11.04 |
Fluvo-aquic soil | 24.93 | 12.95 | 791.14 | 1.71 | 8.48 | 53.84 | 30.62 | 37.71 |
Table 2.
Regression analysis (y = b0eb1x) of the relationship of the WE-P concentration (y, mg·kg−1) with the distance from the fertilizer site (x, mm) in the soils. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Table 2.
Regression analysis (y = b0eb1x) of the relationship of the WE-P concentration (y, mg·kg−1) with the distance from the fertilizer site (x, mm) in the soils. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Treatments | Latosolic Red Soil | Fluvo-aquic Soil |
---|
b0 (mg·kg–1) | b1 | R2 | Significance | b0 (mg·kg–1) | b1 | R2 | Significance |
---|
MAP | 1206.04 | −0.20 | 0.952 | p < 0.001 | 465.16 | −0.18 | 0.995 | p < 0.001 |
MAP + 1/3RS | 1211.67 | −0.20 | 0.942 | p < 0.001 | 1026.23 | −0.22 | 0.990 | p < 0.001 |
MAP + 1/2RS | 1247.92 | −0.20 | 0.950 | p < 0.001 | 1077.00 | −0.21 | 0.985 | p < 0.001 |
MAP + RS | 1461.94 | −0.21 | 0.942 | p < 0.001 | 980.97 | −0.21 | 0.989 | p < 0.001 |
MAP + 2RS | 1420.93 | −0.21 | 0.950 | p < 0.001 | 1051.88 | −0.23 | 0.982 | p < 0.001 |
Table 3.
Regression analysis (y = b0eb1x) of the relationship of AE-P (y, mg·kg−1) with the distance from the fertilizer site (x, mm) in the soils. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Table 3.
Regression analysis (y = b0eb1x) of the relationship of AE-P (y, mg·kg−1) with the distance from the fertilizer site (x, mm) in the soils. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Treatments | Latosolic Red Soil | Fluvo-aquic Soil |
---|
b0 (mg·kg–1) | b1 | R2 | Significance | b0 (mg·kg–1) | b1 | R2 | Significance |
---|
MAP | 2331.76 | −0.21 | 0.978 | p < 0.001 | 4183.52 | −0.23 | 0.976 | p < 0.001 |
MAP + 1/3RS | 2151.70 | −0.20 | 0.989 | p < 0.001 | 3103.85 | −0.21 | 0.974 | p < 0.001 |
MAP + 1/2RS | 1982.15 | −0.20 | 0.994 | p < 0.001 | 3644.76 | −0.22 | 0.981 | p < 0.001 |
MAP + RS | 1880.28 | −0.19 | 0.984 | p < 0.001 | 3122.29 | −0.21 | 0.990 | p < 0.001 |
MAP + 2RS | 1909.21 | −0.20 | 0.991 | p < 0.001 | 3356.02 | −0.21 | 0.988 | p < 0.001 |
Table 4.
The mass of soil slice (g). MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Table 4.
The mass of soil slice (g). MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Soil Section | Latosolic Red Soil | Fluvo-aquic Soil |
---|
MAP | MAP + 1/3RS | MAP + 1/2RS | MAP + RS | MAP + 2RS | MAP | MAP + 1/3RS | MAP + 1/2RS | MAP + RS | MAP + 2RS |
---|
0–5 | 8.72 | 8.67 | 8.80 | 8.79 | 8.79 | 8.91 | 8.98 | 8.99 | 9.01 | 9.02 |
5–10 | 8.80 | 8.72 | 8.84 | 8.77 | 8.78 | 9.05 | 9.07 | 9.02 | 9.03 | 9.03 |
10–15 | 8.69 | 8.63 | 8.69 | 8.75 | 8.81 | 9.01 | 9.10 | 8.90 | 9.03 | 9.03 |
15–20 | 8.66 | 8.67 | 8.86 | 8.72 | 8.71 | 9.10 | 8.98 | 9.00 | 8.96 | 9.02 |
20–25 | 8.61 | 8.75 | 8.85 | 8.77 | 8.87 | 8.89 | 9.01 | 9.07 | 8.99 | 8.89 |
25–30 | 8.79 | 8.68 | 8.67 | 8.88 | 8.80 | 8.96 | 8.95 | 8.99 | 9.00 | 9.03 |
Table 5.
