Relationship between phosphorus fractions and properties of highly calcareous soils

Soil Research ◽  
2007 ◽  
Vol 45 (4) ◽  
pp. 255 ◽  
Author(s):  
Ebrahim Adhami ◽  
Hamid Reza Memarian ◽  
Farzad Rassaei ◽  
Ehsan Mahdavi ◽  
Manouchehr Maftoun ◽  
...  
Keyword(s):  
Calcareous Soils ◽  
Hydroxylamine Hydrochloride ◽  
Inorganic Phosphorus ◽  
Influential Factor ◽  
Sequential Fractionation ◽  
Inorganic P ◽  
Soil P ◽  
Fractionation Procedure ◽  
Extractable P ◽  
P Content

Inorganic phosphorus (P) sequential fractionation schemes are applicable techniques to interpret soil P status. The present study was initiated to determine the origin of various P fractions in highly calcareous soils. Inorganic P forms were determined by a sequential fractionation procedure extracting with NaOH (NaOH-P), Na citrate-bicarbonate (CB-P), Na citrate 2 times (C1-P and C2-P), Na citrate-ascorbate (CAs-P), Na citrate-bicarbonate-dithionite (CBD-P), Na acetate (NaAc-P), and HCl (HCl-P). Results showed that NaOH-P was negatively correlated with active iron oxides. CB-P was positively correlated with silt content and negatively related to citrate-bicarbonate-dithionite extractable Fe (Fed). This result illustrates the weathering effect on Ca-P, with Ca-P content declining as a consequence of weathering. A negative correlation was observed between C1-P and citrate ascorbate extractable Fe (FeCAs). Second citrate extractable P (C2-P) was negatively related to calcium carbonate equivalent and positively related to hydroxylamine-hydrochloride and neutral ammonium acetate-hydroquinone extractable Mn (Mnh and Mnq). Fine silt (Fsilt) was the most influential factor affecting CAs-P. It seemed citrate-dithionite-bicarbonate extractable Al (Ald), Mnh, and Mnq have been sinks for CBD-P, while free iron oxide compounds (Feo, Fec, and FeCAs) were a major contributing factor for the formation of NaAc-P. Stable P compounds (HCl-P) of highly calcareous soils originated from coarse silt (Csilt) and hydroxylamine-hydrochloride extractable Mn (Mnh).

Phosphorus solubility in Manitoba soils treated with pig manure from phytase supplemented diets

2011 ◽  
Vol 91 (6) ◽  
pp. 947-955 ◽  
Author(s):  
D. V. Ige ◽  
O. S. Abioye ◽  
O. O. Akinremi ◽  
C. M. Nyachoti ◽  
D. N. Flaten
Keyword(s):  
Calcareous Soils ◽  
Complete Removal ◽  
Land Application ◽  
Pig Manure ◽  
Inorganic P ◽  
Soil P ◽  
Extractable P ◽  
P Content ◽  
Total Elimination ◽  
Phosphorus Solubility

Ige, D. V., Abioye, O. S., Akinremi, O. O., Nyachoti, C. M. and Flaten, D. N. 2011. Phosphorus solubility in Manitoba soils treated with pig manure from phytase supplemented diets. Can. J. Soil Sci. 91: 947–955. Phytase supplementation has been shown to reduce manure P content. However, this manipulation can influence manure P solubility upon land application. Therefore, the objectives of this study were to investigate the solubility of P in soils amended with manure from diets with reduced or no inorganic P supplement with and without phytase addition and to evaluate the influence of soil type on the solubility of manure P from phytase supplemented pig diets. Two calcareous and two non-calcareous Manitoba soils were amended with manure produced by pigs that were fed with diets containing different levels of supplemental inorganic P with and without phytase. Manure was applied at the rate of 75 kg P ha−1and the amended soils were incubated for 1, 4 and 16 wk. Soil P was extracted with water (H2O-P), Olsen (Ols-P) and Mehlich-3 (M3-P) solutions. Manure application mostly increased H2O-P above the control. Complete removal of supplemental inorganic P from the diet irrespective of phytase addition significantly increased M3-P (P<0.05) in the two calcareous soils during the 16-week incubation. Similarly, when no supplemental inorganic P was included in the diet, Ols-P was increased in the fine textured, calcareous soil at 16th week of incubation. Thus, the complete removal of inorganic P from pig diet has potential to increase P solubility in some soils. Addition of phytase to pig diet did not have consistent effects on the soil extractable P in these soils. Soil factor had the greatest influence (77 to 94%) on P solubility. Our results showed that while phytase supplementation with concurrent reduction in inorganic P will reduce manure P with no adverse effect on P solubility in soils, total elimination of dietary inorganic P through the use of greater rate of phytase may not be feasible as this has the potential to increase P solubility in some soils.

