Phosphorus efficiency in a long-term wheat–rice cropping system in China

2010 ◽  
Vol 149 (3) ◽  
pp. 297-304 ◽  
Author(s):  
X. TANG ◽  
X. SHI ◽  
Y. MA ◽  
X. HAO

SUMMARYLong-term (over 14 years) experiments on winter wheat (Triticum aestivum L.)–rice (Oryza sativa L.) crop rotations were conducted in Southwest China to investigate phosphorus (P) fertilizer utilization efficiency, including the partial factor productivity (PFP), agronomic efficiency (AE), internal efficiency (IE), partial P balance (PPB), recovery efficiency (RE) and the mass (input–output) balance. The seven treatments were Control, N, NP, NK, NPK, NPKM and NPKSt, representing various combinations of inorganic fertilizers (N, P and K), manure (M) and the application of rice straw (St). Without P application, the soil could supply c. 14·7–22·5 kg P/ha annually and produce, on average, c. 1·8 t/ha wheat and 6·0 t/ha rice. Phosphorus fertilization increased crop yields by 65·5 and 11·4% for wheat and rice, respectively, over the 14 years. The PFP values ranged from 80·2 to 177 kg grain/kg P fertilizer for wheat and from 222 to 255 kg/kg for rice in the NPK treatments. However, the mean AE over the 14-year period was 31·9 and 21·3 kg grain/kg inorganic P fertilizer for wheat and rice, respectively. The mean IE was 214 and 318 kg grain/kg P uptake for wheat and rice, respectively, during the cultivation period. The PPB for the whole rotation system over the 14 years ranged from 0·58 to 0·64. However, the mean RE of P fertilizer was 0·26 (varying from 0·22 to 0·29) in the wheat–rice cropping system over the 14-year period. For every 100 kg surplus P/ha per year, the concentration of soil P extracted by 0·5 m NaHCO3 at pH 8·5 (Olsen-P) would increase by, on average, 4·12 mg/kg in soil. For the wheat–rice cropping system, the current P application rate of 55–65 kg P/ha per year is able to sustain annual yields of about 3 t/ha for wheat and 7 t/ha for rice. This study suggests that, in order to achieve higher crop yields, the P fertilizer utilization efficiency should be considered when making P fertilizer recommendations in wheat–rice cropping systems.

2021 ◽  
Vol 9 ◽  
Author(s):  
Wenjia Yu ◽  
Haigang Li ◽  
Peteh Mehdi Nkebiwe ◽  
Guohua Li ◽  
Torsten Müller ◽  
...  

Modern phosphate (P) fertilizers are sourced from P rock reserves, a finite and dwindling resource. Globally, China is the largest producer and consumer of P fertilizer and will deplete its domestic reserves within 80 years. It is necessary to avoid excess P input in agriculture through estimating P demand. We used the legacy P assessment model (LePA) to estimate P demand based on soil P management at the county, regional, and country scales according to six P application rate scenarios: (1) rate in 2012 maintained; (2) current rate maintained in low-P counties and P input stopped in high-P counties until critical Olsen-P level (CP) is reached, after which rate equals P-removal; (3) rate decreased to 1–1.5 kg ha−1 year−1 in low-P counties after CP is reached and in high-P counties; (4) rate in each county decreased to 1–8 kg ha−1 year−1 after soil Olsen-P reached CP in low P counties; (5) rate in each county was kept at P-removal rate after reduction; (6) P input was kept at the rate lower than P-offtake rate after reduction. The results showed that the total P fertilizer demand of China was 750 MT P2O5, 54% of P fertilizer can be saved from 2013 to 2080 in China, and soil Olsen-P of all counties can satisfy the demand for high crop yields. The greatest potential to decrease P input was in Yangtze Plain and South China, which reached 60%. Our results provide a firm basis to analyze the depletion of P reserves in other countries.


2010 ◽  
Vol 113-116 ◽  
pp. 155-160
Author(s):  
Quan Lai Zhou ◽  
Mu Qiu Zhao ◽  
Cai Yan Lu ◽  
Yi Shi ◽  
Xin Chen

This study investigated the effects of different rates of phosphorus application on vertical transference of P. An aquatic brown paddy soil was filled in organic glass columns using for the leaching experiments. The results indicated that significant vertical transference was found using change of Olsen-P and CaCl2-P. The transference distance was no more than 10cm when P application rate between 200 and 800 kg P ha-1, and was more than 10cm as P application rate above 800 kg P ha-1. We obtained the threshold value of Olsen-P was 53.7 mg kg-1 by split-line model, and calculated that the threshold value of P fertilizer application rate was 382.1 kg P ha-1 by relationship of soil Olsen-P concentration and P application rate. The soil P transference increased, if P application rate was above 382.1 kg P ha-1. It would be helpful for controlling the P fertilizer amount by field to decrease P loss.


