Boron Availability in Building up Fertility in Cerrado Soil of Tocantins

ABSTRACT

The expansion of agricultural activity in the Cerrado biome raises the importance of building soil fertility in micronutrients, however, the dynamics of these elements in different soil classes remains to be understood. The objective aimed to evaluate the availability of boron (B) in the soil in function of sources and incubation times to build the fertility of Oxisol and Entisol (Quartzipsamment). The experimental design was completely randomized with 50 treatments obtained in a 5 × 10 factorial scheme, being: five sources (boric acid, sodium octaborate, sodium tetraborate, boron oxide, and boron oxisulphate) and ten incubation times (0, 5, 10, 15, 25, 40, 55, 70, 85 and 100 days), with three repetitions. For all sources, the applied B dose was 4.0 mg dm^?3 in soil samples of 0.5 dm³, with pH corrected to 6.0. In the two soils evaluated, borate fertilization promoted significant effects (p ≤ 0.05) on the availability of B and the efficiency of fertilization over the incubation time. The highest levels of B available in soils resulted from the use of less soluble sources, representing a fertilization efficiency above 75% when using boron oxisulphate in the Oxisol and greater than 85% with the use of boron oxide in the Entisol. The sources of greater solubility achieved an average efficiency of 10.66%. It is concluded that fertilization with borate sources affects the availability of boron to the building of soil fertility, however, the most soluble ones are less efficient to maintain good availability (>0.5 mg dm^?3) after 40 days of application.     

Effect of Oxalic and Citric Acids on Zinc Release Kinetic in Two Calcareous Soils

Rate of zinc (Zn) release from solid to solution phase by organic acids can influence Zn availability in calcareous soils. The objective of the present study was to investigate the effect of different concentrations (1.1, 2.2, and 3.3 mM) of oxalic acid and citric acid on the kinetic release of Zn from two calcareous soils from Eastern Iran. The two organic acids showed significant difference in Zn release from studied soils. Cumulative Zn release during 72 h ranged from 5.85 to 10.4 mg kg^?1 in soil 1 and ranged from 8.7 to 16.9 mg kg^?1 in soil 2 using different concentrations of oxalic acid. The amount of cumulative Zn release after 72 h in soil 1 ranged from 13.65 to 28.77 mg kg^?1 and from 17.63 to 23.13 mg kg^?1 when different concentrations of citric acid was used. In general, Citric acid released 38% more Zn from soils than oxalic acid. The release of Zn from soils increased with citric acid concentration but decreased with increasing of oxalic acid concentrations in the solution. The simplified Elovich equation best described Zn release as a function of time (r² = 0.93 and SE = 0.78). From the present study, Zn release from soils can be limited by the higher concentration of oxalic acid, while citric acid is suitable for enhancing soil lability of Zn.     

Low-molecular weight organic acids improve plant availability of phosphorus in different textured calcareous soils

Understanding the role of organic acids on phosphorus (P) sorption capacity of soils is very important for its economic and friendly management. Combining P application with low-molecular weight organic acids could result in its higher plant availability for prolonged time. Therefore, citric and oxalic acid (at the rate of 1.0 mM kg^?1 soil) were evaluated for their effect on P sorption capacity and its plant availability in two different textured calcareous soils. Organic acids decreased P sorption capacity and organic carbon partition coefficient (K_oc) whereas increased Gibbs free energy (ΔG) of P. Organic-acid-treated soils required lesser quantity of P fertilizer to produce soil solution P concentration optimum for plant growth (external P requirement [EPR_0.2]), that is, 0.2 mg L^?1. Citric acid was efficient than oxalic acid in the above effects. P sorption parameters of Freundlich model were negatively correlated with lime potential and ΔG whereas had positive correlation (P < 0.05) with EPR_0.2 and K_oc. Incubation with oxalic acid increased available P in loamy sand and loam soil by 20% and 30%, respectively. Thus, organic acids could help reduce application rate of P fertilizer through lowering its adsorption in highly P-fixing soils without compromise on yield.     

