Effects of Freezing and Thawing on Soil Phosphorus of Protective Farmland

2013 ◽  
Vol 726-731 ◽  
pp. 1309-1313
Author(s):  
Yun Jiang Liang ◽  
Min Jie Fu ◽  
Huan Liu ◽  
Guang Bo Xu
Keyword(s):  
Phosphorus Content ◽  
Chemical Properties ◽  
Water Soluble ◽  
Available P ◽  
Available Phosphorus ◽  
Content Increase ◽  
Freezing And Thawing ◽  
Thaw Cycle ◽  
P Content ◽  
Low Strength

Freezing and thawing of soil is an abiotic stress, and has direct effect on chemical properties, physical properties and biological properties. In order to research effect of freezing and thawing on soil chemical properties, experiments of freeze-thaw cycle were simulated, and different forms phosphorus was measured. Results show that freezing and thawing made water-soluble and loosely combined phosphorus content decrease, but made calcium P content increase. Low-strength freezing and thawing cycle made aluminum P content increase, but made iron P content decrease. To soil of low accumulation phosphorus, low-strength freezing and thawing made occluded P content decrease and be released, but high-strength freezing and thawing made occluded P content increase. Inorganic phosphorus content had an ascending trend with enhancing of freezing and thawing, but organic phosphorus content had a descending trend. Under low-strength freezing and thawing, available P content of soil of low accumulation phosphorus had an ascending trend, and available P content of soil of high accumulation phosphorus had a descending trend, but available phosphorus content had no great changes when strength of freezing and thawing continued to increase.

scholarly journals Changes of soil bioavailable phosphorus content in the long-term field fertilizing experiment

2019 ◽  
Vol 14 (No. 4) ◽  
pp. 240-245 ◽  
Author(s):  
Martin Kulhánek ◽  
Jindřich Černý ◽  
Jiří Balík ◽  
Ondřej Sedlář ◽  
Filip Vašák
Keyword(s):  
Field Experiments ◽  
Phosphorus Content ◽  
Spring Barley ◽  
Farmyard Manure ◽  
Mineral Nitrogen ◽  
Available P ◽  
Content Increase ◽  
Bioavailable Phosphorus ◽  
P Content

The aim of this study is to describe the changes of bioavailable phosphorus content in soil in long-term 18 years field experiments with different fertilizing systems. The field experiments are located at three sites with different soil and climatic conditions in the Czech Republic (Červený Újezd, Humpolec and Prague-Suchdol). Same fertilizing systems and crop rotation (potatoes (maize) – winter wheat – spring barley) are realized at each site with following fertilizing treatments: (1) unfertilized treatment (control), (2) farmyard manure (FYM), (3) and (4) sewage sludge (SS 1 and SS 3), (5) mineral nitrogen (N), (6) mineral nitrogen with straw (N + straw) and (7) mineral nitrogen with phosphorus and potassium (NPK). The long-term fertilizing effect on available P content changes in soil was observed. Bioavailable phosphorus content in soil increased in treatments with organic fertilization after 18 year experiment at all sites. The treatments SS 3 had the highest increase at all sites. The highest bioavailable P content increase compared to control (258 mg/kg) was determined at site Červený Újezd. On the contrary, available phosphorus content decreased at treatments with mineral fertilization and control treatment among all sites. Bioavailable P content decrease in the treatment NPK was observed, although phosphorus was applied. The lowest differences in available P content among all fertilizing treatments were observed at the location Prague-Suchdol.  

Effect of Soil Available Phosphorus Levels on Chickpea (Cicer arietinum L.) - Rhizobia Symbiotic Association

2020 ◽  
Author(s):  
Khadraji Ahmed ◽  
Bouhadi Mohamed ◽  
Ghoulam Cherk
Keyword(s):  
Cicer Arietinum ◽  
Available P ◽  
Phosphorus Concentration ◽  
Available Phosphorus ◽  
Symbiotic Association ◽  
P Deficiency ◽  
Soil P ◽  
P Content ◽  
Nodule Biomass ◽  
Soil Available P

