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Journal of Environment and Earth Science www.iiste.org 
ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) 
Vol.4, No.15, 2014 
Effect of Applied Phosphorus on the Availability of 
Micronutrients in Alkaline-Calcareous Soil 
Fayaz Ali1 Arooj Sadiq1 Irshad Ali1 Muhammad Amin2* Muhammad Amir3 
1.Department of Soil and Environmental Sciences, The University of Agriculture Peshawar Pakistan 
2.Department of Agricultural Chemistry, The University of Agriculture Peshawar Pakistan 
3.Department of Plant Breeding and Genetics, The University of Agriculture Peshawar Pakistan 
*For Correspondence Email: agrian.amin06@gmail.com 
Abstract 
The present experiment was carried out to study the effect of applied phosphorus on the availability of 
micronutrients in alkaline-calcareous soil. For this purpose an incubation experiment was conducted in the 
laboratory of Soil and Environmental Sciences Department, The University of Agriculture Peshawar Pakistan 
during 2009 with variable amounts of phosphorus, i.e. 0, 30, 60, 90, 120 and 150 kg P ha-1 in the form of single 
super phosphate. The experiment was conducted in completely randomized block design with three replications 
consisted of 100 g of soil in each pot. The experiment was incubated for 28 days under normal conditions. The 
soil was kept moist up to field capacity condition throughout the incubation period. Results regarding the effect 
of phosphorus application on the availability of micronutrients showed non-significant differences in the 
treatments of applied phosphorus, but the trend of each micronutrient was obvious. The overall results showed 
that as the application of phosphorus increases, the concentrations of B, Zn and Cu gradually decreases, which 
indicate negative interactions, while the concentrations of P, Fe and Mn increases perhaps due to positive 
interactions with applied phosphorus during incubation period. Results further showed as the applied P (from 
single super phosphate) increases the pH-values gradually decreases, which resulted significantly negative 
correlation with one another (r2 = 0.83). These results indicate that with the application of P as single super 
phosphate reduced the pH of soil and has favorable effect on the solubility of micronutrients, specifically Fe and 
Mn in the alkaline-calcareous soils. 
Keywords: Phosphorus, Micronutrients availability 
143 
INTRODUCTION 
Phosphorus is the second major essential element and is required by plants for root development, cell 
division, flowering seed and fruit formation (Brady, 1984). Phosphorus in soils occurs in the form of primary and 
secondary orthophosphate. Most possibly all crops take up H2PO4 
- more readily than HPO4 
-- and above pH 7.0 
the relative concentration of the divalent ion is greater than that of monovalent ion. 
In Pakistan, farmers are using various phosphatic fertilizers such as single super phosphate, triple super 
phosphate, di-ammonium phosphate and nitro phosphate for getting the increase yield of various crops. On the 
other hand, excess and imbalance use of P-fertilizers may effect the solubility of micronutrients (Zn, B, Cu, Fe 
and Mn), which cause reduced crops yield. A number of field and green house experiments on the micronutrients 
status in soils and their response to various crops have indicated that some of the areas of Khyber Pakhtunkhwa 
are deficient in one or more trace elements (Khattak et al., 1983). The deficiency or unavailability of these 
micronutrients are probably the result of various factors, such as calcareous nature and alkaline reactions soils, 
introduction of high yielding varieties, heavy application of high grade fertilizers, low organic matter, and 
imbalance use of nutrient or excess of certain phosphatic fertilizers, which not only suppress the crops yield, but 
also reduced the availability of micronutrients, perhaps due to chemical or physiological interactions in soil-plant 
systems. However, these interactions are designated as phosphorus induced micronutrients disorders (Timmer 
and Teng, 1990), though phosphorus induced micronutrients deficiency is not common to all soils, crop species 
and environmental conditions, but it has been proved in various soils and crops (Haldar and Mandal, 1981; 
Badhe and Mundwaik, 1982; Cakmak and Marschner, 1987; Wang et al., 1990; Moustaoui et al., 1991; Ajouri et 
al., 2004; Stanislawska-Glubiak and Korzeniowska, 2005). 
So, it is evident from the literature that phosphorus interfere in the availability of micronutrients in soils 
and uptake by plants, but no detail study have been carried out to find out the balance application of various 
phosphate fertilizer on the availability of micronutrients in alkaline-calcareous soils. Therefore, the main aim of 
the present project is to investigate the relationship and availability of micronutrients with phosphorus in soil by 
applying phosphate fertilizer to soil with the following main objectives were to investigate the effect of applied 
phosphorus on the availability of micronutrients (Zn, Cu, Fe, Mn and B) in alkaline-calcareous soils. 