2021 ◽  
Vol 33 (1) ◽  
Author(s):  
Nina Siebers ◽  
Liming Wang ◽  
Theresa Funk ◽  
Sabine von Tucher ◽  
Ines Merbach ◽  
...  

Abstract Background The phosphorus (P) stocks of arable subsoils not only influence crop production but also fertilizer P sequestration. However, the extent of this influence is largely unknown. This study aimed to (i) determine the extent of P sequestration with soil depth, (ii) analyze P speciation after long-term P fertilization, and (iii) compare soil P tests in predicting crop yields. We analyzed four long-term fertilizer trials in Germany to a depth of 90 cm. Treatments received either mineral or organic P, or a combination of both, for 16 to 113 years. We determined inorganic and organic P pools using sequential extraction, and P speciation using 31P nuclear magnetic resonance (NMR) and X-ray absorption near edge structure (XANES) spectroscopy. In addition, we applied three P soil tests, double-lactate (DL), calcium acetate lactate (CAL), and diffusive gradients in thin films (DGT). Results The results suggested that plants are capable of mobilizing P from deeper soil layers when there is a negative P budget of the topsoil. However, fertilization mostly only showed insignificant effects on P pools, which were most pronounced in the topsoil, with a 1.6- to 4.4-fold increase in labile inorganic P (Pi; resin-P, NaHCO3–Pi) after mineral fertilization and a 0- to 1.9-fold increase of organic P (Po; NaHCO3–Po, NaOH–Po) after organic P fertilization. The differences in Po and Pi speciation were mainly controlled by site-specific factors, e.g., soil properties or soil management practice rather than by fertilization. When modeling crop yield response using the Mitscherlich equation, we obtained the highest R2 (R2 = 0.61, P < 0.001) among the soil P tests when using topsoil PDGT. However, the fit became less pronounced when incorporating the subsoil. Conclusion We conclude that if the soil has a good P supply, the majority of P taken up by plants originates from the topsoil and that the DGT method is a mechanistic surrogate of P plant uptake. Thus, DGT is a basis for optimization of P fertilizer recommendation to add as much P fertilizer as required to sustain crop yields but as low as necessary to prevent harmful P leaching of excess fertilizer P.


2014 ◽  
Vol 60 (No. 8) ◽  
pp. 351-357 ◽  
Author(s):  
A. Das ◽  
Sharma RP ◽  
N. Chattopadhyaya ◽  
R. Rakshit

We measured the long-term (28 years) sustainability of rice-wheat cropping system under integrated nutrient management practices emphasizing the trends in grain yields, sustainable yield index (SYI) and nutrient budgeting. The data of long-term experiment revealed that grain yield of both rice and wheat declined under control and sub-optimal fertilizer inputs (50% or 75% recommended fertilizer NPK). Negative yield trend (slope) was observed in control plots for rice (&ndash;0.0296) and wheat (&ndash;0.0070); whereas positive yield trend was observed under treatments receiving organic supplements. The SYI values indicate that rice yields are more sustainable than wheat. Data on apparent nutrient balance showed a deficit of N (&ndash;42.2 kg/ha/year), P (&ndash;9.1 kg/ha/year) and K (&ndash;52.2 kg/ha/year) under control plots. Surprisingly, there was net depletion of K under the organic supplemented plots. Correlation study revealed that apparent balance of K was negatively correlated with SYI (r = &ndash;0.921 for rice; r = &ndash;0.914 for wheat) and yield slope (r = &ndash;0.870 for rice; r = &ndash;0.896 for wheat). If the trend of K imbalance is not reversed, the potential to improve N and P fertilizer use efficiency and crop yields will be limited.


2010 ◽  
pp. 20-29
Author(s):  
AL Shah ◽  
JC Biswas ◽  
ARM Solaiman ◽  
GM Panaullah

