Comparative performance of six Stylosanthes species in three acid soils

1980 ◽  
Vol 31 (1) ◽  
pp. 61 ◽  
Author(s):  
MMde Carvalho ◽  
CS Andrew ◽  
DG Edwards ◽  
CJ Asher ◽  
Carvalho MM De
Keyword(s):  
Maximum Yield ◽  
Acid Soils ◽  
Aluminium Toxicity ◽  
Exchange Capacity ◽  
Plant Performance ◽  
Aluminium Content ◽  
Comparative Performance ◽  
Aluminium Concentration ◽  
Nitrogen Deficiencies ◽  
Yield Responses

The yield rcsponse of six Stylosanthes species to a factorial combination of four lime rates and two phosphorus levels applied to three acid soils (Coolum, Kogan, Rochedale) was determined in a pot experiment. The unlimed soils were of similar pH, but differed widely in exchangeable aluminium content. Aluminium toxicity appeared to be a major limitation to growth in the three soils. In the unlimed soils, the most severe yield restriction was observed in the Coolum soil, which had the highest soluble aluminium concentration (55 �M), and the least restriction in the Kogan soil, which had the lowest soluble aluminium concentration (37 �M). All six species achieved maximum yield in the three soils when the soluble aluminium concentration was reduced to values below 21 �M . The strong yield responses observed with little change in soluble aluminium at the higher lime rates in the Coolum and Rochedale soils may be due to either a further reduction in aluminium toxicity associated with increasing concentration of soluble polymeric species or the direct alleviation of hydrogen ion toxicity. The observed responses to lime do not appear to involve direct calcium effects, nor do they involve alleviation of manganese toxicity or molybdenum deficiency. Maximum yield was associated with reduction in aluminium saturation to less than 5% of the effective cation exchange capacity in all three soils. However, when examined across the three soils, aluminium saturation and also the exchangeable aluminium content were both unsatisfactory predictors of plant performance. The largest and smallest restrictions on growth were observed in soils with similar aluminium saturation (Coolum 14.4%, Kogan 17.6% respectively), while the Rochedale soil with its much higher aluminium saturation (42.0%) was intermediate in degree of growth restriction. Phosphorus and nitrogen deficiencies also limited plant growth, but the magnitude of their effects varied among soils and species.

scholarly journals Bioaccumulation and Effects of Aluminium on Plant Growth in Three Culture Plants Species

2019 ◽  
Vol 70 (2) ◽  
pp. 602-604 ◽  
Author(s):  
Bogdan-Stefan Negreanu-Pirjol ◽  
Ticuta Negreanu-Pirjol ◽  
Rodica Sirbu ◽  
Dan Razvan Popoviciu
Keyword(s):  
Plant Growth ◽  
Acid Soils ◽  
Absorption Spectrometry ◽  
Aluminium Toxicity ◽  
Triticum Aestivum L ◽  
Shoot Length ◽  
Aluminium Content ◽  
Aluminium Concentration ◽  
Dry Biomass ◽  
Major Factors

Aluminium toxicity is one of the major factors that limit plant growth and development in many acid soils, by multiple, and still poorly understood mechanisms. In this paper, the aluminium content determinations were done through atomic absorption spectrometry method, on seedlings of three culture plants, Helianthus annuus L. (sunflower), Sinapis alba L. (white mustard) and Triticum aestivum L. (wheat), grown in hydroponic conditions with different aluminium concentrations (50, 100 and 250 mg/kg) expose. AAS data were correlated with biometrical determinations (shoot length and dry biomass) and leaf pigments concentration assessment. Results emphasize that none of the selected species accumulates aluminium in aboveground organs such as shoots and leaves, indicating that root exclusion and/or sequestration are the strategies employed by all three species for limiting aluminium toxicity. In all three studied species, both average shoot length and dry biomass tended to be lower at higher aluminium concentration. Due to high variations among seedlings grown at the same aluminium concentration expose, these differences are not statistically significant. In sunflower seedlings, chlorophyll a and carotenoids had maximum values at the highest aluminium concentration (250 mg/kg), while chlorophyll b was more abundant at 100 mg/kg. In mustard, all pigments had their maximum concentrations at 100 mg/kg, while in wheat, an aluminium concentration increase progressively lead to a drop in pigments concentration.