Effects of low-molecular-mass organic acids on P nutrition and some plant properties of Hordeum vulgare

One of the strategies of the plants growing in phosphorus (P)-deficient environments is to exudate low-molecular-weight organic acids (LMWOA). Thus, we aimed to investigate the effect of LMWOA on phosphorus uptake of barley from either fertilizer or inherited soil phosphorus. The experiment was set up in full factorial arrangement in completely randomised design with two phosphorus (0 and 50 mg P kg^?1), five organic acids, LMWOA (malic acid, oxalic acid, citric acid, acetic acid, ascorbic acid), and four organic acid rates (0, 10, 20, and 30 mmol kg^?1). The effects of LMWOA on yield in descending order were: oxalic acid > ascorbic acid > malic acid > acetic acid > citric acid. The maximum P concentration in grain was obtained at 30 mmol kg^?1 LMWOA treatments. As a result, it was found that oxalic acid was the most effective LMWOA in increasing nutrient uptake induced grain yield with and without phosphorous fertilizer application.     

Phytoextraction of Lead from Soil from a Battery Recycling Site: The Use of Citric Acid and NTA

Phytoextraction is a soil remediation technique involving plants that concentrate heavy metals in their shoots, which may be removed from the area by harvest. The application of synthetic chelants to soil increases metal solubility, and therefore enhances phytoextraction. However, synthetic chelants degrade poorly in soil, and metal leaching poses a threat to human and animal health. The aim of this study is to assess the use of two biodegradable chelants (citric acid and nitrilotriacetic acid (NTA)) for Pb phytoextraction by maize from a soil contaminated by battery-casing disposal. In order to assess the behavior of a non-degradable chelant, ethylenediaminetetraacetic acid (EDTA) was also included in the experiment. The chelants NTA and EDTA were applied to soil pots at rates of 0, 3, 5, 7, and 10 mmol kg^?1 of soil. The rates used to citric acid were 0, 5, 10, 15, and 30 mmol kg^?1. Maize plants were grown for 72 days and chelants were applied 9 days before harvest. Soil samples were extracted with CaCl₂ to assess the Pb solubility after chelants application. The results showed that NTA was more efficient than citric acid to solubilize Pb from soil; however, citric acid promoted higher net removal of Pb (120 mg pot^?1) than NTA (57 mg pot^?1). Thus, the use of citric acid, a biodegradable organic acid, could be feasible for enhancing the phytoextraction of Pb from the site studied with no environmental constraints.     

Toxicity of imidacloprid to the earthworm Eisenia andrei and collembolan Folsomia candida in three contrasting tropical soils

Purpose

Imidacloprid is a widely used seed dressing insecticide in Brazil. However, the effects of this pesticide on non-target organisms such as soil fauna still present some knowledge gaps in tropical soils. This study aimed to assess the toxicity and risk of imidacloprid to earthworms Eisenia andrei and collembolans Folsomia candida in three contrasting Brazilian tropical soils.

Materials and methods

Acute and chronic toxicity assays were performed in the laboratory with both species in a tropical artificial soil (TAS) and in two natural soils (Oxisol and Entisol), at room temperature of 25 °C. The ecological risk was calculated for each species and soil by using the toxicity exposure ratio (TER) and hazard quotient (HQ) approaches.

Results and discussion

Acute toxicity for collembolans and earthworms was higher in Entisol (LC₅₀?=?4.68 and 0.55 mg kg^?1, respectively) when compared with TAS (LC₅₀?=?10.8 and 9.18 mg kg^?1, respectively) and Oxisol (LC_{50collembolans}?=?25.1 mg kg^?1). Chronic toxicity for collembolans was similar in TAS and Oxisol (EC_{50 TAS}?=?0.80 mg kg^?1; EC_{50 OXISOL}?=?0.83 mg kg^?1), whereas higher toxicity was observed in Entisol (EC₅₀?=?0.09 mg kg^?1). In chronic assays with earthworms, imidacloprid was also more toxic in Entisol (EC₅₀?=?0.21 mg kg^?1) when compared to TAS (EC₅₀?=?1.89 mg kg^?1). TER and HQ values indicated a significant risk of exposure of the species to imidacloprid in all soils tested, and the risk in Entisol was at least six times higher than in Oxisol or TAS.

