Yield responses of two ryegrass and two white clover varieties grown in contrasting mixtures with applications of phosphate at different depths and on different soils

To validate earlier findings using ³²P in upland soil and at different depths in lowland soil, ryegrass varieties S.23 or Titania were grown in mixtures with white clover varieties S.184 or Olwen. Unlabelled phosphate (0 or 43 kg P/ha) was applied to the surface or at 30 cm depth in lowland soil, and dry matter yields of grass and clover were measured. In June, on lowland soil, the greatest yield of clover was obtained by surface application. The most productive mixture was S.23/Olwen, although in August Titania outyielded S.23. By October S.23 again outyielded Titania. These results validated the isotopically discovered interactions between phosphate depth and grass/clover mixtures. On upland peat and mineral soil, 0 or 43 kg P/ha was surface applied to the same varietal mixtures. In May, phosphate application to mineral soil slightly decreased clover presence, while clover was increased by mixture with Titania rather than S.23. In July, no significant phosphate effects were found, but in October phosphate increased clover yield and, at least on mineral soil, S.23/Olwen responded most.     

Distribution of potassium in the soil profile of a sandplain soil under pasture species

The influence of pasture species and pasture/crop rotations on the fate of K fertilizer in the soil profile of a sandplain soil was investigated. Results for Lupinus cosentinii, subterranean clover and a subterranean clover/wheat rotation are presented. Potassium was applied as KCl at six rates up to 150 kg K ha^-1 for three years; bicarbonate-extractable K was measured at five depths in the profile (0–100 cm) for four years. The net change in available K in the top 100 cm of the profile (kg ha^-1) was calculated. There was a gradual increase in K down the profile under all species with fertilizer application. The increase was largest for L. cosentinii, which also appeared to redistribute K from below 100 cm to the soil surface. The K residual value on this soil type was higher than expected with most of the fertilizer applied over three years being retained in the top 100 cm.     

Effects of phosphate sorptivity on long-term plant recovery and effectiveness of fertilizer phosphate in soils

Summary A greenhouse experiment was carried out on 30 soils of eastern Australia in the first year and 15 soils in the following years to determine the effects of soil phosphate sorptivity and phosphate removal in harvested material on effectiveness and recovery of fertilizer phosphate by white clover during a four year period.Phosphate recovery by the clover and fertilizer effectiveness were primarily negative functions of phosphate sorptivity. After the first year there was a progressive decrease in the sorptivity effect such that the subsequent decreases in phosphate recovery and effectiveness were largest on weakly sorptive soils and smallest on strongly sorptive soils. In the long term the cumulative effects of the apparently slow immobilizing reactions on the weakly sorptive soils tended to equalize the effects of faster reactions on strongly sorptive soils so that the actual recovery and effectiveness in the final year were similar on all soils regardless of their sorptivities. The cumulative recovery and cumulative effectiveness in the long term, however, remained strongly negative functions of sorptivity. Phosphate removal in harvested material caused large decreases in phosphate effectiveness on all soils and particularly on weakly sorptive soils.     

The distribution and condition of soil phosphate under old permanent pasture

Summary The distribution and condition of soil phosphate under old permanent pasture on Tree Field at Cockle Park was investigated. Two cereal crops were then grown to estimate the residual value of the phosphatic dressings which had been applied over a long period of time.The total-phosphate content of Tree Field soil was found to be concentrated in the surface layers and to a lesser extent at depths of 36 inches. The total-phosphate contents of horizons between depths of 12 to 24 inches were relatively low. The penetration of the phosphatic fertilisers was found to be limited to the surface horizons.The availability of the phosphatic reserves differed in the surface layers of the plots. Plots which had received superphosphate or basic slag and lime had relatively large amounts of total phosphate in available form at these depths. Evidence of the possible utilisation of available phosphate by the original sward at a depth of 36 inches was found.The cropping potential of the plot which had received basic slag and lime was found to be superior to that of the remaining plots.     

