scholarly journals Effect of cumulative fertilizer dressings on the phosphorus status of mineral soils I Changes in inorganic phosphorus fractions

1989 ◽  
Vol 61 (2) ◽  
pp. 55-59 ◽  
Author(s):  
Helinä Hartikainen
Keyword(s):  
Inorganic Phosphorus ◽  
Soluble Form ◽  
P Fertilization ◽  
P Fractions ◽  
Inorganic P ◽  
Extractable P ◽  
Inorganic P Fractions ◽  
Phosphorus Status ◽  
Mineral Soils ◽  
Inorganic Phosphorus Fractions

Surface soil samples were collected from 16 P fertilization trials before onset of the experiments and after seven years of cultivation. The changes in the inorganic P fractions were investigated in plots amended annually with 0, 30 or 60 kg of P ha-1. In the clay soils, cultivation without P fertilization depleted the NH4F-extractable and NaOH-extractable P reserves by 22—69 kg ha-1 ; in the coarser soils, the respective depletion was 8—140 kg ha-1. H2S04-soluble P decreased in seven soils by 16—34 kg ha-1. In the plots amended totally with 210 or 420 kg of P ha-1, on the other hand, these P fractions increased by 24—174 and 46—368 kg ha-1, respectively. The higher the P dressing was, the more the added P tended to accumulate in the fluoride-soluble form as compared to the alkali-soluble form.

Soil Inorganic Phosphorus Fractions as Affected by Fertilization

2011 ◽  
Vol 322 ◽  
pp. 108-111 ◽  
Author(s):  
Bao Tong Huang ◽  
Hua Zhou ◽  
Huai Xiang Ding
Keyword(s):  
Inorganic Phosphorus ◽  
Inorganic P ◽  
Liaohe River ◽  
Inorganic P Fractions ◽  
P Application ◽  
River Plain ◽  
P Addition ◽  
Liaohe River Plain ◽  
Different Levels ◽  
Inorganic Phosphorus Fractions

A fifteen-year field trial (started in 1990) was conducted to determine the inorganic P fractions under 8 classical modes of fertilization in the lower reach of Liaohe River Plain. The results showed that Ca2-P, Ca8-P, Al-P and Fe-P decreased in the absence of P application, while increased with supplemental P addition. Interestingly, O-P and Ca10-P, with low bioavailability, increased at different levels under all treatments after 15 years. The contents of inorganic P were low in crop stalk, indicating that P supplying capacity was weak. On the contrary, both fresh pig excretion and decomposed manure were huge inorganic P pools.

scholarly journals Phosphorus saturation of Finnish soils: evaluating an easy oxalate extraction method

2000 ◽  
Vol 9 (1) ◽  
pp. 61-70 ◽  
Author(s):  
R. UUSITALO ◽  
H.-R. TUHKANEN
Keyword(s):  
Clay Content ◽  
P Fractions ◽  
Runoff Water ◽  
Inorganic P ◽  
P Concentration ◽  
Extractable P ◽  
Inorganic P Fractions ◽  
Phosphorus Saturation ◽  
Labile P ◽  
Oxalate Extraction

The aim of this study was to test whether phosphorus saturation of surface sorption sites of (oxyhydr)oxides of aluminium (Al) and iron (Fe) in Finnish soils can be assessed using a single oxalate extraction and, if so, whether the results are closely related to the P forms likely to influence the P concentration in runoff waters. Ten soil samples with varying clay content and P status were studied. Desorption tests were conducted by submitting the soils sequentially to nine anion exchange resin (AER) extractions. Sorption of P was studied by shaking the soils in P standard solutions (0-250 ppm). Soil inorganic P was characterised by sequentially extracting P from the fractions assumed to be connected to Al and Fe compounds and present as the stable apatitic form. The desorption studies and the fractioning of inorganic P suggested that oxalate solution dissolves apatitic P and/or other relatively stable P-bearing compounds, probably referring to the sum of inorganic P fractions rather than labile P. The amount of P desorbed in the nine AER extractions was about 80-280 mg/kg, whereas oxalate extracted about 490-1100 mg P/kg, which approximated the sum of the inorganic P fractions. Therefore, in soils high in apatitic P, oxalate-extractable P does not seem to be a reliable measure of the P saturation of Al and Fe oxide surfaces that regulate the P concentration in soil solution and runoff water.;

scholarly journals Watersoluble phosphorus in Finnish mineral soils and its dependence on soil properties

