Sodium bicarbonate‐DTPA test for macro‐and micronutrient elements in soils

Abstract

Individual soil tests are used to assess plant nutrient element needs. Separate soil tests, however, are time consuming and costly. Our objective was to develop a 0.5M sodium bicarbonate (NaHCO₃) soil phosphorus (P) test in combination with 0.005M diethylenetriaminepentaacetic acid (DTPA) so macronutrient dements: ammonium‐nitrogen (NH₄‐N), nitrate‐nitrogen (NO₃‐N), P, potassium (K), calcium (Ca), and magnesium (Mg); and micronutrients: iron (Fe), manganese (Mn), zinc (Zn), and copper (Cu) could be quantified in one extraction. The NaHCO₃‐DTPA extracting solution is a combination of 0.5M NaHCO₃ and 0.005M DTPA and has a pH of 7.60±0.05. Sodium in the solution enhances the NH₄, K, Ca, and Mg extraction; bicarbonate (HCO₃) is for P extraction; DTPA chelates Ca, Mg, and micronutrients; and the water is for NO₃ extraction. Soil samples (0–15 cm depth) came from two sources. The first set was from 12 N x P dryland proso millet (Panicum miliaceum L.) experiments, conducted from 1985 through 1987 in eastern Colorado. These soils were extracted with potassium chloride (KCl), NaHCO₃, ammonium acetate (CH₃‐COONH₄), DTPA, ammonium bicarbonate DTPA (AB‐DTPA), and with the NaHCO₃‐DTPA solutions. The second set included 25 soils from Alabama, Georgia, North Carolina, and South Carolina and were analyzed only for available P with the NaHCO₃ and NaHCO₃‐DTPA methods. Simple linear correlations for macronutrient elements and micronutrients were highly significant. Critical levels for the macronutrient elements: NO₃‐N, P, and K were 27, 11, and 144 mg kg^‐1, respectively; and the critical levels for the micronutrients: Fe, Mn, Zn, and Cu were 3.9, 0.35, 0.97, and 0.24 mg kg^‐1, respectively.     

Underestimation of Available Phosphorus by Resin–Bicarbonate and Olsen Tests in Calcareous Soils treated with Gypsum

In the present study, Olsen [0.5 M sodium bicarbonate (NaHCO₃), pH 8.5] and resin–bicarbonate (HCO₃) tests underestimated available phosphorus (P) in calcareous soils treated with gypsum (CaSO₄). The reaction of CaSO₄ and HCO₃ ^? ion or resin–HCO₃ to form calcium carbonate (CaCO₃) precipitate reduced the strength of the Olsen NaHCO₃ extractant and resin–HCO₃ strip for P extraction. The iron (Fe) oxide–impregnated filter paper (Pi strip) was independent of CaSO₄ influence and thus correctly estimated soil‐available P with respect to plant response to soil‐available P. Two greenhouse experiments were conducted with maize and wheat grown on calcareous soils treated with different rates of CaSO₄. The results confirmed that Olsen and resin–HCO₃ tests should not be used to measure available P or labile P in the P fractionation scheme in the calcareous soils containing significant amounts of gypsum.     

Relationship between leaf apoplast pH and iron chlorosis of sunflower (Helianthus annuus L.)

A hypothesis has been presented and tested that bicarbonate (HCO₃) and nitrate (NO₃) are the most important anions inducing iron (Fe) chlorosis because these anions increase the pH of leaf apoplast which in turn depresses ferric‐iron [Fe(III]) reduction, and hence, the uptake of Fe into the symplasm. Experiments with young sunflower (Helianthus annuus) plants showed that nutrition with NO₃ as the sole nitrogen (N) source induced chlorosis whereas ammonium nitrate (NH₄NO₃) did not. Monohydrogen carbonate (bicarbonate) also favoured the development of chlorosis. The degree of chlorosis was not related to the Fe concentration in the leaves. Both anion species, NO₃ and HCO₃, increased the pH of the leaf apoplast which was measured by means of the fluorescence dye 5‐carboxyfluorescein. A highly significant negative correlation between leaf apoplast pH and chlorophyll concentration in the leaves (r = ‐0.97) was found. Ferric‐Fe reduction in the apoplast—measured by means of ferrocene—provided evidence that a low leaf apoplast pH, obtained with ammonium (NH₄) supply, favoured the reduction of Fe(III) as compared with a higher leaf apoplast pH obtained with NO₃ supply. These results support the hypothesis tested.     

