scholarly journals Phosphorus Availability for Irrigated Rice Cultivated Under No-Tillage and Different Phosphate Sources

2018 ◽  
Vol 10 (5) ◽  
pp. 276
Author(s):  
Magali De Ávila Fortes ◽  
Rogério Oliveira de Sousa ◽  
Algenor da Silva Gomes ◽  
Fabiana Schmidt ◽  
Walkyria Bueno Scivittaro ◽  
...  

The objective of this work was to evaluate the response of irrigated rice to phosphate fertilization using triple superphosphate (TSP) and Arad phosphate rock (APR), and the phosphate residual effects of upland crops in no-tillage system on the following rice crop. Also, it aimed to evaluate the efficiency of Mehlich-1 and anion exchange resin as soil P extractors. Two experiments were conducted in Albaqualf soil under irrigated conditions in the southern region of Rio Grande do Sul State. The experiments were designed as random blocks with four replications and the treatments were displayed as a 2 × 2 factorial (TSP and APR, with and without annual P application as TSP). No yield responses to phosphate were observed. Phosphate fertilization performed on upland crops (maize and soybeans) presented a residual effect on the rice crop even after four years of consecutive cropping under no-tillage. The extractors Mehlich-1 and AER were equally efficient in the evaluation of P availability for the rice crop. P content values obtained by both methods did show a significant correlation with accumulated plant P. The APR presents a similar performance as the TSP in regard to phosphate nutrition in irrigated rice when rotated with upland crops under no-tillage system.

2012 ◽  
Vol 33 (6) ◽  
pp. 2187-2198 ◽  
Author(s):  
Juliano Magalhaes Barbosa ◽  
Claudia Fabiana A Rezende ◽  
Wilson Mozena Leandro ◽  
Rafael Felippe Ratke ◽  
Eliana Paula Fernandes

2021 ◽  
Vol 213 ◽  
pp. 105152
Author(s):  
Leandro Michalovicz ◽  
Cassio Antonio Tormena ◽  
Marcelo Marques Lopes Müller ◽  
Warren A. Dick ◽  
Eduardo Cimino Cervi

Soil Research ◽  
2005 ◽  
Vol 43 (2) ◽  
pp. 203 ◽  
Author(s):  
T. M. McBeath ◽  
R. D. Armstrong ◽  
E. Lombi ◽  
M. J. McLaughlin ◽  
R. E. Holloway

Recent field trials on alkaline soils in southern Australia showed significant grain yield responses to liquid compared with traditional granular forms of P fertiliser. However the advantages of liquid over granular P forms of fertiliser has not been consistent on all soil types. In order to better predict the soil types on which liquid P fertilisers are likely to have potential, a glasshouse trial was conducted to compare the responsiveness of wheat to both liquid and granular forms of P on a wide range of Australian soils. A granular P fertiliser (triple superphosphate) and 2 liquid fertilisers (phosphoric acid and ammonium polyphosphate) were compared at a rate equivalent to 12 kg P/ha in 29 soils representing many of the soil types used for grain production in Victoria and South Australia. Wheat biomass was enhanced by P application in 86% of the soils tested. In 62% of the P-responsive soils, wheat dry matter was significantly greater when liquid P fertilisers were used compared with the granular form. Chemical analysis of the soils tested showed that the better performance of liquid P forms was not correlated to total P concentration in soil, P buffer capacity, or P availability as measured by Colwell-P. However, there was a significant positive relationship between calcium carbonate (CaCO3) content of soil and wheat responsiveness to liquid P fertiliser.


1965 ◽  
Vol 1 (3) ◽  
pp. 193-200 ◽  
Author(s):  
A. W. Moore

SummaryExperiments involving N, P, and K fertilization, and height and frequency of cutting, were carried out on a mixed pasture of giant stargrass (Cynodon plectostachyus) and centro (Centrosema pubescens) at the University of Ibadan during the growing seasons 1951–61. For the first cut after fertilization yield responses of 17 and 24 per cent resulted from applications of 50 and 100 lb N per acre respectively in various experiments but the effect was transient and recovery of fertilizer nitrogen probably did not exceed 30 per cent. Nitrogen fertilization of sown pastures is unlikely to be an economic practice in Nigeria in the forseeable future. Yield responses of 30 per cent resulted from applications of 2½ and 5 cwt superphosphate per acre with a marked residual effect two years after application. Significantly higher concentrations of extractable inorganic soil P at the higher P fertilization rate after 2 years were largely a reflection of the levels of the iron phosphate fraction, but similar trends were evident in the aluminium and calcium phosphate fractions. No differences were found in total, organic, or residual P. The proportion of centro in one 1959 cut for the 0 and 5 cwt rates of superphosphate were 46 and 38 per cent whereas N had no effect, the reverse of the response normally encountered in a temperate mixed pasture. No response to K was obtained. Increased frequency and height of cutting both resulted in decreased yields of dry matter but cutting at 2–4 inches at 8-weekly intervals appears to be the most satisfactory method of managing this pasture for hay production, with yields of approximately 2¼ tons dry matter per acre.