Background: Growing chickpea (Cicer arietinum) plants is affected by several environmental constraints as osmotic stress and nutrients deficiency particularly phosphorus (P). For other legume species, it was confirmed that P deficiency affects negatively their rhizobial symbiosis. The purpose of this study was to assess the effect of soil available P level on chickpea-rhizobia symbiosis under field conditions at Oualidia region of Morocco. Methods: Ten farmers’ fields with different soil available P levels were considered to carry out this study based on samples of 10 plants per plot. Result: The results showed that the plants from soil 7, with the lowest pH and the highest available P level (23.52ppm), presented high shoot dry weight (38.3 g/plant). Meanwhile the soil 5 with the lowest available P content showed low plant growth. The shoot P content was positively linked to soil P level but nodule biomass showed an irregular variation with soil available P level. Furthermore, it was confirmed that adequate plant P nutrition results in high chickpea yield and it was the case for plants from soil 7 presenting a mean yield of 62 seeds per plant). Finally, strong correlation was noted between yield and phosphorus concentration in soil (r=0.94).

scholarly journals Does thermal carbonization (Biochar) of organic material increase more merits for their amendments of sandy soil?

2014 ◽  
Vol 6 (1) ◽  
pp. 535-558 ◽  
Author(s):  
Y. Wu ◽  
G. Xu ◽  
J. N. Sun ◽  
H. B. Shao
Keyword(s):  
Soil Ph ◽  
Saline Soil ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Low Fertility ◽  
Available P ◽  
Available Phosphorus ◽  
Furfural Residue ◽  
Leaching Solution ◽  
Physical And Chemical

Abstract. Organic materials (e.g. furfural residue) are generally believed to improve the physical and chemical properties of the soils with low fertility. Recently, biochar have been received more attention as a possible measure to improve the carbon balance and improve soil quality in some degraded soils. However, little is known about their different amelioration of a sandy saline soil. In this study, 56d incubation experiment was conducted to evaluate the influence of furfural and its biochar on the properties of saline soil. The results showed that both furfural and biochar greatly reduced pH, increased soil organic carbon (SOC) content and cation exchange capacity (CEC), and enhanced the available phosphorus (P) in the soil. Furfural is more efficient than biochar in reducing pH: 5% furfural lowered the soil pH by 0.5–0.8 (soil pH: 8.3–8.6), while 5% biochar decreased by 0.25–0.4 due to the loss of acidity in pyrolysis process. With respect to available P, 5% of the furfural addition increased available P content by 4–6 times in comparison to 2–5 times with biochar application. In reducing soil exchangeable sodium percentage (ESP), biochar is slightly superior to furfural because soil ESP reduced by 51% and 43% with 5% furfural and 5% biochar addition at the end of incubation. In addition, no significant differences were observed between furfural and biochar about their capacity to retain N, P in leaching solution and to increase CEC in soil. These facts may be caused by the relatively short incubation time. In general, furfural and biochar have different amendments depending on soil properties: furfural was more effectively to decrease pH and to increase available P, whereas biochar played a more important role in increasing SOC and reducing ESP of saline soil.

scholarly journals Dietary Available Phosphorus Affected Growth Performance, Body Composition, and Hepatic Antioxidant Property of Juvenile Yellow CatfishPelteobagrus fulvidraco

2012 ◽  
Vol 2012 ◽  
pp. 1-9 ◽  
Author(s):  
Qin Tang ◽  
Chunfang Wang ◽  
Congxin Xie ◽  
Jiali Jin ◽  
Yanqing Huang
Keyword(s):  
Body Composition ◽  
Growth Performance ◽  
Lipid Content ◽  
Antioxidant Property ◽  
Available P ◽  
Available Phosphorus ◽  
Body Lipid ◽  
Yellow Catfish ◽  
P Content ◽  
P Utilization

An 8-week feeding trial was carried out with juvenile yellow catfish to study the effects of dietary available phosphorus (P) on growth performance, body composition, and hepatic antioxidant property. Six pellet diets were formulated to contain graded available P levels at 0.33, 0.56, 0.81, 1.15, 1.31, and 1.57% of dry matter, respectively. Triplicate tanks with each tank containing 60 juveniles (3.09 ± 0.03 g) were fed one of the six experimental diets for 8 weeks. Specific growth rate, feeding rate, and protein efficiency ratio were significantly higher at 0.81% dietary available P. Efficiency of P utilization distinctly decreased with increasing P level. Body lipid content significantly decreased while body ash and feces P content significantly increased with increasing P level. Quadratic regression analysis indicated that vertebrae P content was maximized at 1.21% dietary available P. Fish fed 1.57% dietary available P had highest activity of hepatic superoxide dismutase and catalase and malonaldehyde content. In conclusion, decreasing dietary available P increased P utilization efficiency and body lipid content while decreased vertebrae P content. Juvenile yellow catfish were subjected to oxidative damage under the condition of high dietary P content (1.57%), and the damage could not be eradicated by their own antioxidant defense system.