Interactions between white clover and ryegrass under contrasting nitrogen availability: N2 fixation,N fertilizer recovery,N transfer and water use efficiency

Seasonal variation in N₂ fixation, N transfer from clover to ryegrass, and soil N absorption in white clover–ryegrass swards were investigated under field conditions over three consecutive years. The plots were established with different seeding ratios of clover and ryegrass and contrasting fertilizer N ranging from 3 to 72 kg ha^-1 year^-1.An initially poor clover population needed at least one growing season to reach the same yield output as an initially well established clover population. The clover content of the sward decreased by the annual application of 72 kg N ha^-1 but not by smaller N dressings.The total amount of atmospherically derived N in clover growing in mixture with ryegrass was, on average over the three years equal to 83, 71, 68 and 60 kg N ha^-1 for the treatments of 3, 24, 48 and 72 kg N ha^-1, respectively. The proportion of atmospherically derived N declined with increasing N application, but never became smaller than 80% of total clover N. The proportion of atmospherically derived N in a pure stand white clover amounted to 60–80% of the total N content, equivalent to 109, 110, 103 and 90 kg N ha^-1 for the treatments of 3, 24, 48 and 72 kg N ha^-1, respectively.Only small amounts of atmospherically derived N was transferred to the associated ryegrass during the first production year, while in each of the following years up to 21 kg ha^-1 was transferred. The average amount of N transferred from clover to ryegrass was equivalent to 3, 16 and 31% of the N accumulated in ryegrass in the first, second and third production year, respectively. Expressed relative to the total amount of fixed N₂ in the clover–ryegrass mixture, the transfer amounted to 3, 17 and 22% in the first, second and third production year, respectively. Thus transfer of atmospherically derived N from clover contributed significantly to the N economy of the associated ryegrass.The clover–ryegrass mixture absorbed constantly higher amount of soil derived N than the pure stands of the two species. Only 11% of the total accumulated fertilizer N and soil derived N in the mixture was contained within the clover component. Lower water use efficiencies for the plants grown in mixture compared to pure stands were mainly related to the increased N uptake in the mixture, with the subsequent increase in growth compared to the pure stands.It is concluded that positive interactions between clover and ryegrass growing in mixture ensure a more efficient fixation of atmospheric N₂ and absorption of fertilizer N and soil derived N than pure stands of the same species.     

Studies on soil rhizosphere: speciation and availability of Cd

ABSTRACT

The rhizosphere soils of two durum wheat (Triticum turgidum var. durum L.) cultivars Kyle and Areola grown in two selected soils of southern Saskatchewan were collected both at 2-week and 7-week plant growth stages. The cadmium availability index (CAI), determined as M NH₄CI-extractable Cd, pH and the distribution of the particulate- bound Cd species of the soils were carried out and the data were discussed in comparison with those of the corresponding bulk soil. At the 2-week growth stage, the pH of the rhizosphere soil was less than that of the corresponding bulk soil and the CAI values were higher in the rhizosphere soil, indicating that more Cd was complexed with the low-molecular-weight organic acids (LMWOAs) at the soil-root interface and was extractable by M NH₄CI. Compared with the bulk soils, the CAI values were 2–9 times higher in the soil rhizosphere of the plots fertilized with Idaho monoammonium phosphate fertilizer at 2-week growth stage, which is attributed to the combined effects of the Cd introduced into the soil rhizosphere from the fertilizer (Cd content of the fertilizer was 144 mg kg^?1) and complexation reactions of phosphate and LMWOAs with soil Cd. At 7-week plant growth stage, such differences were not observed. The increased amounts of carbonate-bound and metal-organic complex-bound Cd species of the rhizosphere soils are due to the increased amounts of carbonate, a product of plant respiration, and the LMWOAs at the soil-root interface, respectively. Simple correlation analysis of the data showed that the CAI of the rhizosphere soils of the control plots correlated at least two orders of magnitude better with the metal-organic complex-bound Cd whereas the CAI of the rhizosphere soils treated with Idaho phosphate correlated better with carbonate-bound Cd species in comparison to other species.     