1982 ◽  
Vol 54 (2) ◽  
pp. 89-98
Author(s):  
Helinä Hartikainen
Keyword(s):  
Water Soluble ◽  
Clay Soils ◽  
Molar Ratio ◽  
Inorganic P ◽  
Decisive Importance ◽  
Extractable P ◽  
Average Water ◽  
Inorganic P Fractions ◽  
Mineral Soils

Water soluble phosphorus ranged from 0.2 mg to 117.8mg/kg in 104 surface soil samples studied. On the average, water extracted less P from the heavy clay soils (4.8 ± 2.2mg/kg) than from the coarser clays (12.8 ± 4.6 mg/kg) and non-clay soils (13.3 + 7.2 mg/kg). Water extraction seemed to illustrate ’’the effective” P status, it is that determined by the quantity and quality of sorption components in soil, soil pH and the content of organic carbon. These factors did not affect the amounts of P dissolved in water directly but inderectly by controlling the nature of P bonding which, in turn, seems to be of decisive importance in the extractability of P into water. The P supplying power of a given fraction is obviously controlled by the quantity of corresponding sorption agent. Water extractable P correlated most closely with the molar ratio of NH4F soluble P to oxalate extractable Al (r=0.93***, n= 103). However, according to the theory presented, with progressing desorption, P starts to mobilize also from the NaOH soluble fraction, its significance being the more apparent the greater the corresponding molar ratio NaOH-P/Fe is. In addition, the role and significance of other inorganic P fractions were discussed.

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).

Dynamics of phosphorus fractions in soils treated with dairy manure

Soil Research ◽  
2020 ◽  
Vol 58 (3) ◽  
pp. 289
Author(s):  
L. B. Braos ◽  
A. C. T. Bettiol ◽  
L. G. Di Santo ◽  
M. E. Ferreira ◽  
M. C. P. Cruz
Keyword(s):  
P Uptake ◽  
Dairy Manure ◽  
P Availability ◽  
Organic P ◽  
Triple Superphosphate ◽  
P Fractions ◽  
Inorganic P ◽  
Soil P ◽  
Plant P Uptake ◽  
Inorganic P Fractions

The evaluation of phosphorus (P) transformations in soil after application of manure or mineral P can improve soil management and optimise P use by plants. The objectives of the present study were to assess organic and inorganic P forms in two soils treated with dairy manure and triple superphosphate and to establish relationships between soil P fraction levels and P availability. Soil organic and inorganic P fractions were quantified using a pot experiment with two soils, a typical Hapludox and an arenic Hapludult, with three types of fertiliser treatments applied (no fertiliser application, application of dairy manure, and application of triple superphosphate, by adding 100 mg P dm–3 in the form of fertiliser in the two latter treatments) and four incubation times (15, 45, 90, and 180 days). Inorganic P was fractionated into aluminium-bound, iron-bound, occluded, and calcium-bound P. Organic P was extracted sequentially using sodium bicarbonate, hydrochloric acid, microbial biomass, sodium hydroxide, and residual organic P. After incubation, maize plants were cropped to quantify dry matter yield and absorbed P. Application of dairy manure resulted in a significant increase in most of the organic P fractions, and application of triple superphosphate led to a significant increase in inorganic P fractions. Both fertilisers raised labile organic P fractions in the two soils. The major sinks of P in Hapludox were occluded and fulvic acid-associated P. In contrast, the major sink of P in Hapludult was iron-bound P. The available P levels were stable after application of dairy manure, and decreased with time when fertilised with triple superphosphate. In the Hapludox, the organic P fractions had a significant positive correlation with P uptake by plants. The results suggest that organic P mineralisation plays a more significant role in plant P uptake in the Hapludox soil and inorganic P forms are the main contributors to plant P uptake in the Hapludult soil.