Conclusions

The toxicity and risk of imidacloprid varied significantly between tropical soils, being the species exposure to this pesticide particularly hazardous in very sandy natural soils such as Entisol.

     

Phosphorus Nutrition of Upland Rice,Dry Bean,Soybean, and Corn Grown on an Oxisol

Rice, dry bean, corn, and soybean are important food crops. Phosphorus (P) deficiency is one of the most yield-limiting factors for these crops grown on highly weathered Brazilian Oxisols. Four greenhouse experiments were conducted to determine P requirements of these four crops. The P levels used were 0, 50, 100, 200, and 400 mg kg^?1. Growth, yield, and yield components evaluated of four crop species were significantly increased with the application of P fertilization. Most of the responses were quadratic in fashion when the P was applied in the range of 0 to 400 mg kg^?1. Maximum grain yield of upland rice was obtained with the application of 238 mg P kg^?1 of soil, maximum dry bean grain yield was obtained with the application of 227 mg P kg^?1 of soil, and maximum grain yield of soybean was obtained with the application of 224 mg P kg^?1 of soil. Maximum shoot growth of corn was obtained with the addition of 323 mg P kg^?1 of soil. Most of the growth and yield components had significant positive association with grain yield or shoot dry weight. Phosphorus concentration and uptake were greater in the grain compared to straw in upland rice and dry bean plants. Overall, P-use efficiencies decreased with increasing P rates.     

Citric acid enhances the mobilization of organic phosphorus in subtropical and tropical forest soils

Low-molecular-weight organic acids are considered to be effective in the release of inorganic phosphorus (P) but their effectiveness to mobilize organic P is not well understood. The aim of this study was to examine the role of three common organic acids (maleic, oxalic, and citric acids) in mobilizing organic P in forest soils. Soil samples tested in this study were collected from either native or plantation forests in subtropical and tropical Australia with 16–87% of soil total P being in organic form. At a concentration of 10 mM organic acid kg^?1 soil, all three organic acids did not enhance the release of inorganic P as compared with water, whereas the three organic acids displayed different capacities in mobilizing organic P. Citric acid significantly enhanced the solubilization of organic P by 34.7% as compared with water; whereas no significant differences were observed in the mobilization of organic P among maleic acid, oxalic acids, and water. The amount of organic P solubilized by citric acid was not correlated with soil pH but increased with increasing soil organic P as the values were below 200 mg kg.^?1 The possible mechanisms of the effective mobilization of organic P by citric acid were discussed. Our results implied that organic P might play an important role in P nutrition of plants in subtropical and tropical forests due to its substantial proportion in soil P and the effective mobilization by organic acids.     

Zinc,Copper, Boron and Iron Requirement of Upland Rice Grown on a Brazilian Oxisol

Deficiency of micronutrients increasing in field crops, including upland rice in recent years. The objective of this study was to determine requirement of zinc (Zn), copper (Cu) boron (B) and iron (Fe) for upland rice grown on a Brazilian Oxisol. The levels used were: Zn (0, 10, 20, 40, and 80 mg kg^?1), Cu (0, 5, 10, 20 and 40 mg kg^?1), B (0, 5, 10, 20 and 40 mg kg^?1) and Fe (0, 250, 500, 1000, and 2000 mg kg^?1). Plant height, straw yield, grain yield, panicle number and grain harvest index (GHI) were significantly improved with the addition of these micronutrients. Root growth was also improved with the application of micronutrients, except with the addition of B. Maximum grain yield was obtained with the addition of 51 mg Zn, 24 mg Cu, 5 mg B kg^?1, and 283 mg Fe kg^?1 soil. Similarly, maximum straw yield was obtained with the addition of 38 mg Zn, 17 mg Cu, 6 mg B kg^?1, and 1500 mg Fe kg^?1 soil. Maximum plant height was obtained with the addition of 54 mg Zn, 10 mg B kg^?1, and 1197 mg Fe kg^?1 soil. Copper did not affect plant height significantly. Maximum panicle number was obtained with the addition of 22 mg Cu kg^?1, 3 mg B kg^?1, and 1100 mg Fe kg^?1 soil. Zinc did not affect panicle number significantly. Maximum GHI was obtained with the addition of 61 mg Zn kg^?1, and 8 mg B kg^?1. Zinc was had a linear increase in GHI in the range of 0 to 80 mg kg^?1, and Fe showed a negative relationship with GHI.     