Competition between Subterranean Clover and Rygrass for uptake of 15N-labeled fertilizer

Grasses and legumes are often grown together for improving quality of forage and for better yield when soil N availability is limiting. One compatible mixture is Trifolium subterranium L., subterranean clover and Lolium multiflorum Lam, ryegrass.Experiments were conducted with plants grown in a glasshouse and plant growth chambers to determine the competitive ability of these plants for fertilizer N. Fertilizer N was enriched with ¹⁵N to measure the contribution of dinitrogen fixation and fertilizer N to the growth of clover. In pure stands, with increased fertilizer N, the legume took up similar quantities of mineral N as the grass to make up for the deficit due to less dinitrogen fixation but in mixed stands the grass by far outcompeted the legume. The growth of clover suffered due to lack of N both from less dinitrogen fixation and the inability to compete with the grass for mineral N. Increasing levels of fertilizer N reduced dinitrogen fixation by the clover. When growing with the clover the grass did not receive N from the clover. A laboratory experiment using ¹⁵N label on pure stands of the two species indicated that the grass had an inherent capability of absorbing almost twice the amount of mineral N as the legume under the same conditions even when root weight and volume was not larger for the grass. The results of this research provide insight into the often observed phenomenon that growth of clover is reduced when grown with grass in proportion to the amount of mineral N provided. This revised version was published online in June 2006 with corrections to the Cover Date.     

Phosphate supplying power of rock phosphates in an oxisol

Summary The P-supplying power of triple superphosphate, three apatitic rock phospates and a calcined aluminum rock phosphate were tested by measuring the quantities of fertilizer P recovered in soybean and in four chemical extractants, after 3-day and 75-day periods of contact between soil and fertilizer.The triple superphosphate supplied the highest amounts of P, but it lost efficiency during the longer incubation period. The rock phosphates maintained their original efficiencies, probably as a result of a balance between P released from the fertilizer and P converted into non-labile forms.The following coefficients of correlation between P uptake by soybean from an acid oxisol and P extracted by chemical extractants, after the two incubation periods, were found: 0.902^** for 0.01M CaCl₂; 0.823^** for anion-exchange resin; 0.720^** for 0.03N NH₄F+0.025N HCl; –0.037 (n.s.) for 0.025N H₂SO₄+0.050N HCl.The acid NH₄F solubilized residual calcined aluminum phosphate particles, and double acid extracted P from residual apatite particles, thus accounting for their poorer performances in predicting availability of fertilizer P.The relative efficiencies of the rock phosphates could largely be predicted after an incubation period of only three days. This finding attests to the presence in these rock phosphates of an easily soluble fraction of P which is not indicative of the degree of reactiveness of the phosphate as a whole.on leave at the Agricultural University during 1977.     

Effects of vesicular-arbuscular mycorrhiza on the size of the labile pool of soil phosphate

Summary Inoculation of lettuce, onion and clover with VA mycorrhizal fungus (Glomus mosseae) increased plant yields and phosphate uptake in three soils that had been depleted in phosphate. From two soils in which the labile pool of phosphate had been labelled with³²P, the specific activity of plant phosphate was the same whether the plants were mycorrhizal or non-mycorrhizal. In a third soil (Sonning) the specific activity was lower in lettuce and clover when the plants were mycorrhizal. When the experiment was repeated with the same soil under conditions that gave lower growth rates, the specific activity was the same in mycorrhizal and non-mycorrhizal plants. The lower specific activity in lettuce and clover in the first experiment is atributed to greater release of slowly exchanging phosphate (which is not in equilibrium with the added³²P), caused by the high uptake of phosphate by the mycorrhizal plants. When they occur, lower specific activities in mycorrhizal plants may therefore not necessarily indicate a solubilizing effect of the mycorrhiza on soil phosphate.     