MATERIALS AND METHODS 
Experimental description 
A pot experiment was carried out in the laboratory of Soil and Environmental Sciences Department,
Journal of Environment and Earth Science www.iiste.org 
ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) 
Vol.4, No.15, 2014 
The University of Agriculture Peshawar Pakistan, with variable amounts of phosphorus, i.e. 0, 30, 60, 90, 120 
and 150 kg P ha-1 in the form of single super phosphate. The experiment was conducted in completely 
randomized block design with three replications consisted of 100 g of soil in each pot. The experiment was 
incubated for 28 days under normal conditions. The soil was kept moist up to field capacity condition throughout 
the incubation period. Before phosphorus fertilizer application the original soil sample was analyzed for various 
physico-chemical characteristics and the desired nutrients status by the routine standard procedures. 
144 
Soil analysis of incubated pots 
After termination of the experiment, soil from each incubated pot was collected and analyzed for pH in 
1:5 soil water suspension, the method as suggested by McLean (1982). AB-DTPA extractable P, Zn, Fe, Cu and 
Mn was determined by the procedure as described by Soltanpur and Schwab (1977) and the readings for P (after 
color development procedure) and Zn, Fe, Cu and Mn were taken on spectrophotometer and atomic absorption 
spectrophotometer, respectively. While, B in soil was extracted with hot water followed by Azomethine-H color 
development method as suggested by Bingham (1982). 
Statistical analysis 
Statistical analysis was performed by computer using MSTAT-C package. The collected data was 
analyzed using ANOVA and the means were compared by LSD-test of significance (Steel et al., 1997). 
RESULTS AND DISCUSSION 
Physico-chemical characteristic of experimental soil 
Before conducting the incubation experiment in the laboratory the experimental soil was analyzed for 
various physico-chemical characteristics and nutrient status (Table 1). Results showed that the experimental soil 
was silt loam in texture, alkaline in reaction, non-saline and calcareous in nature, low in organic matter, AB-DTPA 
extractable phosphorus, zinc and iron, while copper, manganese and HWS-boron, contents were adequate 
as reported the critical limits in soil for these nutrients by Soltanpur and Schwab (1977) and Sillanpaa (1982), 
respectively. 
Table 1: Physico-chemical characteristics of experimental soil 
Properties Units Values 
Sand % 33.4 
Silt % 58.2 
Clay % 8.40 
Textural class --- Silt loam 
PHs (1:5) --- 7.73 
ECs (1:5) dSm-1 0.33 
Organic matter % 0.65 
Lime % 11.50 
HWS-boron mg kg-1 0.70 
AB-DTPA extractable P mg kg-1 4.08 
AB-DTPA extractable Zn mg kg-1 1.05 
AB-DTPA extractable Cu mg kg-1 3.43 
AB-DTPA extractable Fe mg kg-1 2.78 
AB-DTPA extractable Mn mg kg-1 3.30 
Micronutrient concentrations of incubated soil 
Results of the incubated soil showed that as the phosphorus application increases the concentration of P 
in soil significantly increases in a linear fashion (Table 2). Although the P concentrations in some incubated 
treatments were still not reached to the sufficiency level with applied graded P, which indicate that the test soil 
was poor in available P (Soltanpour and Schwab, 1977), or may be due to the adsorption of phosphate ions in the 
soil due to alkaline reaction and calcareous nature of the incubated soil.
Journal of Environment and Earth Science www.iiste.org 
ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) 
Vol.4, No.15, 2014 
Table 2: Effect of phosphorus supply on the availability of micronutrients in soil 
145 
Applied P 
(kg ha-1) 
Concentration 
------------------------------------ mg kg-1----------------------------------- 
P B Zn Cu Fe Mn 
0 4.14 0.75 1.96 4.20 2.28 3.73 
30 4.24 0.77 1.55 3.89 2.44 4.20 
60 5.75 0.65 1.61 3.99 3.17 4.57 
90 7.65 0.55 1.32 3.79 3.06 4.50 
120 8.72 0.65 1.01 3.59 3.92 4.67 
150 9.91 0.53 1.02 3.25 3.46 4.71 
LSD (P<0.05) 1.72 NS NS NS NS NS 
CV % 14.00 19.58 29.29 17.78 26.21 24.52 
Results regarding the effect of phosphorus application on the availability of micronutrients showed non-significant 
differences but the trend of each micronutrient was obvious (Table 2). Boron showed a decreasing 
trend with applied phosphorus. The decreasing trend of B in soil seems to be due anion competition between P 
and B, which reduced the availability of B in soil. These results are in line with the previous work of Gunes and 
Alpaslan (2000) who reported that B was more toxic in the absence rather than the presence of P and this toxicity 
could be alleviated with the application of P in the calcareous soils of semi-arid areas. 