Fulvic acid in foliar spray is more effective than humic acid via soil in improving coffee seedlings growth

ABSTRACT

Humic (HA) and fulvic (FA) acids improve the nutrient availability and uptake by plants but some aspects of their agronomic use still need to be clarified. The effects of HA soil application and FA foliar application on the growth, Zn and B uptake by coffee seedlings were evaluated. HA was added to an Oxisol at concentrations 0, 10, 25, 50, 75 and 100 mg kg^?1 (C-HA), in both limed (pH 6.2) and overlimed (pH 7.2) conditions. FA (0, 0.2, 0.5 and 1 g L^?1 C-FA) was applied to coffee leaves in three different application modes (M): with 0.3% Zn and 0.6% B supplied via foliar (M₁), 0.6% B and 1.2% Zn supplied via foliar (M₂) and 1.2 mg kg^?1 B and 6 mg kg^?1 Zn supplied via soil (M₃). HA addition in soil significantly (p < 0.05) reduced leaf B and Zn accumulation and coffee growth in both pH conditions. In the M₁ and M₂, FA application significantly (p < 0.05) increased the shoot growth at 0.59 and 0.45 g L^?1 and B accumulation at 0.96 and 0.45 g L^?1 C-FA. Foliar application of C-FA, instead soil application of C-HA, is a suitable practice to improve coffee seedlings growth and nutrition on Oxisol.     

Yield,yield components,soil fertility,and nutritional status of soybean as influenced by limestone and copper interactions

Abstract

Continuous limestone application can inhibit the copper (Cu) uptake by plants. This experiment was carried out in greenhouse conditions using two soils (Typic Oxisol and Typic Entisol) with different clay and soil organic matter (SOM) levels to evaluate the effects of liming on Cu fertilization. The treatments consisted of two dolomitic limestone rates (0 and 7.5?g per pot, equivalent to 0 and 5.0?Mg ha^?1) and five Cu rates (0, 2, 4, 8, and 16?mg kg^?1). Regardless of the soil type, the limestone and Cu rate interaction did not affect the grain yield (GY), however, they did increase the productivity, shoot dry weight yield (SDWY), number of grains per pod, number of pods per pot, pod weight per pot, weight of 100 seeds, root volume, photosynthetic rate, and chlorophyll, and Ca, Mg, and Cu contents in the soil and leaves. It was concluded that for soybeans cultivated in Typic Entisol and Typic Oxisol, there was no association between 5.0?Mg ha^?1 of limestone and the Cu rates. However, in isolation, limestone and Cu rate caused a significant increase in the soybean productivity, physiological components, and yield characteristics.     

Remediation of Metal Contaminated Soil by Organic Metabolites from Fungi I—Production of Organic Acids