Growth responses of mycorrhizal and non-mycorrhizal tropical forage species to different levels of soil phosphate

Three tropical forage legumes, Stylosanthes capitata, Pueraria phaseoloides and Centrosema macrocarpum, and one grass, Brachiaria dictyoneura, were grown in a sterile phosphate deficient soil amended with soluble or rock phosphate at rates ranging from 0 to 400 mg kg^-1 soil. The effects of inoculation with Glomus manihotis on mycorrhizal infection and plant growth were assessed. Early growth and nodulation of P. phaseoloides in soil with and without rock phosphate fertilizer were also determined. In the legumes, mycorrhizal infection was high at all P levels and sources, except for a significant decrease of infection in S. capitata at high levels of superphosphate. Plant growth was significantly increased by phosphate fertilizer and mycorrhizal inoculation. Mycorrhizal responses were more pronounced at low P levels with both P sources. In B. dictyoneura mycorrhizal infection was decreased with increasing additions of P. No effects of mycorrhizal inoculation (except with no added P) were observed. Growth and nodulation of P. phaseoloides were greatly stimulated by mycorrhizal inoculation.     

Effects of vesicular-arbuscular mycorrhiza on the availability of iron phosphates to plants

Summary The effect of inoculation with a mycorrhizal fungus on the growth of subterranean clover and of ryegrass was measured using three sources of phosphorus with different solubilities. These were (in order of decreasing solubility): potassium dihydrogen phosphate, colloidal iron phosphate and crystalline iron phosphate. Mycorrhizal infection increased growth more for subterranean clover than for ryegrass for all sources of phosphorus. For both species the greatest benefit from mycorrhizal inoculation was obtained with the least soluble source of iron phosphate. It is suggested that the mycorrhizas were able to explore the soil more thoroughly and hence were able to locate and use the point sources of phosphorus in the insoluble iron phosphates.     

The dependence of isotopically exchangeable phosphate (L-value) on phosphate uptake

Summary L-values were determined using clover and ryegrass, grown either separately or together, in soil or soil/sand media. Where the two species were grown in the same pot, there was no interspecific effect on L-value. However, as the experiment progressed L-values increased and clover and ryegrass grown separately gave different values. The increases can be explained by P uptake, single regressions of L-value on phosphate uptake accounting for 86 and 88 per cent of the variations in L-value on the two soils used, with little improvement for treating the two crops separately. The most likely explanation for the observation is that the phosphate stress placed on the soil system caused mobilization of previously non-labile P by the dissolution of sparingly soluble phosphate compounds.     

Native soil and fresh fertilizer phosphorus uptake as affected by rate of application and P fertilizers

³²P labelled fertilizers were used to measure native soil and fresh fertilizer phosphorus uptake byLolium perenne L. in greenhouse experiments. The P source evaluation was carried out for multiple rates of application for a standard P fertilizer (DAP) on low and medium soil P levels and for North Carolina rock phosphate (RP) at the medium soil P level only. At the low soil P level, the native P uptake increase was independent of P-DAP applied, and represented 19% of the nil P uptake. At the medium soil P level, the variability of the native soil as a nutrient P source depended on the phosphate fertilizer applied, and the rate of application. Consequently the amount of total P uptake could conceal differences in P fertilizer evaluations as the nutrient P source. Fresh P uptake increased linearly with the rates of P applied as standard or tested P fertilizer. The comparison of various P sources by means of fresh P uptake ratio (i.e. fresh P uptake from tested phosphate divided by fresh P uptake from standard phosphate) was independent of the rate of application. It was therefore suggested that various phosphorus sources be evaluated by measuring the fresh P uptake for a single rate of application.     

The effect of phosphate withdrawal by plant and by an anion-exchange resin on the phosphate potential of a soil

Summary Varying degrees of phosphate depletion by plants and AER were brought about in two acid soils. After depletion, the monocalcium phosphate potential was determined in soil suspended in dilute CaCl₂ solution.The results showed that phosphate depletion either by plants or AER did not change the phosphate potential of a soil. It seemed that some of the labile phosphate removed by plants was replaced by a mobilization of non-labile soil phosphate fraction in the soil.The constancy of the phosphate potential indicated that the concentration of phosphate in the soil solution was controlled by the solubility of sparingly soluble soil phosphates. The data implied that it was the solubility of hydroxyapatite which determined the phosphate potential of both soils.     