Micronutrients (cations) such as Zn and Cu also showed a decreasing trend with increasing the graded 
phosphorus application to soil (Table 2). This reduced availability due to interference of applied phosphorus is 
very common in soils. Perhaps due to the formation of insoluble forms of zinc and copper, such as Zn-phosphate 
and Cu-phosphate, respectively. Similar negative interactions between phosphorus and these micronutrients were 
reported by Mandal and Haldar (1980) they noted that applied phosphorus decreased the content of DTPA-extractable 
Zn and Cu in soils, the rate of decrease gradually declining with the progress of the incubation period. 
Rest of the micronutrients (cations) such as Fe and Mn showed an opposite trend with regard to applied 
phosphorus (Table 2). It is evident from the results as the applied phosphorus increases the concentrations of Fe 
and Mn also increased, perhaps due the positive interactions between applied phosphorus and these two 
micronutrients in the soil. Because increased applied phosphorus increased the extractable Fe and Mn and 
lowered the soil pH, causing these metals to be more soluble during incubation period. Similar results were 
reported by Shuman (1988). 
The overall results showed that as the application of phosphorus from single super phosphate increases, 
the soil pH gradually decreases (due to the acidic pH of the fertilizer) along the concentrations of B, Zn and Cu, 
which indicate negative interactions, while the concentrations of P, Fe and Mn increases may be due to positive 
interactions with applied phosphorus during incubation period. 
Soil pH of incubated soil 
Soil pH of the incubated soil was determined at the termination of experiment. Results showed as the 
graded applied P (from single super phosphate) increases the pH-values gradually decreases, which resulted 
significantly negative correlation with one another (Figure 1). However, statistical analysis showed that the 
differences in the pH-values among various treatments were not very large. These results indicate that with the 
application of P as single super phosphate reduced the pH of soil and has favorable effect on the solubility of 
micronutrients in the alkaline-calcareous soils.
Journal of Environment and Earth Science www.iiste.org 
ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) 
Vol.4, No.15, 2014 
y = -0.0166x + 7.7558 
R2 = 0.8265 
0 30 60 90 120 150 
Applied P kg ha-1 
Figure 1: Relationship between applied P and soil pH 
146 
Soil pH 
SUMMARY 
7.78 
7.71 
7.64 
7.57 
7.50 
An incubation experiment was conducted in the laboratory of Soil and Environmental Sciences 
Department, The University of Agriculture Peshawar Pakistan, with variable amounts of phosphorus, i.e. 0, 30, 
60, 90, 120 and 150 kg P ha-1 in the form of single super phosphate. The experiment was conducted in 
completely randomized block design with three replications consisted of 100 g of soil in each pot. The 
experiment was incubated for 28 days under normal conditions. The soil was kept moist up to field capacity 
condition throughout the incubation period. Before phosphorus fertilizer application the original soil sample was 
analyzed for the desired nutrients status and the results showed that AB-extractable P, Zn and Fe were low, while 
HWS-B, Cu and Mn were adequate. 
Results regarding applied phosphorus on the availability of micronutrients showed non-significant 
differences, but the trend of each micronutrient were obvious. Boron showed a decreasing trend with applied 
phosphorus. The decreasing trend of B in soil seems to be due to anion competition between P and B, which 
reduced the availability of B in soil. Micronutrients (cations) such as Zn and Cu also showed a decreasing trend 
with increasing the graded phosphorus application to soil. This reduced availability perhaps due to the formation 
of insoluble forms of zinc and copper, such as Zn-phosphate and Cu-phosphate, respectively. While, 
micronutrients (cations) such as Fe and Mn showed an opposite trend with regard to applied phosphorus. Results 
showed as the applied phosphorus increases the concentrations of Fe and Mn also increased, perhaps due the 
positive interactions. Because applied phosphorus increased the extractable Fe and Mn and lowered the soil pH, 
causing these metals to be more soluble during incubation period. 
The overall results showed that as the application of phosphorus from single super phosphate increases, 
the soil pH gradually decreases (due to the acidic pH of the fertilizer) along with the concentrations of B, Zn and 
Cu, which indicate negative interactions, while the concentrations of P, Fe and Mn increases may be due to 
positive interactions with applied phosphorus. 
CONCLUSIONS 
The following conclusions were drawn from the present piece of work 
i. The experimental soil was silt loam in texture, alkaline in reaction, non-saline and calcareous in 
nature, low in organic matter, AB-DTPA extractable phosphorus, zinc and iron, while copper, 
manganese and HWS-boron, contents were adequate compared with the reported critical limits in 
soil for these nutrients in the literature. 
ii. The overall results showed that as the application of phosphorus from single super phosphate 
increases, the soil pH gradually decreases (due to the acidic pH of the fertilizer) along with the 
concentrations of B, Zn and Cu, which indicate negative interactions, while the concentrations of P, 
Fe and Mn increases may be due to positive interactions with applied phosphorus during incubation
Journal of Environment and Earth Science www.iiste.org 
ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) 
Vol.4, No.15, 2014 
147 
period. 
iii. As the applied P (from single super phosphate) increases the pH-values gradually decreases, which 
resulted significantly negative correlation with one another (r2 = 0.83). These results indicate that 
with the application of P as single super phosphate reduced the pH of soil and has favorable effect 
on the solubility of micronutrients, specifically Fe and Mn in the alkaline-calcareous soils. 
iv. Further comprehensive studies are warranted to find out the effect of applied phosphorus on the 
availability of micronutrients on various soils under controlled conditions. 