SORPTION OF CARBON AND PHOSPHORUS FROM LIQUID POULTRY MANURE BY SOIL AGGREGATES OF DIFFERING SIZE

1985 ◽  
Vol 65 (3) ◽  
pp. 467-473 ◽  
Author(s):  
V. K. BHATNAGAR ◽  
M. H. MILLER
Keyword(s):  
Soil Aggregates ◽  
Poultry Manure ◽  
Aggregate Size ◽  
Liquid Manure ◽  
Inorganic P ◽  
Supernatant Liquid ◽  
Extractable P ◽  
P Content ◽  
Manure Slurry ◽  
Total P

A series of laboratory experiments was conducted to determine the mechanism(s) responsible for a previously reported observation that addition of liquid manure to soil increased the NaHCO3-extractable P (Ext-P) of large aggregates (> 2 mm) more than that of smaller aggregates whereas addition of an inorganic P solution did not. Application of liquid poultry manure increased the total P, Ext-P and total C concentrations in large aggregates (> 2 mm) much more (> 2.5 ×) than that in small aggregates (< 1 mm). Addition of inorganic P solution or of supernatant liquid from a centrifuged manure slurry increased the P content of the large aggregates only slightly (1.2 ×). A greater increase in Ext-P in large aggregates was observed even when the smaller aggregates were purposely layered on top of the larger ones prior to addition of the liquid manure. A similar but less pronounced effect of aggregate size on increase in P or C concentration was observed when different sized aggregates were left in contact with an effectively infinite source of liquid manure for 24 h. It is concluded that the larger aggregates absorbed more of the bulk manure slurry than smaller aggregates. A partial sealing of small aggregates by particulates is suggested as a possible mechanism. Key words: Carbon, phosphorus, liquid manure, soil aggregates

Soil phosphorus depletion capacity of arbuscular mycorrhizae formed by maize hybrids

2003 ◽  
Vol 83 (4) ◽  
pp. 337-342 ◽  
Author(s):  
A. Liu ◽  
C. Hamel ◽  
S. H. Begna ◽  
B. L. Ma ◽  
D. L. Smith
Keyword(s):  
Plant Biomass ◽  
Arbuscular Mycorrhizal ◽  
Am Fungi ◽  
P Uptake ◽  
Maize Hybrids ◽  
Soil P ◽  
Extractable P ◽  
P Content ◽  
Total P ◽  
Extractable Soil

The ability of arbuscular mycorrhizal (AM) fungi to help their host plant absorb soil P is well known, but little attention has been paid to the effect of AM fungi on soil P depletion capacity. A greenhouse experiment was conducted to assess, under different P levels, the effects of mycorrhizae on extractable soil P and P uptake by maize hybrids with contrasting phenotypes. The experiment had three factors, including two mycorrhizal treatments (mycorrhizal and non-mycorrhizal), three P fertilizer rates (0, 40, and 80 mg kg-1) and three maize hybrids [leafy normal stature (LNS), leafy reduced stature (LRS) and a conventional hybrid, Pioneer 3979 (P3979)]. Extractable soil P was determined after 3, 6 and 9 wk of maize growth. Plant biomass, P concentration and total P content were also determined after 9 wk of growth. Fertilization increased soil extractable P, plant biomass, P concentration in plants and total P uptake. In contrast to P3979, the LNS and LRS hybrids had higher biomass and total P content when mycorrhizal. Mycorrhizae had less influence on soil extractable P than on total P uptake by plants. The absence of P fertilization increased the importance of AM fungi for P uptake, which markedly reduced soil extractable P under AM plants during growth. This effect was strongest for LNS, the most mycorrhizae-dependent hybrid, intermediate for LRS, and not significant for the commercial hybrid P3979, which did not respond to AM inoculation. Key words: Arbuscular mycorrhizal fungi, extraradical hyphae, maize hybrid,plant biomass, P uptake, soil extractable P

scholarly journals Phosphorus leaching in sandy soils .II. Laboratory studies of the long-term effects of the phosphorus source