Rapidly extracted (0.02 M CaCl2-soluble) reactive aluminum as a measure of aluminum toxicity in soils

Soil Research ◽  
1989 ◽  
Vol 27 (4) ◽  
pp. 663 ◽  
Author(s):  
EA Close ◽  
HKJ Powell
Keyword(s):  
Salicylic Acid ◽  
White Clover ◽  
Aluminum Toxicity ◽  
Maximum Yield ◽  
Acid Soils ◽  
Aluminium Toxicity ◽  
Field Method ◽  
Colorimetric Analysis ◽  
Aluminium Species

This paper examines the use of short extraction times, and the determination of aluminium with chrome azurol S (CAS), for the estimation of 0.02 M CaCl2-soluble aluminium in soils. It reports the correlation between CAS-reactive aluminium in 5 min extracts and percent maximum yield of white clover (Trifolium repens) for a series of acid soils. The reactivity of soluble and colloidal aluminium species with the metallochromic reagent CAS has been assessed. ~ l ( a q ) ~ + , simple hydroxy species and complexes of weakly binding ligands (salicylic acid, tannins) are CAS-reactive (2 rnin). In contrast, complexes of strongly binding ligands (citric acid, fulvic acid) are not CAS-reactive ([Al] ~ [L] ~ [CAS] ~ 1-2~10-5 M). For a series of six limed phosphated topsoils and subsoils (pH 4.2-5.5), 0.02 M CaCl2- soluble aluminium, as determined with CAS, was negatively correlated against the percent maximum yield of white clover; r2 = -0.73** (5 min extraction), n = 20. This correlation is similar to that for yield against total aluminium as determined by atomic absorption spectroscopy after 60 min extraction (r2 = -0.77**). However, the colorimetric analysis is more convenient and sensitive; further, it does not measure colloidal and polymeric aluminium species (which may not be plant-available). The satisfactory correlation achieved for short extraction times suggests use of CAS for a rapid field method for aluminium toxicity in soils.

The assessment of available manganese and aluminium status in acid soils under subterranean clover pastures of various ages

1983 ◽  
Vol 23 (121) ◽  
pp. 192 ◽  
Author(s):  
SM Bromfield ◽  
RW Cumming ◽  
DJ David ◽  
CH Williams
Keyword(s):  
Ammonium Acetate ◽  
New South ◽  
Acid Soils ◽  
Subterranean Clover ◽  
Exchange Capacity ◽  
Manganese Toxicity ◽  
Manganese Concentration ◽  
South Wales ◽  
Yield Responses ◽  
Practical Measure

Three methods of estimating available manganese and aluminium status in acid soils were compared on three groups of soils from the Pejar district near Goulburn, New South Wales in which differences in pH had been brought about by different periods under subterranean clover pasture. Managanese extracted by 0.01 M calcium chloride gave the best correlation with the manganese concentration in rape and subterranean clover grown in pot culture, and provided the best index of available manganese. Soil solution manganese was inferior to CaCl2-extractable manganese and was more difficult to determine. Extraction with neutral ammonium acetate was unsatisfactory because this reagent overestimated available forms of manganese in soils containing high levels of reactive manganese. Aluminium extracted by 0.01 M CaCl2 was well correlated with exchangeable aluminium and with percentage aluminium saturation of the effective cation exchange capacity. None of the three measures of aluminium status alone was an effective index for predicting lime response by rape on these soils because both manganese and aluminium status were involved in this response. These three parameters were equally effective in multiple regressions for yield responses of rape to lime. Because of its relative ease of determination, CaCl2 extraction is preferred as a practical measure of aluminium status. Aluminium interacted with and increased the toxic effects of manganese in rape. Thus CaCl2-extractable manganese alone only provided a satisfactory index of a 'critical' value for manganese toxicity in rape for soils low in available aluminium. Subterranean clover was only slightly affected by aluminium and manganese levels in these soils, and manganese toxicity symptoms were only observed on soils containing 50 ppm or more CaCl2-extractable manganese. Nodulation failure in pots occurred in all soils with pH below 5.2 (water) or below 4.3 in CaCl2, whereas nodulation was normal when these soils were treated with CaCO3 to raise the pH to 5.8-6.0 (water). With one exception nodulation appeared adequate at field sites from which soils showing nodulation failure in the glasshouse had been collected.