LITERATURE CITED 
Ajouri, A., H. Asgedom and M. Becker. 2004. Seed priming enhances germination and seedling growth of barley 
under conditions of P and Zn deficiency. J. Plant Nutr. and Soil Sci. 167: 630-636. 
Badhe, N.N. and S.P. Mundwaik. 1982. Effect of phosphorus concentration on Fe, Zn, Cu and Mn utilization by 
sorghum and wheat. Ind. J. Agric. Univ. Maharashtra 7(2): 148-150. 
Bingham, F.T. 1982. Boron. p. 431-448. In: Methods of Soil Analysis Part-2 Chemical and mineralogical 
properties (A.L. Page (ed.), ASA, Madison, WI, USA. 
Brady, N.C. 1984. The nature and properties of soils, (9th Edition) Macmillan Publishing inc., New York, USA. 
Cakmak, I. and H. Marschner. 1987. Mechanism of phosphorus-induced zinc deficiency in cotton. III. Changes 
in physiological availability of zinc in plants. Physiologia Plantarum 70: 13-20. 
Gunes, A., and M. Alpaslan. 2000. Boron uptake and toxicity in maize genotypes in relation to boron phosphorus 
supply. J. plant Nutr. 23(4): 541-550. 
Haldar, M. and L.N. Mandal. 1981. Effect of phosphorus and zinc on the growth and phosphorus, zinc, copper, 
iron and manganese nutrition of rice. Plant Soil 59: 415-425. 
Isaac, R.A. and J.D. Kerber. 1971. Atomic absorption and flame photometery: techniques and uses in soil, plant 
and water analysis. In: Instrumental methods for analysis of soil and plant tissue. Walsh, L.M (Ed). Soil 
Sci. Soc. Am. Madison, USA. 
Khattak, J.K., S. Parveen and A.U. Bhatti. 1983. Micronutrient status of NWFP soils and their response to 
various crops. Bull. SS-1. Dep. of Soil Sci. NWFP Agric. Univ. Peshawar. 
Mandal, L.N. and M. Haldar. 1980. Influence of phosphorus and zinc application on the availability of zinc, 
copper, iron, manganese and phosphorus in waterlogged rice soil. Soil Sci. 139(5): 251-257. 
McLean, E.O. 1982. Soil pH and lime requirement. In: A.L. Page., R.H. Miller and D.R. Keeny, (ed). Methods 
of Soil Anal. Part-2 (2nd ed.). Am. Soc. Agron 9: 199-208. 
Moustaoui, D., M. Verloo and J. Pauvels. 1991. Contribution to the study of phosphorus-zinc interaction. 
Pedologie, 41(3): 251-261. 
Nelson, D.W. and L.E. Sommers. 1996. Total carbon, organic carbon and organic matter. In: Methods of Soil 
Analysis Part-3 (D.L. Sparks, ed) SSSA Book Series No. 5, SSSA, Inc: Madison, Wisconsin, USA. PP. 
961-1010. 
Rhoades, J.D. 1996. Salinity: Electrical Conductivity and total dissolved salts. In: D.L. Sparks (ed). Methods of 
Soil Anal. Part-3. Am. Soc. Agron. Inc. Madison WI USA. 14: 417-436. 
Shuman, L. M. 1988. Effect of phosphorus level on extractable micronutrients and their distribution among soil 
fractions. Soil Sci. Soc. Am. J. 52: 136-141 
Sillanpa, M. 1982. Micronutrient and nutrient status of soil. A global study, FAO Soil Bulleton No. 48: Rome. 
Soil and plant analysis council. 2004. Soil Analysis. Hand Book of Reference Methods, CRC press, USA. 
Soltanpur, P.N. and A.P. Schwab. 1977. A new soil test for simultaneous extraction of macro and micro nutrients 
in alkali soils. Comm. Soil Sci. and Plant Anal. 8: 195-207. 
Stanislawaska-Glubiak, E. and J. Korzeniowska. 2005. Effect of excessive zinc content in soil on the phosphorus 
content in wheat plants. Elect. J. Polish Agric. Univ. 8(4): 1-8. 
Steel, R.G.D., J.H. Torrie and D.A. Dicke. 1997. Principles and Procedures of Statistics. A biometrical approach 
3rd edition. The McGraw-Hill, componies, Inc, NY. USA. 