Soil P availability, inorganic P fractions and yield effect in a calcareous soil with plastic-film-mulched spring wheat

2012 ◽  
Vol 137 ◽  
pp. 221-229 ◽  
Author(s):  
Bin Hu ◽  
Yu Jia ◽  
Zhi-hong Zhao ◽  
Feng-min Li ◽  
Kadambot H.M. Siddique
Keyword(s):  
Spring Wheat ◽  
Calcareous Soil ◽  
P Availability ◽  
Plastic Film ◽  
P Fractions ◽  
Inorganic P ◽  
Soil P ◽  
Soil P Availability ◽  
Inorganic P Fractions

scholarly journals Comparison of phosphorus fraction distribution and influencing factors of suspended and surface sediments in the Tiaoxi watershed, China

2017 ◽  
Vol 75 (9) ◽  
pp. 2108-2118 ◽  
Author(s):  
Hongmeng Ye ◽  
Xuyin Yuan ◽  
Lei Han ◽  
Heng Yin ◽  
Jing Jin
Keyword(s):  
Surface Sediments ◽  
Anthropogenic Activities ◽  
Principal Component ◽  
Suspended Sediments ◽  
Inorganic Phosphorus ◽  
P Fractions ◽  
Fraction Distribution ◽  
Inorganic P Fractions ◽  
P Fraction ◽  
Major Factors

Suspended and surface sediments from the Tiaoxi watershed, fed by the Xitiaoxi and Dongtiaoxi rivers, were analyzed for total phosphorus (TP) and the inorganic P fractions of loosely adsorbed P that were extractable with NH4Cl (NH4Cl-P), reductant P (BD-P), metal oxide-bound P extractable with NaOH (NaOH-P), and calcium-bound, HCl-extractable P (HCl-P), while other physicochemical compositions were also determined. The spatial variations of P fractions in these sediments were investigated, and the major factors influencing the various fractions were explored by multivariate statistics. Compared to surface sediments, suspended sediments contained considerably higher concentrations of total nitrogen, TP, organic matter, Al, Fe, Mn and biologically available P (BAP, given as NH4Cl-P, BD-P and NaOH-P combined) and lower concentrations of Si, Ca and HCl-P in the studied catchments. Dongtiaoxi sediments had higher TP, inorganic phosphorus and HCl-P concentrations and a lower BAP content compared with Xitiaoxi sediments, trends that were associated with local geological backgrounds, landscapes and anthropogenic characteristics. The results of principal component analysis showed different effects of sediment properties on P fraction distributions for Xitiaoxi and Dongtiaoxi sediments. The sediment components and structure exert a strong influence on BAP in Xitiaoxi sediments, in contrast to Dongtiaoxi sediments, where P fractions are mainly affected by urbanization and other anthropogenic activities such as shipping.

scholarly journals Use of near-infrared spectroscopy to assess phosphorus fractions of different plant availability in forest soils

2015 ◽  
Vol 12 (11) ◽  
pp. 3415-3428 ◽  
Author(s):  
J. Niederberger ◽  
B. Todt ◽  
A. Boča ◽  
R. Nitschke ◽  
M. Kohler ◽  
...  
Keyword(s):  
Infrared Spectroscopy ◽  
Near Infrared Spectroscopy ◽  
Forest Soils ◽  
Soil Type ◽  
Near Infrared ◽  
Soil Samples ◽  
P Fractions ◽  
Inorganic P ◽  
Plant Availability ◽  
Inorganic P Fractions