Investigations were made on living strains of fungi in a bioremediation process of three metal (lead) contaminated soils. Three saprotrophic fungi (Aspergillus niger, Penicillium bilaiae, and a Penicillium sp.) were exposed to poor and rich nutrient conditions (no carbon availability or 0.11 M d-glucose, respectively) and metal stress (25 µM lead or contaminated soils) for 5 days. Exudation of low molecular weight organic acids was investigated as a response to the metal and nutrient conditions. Main organic acids identified were oxalic acid (A. niger) and citric acid (P. bilaiae). Exudation rates of oxalate decreased in response to lead exposure, while exudation rates of citrate were less affected. Total production under poor nutrient conditions was low, except for A. niger, for which no significant difference was found between the poor and rich control. Maximum exudation rates were 20 µmol oxalic acid g^?1 biomass h^?1 (A. niger) and 20 µmol citric acid g^?1 biomass h^?1 (P. bilaiae), in the presence of the contaminated soil, but only 5 µmol organic acids g^?1 biomass h^?1, in total, for the Penicillium sp. There was a significant mobilization of metals from the soils in the carbon rich treatments and maximum release of Pb was 12% from the soils after 5 days. This was not sufficient to bring down the remaining concentration to the target level 300 mg kg^?1 from initial levels of 3,800, 1,600, and 370 mg kg^?1in the three soils. Target levels for Ni, Zn, and Cu, were 120, 500, and 200 mg kg^?1, respectively, and were prior to the bioremediation already below these concentrations (except for Cu Soil 1). However, maximum release of Ni, Zn, and Cu was 28%, 35%, and 90%, respectively. The release of metals was related to the production of chelating acids, but also to the pH-decrease. This illustrates the potential to use fungi exudates in bioremediation of contaminated soil. Nonetheless, the extent of the generation of organic acids is depending on several processes and mechanisms that need to be further investigated.     

Lowland Rice Response to Thermophosphate Fertilization

Abstract

Use of adequate rates of phosphorus (P) in crop production on high‐P‐fixing acid soils is essential because of high crop response to P fertilization and the high cost of P fertilizers. Information on lowland rice response to thermophosphate fertilization grown on Inceptisols is limited, and data are also lacking for soil‐test‐based P fertilization recommendations for this crop. The objective of this study was to evaluate response of lowland rice to added thermophosphate and to calibrate P soil testing for making P fertilizer recommendations. A field experiment was conducted for two consecutive years in central Brazil on a Haplaquept Inceptisol. The broadcast P rates used were 0, 131, 262, 393, 524, and 655 kg P ha^?1, applied as thermophosphate Yoorin. Rice yield and yield components were significantly increased with the application of P fertilizer. Average maximum grain yield was obtained with the application of 509 kg P ha^?1. Uptake of macro‐ and micronutrients had significant quadratic responses with increasing P rates. Application of thermophosphate significantly decreased soil acidity and created favorable macro‐ and micronutrient environment for lowland rice growth. Across 2 years, soil‐test levels of Mehlich 1–extractable P were categorized, based on relative grain yield, as very low (0–17 mg P kg^?1 soil), low (17–32 mg P kg^?1 soil), medium (32–45 mg P kg^?1 soil), or high (>45 mg P kg^?1 soil). Similarly, soil‐test levels of Bray 1–extractable P across 2 years were very low (0–17 mg P kg^?1 soil), low (17–28 mg P kg^?1 soil), medium (28–35 mg P kg^?1 soil), or high (>35 mg P kg^?1 soil). Soil P availability indices for Mehlich 1 extractant were slightly higher at higher P rates. However, both the extracting solutions had highly significant association with grain yield.     

Can root exudate components influence the availability of pyrene in soil?

Purpose

Little information is currently available regarding the influence of different root exudate components (RECs) on the availability of persistent organic pollutants in the soil environment. In this study, we investigated the impacts of different RECs including organic acids, amino acids, and fructose on the availability of pyrene as a representative polycyclic aromatic hydrocarbon (PAH) in soils.

Materials and methods

Citric acid, oxalic acid, malic acid, serine, alanine, and fructose were used in the experiments as representative RECs. Pyrene-spiked soils (TypicPaleudalfs) with present RECs were incubated for 30 days, and the available fraction of pyrene was determined using n-butanol extraction procedure.

Results and discussion

The amount of n-butanol-extractable pyrene in soil increased with the addition of tested RECs and increased when REC concentrations are enhanced within the range of 0–21 g kg^?1. The extractability of pyrene in soil with REC treatments and the enhancement ratio (r, %) of the extractable pyrene in soil by the addition of RECs after a 30-day incubation decreased in the following order: organic acids (oxalic acid ≥ citric acid > malic acid) > amino acid (alanine > serine) > fructose. This decrease was observed irrespective of soil sterilization, although the concentrations of extractable pyrene were lower in non-sterilized soils compared to sterilized soils. The concentrations of metal cations and dissolved organic matter (DOM) in solution increased when organic acids were added.