Timmer, V.R. and Y. Teng. 1990. Phosphorus-induced micronutrient disorders in hybrid popular. Responses to 
zinc and copper in greenhouse culture. Plant Soil 126(1): 31-39. 
Wang, H.X., J.L. Wu, T.J Zhang, O.X. Wu, Y. Chen, J.S. Bian and F. Shaan. 1990. Study on interaction between 
P and Zn and their influence on the growth of maize seedlings in calcareous soils. Act. Pedologica 
Sinica 27(3): 241-249.
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Effect of applied phosphorus on the availability of micronutrients in alkaline calcareous soil

  • 1. Journal of Environment and Earth Science www.iiste.org ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) Vol.4, No.15, 2014 Effect of Applied Phosphorus on the Availability of Micronutrients in Alkaline-Calcareous Soil Fayaz Ali1 Arooj Sadiq1 Irshad Ali1 Muhammad Amin2* Muhammad Amir3 1.Department of Soil and Environmental Sciences, The University of Agriculture Peshawar Pakistan 2.Department of Agricultural Chemistry, The University of Agriculture Peshawar Pakistan 3.Department of Plant Breeding and Genetics, The University of Agriculture Peshawar Pakistan *For Correspondence Email: agrian.amin06@gmail.com Abstract The present experiment was carried out to study the effect of applied phosphorus on the availability of micronutrients in alkaline-calcareous soil. For this purpose an incubation experiment was conducted in the laboratory of Soil and Environmental Sciences Department, The University of Agriculture Peshawar Pakistan during 2009 with variable amounts of phosphorus, i.e. 0, 30, 60, 90, 120 and 150 kg P ha-1 in the form of single super phosphate. The experiment was conducted in completely randomized block design with three replications consisted of 100 g of soil in each pot. The experiment was incubated for 28 days under normal conditions. The soil was kept moist up to field capacity condition throughout the incubation period. Results regarding the effect of phosphorus application on the availability of micronutrients showed non-significant differences in the treatments of applied phosphorus, but the trend of each micronutrient was obvious. The overall results showed that as the application of phosphorus increases, the concentrations of B, Zn and Cu gradually decreases, which indicate negative interactions, while the concentrations of P, Fe and Mn increases perhaps due to positive interactions with applied phosphorus during incubation period. Results further showed as the applied P (from single super phosphate) increases the pH-values gradually decreases, which resulted significantly negative correlation with one another (r2 = 0.83). These results indicate that with the application of P as single super phosphate reduced the pH of soil and has favorable effect on the solubility of micronutrients, specifically Fe and Mn in the alkaline-calcareous soils. Keywords: Phosphorus, Micronutrients availability 143 INTRODUCTION Phosphorus is the second major essential element and is required by plants for root development, cell division, flowering seed and fruit formation (Brady, 1984). Phosphorus in soils occurs in the form of primary and secondary orthophosphate. Most possibly all crops take up H2PO4 - more readily than HPO4 -- and above pH 7.0 the relative concentration of the divalent ion is greater than that of monovalent ion. In Pakistan, farmers are using various phosphatic fertilizers such as single super phosphate, triple super phosphate, di-ammonium phosphate and nitro phosphate for getting the increase yield of various crops. On the other hand, excess and imbalance use of P-fertilizers may effect the solubility of micronutrients (Zn, B, Cu, Fe and Mn), which cause reduced crops yield. A number of field and green house experiments on the micronutrients status in soils and their response to various crops have indicated that some of the areas of Khyber Pakhtunkhwa are deficient in one or more trace elements (Khattak et al., 1983). The deficiency or unavailability of these micronutrients are probably the result of various factors, such as calcareous nature and alkaline reactions soils, introduction of high yielding varieties, heavy application of high grade fertilizers, low organic matter, and imbalance use of nutrient or excess of certain phosphatic fertilizers, which not only suppress the crops yield, but also reduced the availability of micronutrients, perhaps due to chemical or physiological interactions in soil-plant systems. However, these interactions are designated as phosphorus induced micronutrients disorders (Timmer and Teng, 1990), though phosphorus induced micronutrients deficiency is not common to all soils, crop species and environmental conditions, but it has been proved in various soils and crops (Haldar and Mandal, 1981; Badhe and Mundwaik, 1982; Cakmak and Marschner, 1987; Wang et al., 1990; Moustaoui et al., 1991; Ajouri et al., 2004; Stanislawska-Glubiak and Korzeniowska, 2005). So, it is evident from the literature that phosphorus interfere in the availability of micronutrients in soils and uptake by plants, but no detail study have been carried out to find out the balance application of various phosphate fertilizer on the availability of micronutrients in alkaline-calcareous soils. Therefore, the main aim of the present project is to investigate the relationship and availability of micronutrients with phosphorus in soil by applying phosphate fertilizer to soil with the following main objectives were to investigate the effect of applied phosphorus on the availability of micronutrients (Zn, Cu, Fe, Mn and B) in alkaline-calcareous soils. MATERIALS AND METHODS Experimental description A pot experiment was carried out in the laboratory of Soil and Environmental Sciences Department,