Responses of five pasture species to phosphorus, lime, and nitrogen on an infertile acid soil with a high phosphate sorption capacity

1970 ◽  
Vol 21 (5) ◽  
pp. 677 ◽  
Author(s):  
KR Helyar ◽  
AJ Anderson
Keyword(s):  
Soil Ph ◽  
White Clover ◽  
Phosphorus Deficiency ◽  
Acid Soil ◽  
Maximum Yield ◽  
Subterranean Clover ◽  
Aluminium Toxicity ◽  
Exchange Capacity ◽  
Growth Responses ◽  
Phosphorus Requirement

The growth responses of Lolium pevenne L. cv. Clunes, Phalavis tubevosa L. cv. Australian Commercial, Trifolium subterraneurn L. cv. Mount Barker, Trifolium vepens L. cv. Victorian, and Medicago sativa L. cv. Hunter River to lime, superphosphate, and nitrogen were compared in a field experiment on a soil with a pH of 4.9-5.4 (115 soil/water ratio) and with the cation exchange capacity 25-50% saturated by aluminium. The soil had a high phosphorus requirement. The effects of superphosphate and lime on the sodium bicarbonate extractable phosphorus levels and on the soil pH are discussed. Lucerne was one of the least productive species at most harvests. It required more superphosphate than subterranean clover, perennial ryegrass, or white clover to attain any given percentage of maximum yield. The visual symptoms of the plants and the yield interactions showed little evidence of effects of high aluminium, which indicated that the superphosphate was needed to correct phosphorus deficiency rather than to counteract any aluminium toxicity. The initial soil pH was somewhat higher than the levels previously found to be associated with aluminium toxicity on the soil in pots. Phalaris growth was increased to the highest superphosphate level, but growth at lower levels improved with time. Subterranean clover growth was depressed by the highest superphosphate level early in the season. The other species were not affected in this way. More lime was needed for lucerne than for white clover, which in turn needed more lime than subterranean clover. Nitrogen decreased the response of clover to lime, and the evidence indicates that the response of the legumes to lime was due mainly to the effect of lime in improving nodulation and nitrogen fixation. The lime-treated subterranean clover responded to nitrogen, especially in the first few months after sowing. The grasses responded markedly to nitrogen, while lime had a small effect on their growth and response to nitrogen. In no case did lime decrease the requirement for superphosphate.

Liming effects on soil exchangeable and soil solution cations of 4 soil types in north-eastern Victoria

Soil Research ◽  
1995 ◽  
Vol 33 (2) ◽  
pp. 277 ◽  
Author(s):  
WJ Slattery ◽  
GR Morrison ◽  
DR Coventry
Keyword(s):  
Grain Yield ◽  
Cation Exchange ◽  
Soil Solution ◽  
Cation Exchange Capacity ◽  
Acid Soils ◽  
Exchange Capacity ◽  
Soil Types ◽  
Organic C ◽  
North Eastern ◽  
Yield Responses

The effects of lime additions on exchangeable and soil solution cations of four soil types in north-eastern Victoria are discussed. Liming significantly (P < 0.05) reduced the concentration of exchangeable (1 M KCl), extractable (0.01 M CaCl2), soil solution total and monomeric aluminium. Raising the soil pHCa to 4.8 decreased Ale, concentrations below 1 mg kg-1, Al saturation % of the effective cation exchange capacity below 5 and AlTot below 5 PM; and raising the soil pHCa to 5.8 decreased MnCa concentrations below 10 mg kg-1 and AlTot below 2�m on the four soil types used in this study. Grain yield responses were best described by the sum of the activities of the Al monomers. Where organic C was present, responses could also be attributed to the complexing of monomeric Al. Grain yield responses could not always be reliably predicted by the Al saturation % of the effective cation exchange capacity. Liming significantly (P < 0.05) increased the concentration of Ca in the ECEC, but the Ca activity was not well correlated with lime response for all sites. The In ratio of aCa2+/�aAl- mono shows promise in predicting negative responses to lime applications (with values > 6) where soil pHCa is less than 5. The combination of Ca activity and the sum of the activity of the Al monomers, together with organic C content, may provide a better description of the responsiveness of acid soils to lime applications.