Iron chlorosis development and growth response of peach rootstocks to bicarbonate 1

For dicots, bicarbonate (HCO₃‐) is regarded as a main factor in the induction of iron (Fe) chlorosis in calcareous soils, and sand and solution culture. In sand culture experiments, peach [Prunus persica (Batsch) L.] rootstock developed chlorosis only when HCO₃‐ levels were equal to or higher than 6 mM. Above this level, chlorosis increaeed as HCO3‐ level was increased. In spite of the lack of chlorosis at to or below 6 mM of HCO₃‐, large growth reductions (40–60% reduction in fresh shoot weight) were seen in all rootstocks, although the tolerant rootstock had less reduction than the more susceptible rootstocks. Shoot growth was affected by HCO₃‐ more than was root growth.     

Comparative investigation on the susceptibility of faba bean (Vicia faba L.) and sunflower (Helianthus annuus L.) to iron chlorosis

Comparative physiological studies on iron (Fe) chlorosis of Vicia faba L. and Helianthus annuus L. were carried out. High internal Fe contents in Vicia cotyledons (16–37 μg) were completely used for plant growth and Fe chlorosis was not inducible by the application of nitrate (with or without bicarbonate). In Helianthus, low quantities of Fe in the seeds (4 μg) were insufficient for normal growth and without Fe in the nutrient solution, Fe chlorosis was obtained in all treatments. This chlorosis was an absolute Fe deficiency. Also, the treatment with 1 μM Fe in the nutrient solution and nitrate (with or without bicarbonate) led to severe chlorotic symptoms associated with low leaf Fe concentrations and high Fe concentrations in the roots. In contrast, Helianthus grown with NH₄NO₃ and 1 μM Fe had green leaves and high leaf Fe concentrations. However, with NO₃ supply (with or without bicarbonate), Fe translocation from the roots to the upper plant parts was restricted and leaves were chlorotic. Chlorotic and green sunflower leaves may have the same Fe concentrations, leaf Fe concentration being dependent on Fe translocation into the leaf at the various pH levels in the nutrient solution. At low external pH levels (controlled conditions) more Fe was translocated into the leaf leading to similar leaf Fe concentrations with higher chlorophyll concentrations (NH₄NO₃) and with lower chlorophyll concentrations (NO₃). This indicates a lower utilization of leaf Fe of NO₃ grown sunflower plants. Utilization of Fe in faba bean leaves is presumably higher than in sunflower leaves. In Vicia xylem sap pH was not affected by nitrate. In contrast, the xylem sap pH in Helianthus was permanently increased by about 0.4 pH units when fed with nitrate (with or without bicarbonate) compared with NH₄NO₃ nutrition. The xylem sap pH is indicative of leaf apoplast pH. From our earlier work (Mengel et al., 1994; Kosegarten und Englisch, 1994) we therefore suppose that in Helianthus, Fe immobilization occurs in the leaf apoplast due to high pH levels when grown with nitrate (with or without bicarbonate).     

Effect of bicarbonate on iron reduction by soybean roots 1

Release of reducing compounds by soybean (Glycine max (L.) Merr.] roots has been identified as an adaptive response mechanism to iron‐deficiency conditions which result in chlorosis. These compounds facilitate the conversion of Fe⁺³ to the metabolically active Fe⁺² form, allowing for increased uptake by roots in solution culture experiments. Degree of chlorosis is closely associated with HCO₃ concentration; however, the relationship between that ion and root reduction potential apparently has not been studied. We examined the effect of HCO₃‐ on root reduction potential of ten commercially‐grown soybean cultivars known to differ in chlorosis expression in the field. Root reduction potential was measured spectrophotometrically at 594 nm on samples of nutrient solution containing reduced Fe⁺² . Plants were grown with 5 mM NaHCO₃ or in HCO₃ ^‐‐free solutions. Averaged over cultivars, 0.205 umoles Fe⁺³ were reduced in the HCO₃ ^‐‐free solutions while only 0.009 umoles Fe⁺³ were reduced in the solutions containing HCO₃ ^‐. No significant differences were observed among cultivars for root reduction potential within either HCO₃ ^‐ treatment. Results from this study suggest that HCO₃ ^‐ may inhibit iron absorption by limiting the ability of roots to release reducing compounds which make available Fe⁺2 in the soil solution. This may partially explain the role of HCO₃ ^‐ in reducing chlorosis.     