  • 2. Journal of Environment and Earth Science www.iiste.org ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) Vol.4, No.15, 2014 The University of Agriculture Peshawar Pakistan, with variable amounts of phosphorus, i.e. 0, 30, 60, 90, 120 and 150 kg P ha-1 in the form of single super phosphate. The experiment was conducted in completely randomized block design with three replications consisted of 100 g of soil in each pot. The experiment was incubated for 28 days under normal conditions. The soil was kept moist up to field capacity condition throughout the incubation period. Before phosphorus fertilizer application the original soil sample was analyzed for various physico-chemical characteristics and the desired nutrients status by the routine standard procedures. 144 Soil analysis of incubated pots After termination of the experiment, soil from each incubated pot was collected and analyzed for pH in 1:5 soil water suspension, the method as suggested by McLean (1982). AB-DTPA extractable P, Zn, Fe, Cu and Mn was determined by the procedure as described by Soltanpur and Schwab (1977) and the readings for P (after color development procedure) and Zn, Fe, Cu and Mn were taken on spectrophotometer and atomic absorption spectrophotometer, respectively. While, B in soil was extracted with hot water followed by Azomethine-H color development method as suggested by Bingham (1982). Statistical analysis Statistical analysis was performed by computer using MSTAT-C package. The collected data was analyzed using ANOVA and the means were compared by LSD-test of significance (Steel et al., 1997). RESULTS AND DISCUSSION Physico-chemical characteristic of experimental soil Before conducting the incubation experiment in the laboratory the experimental soil was analyzed for various physico-chemical characteristics and nutrient status (Table 1). Results showed that the experimental soil was silt loam in texture, alkaline in reaction, non-saline and calcareous in nature, low in organic matter, AB-DTPA extractable phosphorus, zinc and iron, while copper, manganese and HWS-boron, contents were adequate as reported the critical limits in soil for these nutrients by Soltanpur and Schwab (1977) and Sillanpaa (1982), respectively. Table 1: Physico-chemical characteristics of experimental soil Properties Units Values Sand % 33.4 Silt % 58.2 Clay % 8.40 Textural class --- Silt loam PHs (1:5) --- 7.73 ECs (1:5) dSm-1 0.33 Organic matter % 0.65 Lime % 11.50 HWS-boron mg kg-1 0.70 AB-DTPA extractable P mg kg-1 4.08 AB-DTPA extractable Zn mg kg-1 1.05 AB-DTPA extractable Cu mg kg-1 3.43 AB-DTPA extractable Fe mg kg-1 2.78 AB-DTPA extractable Mn mg kg-1 3.30 Micronutrient concentrations of incubated soil Results of the incubated soil showed that as the phosphorus application increases the concentration of P in soil significantly increases in a linear fashion (Table 2). Although the P concentrations in some incubated treatments were still not reached to the sufficiency level with applied graded P, which indicate that the test soil was poor in available P (Soltanpour and Schwab, 1977), or may be due to the adsorption of phosphate ions in the soil due to alkaline reaction and calcareous nature of the incubated soil.
  • 3. Journal of Environment and Earth Science www.iiste.org ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) Vol.4, No.15, 2014 Table 2: Effect of phosphorus supply on the availability of micronutrients in soil 145 Applied P (kg ha-1) Concentration ------------------------------------ mg kg-1----------------------------------- P B Zn Cu Fe Mn 0 4.14 0.75 1.96 4.20 2.28 3.73 30 4.24 0.77 1.55 3.89 2.44 4.20 60 5.75 0.65 1.61 3.99 3.17 4.57 90 7.65 0.55 1.32 3.79 3.06 4.50 120 8.72 0.65 1.01 3.59 3.92 4.67 150 9.91 0.53 1.02 3.25 3.46 4.71 LSD (P<0.05) 1.72 NS NS NS NS NS CV % 14.00 19.58 29.29 17.78 26.21 24.52 Results regarding the effect of phosphorus application on the availability of micronutrients showed non-significant differences but the trend of each micronutrient was obvious (Table 2). Boron showed a decreasing trend with applied phosphorus. The decreasing trend of B in soil seems to be due anion competition between P and B, which reduced the availability of B in soil. These results are in line with the previous work of Gunes and Alpaslan (2000) who reported that B was more toxic in the absence rather than the presence of