Effects of Application Method and Rate on Control of Sclerotinia Blight of Peanut with Iprodione and Fluazinam1

2001 ◽  
Vol 28 (1) ◽  
pp. 28-33 ◽  
Author(s):  
J. P. Damicone ◽  
K. E. Jackson
Keyword(s):  
Disease Control ◽  
Disease Incidence ◽  
Maximum Yield ◽  
Wide Band ◽  
Yield Response ◽  
Application Method ◽  
Sclerotinia Blight ◽  
Progress Curve ◽  
Application Methods ◽  
Yield Responses

Abstract Two trials with iprodione and three trials with fluazinam were conducted to assess the effects of application method and rate on the control of Sclerotinia blight of peanut with fungicide. In order to concentrate the fungicides near the crown area where the disease causes the most damage, applications were made through a canopy opener with a single nozzle centered over the row to achieve a 30.5-cm-wide band (canopy opener), and through a single nozzle centered over the row to achieve a 46-cm-wide band (band). Broadcast applications were compared to these methods at rates of 0, 0.28, 0.56, and 1.12 kg/ha on the susceptible cultivar Okrun. Sclerotinia blight was severe, with &gt; 70% disease incidence and &lt; 2000 kg/ha yield for the untreated controls in each trial. Linear reductions in area under the disease progress curve (AUDPC), but not final disease incidence, with iprodione rate were significant (P &lt; 0.05) for all methods of application. However, the rate of decrease did not differ among application methods. Linear increases in yield with rate of iprodione were greater for canopy opener compared to the band or broadcast applications. Only a 50% reduction in AUDPC and a maximum yield of &lt; 2700 kg/ha was achieved with iprodione using the best method. At the maximum rate of 1.12 kg/ha, fluazinam provided &gt; 75% disease control and &gt; 4000 kg/ha yield for all application methods. Differences in disease control and yield among application methods only occurred at the 0.28 and 0.56 kg/ha rates of fluazinam. Reductions in AUDPC with fluazinam rate were quadratic for all application methods, but AUDPC values were less for the canopy opener and band methods at 0.28 and 0.56 kg/ha compared to the broadcast methods. The yield response to rate for broadcast applications of fluazinam was linear. However, predicted yield responses to fluazinam rate were quadratic for the band and canopy opener methods and approached the maximum response at 0.84 kg/ha. Targeting fungicide applications using the band and/or canopy opener methods was beneficial for fluazinam at reduced rates. Disease control with iprodione was not adequate regardless of application method.

Effects of biochars generated from crop residues on chemical properties of acid soils from tropical and subtropical China

Soil Research ◽  
2012 ◽  
Vol 50 (7) ◽  
pp. 570 ◽  
Author(s):  
Jin-Hua Yuan ◽  
Ren-Kou Xu
Keyword(s):  
Soil Ph ◽  
Crop Residues ◽  
Chemical Properties ◽  
Acid Soils ◽  
Base Cations ◽  
Exchange Capacity ◽  
Chemical Compositions ◽  
Subtropical China ◽  
Exchangeable Base Cations ◽  
Exchangeable Acidity

The chemical compositions of biochars from ten crop residues generated at 350°C and their effects on chemical properties of acid soils from tropical and subtropical China were investigated. There was greater alkalinity and contents of base cations in the biochars from legume residues than from non-legume residues. Carbonates and organic anions of carboxyl and phenolic groups were the main forms of alkalis in the biochars, and their relative contributions to biochar alkalinity varied with crop residues. Incubation experiments indicated that biochar incorporation increased soil pH and soil exchangeable base cations and decreased soil exchangeable acidity. There were greater increases in soil pH and soil exchangeable base cations, and a greater decrease in soil exchangeable acidity, for biochars from legume than from non-legume residues. The biochars did not increase the cation exchange capacity (CEC) of soils with relatively high initial CEC but did increase the CEC of soils with relatively low initial CEC at an addition level of 1%. The incorporation of biochars from crop residues not only corrected soil acidity but also increased contents of potassium, magnesium, and calcium in these acid soils from tropical and subtropical regions and thus improved soil fertility.