RELATIVE SUSCEPTIBILITY OF SOME PRUNUS ROOTSTOCKS IN HYDROPONICS TO IRON DEFICIENCY

The susceptibility of eleven Prunus rootstocks to iron (Fe) deficiency was studied in hydroponics by growing them with 20 μM Fe, 0 μM Fe or 3 μM Fe+10 mM sodium bicarbonate. Based on the intensity of leaf chlorosis, the peach-almonds PR 204/84, Stylianidis K and KID2, produced at the Pomology Institute of Naoussa (Greece), showed the same or even greater tolerance than GF 677, the Greek peach-almond Retsou x Nemaguard, the plum-almond Myrandier 617 and the peaches GF 305, IDS 37, Greek wild peach seedling the greatest susceptibility whereas the plums St. Julien GF655/2 and Myrobalan 29C intermediate. Rootstocks without Fe presented significantly lower nitrogen and Fe whereas with bicarbonate significantly lower nitrogen, phosphorus, Fe and zinc. Root ferric chelate reductase activity was significantly increased in ?Fe rootstocks but negatively correlated with their tolerance; physiological and morphological changes were observed along a zone of a few centimeters length, 1–2 mm behind the root tip.     

Selection of Suitable Extractant for Predicting the Response of Chickpea to Zinc Application in Vertisols

Twenty-four surface soils (0–15 cm) were collected from Tal land soils (vertisols) in the southern part of Bihar state in India. Six extractants were used to predict the extractability and their suitability for measuring available zinc (Zn) in these soils. Pot experiment with chickpea (Cicer arietinum cv. C-235) as test crop was conducted with five levels of Zn (0, 2.5, 5.0, 7.5, and 10.0 mg kg^?1) to determine critical levels of Zn in soils and chickpea. The efficiency rating of different extractants in extracting available Zn from soils followed the order ethylenediaminetetraacetic acid (EDTA)–ammonium carbonate [(NH₄)₂CO₃] > diethylenetriaminepentaacetic acid (DTPA)–ammonium bicarbonate (NH₄HCO₃) > DTPA– calcium chloride (CaCl₂) > DTPA–sodium bicarbonate (NaHCO₃) > magnesium nitrate [Mg (NO₃)₂] > magnesium chloride (MgCl₂). The DTPA-CaCl₂-extractable Zn was significantly and positively correlated with clay, organic carbon, cation exchange capacity, dry-matter yield, and plant Zn concentration and uptake but significantly and negatively correlated with soil pH. These properties attributed 87% variability in DTPA-CaCl₂-extractable Zn.     

Investigation of relationships between iron status of peach leaves and soil properties

This study investigated those soil factors related to iron (Fe) chlorosis between Fe status of peach leaves and some soil properties in the Antalya region of Turkey. The total Fe content of leaves was negatively correlated with soil pH and the organic matter content of the soils. Extractable Fe (by 1N HCl) was negatively correlated with the calcium carbonate (CaCO₃) and bicarbonate (HCO₃‐) content of the soils. In addition, both total‐ and extractable‐Fe contents of leaves were also negatively correlated with the copper (Cu) content of the soils. On the other hand, significant correlations were found among the Fe index, P/Fe ratio of leaves, and soil pH, phosphorus (P), zinc (Zn), and Cu content of the soils. It appears from these studies that high pH, and the CaCO₃, HCO₃‐, and Cu contents are effective soil factors affecting the availability of Fe and its uptake by the peach trees, and these soil factors were associated with severity of Fe chlorosis in the studied area.     

Influence of Potassium Substitution by Rubidium and Sodium on Growth,Ion Accumulation,and Ion Partitioning in Bean under High Alkalinity

ABSTRACT

The effects of partial and complete substitution of potassium (K⁺) by rubidium (Rb⁺) and sodium (Na⁺) on plant growth and ion accumulation and partitioning was studied in bean young plants cultivated in nutrient solution with or without bicarbonate (HCO₃ ^?)-induced alkalinity. Plant growth was significantly decreased due to alkalinity and the substitution of K⁺, being leaves more affected than roots. Rubidium caused a severe toxicity reflected in a reduction in root dry mass and total chlorophyll concentration. Ion partitioning was markedly altered by alkalinity. Content of nitrogen (N), calcium (Ca), magnesium (Mg), iron (Fe), K, and Na were more accumulated in the roots in HCO₃ ^?-treated plants, while decreased in the shoot. Iron (Fe) was accumulated at similar extent in plants with and without high alkalinity, except in plants grown in Rb⁺ solutions. However, Fe was more accumulated in the roots, suggesting that chlorophyll synthesis was impaired by reduced translocation or internal inactivation of Fe. Zinc total uptake was severely reduced under high alkalinity in plants grown in Na⁺ solutions, maybe due to decreased Zn activity. Calcium was translocated more actively to the leaves and Mg was accumulated more in the roots of plants in Na⁺solutions. Despite the severe decrease in plant dry mass caused by Rb⁺, there was a higher translocation of N, phosphorus (P), Ca, Mg, Fe, zinc (Zn), copper (Cu), and manganese (Mn) from the roots to the leaves.     