一株新的溶磷草生欧文氏菌的分离、鉴定及其溶磷效果的初步研究

从湖南、湖北、云南等地磷矿开采场的土壤样品中筛选到一株溶磷能力较强的菌株P21,结合生理生化指标和16S rDNA序列分析鉴定其属于草生欧文氏菌菠萝变种(Erwinia herbicola var.ananas).该菌能溶解磷酸三钙、羟基磷灰石、磷酸铁、磷酸锌,其中对磷酸三钙和羟基磷灰石的每升液体培养基溶磷量(P2O5)分别高达1206.20mg、529.67mg.溶磷菌草生欧文氏菌菠萝变种P21对产地不同的8种磷矿石溶解能力不同,对云南晋宁和昆阳、四川雅安、江苏锦屏等地磷矿石有较强的溶解能力,每升液体培养基溶磷量分别为96.64mg、78.46mg、67.07mg、65.24mg,对其它产地的磷矿石溶解能力较差.实验表明,培养液的pH下降与溶磷菌P21的溶磷量无直接关系.     

Bioturbation-induced phosphorous release from an insoluble phosphate source

The influence of bioturbation caused by common carp fry in 5 L jars (5 L each) in the laboratory and in 150 L outdoor vats in increasing the fertilizer value of phosphate rock was evaluated. Soluble reactive phosphate (SRP) was determined to quantify the effects of bioturbation, fish excrements and soil. The level of SRP was always lowest in the control series. Introduction of common carp fry resulted in a net increase of 0.09-0.10 mg L(-1) of SRP attributable to the effect of fish excrement. Bioturbation caused by common carp resulted in a 64.8-90% influx of phosphate from bottom soil in the presence of phosphate rock but only about 6.3-7.2% in the absence of phosphate rock. The bioturbation that occurred in these treatments resulted in a significant release of phosphorous into the overlying water from the apatite source. The results confirm the benefits of the application of environmentally friendly phosphate rock in fish farming ponds at low cost.     

磷肥施用方式及类型对冬小麦产量和磷素吸收的影响

采用田间微区试验研究不同磷肥施用方式和种类对冬小麦生长和当季磷素吸收的影响.磷肥种类为磷酸二氢钙(MCP)和磷酸氢二铵(DAP),施用方式包括表面撒施,种子正下方5 cm条施,种子下方5 cm、偏3 cm条施,种子下方5 cm、偏10 cm条施,种子正下方20%土体混施5种.结果表明: 种子正下方5 cm条施对小麦的增产效果最高,其中磷酸二氢钙的产量达到7.63 t·hm^-2,磷酸氢二铵的产量达到7.99 t·hm^-2,分别较农民习惯撒施方式增产10.3%和10.7%.在5种施磷方式中,偏10 cm条施的小麦产量最低(6.60～6.77 t·hm^-2).种子正下方5 cm条施和20%土体混施处理的小麦总吸磷量均处于较高水平(34.4～35.6 kg·hm^-2),偏10 cm条施在小麦各生长阶段的吸磷量均显著低于其他施磷方式,但磷酸氢二铵偏10 cm条施的小麦总吸磷量较磷酸二氢钙高11.9%.表明将磷肥近距离集中施用于种子附近为该地区较为合理的施磷方式,在偏远距离条施下磷酸氢二铵对小麦的磷素吸收利用效果优于磷酸二氢钙.     

