Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Effect of different types and levels of phosphorous fertilizers on kinetics of phosphorous release in the soil

View through CrossRef
A field experiment was carried out in one of the fields of Diwaniya governorate for the agricultural season 2019 to study the effect of adding organic fertilizer and sources of phosphate fertilizer during the growth stages of the maize plant (Zea mays. L) and its reflectance on growth and productivity of the plant. The experiment was conducted according to the design of the (split-split plots and included two levels of the organic fertilizer(L1-L0) standing for (0- 1.5 tons) and three sources of the following fertilizers: Tri super phosphate TSP, DiAmmonium phosphate DAP and Urea UP) as add to control treatment (p0) symbolized by p1, p2, p3, respectively. The seeds of maize (Zea mays. L) Behoth 5018s cultivar were planted in a 25 kg/H range. The kinetics of phosphorous in the soil were studied. The phosphorus release rate was determined during the stages of plant growth, and the best equation in describing the mechanism of desorption in the stages of plant growth (25, 50, 75, 100 and 125 days). The results showed that all used equations (first-order, diffusion and Elovich) have described the mechanism of phosphorous release from a solid phase to the soil solution. All equations gave a highly significant correlation (r) between released phosphorous in the stages of Plant growth. The first-order equation surpassed other equations describing the mechanism of phosphorous release in the soil. The values of the coefficient of phosphorous release rate (KP) ranged between (0.0045 - 0.004 mg. p. kg-1 . Day-1 ) for the equation of first- -order, where the results showed that the linear relationship between the amount of released phosphorous as a function of time for the equation of first-order, is the best equation in describing the release, which indicates the interest in the amount and timing of addition of p fertilizers during the stages of plant growth, according to what was shown in the kinetic equations. Keywords: Phosphorous desorption, fertilizers, maize, kinetic equations, soil solution.
Title: Effect of different types and levels of phosphorous fertilizers on kinetics of phosphorous release in the soil
Description:
A field experiment was carried out in one of the fields of Diwaniya governorate for the agricultural season 2019 to study the effect of adding organic fertilizer and sources of phosphate fertilizer during the growth stages of the maize plant (Zea mays.
L) and its reflectance on growth and productivity of the plant.
The experiment was conducted according to the design of the (split-split plots and included two levels of the organic fertilizer(L1-L0) standing for (0- 1.
5 tons) and three sources of the following fertilizers: Tri super phosphate TSP, DiAmmonium phosphate DAP and Urea UP) as add to control treatment (p0) symbolized by p1, p2, p3, respectively.
The seeds of maize (Zea mays.
L) Behoth 5018s cultivar were planted in a 25 kg/H range.
The kinetics of phosphorous in the soil were studied.
The phosphorus release rate was determined during the stages of plant growth, and the best equation in describing the mechanism of desorption in the stages of plant growth (25, 50, 75, 100 and 125 days).
The results showed that all used equations (first-order, diffusion and Elovich) have described the mechanism of phosphorous release from a solid phase to the soil solution.
All equations gave a highly significant correlation (r) between released phosphorous in the stages of Plant growth.
The first-order equation surpassed other equations describing the mechanism of phosphorous release in the soil.
The values of the coefficient of phosphorous release rate (KP) ranged between (0.
0045 - 0.
004 mg.
p.
kg-1 .
Day-1 ) for the equation of first- -order, where the results showed that the linear relationship between the amount of released phosphorous as a function of time for the equation of first-order, is the best equation in describing the release, which indicates the interest in the amount and timing of addition of p fertilizers during the stages of plant growth, according to what was shown in the kinetic equations.
Keywords: Phosphorous desorption, fertilizers, maize, kinetic equations, soil solution.

Related Results

Ecological soil physics as section of ecological soil science
Ecological soil physics as section of ecological soil science
Nowadays, there is a general penetration of ecology in other related sciences. Soil science is not an exception. To the evidence of this, the works of soil scientists may serve, th...
SOIL TEXTURE AND FERTILIZERS AFFECT NUTRIENT LEACHING
SOIL TEXTURE AND FERTILIZERS AFFECT NUTRIENT LEACHING
Fertilizer applications are essential for agricultural productivity, but proper management is required to prevent nutrient leaching. This study evaluated potassium and phosphorus m...
Composting for Feedlot Manure Management and Soil Quality
Composting for Feedlot Manure Management and Soil Quality
Contemporary industrialized grain and livestock production is Characterized by efficient, large‐scale confined animal feedlot operations (CAFOs) and equally efficient and large‐sca...
Soil-Available Nutrients Associated with Soil Chemical and Aggregate Properties following Vegetation Restoration in Western Sichuan, China
Soil-Available Nutrients Associated with Soil Chemical and Aggregate Properties following Vegetation Restoration in Western Sichuan, China
The status and drivers of soil-available nutrients in plant-recovered soils are not fully understood, limiting our ability to explore the role of soil-available nutrients in soil g...
Developed and Evaluation of Slow Release Phosphorus Fertilizer Using Mono-ammonium Phosphate and Di-ammonium Phosphate
Developed and Evaluation of Slow Release Phosphorus Fertilizer Using Mono-ammonium Phosphate and Di-ammonium Phosphate
Phosphorus (P) availability is generally low in Calcareous soils due to its association with soil constituents forming other P compounds that are of low solubility and availability...

Back to Top