Lime‐induced chlorosis in quince rootstocks: Methodological and physiological aspects

Two quince rootstocks for pear, clone MA and Ct.S.306, were screened to evaluate their threshold tolerance rate to lime‐induced chlorosis. Another important objective was to correlate the results of a chlorophyll analysis with observed chlorosis symptoms. The ron content in leaves was insufficient to determine the amount of iron available to the plant. The use of sodium bicarbonate (NaHCO₃) in the hydroponic culture of pear was found to be the preferable over calcium carbonate (CaCO₃) because of its higher solubility.     

SOIL ALKALINITY. II THE EFFECTS OF Na2CO3 ON IRON AND MANGANESE SUPPLY TO TOMATOES

Sodium carbonate added to nutrient solution in sand culture depressed the growth of tomatoes both by the influence of high pH and HCO₃^? causing chlorosis and by the effect of Na⁺. Foliar sprays of iron and manganese removed chlorosis and increased growth but did not remove the effect of Na. In a sandy soil Na₂CO₃ did not cause chlorosis but Na⁺ depressed yield. Chelated Fe and Mn in the soil solutions (up to 7.3 × 10^?4 M Fe and 2.6 × 10^?5 M Mn at pH 9.0) were sufficient to supply the crop needs as shown by a second sand culture experiment where plants were fed with nutrient solution plus extracted soil solution.     

Effects of NaHCO3 on photosynthetic characteristics,and iron and sodium transfer in pomegranate

In order to study effects of sodium bicarbonate (NaHCO₃) stress in irrigation water on photosynthetic characteristics and iron (Fe) and sodium (Na⁺) translocation content of pomegranate plants, a factorial experiment was conducted based on completely randomized design with three cultivars of pomegranate (“Gorch-e-Dadashi,” “Zagh-e-Yazdi,” and “Ghermez-e-Aliaghai”) and four concentrations of NaHCO₃ (0, 5, 10, and 15 mM), with three replications. The results of plant analysis indicated that NaHCO₃ affected chlorophyll index, F_v/F_m, and performance index (PI) in upper and lower leaves of shoots and also the translocation of Na⁺ and Fe. The results also showed that Fe translocation from root to shoot reduced at 15 mM level of NaHCO₃. The highest Na translocation and the lowest Fe translocation were observed in Zagh-e-Yazdi and Ghermez-e-Aliaghai cultivars, respectively. The ratio of sodium/potassium (Na⁺/K⁺) in stems was higher than that in roots and leaves, and the observed chlorophyll content of upper leaves was also lower than that of lower leaves. Based on the measured parameters Gorch-e-Dadashi cultivar showed less relative sensitivity than other cultivars to NaHCO₃ of irrigation water through maintaining the lower Na⁺ transport to the shoots, and improvement of Fe transport to shoots.     

Prevention of Iron‐Deficiency Induced Chlorosis in Kiwifruit (Actinidia deliciosa) Through Soil Application of Synthetic Vivianite in a Calcareous Soil

Abstract

In this study we have tested the hypothesis that lime‐induced Fe deficiency chlorosis of kiwifruit may be prevented by the application of a synthetic iron(II)‐phosphate analogous to the mineral vivianite [(Fe₃(PO₄)₂·8H₂O)]. Two experiments, under greenhouse and field conditions, were performed. In the greenhouse, 1‐year old micropropagated plants (Actinidia deliciosa, cv. Hayward), grown in 3‐L pots on a calcareous soil, were treated in early autumn with soil‐applied: (1) synthetic vivianite (1.35 g plant^?1) and (2) Fe‐EDDHA (24 mg Fe plant^?1). The synthetic vivianite suspension, prepared by dissolving ferrous sulfate and mono‐ammonium phosphate, was injected into the soil as a sole application whereas the Fe‐EDDHA solution was applied four times at weekly intervals. The field experiment was conducted in a mature drip‐irrigated kiwifruit orchard located on a calcareous soil in the Eastern Po Valley (Italy). Treatments were performed in early autumn by injecting synthetic vivianite (1.8 kg tree^?1) and Fe‐EDDHA (600 mg Fe tree^?1) into four holes in the soil around each tree, at a depth of 25–30 cm. The Fe‐chelate application was repeated at the same rate in the following spring. Untreated (control) plants were used in both experiments. Autumn‐applied Fe fertilisers significantly prevented development of Fe chlorosis under greenhouse conditions whereas in the field only vivianite was effective. In conclusion, these 1‐year results show that vivianite represents an effective alternative to soil‐applied Fe chelates for preventing Fe chlorosis in kiwifruit orchards.     