1994 ◽  
Vol 45 (5) ◽  
pp. 1051 ◽  
Author(s):  
ICR Holford ◽  
GJ Crocker

Eight experiments on acidic soils of the Northern Tablelands of New South Wales were carried out to measure lime effects on clover-based pastures and their response to fertilizer phosphate (P). Each experiment lasted 3 years. The seven soils deficient in P all responded to lime in the first year, and pasture yield responses were associated with lime-induced increases in isotopically exchangeable or soluble soil P or both. Three of these soils were also relatively high in soluble aluminium (Al) or manganese (Mn), and the lime-induced suppression of these toxic cations probably also contributed to the beneficial effects of lime. Negative effects of lime on fertilizer P response were more frequent than positive effects, and tended to occur on higher A1 soils. Lime eliminated the need for fertilizer P on at least three P-deficient soils during the 3 year period of the experiments, and this was also associated with increases in availability and uptake of soil P. Lime suppressed P sorptivity in all soils, but this caused an increase in fertilizer P effectiveness in only two soils (in the first year). Hence, the positive effect of lime on soluble soil P, which occurred on all soils and which would tend to lower fertilizer P effectiveness, seemed to be dominant over its negative effect on soil P sorptivity. Residual effects of lime and fertilizer P were similar, both declining after the first year, with five soils still responsive in the third year.


2018 ◽  
Vol 53 (7) ◽  
pp. 833-839
Author(s):  
Renato Yagi

Abstract: The objective of this work was to evaluate the residual effects of occasional soil tillage in a 17-year-old, no-tillage system, associated with liming and nitrogen fertilization, on the crop yields and chemical properties of a very clayey Oxisol in the South of Brazil. A randomized complete block design in split-split plots was used, with two soil managements (with or without plowing), two liming treatments (with or without the required dose to raise base saturation to 70%), five N doses applied on side-dress (0, 1, 2, 4, and 6 times the recommended amounts), and four replicates. A rotation system was used with corn and soybean in the summer, and with wheat and black oats in the winter. The residual effects of occasional soil tillage in a consolidated no-tillage system do not supplant those of liming applied on soil surface, in periods of water deficit, which subsidizes the recommendation to maintain the system consolidated. Excess N fertilization in no-tillage, with liming applied only on soil surface, may harm wheat yield, acidifying the topsoil and leaching Mg2+ to the subsurface soil layers. Without liming, soil acidification is more intense with N fertilization, which, however, favors the accumulation of organic matter on soil surface in a consolidated no-tillage system.


1978 ◽  
Vol 90 (3) ◽  
pp. 479-494 ◽  
Author(s):  
D. Wilman ◽  
B. M. Ojuederie

SummaryThe 32 combinations of applying or not applying nitrogenous fertilizer on five dates, with 6-week intervals between dates, during one treatment year were compared in three field experiments with Italian ryegrass (Lolium mvltiflorum). Phosphorus (P)and potassium (K) were applied at a uniform, high rate to all plots. All plots were harvested, by cutting, five times during the treatment year and once in May of the subsequent year.Dry-matter yields and dry-matter yield responses to N were lower at the September and October harvests than at the May, June and July harvests. Where no N was applied 6 weeks before a harvest, N applied 12 weeks before that harvest generally increased yields of dry matter, N, P and K. On the other hand, where N was applied 6 weeks before a harvest, N applied 12 weeks before that harvest tended not to increase dry-matter yield and tended to reduce P and K yields. Applying 420 kg N/ha/year compared with nil approximately trebled the amounts of dry matter, P and K harvested in the treatment year. At the May harvest in the subsequent year dry-matter yield was increased by N applied in the treatment year, for all five application dates, although the previous autumn there had been no positive residual effect of the early applications. Apparent recovery of N was low compared with that recorded with Italian ryegrass in Cambridge. The content of N, as well as P and K, in herbage in May was reduced by the application of N the previous year. In the 1972 experiment the proportion of ‘stem’ in the harvested produce was markedly increased by N application. The size of this effect may have been associated with the rather small amount of soil N available. Applied N increased the number of tillers in the sward, but this effect appeared to be rather short-lived. A major reason for the positive effect of applied N on dry-matter yield, including the positive residual effect, appeared to be the increase in leaf blade length and probably sheath length due to N.