Effect of rock phosphate on soil properties and apparent phosphorus recovery in acid soil of Sumatra

The effects of rock phosphate (RP) on soil properties and apparent P recovery of corn in acid soil of Sumatra were investigated. The soil was dominated by kaolinitic minerals, very acid and low in extractable phosphorus. The experiment was conducted in two steps: incubation and greenhouse. The treatments were rock phosphate and triple superphosphate (TSP) at 0, 200, 400 and 600 µg P g^-1 for the incubation experiment, and at 0, 50, 100, 150 and 200 µg P g^-1 for greenhouse experiment In the incubation experiment, rock phosphate reduced exchangeable Al and increased pH_H2O better than TSP, and supplied Bray-1 extractable P as much as did TSP. In the greenhouse experiment, apparent P recovery values of rock phosphate were very close to those of TSP and the values tended to decrease at higher rates of P. Although corn yields of the rock phosphate treatment were lower than TSP, its relative agronomic effectiveness was quite high.     

Yield,root morphology and chemical composition of two pasture legumes as affected by lime and phosphorus applications to an acid soil

Summary Effects of increasing rates of lime (0, 900, 1725, and 3000 kg Ca(OH)₂/ha producing soil pH of 4.0, 4.7, 5.1 and 5.6) and P (50, 150, 250 and 350 kg P/ha) on top and root yield, root morphology and chemical composition of lotus (Lotus pedunculatus Cav.) and white clover (Trifolium repens L.), were studied, using an acid soil in a greenhouse experiment. Increasing rates of applied lime and phosphate resulted in substantial increases in top yields of both species but concomitant increases in root yield were small. In the unlimed soil, lotus out-yielded (tops and roots) white clover at all P levels. However, in the three limed treatments, white clover clearly out-yielded lotus. Yield response curves to applied P levelled off at the two highest lime rates for lotus but not for white clover. Nodulation and N content of white clover increased significantly with increasing lime applications, but for lotus there was a significant decrease in nodulation at the highest lime rate. Increased P rates had a small stimulatory effect on nodulation in both species. Of the total root weight, the percentage contribution of the tap and primary lateral root fractions was smaller and that of the secondary plus tertiary lateral roots was greater for lotus than for white clover although root length per unit weight tended to be larger for white clover at the two highest lime rates. Furthermore, lotus possessed longer and more numerous root hairs than white clover. Lime applications significantly decreased the percentage contribution of the tap and primary lateral roots to the total root weight and increased the percentage contribution of the secondary plus tertiary lateral roots. Al and Mn contents of tops and roots of both species decreased with increasing lime rates. There was a highly significant negative correlation between relative yield and Al content of lotus and white clover tops. In comparison with the limed treatments, in the unlimed treatments a greater percentage of total P, Al, Mn and N content accumulated in the roots of both species. In addition, lotus accumulated a much greater percentage Al in its roots than white clover.     

Influence of pH,exchangeable aluminium and 0.02M CaCl2-extractable aluminium on the growth and nitrogen-fixing activity of white clover (Trifolium repens) in some New Zealand soils

The effects of soil acidity on the growth and N₂-fixing activity of white clover in seven acid topsoils and subsoils of New Zealand were investigated using a glasshouse experiment.The application of phosphate (Ca(H₂PO₄)₂) to the soils resulted in very large increases in white clover growth on all soils. The application of phosphate, as well as increasing P supply, also decreased 0.02M CaCl₂-extractable Al levels, but had little effect on exchangeable Al levels.Where adequate phosphate was applied, increasing rates of lime (CaCO₃) resulted in increased plant growth on most soils. N₂[C₂H₂]-fixing activity was increased by the first level of lime for one soil, but generally remained approximately constant or declined slightly at higher rates of lime. Up to the point of maximum yield, white clover top weight was more highly correlated with 0.02M CaCl₂-extractable soil Al than with exchangeable Al or pH. At pH values greater than 5.5, plant yield declined on some soils, apparently because of Zn deficiency. The data suggest that white clover is unlikely to be affected by Al toxicity at 0.02M CaCl₂-extractable Al levels of less than about 3.3 g g^–1. However, there were differences between soils in apparent plant tolerance to 0.02M CaCl₂-extractable Al, which appeared to be caused by differing C levels in the 0.02M CaCl₂ extracts.