Comparison of different soilless media for growing gerbera under alkalinity stress condition

A factorial experiment was developed with two factors of the growing medium (v/v): 100% coconut fiber (CF), 75% vermicompost+25% perlite (VP), 25% zeolite+75% perlite (ZP), 75% peat+25% perlite (PP), 75% coco chip+25% perlite (CCP), 75% coconut fiber+25% perlite (CFP) and 100% perlite (P); and sodium bicarbonate (NaHCO₃) (0, 20 and 40 mM) involving the growth of gerbera cv. Dafne. Compared with CF substrate, NaHCO₃ in the nutrient solution caused significant decrease in vegetative and reproductive traits and nutrient concentration [especially iron, phosphorus, and magnesium (Fe, P and Mg)] in the rest of the media. The improved crop performance of plants grown onto CF substrate was attributed to their strong capacity to accumulate Fe in the aerial part under alkaline conditions and to maintain a better plant nutritional status (higher P and Mg). It is concluded that the use of CF substrate could provide a useful tool to improve alkalinity tolerance of gerbera plants under NaHCO₃ stress.     

Calcium and bicarbonate effects on the growth and nutrient uptake of burley tobacco seedlings: Hydroponic culture 1

Abstract

In soilless production systems, water quality can have a major impact on the growth of plants. It has become evident that moderately alkaline water is a problem for tobacco transplant growers in some regions of Kentucky. To determine the level of bicarbonate (HCO₃ ^?) alkalinity, which is detrimental to burley tobacco transplants, and to better understand the effect of calcium (Ca) and the interaction of HCO₃ ^? and Ca on the growth of burley tobacco transplants grown in a float system, three levels of CaCl₂ (25,75, and 125 mg L^?1 Ca⁺⁺) in factorial combination with five levels of HCO₃ ^? (0, 122, 244, 366, and 488 mg HCO₃ ^?L^?1) were tested in nutrient solution culture. Four‐week‐old burley tobacco (Nicotiana tabacum L. var. KY‐907) seedlings were transplanted to 18‐L containers filled with aerated Hoagland's solution with the different levels of calcium and HCO₃ ^? for two weeks. High HCC₃ ^? alkalinity caused root system damage and plant growth inhibition, but did not induce iron (Fe) chlorosis. A significantly lower concentration of Zinc (Zn) was measured in the shoots as HCO₃ ^? levels in solution increased. In the presence of high calcium, plant growth was not significantly improved. No significant interaction of HCO₃ ^? and Ca on growth or nutrient uptake was observed in this study.     

Effect of potassium salts on alleviation of lime‐induced chlorosis in soybean 1

Studies were conducted to determine the efficacy of K salts in alleviating lime‐induced chlorosis. Greenhouse studies using a Gibbon silt loam [fine‐silty, mixed (calcareous), mesic Typic Haplaquoll] and a 1: 1 mixture of Gibbon soil and washed sand were conducted with KCl, KNO₃, K₂SO₄, K₂HPO₄, or KHCO₃ applied at rates of 0, 250, and 500 mg K/kg soil. An FeEDDHA treatment was included for comparison. Similar studies were conducted at two field sites known to produce lime‐induced chlorosis. Potassium salts were applied at 0, 20, and 40 g K/m of row. In the greenhouse, plants treated with KCl, KNO₃, and K₂SO₄ on Gibbon soil were less chlorotic than controls or plants treated with K₂HPO₄, or KHCO₃. No K treatment totally alleviated chlorosis except FeEDDHA. Chlorophyll correlated positively with chlorosis rating. No relationship was found between leaf Fe uptake and chlorosis. Plants grown in soil/sand exhibited no chlorosis and had lower Fe uptake than plants grown in Gibbon soil. Thus chlorosis was not due strictly to low soil‐Fe availability or inadequate Fe uptake. Bicarbonate in the soil solutions of both growth media treated with KCl was lower than controls which may explain the reduced chlorosis associated with this treatment.