P and this toxicity could be alleviated with the application of P in the calcareous soils of semi-arid areas. Micronutrients (cations) such as Zn and Cu also showed a decreasing trend with increasing the graded phosphorus application to soil (Table 2). This reduced availability due to interference of applied phosphorus is very common in soils. Perhaps due to the formation of insoluble forms of zinc and copper, such as Zn-phosphate and Cu-phosphate, respectively. Similar negative interactions between phosphorus and these micronutrients were reported by Mandal and Haldar (1980) they noted that applied phosphorus decreased the content of DTPA-extractable Zn and Cu in soils, the rate of decrease gradually declining with the progress of the incubation period. Rest of the micronutrients (cations) such as Fe and Mn showed an opposite trend with regard to applied phosphorus (Table 2). It is evident from the results as the applied phosphorus increases the concentrations of Fe and Mn also increased, perhaps due the positive interactions between applied phosphorus and these two micronutrients in the soil. Because increased applied phosphorus increased the extractable Fe and Mn and lowered the soil pH, causing these metals to be more soluble during incubation period. Similar results were reported by Shuman (1988). The overall results showed that as the application of phosphorus from single super phosphate increases, the soil pH gradually decreases (due to the acidic pH of the fertilizer) along the concentrations of B, Zn and Cu, which indicate negative interactions, while the concentrations of P, Fe and Mn increases may be due to positive interactions with applied phosphorus during incubation period. Soil pH of incubated soil Soil pH of the incubated soil was determined at the termination of experiment. Results showed as the graded applied P (from single super phosphate) increases the pH-values gradually decreases, which resulted significantly negative correlation with one another (Figure 1). However, statistical analysis showed that the differences in the pH-values among various treatments were not very large. These results indicate that with the application of P as single super phosphate reduced the pH of soil and has favorable effect on the solubility of micronutrients in the alkaline-calcareous soils.
  • 4. Journal of Environment and Earth Science www.iiste.org ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) Vol.4, No.15, 2014 y = -0.0166x + 7.7558 R2 = 0.8265 0 30 60 90 120 150 Applied P kg ha-1 Figure 1: Relationship between applied P and soil pH 146 Soil pH SUMMARY 7.78 7.71 7.64 7.57 7.50 An incubation experiment was conducted in the laboratory of Soil and Environmental Sciences Department, The University of Agriculture Peshawar Pakistan, with variable amounts of phosphorus, i.e. 0, 30, 60, 90, 120 and 150 kg P ha-1 in the form of single super phosphate. The experiment was conducted in completely randomized block design with three replications consisted of 100 g of soil in each pot. The experiment was incubated for 28 days under normal conditions. The soil was kept moist up to field capacity condition throughout the incubation period. Before phosphorus fertilizer application the original soil sample was analyzed for the desired nutrients status and the results showed that AB-extractable P, Zn and Fe were low, while HWS-B, Cu and Mn were adequate. Results regarding applied phosphorus on the availability of micronutrients showed non-significant differences, but the trend of each micronutrient were obvious. Boron showed a decreasing trend with applied phosphorus. The decreasing trend of B in soil seems to be due to anion competition between P and B, which reduced the availability of B in soil. Micronutrients (cations) such as Zn and Cu also showed a decreasing trend with increasing the graded phosphorus application to soil. This reduced availability perhaps due to the formation of insoluble forms of zinc and copper, such as Zn-phosphate and Cu-phosphate, respectively. While, micronutrients (cations) such as Fe and Mn showed an opposite trend with regard to applied phosphorus. Results showed as the applied phosphorus increases the concentrations of Fe and Mn also increased, perhaps due the positive interactions. Because applied phosphorus increased the extractable Fe and Mn and lowered the soil pH, causing these metals to be more soluble during incubation period. The overall results showed that as the application of phosphorus from single super phosphate increases, the soil pH gradually decreases (due to the acidic pH of the fertilizer) along with the concentrations of B, Zn and Cu, which indicate negative interactions, while the concentrations of P, Fe and Mn increases may be due to positive interactions with applied phosphorus. CONCLUSIONS The following conclusions were drawn from the present piece of work i. The experimental soil was silt loam in texture, alkaline in reaction, non-saline and calcareous in nature, low in organic matter, AB-DTPA extractable phosphorus, zinc and iron, while copper, manganese and HWS-boron, contents were adequate compared with the reported critical limits in soil for these nutrients in the literature. ii. The overall results showed that as the application of phosphorus from single super phosphate increases, the soil pH gradually decreases (due to the acidic pH of the fertilizer) along with the concentrations of B, Zn and Cu, which indicate negative interactions, while the concentrations of P, Fe and Mn increases may be due to positive interactions with applied phosphorus during incubation