A study was conducted at the BRRI research farm during 2001 to determine the distribution of soil phosphorus (P) fractions in P-deficient rice soil that received varied amount of P as triple super phosphate (TSP) and di-ammonium phosphate (DAP). Solution P ranged from 0.06 to 0.08 mg L-1 which was significantly greater in long duration variety (LDV) compared to short duration variety (SDV) at Pcontrol conditions. The increase in NaHCO3-Pi pool was 4.5-35.2% greater with LDV compared to SDV at 30-45 kg P ha-1. There was 7-10% greater NaOH-Po after growing LDV compared to SDV at larger P doses as TSP. The buildup of NaOH-Po pool was greater by 18% after growth of SDV compared to LDV when P was added as DAP. The NaOH-Pi fraction increased by about 21-212% with P application compared to P control irrespective of P sources. The larger HCl-Pi fraction buildup (21-152%) took place because of P application either as TSP or DAP, especially with the LDV. The increase in residual-P fraction was 10-158% because of P-fertilization and rice genotypes compared to control. Under Pfertilized conditions, NaHCO3-Pi and NaOH-Po appeared to have acted as sinks of added P-fertilizer. Cultivation of rice genotypes at 30-40 kg P ha-1 under lowland situations further contributes to P buildup in soil which could be utilized in the succeeding crops for profitable farming.


2019 ◽  
Vol 103 (1) ◽  
pp. 43-45 ◽  
Author(s):  
Carlos Crusciol ◽  
João Rigon ◽  
Juliano Calonego ◽  
Rogério Soratto

Some crop species could be used inside a cropping system as part of a strategy to increase soil P availability due to their capacity to recycle P and shift the equilibrium between soil P fractions to benefit the main crop. The release of P by crop residue decomposition, and mobilization and uptake of otherwise recalcitrant P are important mechanisms capable of increasing P availability and crop yields.


2012 ◽  
Vol 58 (No. 5) ◽  
pp. 230-235 ◽  
Author(s):  
Manoj-Kumar ◽  
A. Swarup ◽  
A.K. Patra ◽  
J.U. Chandrakala ◽  
K.M. Manjaiah

In a phytotron experiment, wheat was grown under two levels of atmospheric CO<sub>2</sub> [ambient (385 ppm) vs. elevated (650 ppm)], two levels of temperature (ambient vs. ambient +3&deg;C) superimposed with three levels of phosphorus (P) fertilization: 0, 100, and 200% of recommended dose. Various measures of P acquisition and utilization efficiency were estimated at crop maturity. In general, dry matter yields of all plant parts increased under elevated CO<sub>2</sub> (EC) and decreased under elevated temperature (ET); however, under concurrently elevated CO<sub>2</sub> and temperature (ECT), root (+36%) and leaf (+14.7%) dry weight increased while stem (&ndash;12.3%) and grain yield (&ndash;17.3%) decreased, leading to a non-significant effect on total biomass yield. Similarly, total P uptake increased under EC and decreased under ET, with an overall increase of 17.4% under ECT, signifying higher P requirements by plants grown thereunder. Although recovery efficiency of applied P fertilizer increased by 27%, any possible benefit of this increase was negated by the reduced physiological P efficiency (PPE) and P utilization efficiency (PUtE) under ECT. Overall, there was ~17% decline in P use efficiency (PUE) (i.e. grain yield/applied P) of wheat under ECT. &nbsp;


2020 ◽  
Vol 36 (3) ◽  
pp. 524-535 ◽  
Author(s):  
Stefania C. Appelhans ◽  
Pedro Anibal Barbagelata ◽  
Ricardo Jose Miguel Melchiori ◽  
Flavio Gutierrez Boem

1986 ◽  
Vol 26 (1) ◽  
pp. 115 ◽  
Author(s):  
AL Garside ◽  
MC Fulton

The primary and residual effects of phosphorus (P) fertilizer on soybeans (Glycine max cv. Buchanan) were studied at one site for three seasons on Cununurra clay in the Ord Irrigation Area. Grain yield increased (P< 0.01) with both primary and residual P in all seasons. When grain yields over the 3 years were standardized to eliminate seasonal effects, relative grain yield (RGY) was positively related to each of bicarbonate-extractable soil P (EP), applied fertilizer P (FP) and fertilizer P applied to the previous crop (PFP). Seventy-three per cent of the variation in relative yield within years could be explained by the equation: RGY = 45.44 + 0.64FP + l.84EP + 0.197PFP R 2 = 0 . 7 3 , P < 0.01 Increasing P status was associated with increased plant height, dry matter production and weight of 100 seeds and increased the number of main-stem nodes, nodules, pods per plant and days to maturity, but had no effect on number of seeds per pod and number of days until commencement and completion of flowering. Concentrations of P in the whole tops and uppermost leaf increased with increasing rate of P application. However, there was a significant P x growth stage interaction on nitrogen concentrations in whole tops and upper-most leaf, these being lower in the high-P plots early in the season. Grain protein content increased with increasing P status while oil content was reduced. The results show that rates of P application higher than those being currently used are required to maximize soybean yield on Cununurra clay.


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