Abstract. The analysis of soil phosphorus (P) in fractions of different plant availability is a common approach to characterize the P status of forest soils. However, quantification of organic and inorganic P fractions in different extracts is labor intensive and therefore rarely applied for large sample numbers. Therefore, we examined whether different P fractions can be predicted using near-infrared spectroscopy (NIRS). We used the Hedley sequential extraction method (modified by Tiessen and Moir, 2008) with increasingly strong extractants to determine P in fractions of different plant availability and measured near-infrared (NIR) spectra for soil samples from sites of the German forest soil inventory and from a nature reserve in southeastern China. The R2 of NIRS calibrations to predict P in individual Hedley fractions ranged between 0.08 and 0.85. When these fractions were combined into labile, moderately labile and stable P pools, R2 of calibration models was between 0.38 and 0.88 (all significant). Model prediction quality was higher for organic than for inorganic P fractions and increased with the homogeneity of soil properties in soil sample sets. Useable models were obtained for samples originating from one soil type in subtropical China, whereas prediction models for sample sets from a range of soil types in Germany were only moderately useable or not useable. Our results indicate that prediction of Hedley P fractions with NIRS can be a promising approach to replace conventional analysis, if models are developed for sets of soil samples with similar physical and chemical properties, e.g., from the same soil type or study site.

Changes in the forms and distribution of soil phosphorus due to long-term corn production

1995 ◽  
Vol 75 (3) ◽  
pp. 311-318 ◽  
Author(s):  
John E. Richards ◽  
Thomas E. Bates ◽  
S. C. Sheppard
Keyword(s):  
Sequential Extraction ◽  
Organic Phosphorus ◽  
Inorganic Phosphorus ◽  
P Fertilization ◽  
Corn Production ◽  
Soil P ◽  
Olsen P ◽  
Extractable P ◽  
P Application

Long-term fertilizer-P application affects soil-P distribution and forms. These effects must be characterized to use fertilizer P most efficiently. In three southern Ontario soils of varying texture, we determined changes in soil organic P (Po) and inorganic P (Pi) caused by fertilizer P application (0–90 kg broadcast P ha−1 yr−1 during 10 yr of corn production. Soil P was characterized by (1) annual measurement of 0.5 M NaHCO3-extractable P (Olsen-P) and (2) sequential extraction from soil taken at the beginning of the experiment and after receiving 0 to 90 kg broadcast P ha−1 yr−1 for 10 yr. Fertilizer P increased Olsen-P concentrations in all soils. The increases were proportional to the cumulative amount of P applied. Based on all three soils, 16 kg P ha−1 was required to increase Olsen-P concentrations by 1 mg L−1 soil. After 10 yr of 90 kg broadcast P ha−1 yr−1, labile Pi fractions (resin P and NaHCO3 P) were increased, as was NaOH-extractable Pi in all soils. On the most P-deficient soil (Conestogo SiL), where corn grain yields were increased by fertilizer P, P fertilization also increased HCl-Pi, residual P (H2O2-H2SO4 extractable P) and labile Po (NaHCO3-Po and NaOH-Po). A P balance was calculated, which accounted for additions to, removals from, and changes in the total P status of the 0–20 cm layer. When no broadcast P was applied, there was an unaccounted-for input (possibly from the subsoil), of 20.9 kg P ha−1 yr−1 on the Conestogo SiL. When 90 kg broadcast P ha−1 yr−1 was applied to the Fox SL, the coarsest soil studied, there was a deficit of 30.9 kg P ha−1 yr−1 and elevated Olsen-P concentrations in the 25–36 cm depth, suggesting downward movement on fertilizer P. It appears that subsoil P was involved in the P cycle of these two soils. Key words: Continuous corn, P fertilization, sequential extraction, organic phosphorus, inorganic phosphorus, labile phosphorus, subsoil P, leaching

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