  • 5. Journal of Environment and Earth Science www.iiste.org ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) Vol.4, No.15, 2014 147 period. iii. As the applied P (from single super phosphate) increases the pH-values gradually decreases, which resulted significantly negative correlation with one another (r2 = 0.83). These results indicate that with the application of P as single super phosphate reduced the pH of soil and has favorable effect on the solubility of micronutrients, specifically Fe and Mn in the alkaline-calcareous soils. iv. Further comprehensive studies are warranted to find out the effect of applied phosphorus on the availability of micronutrients on various soils under controlled conditions. LITERATURE CITED Ajouri, A., H. Asgedom and M. Becker. 2004. Seed priming enhances germination and seedling growth of barley under conditions of P and Zn deficiency. J. Plant Nutr. and Soil Sci. 167: 630-636. Badhe, N.N. and S.P. Mundwaik. 1982. Effect of phosphorus concentration on Fe, Zn, Cu and Mn utilization by sorghum and wheat. Ind. J. Agric. Univ. Maharashtra 7(2): 148-150. Bingham, F.T. 1982. Boron. p. 431-448. In: Methods of Soil Analysis Part-2 Chemical and mineralogical properties (A.L. Page (ed.), ASA, Madison, WI, USA. Brady, N.C. 1984. The nature and properties of soils, (9th Edition) Macmillan Publishing inc., New York, USA. Cakmak, I. and H. Marschner. 1987. Mechanism of phosphorus-induced zinc deficiency in cotton. III. Changes in physiological availability of zinc in plants. Physiologia Plantarum 70: 13-20. Gunes, A., and M. Alpaslan. 2000. Boron uptake and toxicity in maize genotypes in relation to boron phosphorus supply. J. plant Nutr. 23(4): 541-550. Haldar, M. and L.N. Mandal. 1981. Effect of phosphorus and zinc on the growth and phosphorus, zinc, copper, iron and manganese nutrition of rice. Plant Soil 59: 415-425. Isaac, R.A. and J.D. Kerber. 1971. Atomic absorption and flame photometery: techniques and uses in soil, plant and water analysis. In: Instrumental methods for analysis of soil and plant tissue. Walsh, L.M (Ed). Soil Sci. Soc. Am. Madison, USA. Khattak, J.K., S. Parveen and A.U. Bhatti. 1983. Micronutrient status of NWFP soils and their response to various crops. Bull. SS-1. Dep. of Soil Sci. NWFP Agric. Univ. Peshawar. Mandal, L.N. and M. Haldar. 1980. Influence of phosphorus and zinc application on the availability of zinc, copper, iron, manganese and phosphorus in waterlogged rice soil. Soil Sci. 139(5): 251-257. McLean, E.O. 1982. Soil pH and lime requirement. In: A.L. Page., R.H. Miller and D.R. Keeny, (ed). Methods of Soil Anal. Part-2 (2nd ed.). Am. Soc. Agron 9: 199-208. Moustaoui, D., M. Verloo and J. Pauvels. 1991. Contribution to the study of phosphorus-zinc interaction. Pedologie, 41(3): 251-261. Nelson, D.W. and L.E. Sommers. 1996. Total carbon, organic carbon and organic matter. In: Methods of Soil Analysis Part-3 (D.L. Sparks, ed) SSSA Book Series No. 5, SSSA, Inc: Madison, Wisconsin, USA. PP. 961-1010. Rhoades, J.D. 1996. Salinity: Electrical Conductivity and total dissolved salts. In: D.L. Sparks (ed). Methods of Soil Anal. Part-3. Am. Soc. Agron. Inc. Madison WI USA. 14: 417-436. Shuman, L. M. 1988. Effect of phosphorus level on extractable micronutrients and their distribution among soil fractions. Soil Sci. Soc. Am. J. 52: 136-141 Sillanpa, M. 1982. Micronutrient and nutrient status of soil. A global study, FAO Soil Bulleton No. 48: Rome. Soil and plant analysis council. 2004. Soil Analysis. Hand Book of Reference Methods, CRC press, USA. Soltanpur, P.N. and A.P. Schwab. 1977. A new soil test for simultaneous extraction of macro and micro nutrients in alkali soils. Comm. Soil Sci. and Plant Anal. 8: 195-207. Stanislawaska-Glubiak, E. and J. Korzeniowska. 2005. Effect of excessive zinc content in soil on the phosphorus content in wheat plants. Elect. J. Polish Agric. Univ. 8(4): 1-8. Steel, R.G.D., J.H. Torrie and D.A. Dicke. 1997. Principles and Procedures of Statistics. A biometrical approach 3rd edition. The McGraw-Hill, componies, Inc, NY. USA. Timmer, V.R. and Y. Teng. 1990. Phosphorus-induced micronutrient disorders in hybrid popular. Responses to zinc and copper in greenhouse culture. Plant Soil 126(1): 31-39. Wang, H.X., J.L. Wu, T.J Zhang, O.X. Wu, Y. Chen, J.S. Bian and F. Shaan. 1990. Study on interaction between P and Zn and their influence on the growth of maize seedlings in calcareous soils. Act. Pedologica Sinica 27(3): 241-249.
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