scholarly journals Impacts of Phosphogypsum, Soluble Fertilizer and Lime Amendment of Acid Soils on the Bioavailability of Phosphorus and Sulphur under Lucerne (Medicago sativa)

Plants ◽  
2020 ◽  
Vol 9 (7) ◽  
pp. 883
Author(s):  
Moussa Bouray ◽  
Jim Moir ◽  
Leo Condron ◽  
Niklas Lehto
Keyword(s):  
Medicago Sativa ◽  
Acid Soils ◽  
Low Fertility ◽  
Dual Roles ◽  
Olsen P ◽  
Positive Effects ◽  
Grassland Ecosystems ◽  
Nitrogen Inputs ◽  
Soluble Fertilizer ◽  
Yield Responses

Legumes play critical dual roles in grazed grassland ecosystems; providing nitrogen inputs and high-quality feed for grazing livestock. However, many species fail to persist in acidic, low fertility soils. A glasshouse study was conducted to investigate the response of lucerne (Medicago sativa) to phosphogypsum (PG), lime and soluble P + S fertilizer (PS) application to two soils. Phosphorus and sulphur were applied through either PG (0, 1, 3 and 9 t ha−1) or P + S fertilizer at equivalent rates to PG. Both PG and PS were applied with or without lime, which was applied at 2 t ha−1. Yield and nutrient uptake of the lucerne was measured, while the soil was analyzed for pH, Olsen P and exchangeable aluminum. Yield responses were significantly different between the two soils. Maximum yields and P and S uptakes were obtained under PG 9 t ha−1 combined with lime. Exchangeable Al decreased in both soils under 1 ha−1 of PG compared with the control. At the highest rate, Olsen P increased by 8 and 6 mg kg−1 for PG and by 6 and 11 mg kg−1 for PS compared with the control for Glenmore and Molesworth soils respectively. Phosphogypsum showed positive effects on P and S bioavailability.

ESTIMATION OF THE INORGANIC AND ORGANIC pH-DEPENDENT CATION EXCHANGE CAPACITY OF THE B HORIZONS OF PODZOLIC AND BRUNISOLIC SOILS

1968 ◽  
Vol 48 (1) ◽  
pp. 53-63 ◽  
Author(s):  
J. S. Clark ◽  
W. E. Nichol
Keyword(s):  
Organic Matter ◽  
Cation Exchange ◽  
Cation Exchange Capacity ◽  
Acid Soils ◽  
Exchange Capacity ◽  
Hydrous Oxides ◽  
Before And After ◽  
Ph Dependent ◽  
The Difference ◽  
Wyoming Bentonite

Heating in hydrogen peroxide, dilute oxalic acid, and dilute aluminum oxalate did not change the effective cation exchange capacity (CEC) or the pH-7 CEC of Wyoming bentonite and Alberni clay soil containing excess Al(OH)x. This indicated that treatment of soils with H2O2 to oxidize organic matter and the possible production of oxalates during oxidation did not change the CEC values of the inorganic fraction of soils even if some clay exchange sites were blocked by hydrous oxides of Al.With soils of pH less than approximately 5.4, oxidation of organic matter did not change the effective CECs although the pH-7 CEC values were decreased. Thus, organic matter in acid soils appeared to have little or no effective CEC. Because of this and the negligible effect of H2O2 oxidation on the CEC values of clays, the difference of the pH-7 CEC of soils before and after H2O2 oxidation provided a simple means of estimating the amount of organic pH-dependent CEC in acid soils.The amount of organically derived pH-dependent CEC was determined in a number of soils by means of peroxide oxidation. The technique provided a useful indication of the quantities of sesquioxide–organic matter complexes accumulated in medium- and fine-textured soils.

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