Soil Research ◽  
1988 ◽  
Vol 26 (1) ◽  
pp. 191 ◽  
Author(s):  
DM Weaver ◽  
GSP Ritchie ◽  
GC Anderson
Keyword(s):  
Sandy Soils ◽  
Summer Rainfall ◽  
Weather Conditions ◽  
Application Rate ◽  
Long Term Effects ◽  
Sequential Fractionation ◽  
Inorganic P ◽  
Coastal Superphosphate ◽  
Extractable P

Long-term phosphorus (P) losses and gains in sandy soils continuously fertilized with either ordinary superphosphate or coastal superphosphate (a granulated mixture of superphosphate, rock phosphate and elemental sulfur) or previously fertilized with superphosphate were investigated under leaching conditions in columns in the laboratory. The soils were subjected to 10 consecutive cycles designed to simulate the mediterranean weather conditions in the Harvey region of the Coastal Plain of Western Australia. Each cycle consisted of a wet phase during which the equivalent of 850 mm of rainfall was leached through the soil and a drier phase during which the soil was incubated in the presence of moisture equivalent to summer rainfall (150 mm). Dissolved inorganic P in the leachate was used as a measure of P loss. A sequential fractionation procedure (a resin extraction followed by 0.5 M sodium bicarbonate, 0.1 M sodium hydroxide and 0.1 M sulfuric acid extractions) and total inorganic and organic P were used to measure changes in P levels in the soils. Phosphorus losses from the previously fertilized soils decreased logarithmically with increasing number of cycles. Total inorganic P and resin-extractable P were able to explain >94% of the variation in P losses. Addition of either fertilizer increased the amount of P leached from the soil and 10-40% more P was leached by adding superphosphate rather than coastal superphosphate. The percentage of the cumulative P lost by leaching decreased with increasing application rate of both fertilizers when expressed as a percentage of the cumulative water plus citrate-soluble P added. Addition of either fertilizer increased the amount of acid-extractable P, but coastal superphosphate had a much greater effect than superphosphate. Leaching losses of P were influenced by fertilizer solubility in the short term (< 1 year). In the long term, however, the water plus citrate-insoluble P in the fertilizers also contributed to P losses by leaching.

ORGANIC AND INORGANIC P CONTENT, MOVEMENT AND MINERALIZATION OF P IN SOIL BENEATH A FEEDLOT

1975 ◽  
Vol 55 (4) ◽  
pp. 457-466 ◽  
Author(s):  
L. B. CAMPBELL ◽  
G. J. RACZ
Keyword(s):  
Field Capacity ◽  
Organic P ◽  
Field Soil ◽  
Inorganic P ◽  
Sample Depth ◽  
Extractable P ◽  
P Content ◽  
Field Samples ◽  
Adjacent Field ◽  
Depth Water

Greater amounts of 0.5 M NaHCO3 and water-extractable P were found in soil beneath a cattle feedlot located on an alkaline sandy soil than in soil in an adjacent non-manured field. The 0.5 M NaHCO3-extractable P contents of the feedlot soil samples were greater than for the adjacent field to a depth of 120–150 cm, suggesting that P from the manure had moved to this depth. Water extracted very little P from all field samples and the feedlot samples obtained below 120 cm. Concentration of total P in the feedlot soil was usually greater than in the corresponding field soil. The field soil contained more organic P than the feedlot soil at depths of 0–90 cm. Organic P concentrations at the 0 to 15-cm depths were 268 and 56 ppm for the field and feedlot sites, respectively. The organic C:N:P ratios for the 0 to 15-cm feedlot and field samples were 214:18:1 and 132:8.7:1, respectively. Mineralization of organic P in laboratory experiments was greater in flooded soils than in soils maintained at field capacity. Rates of mineralization were greater for manured than for non-manured samples. Organic and inorganic P moved at about equal rates in soil treated with manure extract. Rates of movement of both decreased with increasing sample depth in the feedlot soil. The feedlot soil below 30 cm and the field soils exhibited a high potential for inorganic and organic P fixation. Organic and inorganic P applied as manure extract moved faster than an equivalent concentration of P as KH2PO4.