Regression analysis (y = b0eb1x) of the relationship of Olsen-P (y, mg·kg−1) with the distance from the fertilizer site (x, mm) in the soils. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Table 5.
Regression analysis (y = b0eb1x) of the relationship of Olsen-P (y, mg·kg−1) with the distance from the fertilizer site (x, mm) in the soils. MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Treatments | Latosolic Red Soil | Fluvo-aquic Soil |
---|
b0 (mg·kg–1) | b1 | R2 | Significance | b0 (mg·kg–1) | b1 | R2 | Significance |
---|
MAP | 1850.90 | −0.20 | 0.966 | p < 0.001 | 1503.80 | −0.20 | 0.990 | p < 0.001 |
MAP + 1/3RS | 1833.02 | −0.20 | 0.975 | p < 0.001 | 2348.63 | −0.22 | 0.993 | p < 0.001 |
MAP + 1/2RS | 1810.57 | −0.20 | 0.985 | p < 0.001 | 2950.32 | −0.22 | 0.990 | p < 0.001 |
MAP + RS | 1848.49 | −0.20 | 0.974 | p < 0.001 | 2035.64 | −0.20 | 0.992 | p < 0.001 |
MAP + 2RS | 1926.27 | −0.20 | 0.985 | p < 0.001 | 2036.69 | −0.21 | 0.994 | p < 0.001 |
Table 6.
Quantitative relationship among WE-P, AE-P, and Olsen-P (y = a·Olsen-P + b). MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Table 6.
Quantitative relationship among WE-P, AE-P, and Olsen-P (y = a·Olsen-P + b). MAP, MAP + 1/3RS, MAP + 1/2RS, MAP + RS and MAP + 2RS represent treatments monoammonium phosphate alone or in combination with 0.016 g RS, 0.024 g RS, 0.048 g RS and 0.096 g RS, respectively.
Treatments | WE-P | AE-P |
---|
a | b | R2 | Significance | a | b | R2 | Significance |
---|
Latosolic red soil | MAP | 0.63 | 4.13 | 0.998 | p < 0.001 | 1.32 | −12.42 | 0.994 | p < 0.001 |
MAP + 1/3RS | 0.58 | 6.95 | 0.997 | p < 0.001 | 1.25 | −8.04 | 0.998 | p < 0.001 |
MAP + 1/2RS | 0.56 | 10.49 | 0.988 | p < 0.001 | 1.20 | −6.13 | 0.998 | p < 0.001 |
MAP + RS | 0.66 | 1.03 | 0.998 | p < 0.001 | 1.07 | 4.69 | 0.998 | p < 0.001 |
MAP + 2RS | 0.65 | 2.20 | 0.998 | p < 0.001 | 0.99 | 9.68 | 0.991 | p < 0.001 |
Fluvo−aquic soil | MAP | 0.40 | −2.94 | 0.982 | p < 0.001 | 2.82 | −66.32 | 0.949 | p < 0.001 |
MAP + 1/3RS | 0.37 | 4.12 | 0.998 | p < 0.001 | 1.26 | 10.63 | 0.997 | p < 0.001 |
MAP + 1/2RS | 0.39 | 0.32 | 0.997 | p < 0.001 | 1.18 | 0.97 | 0.998 | p < 0.001 |
MAP + RS | 0.44 | 0.20 | 0.998 | p < 0.001 | 1.46 | −6.50 | 0.998 | p < 0.001 |
MAP + 2RS | 0.47 | −5.40 | 0.993 | p < 0.001 | 1.62 | −10.29 | 0.996 | p < 0.001 |