2020 ◽  
Vol 9 (6) ◽  
pp. e143963490
Author(s):  
Marcela Pacola Oliveira ◽  
Cassiano Garcia Roque ◽  
Gabriel Luiz Piati ◽  
Othon Lauar Godinho ◽  
Paulo Eduardo Teodoro

The use of lime, gypsum, and different cover crops may influence the soil physical attributes, the formation of soil coverage before the crop implantation is crucial for the consolidation of the No-Tillage System. This work aimed to evaluate the alterations in the subsoil physical attributes, influenced by different cover crops combined with the application of lime and gypsum, in a no-tillage system in the Cerrado region, the soil of the experiment area was classified as Dystrophic Red Latosol. The experiment was carried out in Chapadão do Sul, state of Mato Grosso do Sul, Brazil, in a complete randomized block design, in a split-plot scheme. Plots consisted of cover crops (Urochloa ruziziensis and Pennisetum glaucum) and fallow; the subplots were formed by gypsum rates (0, 2.3, and 4.6 Mg ha-1); and the sub-sub-plots consisted of lime rates (0, 2, 4, and 6 Mg ha-1), with three replications. The cover crops, Uruchloa ruziziensis, Pennisetum glaucum and the rates of limestone and gypsum do not interfere with the density of the soil. The Uruchloa ruziziensis cover crop provides increased microporosity and total soil porosity. The cover crops Uruchloa ruziziensis and Pennisetum glaucum were not efficient in decompressing the soil in the layers of 0.20 - 0.30 and 0.30 - 0.40 m in depth. The residual effect of the lime rate of 2 Mg ha-1 without gypsum application provided higher total porosity the 0.30 - 0.40 m layer.


2015 ◽  
Vol 39 (3) ◽  
pp. 216-224 ◽  
Author(s):  
Leonardo Ricardo Rotta ◽  
Helder Barbosa Paulino ◽  
Ibanor Anghinoni ◽  
Edicarlos Damacena de Souza ◽  
Guilherme Lopes ◽  
...  

Soil use and fertilizer management as well as cropping systems influence phosphorus (P) availability in the soil. This study evaluated P fractions and availability in a chronosequence of anthropic influence in a Haplic Plinthosol, in sites under no-till for different time periods: seven (NT7), eleven (NT11), and sixteen (NT16) years. Labile P concentrations in the soil accounted for 10%, 8%, and 9% of the total P for treatments NT7, NT11, and NT16, respectively. The labile P values ranged between 99 and 122 mg dm-3andindicatied no time in no-tillage influence on labile P under in the studied Plinthosol. However, moderately labile P contents increased with time: NT7 < NT11 < NT16 (237, 341, and 375 mg dm-3, respectively). This increased followed the elevation in iron oxide contents, indicating a relationship between mineralogy and P accumulation. Regardless of no-tillage period, P contents extracted by Mehlich-1 were lower, underestimating the available P content, when compared with the extraction using a P selective resin. The stocks of labile P were sufficient to maintain high crop yields, according to the recommendations for the Cerrado region. Even if labile P contents are reduced, when adopting no-till system, the contents and stocks of P in the soil after several years were high enough to provide for adequate crop yields.


1989 ◽  
Vol 69 (2) ◽  
pp. 417-423 ◽  
Author(s):  
J. DUVAL ◽  
G. R. MEHUYS ◽  
G. S. V. RAGHAVAN ◽  
S. GAMEDA

Detailed soil profile descriptions were made to assess the residual effect of compaction and tillage treatments applied 10 yr ago on a Ste-Rosalie clay. The treatments applied consisted of five passes at a contact pressure of 61.8 kPa with no tillage, 15 passes of 61.8 kPa with chiselling, moldboard plowing, no tillage, subsoiling, and a control. The results were analyzed using nonparametric statistics. The untilled plots that received 15 wheel passes showed mottling that was more abundant and closer to the surface than the other plots while the subsoiled plots had a finer, less abundant and deeper mottling than the other plots. Peds in the Ae horizon were finer in the subsoiled and chiselled plots and coarser in the untilled plots and conventionally tilled plots that received 15 vehicle passes. It appears from this work that the effect of compaction is very persistent in clay soil and that subsoiling followed by reduced traffic can have a long-term effect on soil structure. Key words: Compaction, tillage, profile descriptions, clay soil


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