Direct and residual effect of phosphorus on dryland barley

1996 ◽  
Vol 126 (2) ◽  
pp. 137-141 ◽  
Author(s):  
P. I. Orphanos
Keyword(s):  
Surface Soil ◽  
Maximum Yield ◽  
Balance Sheet ◽  
Residual Effect ◽  
Threshold Value ◽  
Soil P ◽  
Extractable P ◽  
P Content ◽  
P Balance ◽  
Cropping Seasons

SUMMARYIn a 14-year experiment conducted at Athalassa in the central plain of Cyprus, phosphorus was applied (0, 30 or 60 kg P/ha) annually over the first 5-year period to rainfed barley continually grown and cut for hay at the milk stage of the grain. The bicarbonate-extractable P content in the surface soil was 4 mg/kg at the start and increased to 16 and 25 mg/kg after the five annual applications of 30 and 60 kg P/ha, respectively. The residual effect of P was monitored in the following seven crop seasons, by the end of which soil P had dropped to below the recognised 6 mg/kg threshold value for response to P. The application of P was resumed in the last two experimental seasons (1992/93 and 1993/94). In two cropping seasons, rainfall was < 140 mm and no harvestable yield was obtained. In another two seasons, in which there was adequate rainfall in December and January, there was no response to P, but in the other seasons 30 kg P/ha was sufficient for maximum yield. Concentration of P in the dry matter (DM) harvested increased in proportion to the P applied.A P balance sheet made after the first five P applications and taking into account the amount of P removed in the DM and the increase in soil bicarbonate-extractable P indicated that 29 and 26 % of the P applied with the 30 and 60 kg P/ha rates, respectively, was accounted for.The data indicate that the established threshold value of 6 mg P/kg is valid. The soil tested 180 mg/kg exchangeable K. but application of 240 or 480 kg K/ha did not increase yield.

Transformation of phosphorus in highly calcareous soils under field capacity and waterlogged conditions

Soil Research ◽  
2012 ◽  
Vol 50 (3) ◽  
pp. 249 ◽  
Author(s):  
E. Adhami ◽  
A. Ronaghi ◽  
N. Karimian ◽  
R. Molavi
Keyword(s):  
Calcareous Soils ◽  
Hydroxylamine Hydrochloride ◽  
Field Capacity ◽  
Inorganic Phosphorus ◽  
Influential Factors ◽  
Moisture Regime ◽  
P Fractions ◽  
Waterlogged Condition ◽  
Successive Extraction ◽  
Moisture Regimes

The aim of the present study was to evaluate the transformation of applied inorganic phosphorus (P) in highly calcareous soils under two moisture regimes. The experimental design was a factorial combination of two rates of P (0 and 300 mg P kg–1 as KH2PO4) and two moisture regimes (field capacity, FC; waterlogged, WL) in a completely randomised design in duplicate with 20 surface soil samples. The fractionation sequence of inorganic P included successive extraction with NaHCO3, NH4 acetate buffer (NH4OAc), MgCl2, NH4F, NaOH–Na2CO3 (HC), Na citrate–bicarbonate–dithionite (CBD), and H2SO4 carried out 80 and 160 days after incubation. Recovery of applied P in each fraction was calculated as the difference between samples treated and untreated with P. Results indicated that NaHCO3-P decreased from 80 to 160 days, and the decrement was higher under WL than FC moisture regime. The NH4OAc-P was lower under WL than FC at 160 days, while P associated with free and crystalline Fe and Al oxides (NH4F-P, HC-P, CBD-P) was higher under WL than FC for both incubation periods. Oxalate-, citrate-, and citrate–ascorbate-extractable iron under FC and in conjunction with oxalate- and CBD-extractable aluminium and quinone- and hydroxylamine–hydrochloride-extractable manganese were the most influential factors regulating all P fractions. Results of the present study revealed that transformation of applied P into Al- and Fe-P fractions is not as low as previously reported in highly calcareous soils and that Al- and Fe-P oxides may be important in P transformation of these soils, especially in waterlogged condition.