One field site showed positive effects of K treatments on chlorosis rating, chlorophyll concentration, and seed yield. No treatment was as effective as FeEDDHA in influencing plant growth or yield. Total leaf Fe concentration was unrelated to leaf chlorophyll concentration. Inorganic cation/anion ratios in the plant were from 4.4–8.4 which could cause net H⁺ efflux by the plant and alkalinization of plant tissues. One possibility is that H⁺ efflux solubilizes P in the rhizosphere, which after uptake could immobilize Fe in the plant. Application of KCl, KNO₃, and K₂SO₄ generally lowered HCO₃ content of the upper 15 cm of both soils. High bicarbonate could increase rhizosphere P availability and increase immobilization of Fe in the plant.     

Iron treatment of lime‐induced chlorosis: Implications for chlorophyll,Fe2 +, Fe3 + and K+ in leaves 1

This study addressed some complementary aspects related to plant Fe nutrition. A field and a greenhouse experiment were conducted to monitor changes in chlorophyll, Fe³⁺, Fe²⁺, Ca²⁺ and K⁺ along with the progressive evolution of lime‐induced chlorosis, and following soil (Fe‐EDDHA, Fe‐EDTA, Fe‐DTPA, DTPA) and foliar (Fe‐EDDHA, FeSO₄, “Fe‐Metalosate") treatments, in a chlorosis‐susceptible ornamental plant, Hydrangea macrophylla, over a year's growing period. Though soil Fe‐EDDHA was the most effective compound in alleviating chlorosis symptoms, it became less so with time and was only partly effective as a foliar spray. Leaf analysis showed that as chlorosis intensified and chlorophyll content decreased, phenanthroline ‐ Fe (Fe²⁺) decreased with corresponding increases in total iron (Fe³⁺) and K⁺ concentrations. The reliability of these chlorosis‐indicators was confirmed as the reverse changes occurred upon chlorosis plant recovery.     

Stabilization of Molybdate Reactive Phosphorus in 0.5 M Sodium Bicarbonate Extracts of Soils

Molybdate-reactive phosphorus (MRP) in soil-free 0.5 M sodium bicarbonate (NaHCO₃) extracts of 20 soils held at 22 °C increased 0–25% (median 11%) after 24 h and by 5–120% (median 43%) after 72 h. Addition of 2.5 mL L^?1 of chloroform (1) or 0.25–1 g L^?1 of thymol (2), phenyl mercury acetate (3), sodium cyanide (4), or sodium azide (5) showed that only (2)–(5) at 1 g L^?1 stabilized the MRP for 72 h. Five of the soils were re-extracted with 0.5 M NaHCO₃ containing 1 g L^?1 of (2)–(5): all stabilized MRP for 72 h, and (2) increased MRP for three soils (P < 0.05). For 92 additional soils (0.5–200 mg MRP kg^?1) extracted with 0.5 M NaHCO₃ ± 1 g of sodium azide L^?1, the azide had a negligible effect on MRP extraction, and in its presence, extracted MRP was unchanged after 72 h at 22 °C. We recommend this extractant for wider evaluation.     

Amelioration of copper toxicity by iron on Spinach physiology

The effect of excess copper (Cu) on young spinach (Spinacia oleraced) as well as the role of iron (Fe) for amelioration of toxicity on growth and photosynthesis in Cu‐treated plants was evaluated. Plants treated with 160 μM Cu showed symptoms of heavy metal toxicity, while addition of Fe (40 μM) ameliorates to a certain extent toxic effects of Cu, due to antagonistic action between Cu and Fe. Root length and biomass revealed a lower decrease under Cu+Fe than under Cu treatment. Copper accumulation in plant tissues increased, while Fe, sodium (Na), potassium (K), calcium (Ca), and magnesium (Mg) declined under Cu treatment. The significant increase in chlorophyll fluorescence (F_o) under 160 μM Cu, possibly reflects the more severe damages suffered at the membrane level with respect to Cu+Fe treatment. Copper decreased the efficiency of excitation energy capture by PSH reaction centers and negatively affected the effective antenna size of PSH. Changes in the rate of carbon dioxide (CO₂) assimilation were associated with changes in both stomatal conductance (gs) and mesophyll capacity for photochemistry as well as with lower pigment content. Net CO₂ assimilation, transpiration rate, and stomatal conductance were reduced. These changes at PSII are characteristic of a saturation of photosynthetic metabolic activity. The results suggest a tight linkage between PSII activity and CO₂ fixation under Cu treatment. Amelioration of Cu toxicity was obvious under Fe application.