INORGANIC PHOSPHORUS FORMS IN SOME ALBERTA SOILS AS RELATED TO SOIL DEVELOPMENT, PARENT MATERIAL AND AVAILABLE PHOSPHORUS

1968 ◽  
Vol 48 (3) ◽  
pp. 289-295 ◽  
Author(s):  
T. G. Alexander ◽  
J. A. Robertson
Keyword(s):  
Inorganic Phosphorus ◽  
Soil Development ◽  
Parent Material ◽  
Available P ◽  
Available Phosphorus ◽  
Inorganic P ◽  
Podzolic Soils ◽  
Phosphorus Forms ◽  
P Content ◽  
Close Relationship

Inorganic P forms in 18 profiles representing five great groups of Alberta soils were determined by the modified Chang and Jackson procedure. Ca-P is dominant in the Chernozemic Brown and Black soils and in the C horizons containing CaCO3, while Fe-P and Al-P or Occl-P are the main forms in the Podzolic soils. Three series high in available P contain appreciable amounts of Al-P and Fe-P in their surface horizons. The organic P content is relatively high in the soils exhibiting the least pedogenic development.With increasing degree of soil development, Fe-P and Occl-P tend to increase. However, parent materials have a marked influence on the distribution of inorganic P forms and a close relationship between soil development and distribution of inorganic P forms does not appear to exist in these soils. The Al-P and Fe-P forms seem to be the major sources of available P in the soils studied.

Effects of acid treatment and composting on bones used as fertilizer

2007 ◽  
Vol 55 (1) ◽  
pp. 115-123
Author(s):  
D. Kovács ◽  
G. Kardos ◽  
G. Füleky
Keyword(s):  
Sulphuric Acid ◽  
Acid Treatment ◽  
Phosphorus Content ◽  
Phosphorus Uptake ◽  
Water Soluble ◽  
Available Phosphorus ◽  
Treatment Conditions ◽  
Bone Powder ◽  
Bone Water ◽  
Different Temperatures

The aim of the work was to analyse the compostable properties of bone powder produced via different treatment methods and industrial conditions, and to study their effect on plant growth and phosphorus uptake. The bones were treated in water with different temperatures, bone-water ratios and treatment times. Further treatment was carried out with citric, nitric and sulphuric acid with different concentrations, temperatures, bone-water ratios and treatment times. Industrial bone powder was composted under model industrial conditions.The available phosphorus content of these materials was estimated using ryegrass ( Lolium perenne ) as indicator plant in a climatic chamber.The water-soluble phosphorus content of the bones increased in the citric acid and sulphuric acid treatment, depending on the water treatment conditions and the acid concentration. This increase amounted to about 30 times (0.32–8.51 mg/100 mg) compared to the water treatment.The results of the plant test demonstrated that the phophorus content of treated bone powder and compost was readily available to plants. The phosphorus content of the compost was available over a longer period.

scholarly journals Changes in Soil Available Phosphorus, Leaf Phosphorus Content and Yield of Sword Bean (Canavalia ensiformis (L.) DC.) by Application of SP-36 and Phosphate Rock on Acid Upland Soil of East Lampung

2016 ◽  
Vol 20 (1) ◽  
pp. 29
Author(s):  
Achmad Arivin Rivaie
Keyword(s):  
Soil Ph ◽  
Phosphate Rock ◽  
Phosphorus Content ◽  
Available P ◽  
Available Phosphorus ◽  
Upland Soil ◽  
Canavalia Ensiformis ◽  
Soil Available Phosphorus ◽  
P Fertilizer ◽  
Total P