Forms of phosphorus in virgin and fertilised calcareous soils of Western Australia

Soil Research ◽  
1998 ◽  
Vol 36 (4) ◽  
pp. 585 ◽  
Author(s):  
Abbas Samadi ◽  
R. J. Gilkes
Keyword(s):  
Agricultural Development ◽  
Ammonium Oxalate ◽  
Calcareous Soils ◽  
Organic P ◽  
P Values ◽  
Inorganic P ◽  
Extractable P ◽  
Highly Correlated ◽  
Average Contribution ◽  
Total P

Total phosphorus (P), inorganic P (Pi), organic P, and several Pi fractions were determined for 8 fertilised calcareous soils under agriculture and their virgin analogues under natural bush to ascertain changes due to agricultural development. The relationships between soil properties and forms of P were also determined. In general, agricultural development of soils resulted in increases in total P (average 105% increase), Pi (154%), organic P (49%), Olsen P (200%), Colwell P (100%), and all Pi fractions compared with their virgin analogues. For the virgin soils, the abundance of the Pi fractions was in the order: Al-P>O-P (occluded P)>Fe-P>Ca10-P = Ca2-P>Ca8-P, which changed to Al-P>Ca8-P>Ca2-P>Ca10-P>Fe-P>O-P for fertilised soils. The average contribution of each fraction to the increase in total Pi was Al-P (29%), Ca8-P (26%), Ca2-P (18%), Fe-P (13%), Ca10-P (13%), and O-P (4%). The change in Ca8-P was closely correlated with the content of the active fraction of calcite in the soil (ACCE). The increase in Fe-P associated with agriculture was highly correlated with citrate-dithionite-bicarbonate (CDB) extractable Fe (Fed) and acid-ammonium oxalate extractable Fe (Feo). The increase in Al-P was correlated with the ratio of acid-ammonium oxalate extractable Al (Alo) to Feo. Both Olsen and Colwell NaHCO3-extractable P were highly correlated with Ca2-, Al-, Fe-, and Ca10-P, and total P values. Multiple regression analysis indicated that Ca2-P and Ca10-P were major contributors to available P as determined by the Olsen and Colwell soil tests.

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.

Quantifying the contribution from the soil microbail biomass to the extractable P levels of fresh and air-dried soils

Soil Research ◽  
1985 ◽  
Vol 23 (4) ◽  
pp. 613 ◽  
Author(s):  
GP Sparling ◽  
KN Whale ◽  
AJ Ramsay
Keyword(s):  
Microbial Biomass ◽  
Inorganic Phosphorus ◽  
Microbial Biomass C ◽  
Air Drying ◽  
P Values ◽  
Extractable P ◽  
P Content ◽  
Microbial P ◽  
Drying Treatment ◽  
Substrate Induced Respiration

Levels of P extractable in 0.5 M NaHCO3 and the microbial biomass C were measured on a range of 15 New Zealand pasture soils, with and without an air-drying treatment. The microbial biomass C, estimated using a modified substrate-induced-respiration method, was decreased 11-68% by air-drying. Two soils showed no increase in extractable inorganic phosphorus (P) levels after air-drying, but increases for the other 13 soils ranged over 14-184%. In general, the biomass C was not related to the overall P, levels of moist or air-dried soils. However, the increase in P, after air-drying was related to the microbial P content of the moist soil, estimated by CHCl3 fumigation, and the proportion of the biomass C killed by air-drying. A comparison of the actual measured Pi levels of dried soils and those estimated allowing for the microbial contribution, showed excellent agreement, strongly suggesting that the whole of the Pi increase on air-drying of soils was derived from killed microbial cells. The microbial contribution to Pi levels in NaHCO3 extracts of dried soils ranged over 4-76% and was therefore a significant large proportion in some soils. A large microbial contribution to Pi in extracts is most likely on air-dried soils from under pasture with >2% organic matter and NaHCO3-extractable P values of <20 �g g-1.

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