Conclusions

The tested RECs at concentrations of 0–21 g kg^?1 clearly enhanced the availability of pyrene in soils, and larger amounts of RECs resulted in higher pyrene availabilities in the tested soils. Microbial biodegradation diminished the amount of available pyrene irrespective of the presence of RECs. The mechanism of REC-influenced availability of pyrene in soil may be related to the metal dissolution and release of DOM from soil solids. The results of this study will be useful in assessing PAH-related risks to human health and the environment and will be instructive in food safety and remediation strategies at contaminated sites.     

Degradability of natural and synthetic chelating agents applied to a lead-contaminated soil

Purpose

Studying the rate of chelant degradation is important to select environmental friendly compounds to assist phytoextraction. The objective of the present study was to evaluate degradation rate of complexes formed between synthetic or organic chelants and Pb aiming to increase the efficiency of phytoextraction while reducing adverse effects resulting from the Pb leaching.

Materials and methods

The following six chelating agents were tested: citric acid P.A., commercial citric acid, glutamic acid P.A., monosodium glutamate, nitrilotriacetic acid (NTA), and ethylenediaminetetraacetic acid (EDTA), besides a control treatment (no addition of chelating agent); they were applied at a concentration of 10 mmol dm^?3 in pots containing 1 dm³ of Pb-contaminated soil.

Results and discussion

The results of this study showed that commercial citric acid adequately solubilized Pb to levels suitable for plant uptake and showed relatively rapid biodegradation in soil. Therefore, this commercial product may be a highly promising alternative for phytoextraction studies in the field. EDTA and NTA demonstrated high Pb solubilization ability but degraded comparatively slowly; therefore, they are not recommended for use in phytoextraction due to environmental risks regarding metal leaching.

Conclusions

The results of this study showed that commercial citric acid adequately solubilized Pb to levels suitable for plant uptake and showed relatively rapid biodegradation in soil, which is associated with a low risk of groundwater contamination. Therefore, this environmental friendly and low-cost product may be a highly promising alternative for inducing Pb phytoextraction.

     

Soil Phosphorus Tests for Flooded Rice Grown in Contrasting Soils and Cropping History

Soil phosphorus (P) tests for flooded rice (Oryza sativa L.) generally present uncertainties for estimating P availability. Bray 1, 1% citric acid, Mehlich 3, Olsen extractants (dry samples), and Bray 1 extractant after 3 days (BI3) and 7 days (BI7) of anaerobic incubations were evaluated to estimate P availability for rice in 43 Uruguayan soils. Field trials were conduced at each site (0, 13, 26, and 39 kg P applied ha^?1). Relative yield and absolute and relative yield increases were determined. Extracted P was variable for the different tests. For silty soils, P availability was better estimated by citric acid, Mehlich 3, and Bray 1, with similar soil P critical concentrations (6?8 mg P kg^?1). The BI3 and BI7 tests showed greater soil P critical concentration but poorer correlations with yield indexes. This study contributes to the scientific basis of P fertilization for flooded rice, promoting more effective fertilizer use and minimizing environmental P losses.     

Anionic Exchange Membranes as a Soil Test for Nitrogen Availability

Abstract

A better understanding of nitrogen (N) availability to crops remains an essential key for a productive and safe production system. The main objective of this study was to evaluate the potential of anionic exchange membranes (AEMs) as part of a soil‐testing procedure to predict in situ soil NO₃‐N availability for forage and corn produced in eastern Canada. The AEMs were buried in the surface horizon (0–15 cm) at four experimental sites for forage and at one site for corn. Treatments consisted of five NH₄NO₃ rates (0, 60, 120, 180, and 240 kg N ha^?1) in forage and of six anhydrous ammonia (0, 50, 100, 150, 200, and 250 kg N ha^?1) in corn production. In all sites, NO₃ ^? adsorbed on AEMs (NO_3AEMs) increased significantly with N fertilizer rates, indicating the ability of the AEMs to detect differences between N fertilizer treatments and to predict the soil N availability to crops. The NO_3AEMs fluxes were significantly related to soil NO₃‐N concentration as extracted by water or KCl (0.66≤R²≤0.95). Significant relationships between crop N uptake and NO_3AEMs were obtained (0.52≤R²≤0.94), suggesting that AEMs can be used as an index of soil N availability. Results indicated that AEMs provide a reasonably accurate evaluation of N availability to forage and corn. Because of their low cost, simplicity, and consistency over years, soils, and crops, AEMs could be efficiently used in soil N availability analysis.     