A glasshouse trial was performed to determine changes in phosphorus (P) nutrition and the yield of sword bean (Canavalia ensiformis (L.) DC.) following the application of different rates and types of P fertilizer in an acid upland soil of East Lampung. Two different types of P fertilizer, namely SP-36 (total P = 36%) and Phosphate Rock (PR) (total P = 24.3%, particle size distribution = 75% <0.25 mm, 85% < 0.50 mm, 90% < 1.00 mm) were used in the trial. For the treatment, each P fertilizer type consisted of four rates (0, 50, 100 and 150 mg P2O5 kg-1 soil) that were arranged in a Completely Randomized Design with four replications. The results showed that the application of P fertilizers had significant effects on soil pH, soil plant-available P, the potential-P (HCl 25%), leaf N and P concentrations, the yield of sword bean. Increased rates of both forms of P fertilizer increased the soil pH values. As the soil used had low pH and very high exchangeable Al, hence, this result is most probably related to the addition of Ca2+ to the soil solution that resulted from the P fertiliser applied (liming effect), either from SP-36 (monocalcium phosphate) or PR (flour apatite). There was no difference in soil available P concentration due to the different in P fertilizer types, indicating that 4 months after the fertilizer application, the relatively insoluble Phosphate Rock had the same P solubility with SP-36. Increased rates of both forms of P fertilizer increased the sword bean yield. For the application of 0 kg P2O5 ha-1, although sword bean crops had pods, but, they did not give any seed. Whereas, at the addition of P fertilizer at the rate of 50, 100, and 150 kg P2O5 ha-1 for both P fertilizer types, the crops were able to give the seeds in the pods. [How to Cite: Achmad AR. 2015. Changes in Soil Available Phosphorus, Leaf Phosphorus Content and Yield of Sword Bean (Canavalia ensiformis (L.) DC.) by Application of SP-36 and Phosphate Rock on Acid Upland Soil of East Lampung. J Trop Soils 19: 29-36. Doi: 10.5400/jts.2015.20.1.29][Permalink/DOI: www.dx.doi.org/10.5400/jts.2015.20.1.29]

Interactions of phosphorus content and phytase inclusion in diets for growing pigs: Digestibility and P utilisation

1999 ◽  
Vol 1999 ◽  
pp. 167-167
Author(s):  
K.J. McCracken ◽  
V.E. Beattie ◽  
R.N. Weatherup ◽  
R. W. Henry ◽  
S. Smyth
Keyword(s):  
Bone Strength ◽  
Phosphorus Content ◽  
Growing Pigs ◽  
Available P ◽  
Weaned Pigs ◽  
P Content ◽  
Phosphorus Requirements ◽  
Utilisation Data ◽  
The Impact

There is considerable literature on phosphorus requirements of pigs and on the use of phytase to improve phosphorus digestibility and reduce P excretion. However, much of this has been concentrated on weaned pigs (eg Beers and Jongbloed, 1992), the finishing stage (eg Russoet al, 1995) or the diets used were synthetic (eg Ketarenet al, 1993). The available P requirement for pigs between 20-50 kg was estimated at 3 g/kg by ARC (1981) but the NRC (1998) estimate is 2.3 g/kg. This paper reports digestibility and P utilisation data on 40 kg pigs using the grower diets employed in a study on the impact of commercially feasible reductions in dietary P content and of phytase inclusion on growth and bone strength (Weatherupet al, 1999).

scholarly journals Furfural and its biochar improve the general properties of a saline soil

Solid Earth ◽  
2014 ◽  
Vol 5 (2) ◽  
pp. 665-671 ◽  
Author(s):  
Y. Wu ◽  
G. Xu ◽  
H. B. Shao
Keyword(s):  
Soil Ph ◽  
Saline Soil ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Low Fertility ◽  
Available P ◽  
Available Phosphorus ◽  
Leaching Solution ◽  
Decreasing Ph ◽  
Physical And Chemical

Abstract. Organic materials (e.g., furfural residue) are generally believed to improve the physical and chemical properties of saline soils with low fertility. Recently, biochar has been received more attention as a possible measure to improve the carbon balance and improve soil quality in some degraded soils. However, little is known about their different amelioration of a sandy saline soil. In this study, 56 d incubation experiment was conducted to evaluate the influence of furfural and its biochar on the properties of saline soil. The results showed that both furfural and biochar greatly reduced pH, increased soil organic carbon (SOC) content and cation exchange capacity (CEC), and enhanced the available phosphorus (P) in the soil. Furfural is more efficient than biochar in reducing pH: 5% furfural lowered the soil pH by 0.5–0.8 (soil pH: 8.3–8.6), while 5% biochar decreased by 0.25–0.4 due to the loss of acidity in pyrolysis process. With respect to available P, furfural addition at a rate of 5% increased available P content by 4–6 times in comparison to 2–5 times with biochar application. In reducing soil exchangeable sodium percentage (ESP), biochar is slightly superior to furfural because soil ESP reduced by 51% and 43% with 5% furfural and 5% biochar at the end of incubation. In addition, no significant differences were observed between furfural and biochar about their capacity to retain N, P in leaching solution and to increase CEC in soil. These facts may be caused by the relatively short incubation time. In general, furfural and biochar exhibited a different effect depending on the property: furfural was more effective in decreasing pH and increasing available P, whereas biochar played a more important role in increasing SOC and reducing ESP of saline soil.

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