Biomass Production and Phosphorus Use Efficiency in Two Tithonia diversifolia (Hemsl.) Gray Genotypes

Little information exists on the phosphorus (P) use efficiency of Tithonia diversifolia under varying levels of soil P availability. This study evaluated biomass production, changes in tissue P concentration, P uptake, and P uptake and utilization efficiencies in a Costa Rican and Colombian T. diversifolia genotype when 0, 0.3, 5, and 30 mg P g^?1 were available. Biomass, root length and tissue P concentration increased significantly (P < 0.05) with increasing levels of P availability and with time. Phosphorus uptake (mg plant^?1) was significantly higher (P < 0.05) at 30 mg P g^?1. Phosphorus uptake (mg P mg^?1 P_f) and utilization (mg mg^?1 P) efficiencies were greatest at 0.3 and 5 mg P g^?1. Differences between genotypes showed that T. diversofilia from Colombia had a significantly higher (P < 0.05) biomass, tissue P concentration, root length, and a more effective uptake and utilization of P when availability of this nutrient was low.     

Phytoextraction Potential of Atriplex Nummularia Plants under Nitrogen and Phosphate Fertilization

The soil areas affected by salts have increased in recent years. Searching intensively for management and recovery strategies should help minimize these problems. Studies related to the response of halophytes to fertilization can provide important information regarding the most adequate management for phytoremediation. The aim of this study was to evaluate dry matter production and sodium extraction capacity of atriplex plants, in response to nitrogen doses, with and without phosphorus application. The experiment was carried out in a greenhouse at the Federal Rural University of Pernambuco (UFRPE), in Recife, Pernambuco, Brazil and was set up in a randomized block design, with four replicates, in a 2 × 5 factorial scheme (0 and 134 mg dm^?3 of P and 0, 20, 40, 60, and 80 mg dm^?3 of N). The addition of nitrogen (N) and improved sodium (Na) uptake increased Na contents by 4.1, 3.6, and 1.8 times, for P0, and by 4.0, 8.4, and 2.1, for P134, in leaves, stems, and roots, respectively. There was a decrease in Na both in the saturation-paste extract and in the exchange complex with the increase in N in soil. N supply potentiates Na extraction by Atriplex nummularia, being a feasible technique to recover saline soils through phytoremediation.     

PHOSPHORUS UPTAKE AND USE EFFICIENCY IN FIELD CROPS

Phosphorus (P) is required by crop plants for many physiological and biochemical functions. Knowledge of phosphorus uptake and its use by crop plants is essential for adequate management of this essential nutrient. A field experiment was conducted during four consecutive years to determine P uptake and use efficiency by upland rice, dry bean, corn and soybean grown in rotation on a Brazilian Oxisol. Plant samples were taken at different growth stages during the growth cycle of each crop for phosphorus analysis. Phosphorus concentration (content per unit dry matter) significantly decreased in a quadratic fashion with the advancement of plant age in four crop species. Phosphorus concentration was higher in legumes compared to cereals. Phosphorus uptake in shoot, however, significantly increased in an exponential quadratic fashion with the advancement of plant age of crop species. At harvest, P uptake was higher in grain compared to shoot, indicating importance of this element in improving crop yields. Phosphorus use efficiency (grain or straw yield per unit P uptake) was higher in cereals compared to legumes. The P use efficiency for grain production was 465 kg kg^?1 for upland rice, 492 kg kg^?1 for corn, 229 kg kg^?1 for dry bean and 280 kg kg^?1 for soybean. The higher P use efficiency in cereals was associated with higher yield of cereals compared to legume species.