Chemical Fractions of Zinc and Their Contribution toward Its Availability under Long-Term Integrated Nutrient Management in Rice–Wheat Sequence in an Acidic Alfisol

This study was carried out in an ongoing field experiment initiated during the 1991 kharif season (May–October) on an acidic soil in the Western Himalayas of India to evaluate the effect of integrated nutrient supply on transformation of zinc (Zn) into various chemical pools. The continuous use of chemical fertilizers alone for 20 years brought about marked depletion in different pools of Zn compared to buffer plots, while integrated use of organic and chemical fertilizers recorded greater content than chemically treated plots. Nonspecifically adsorbed exchangeable Zn (Zn I) was the most important fraction of Zn contributing to diethylene triamine penta-acetic acid (DTPA)–extractable Zn. Content of DTPA-extractable Zn also increased in soil with integrated application of chemical fertilizers and organics over the years. Residual Zn was the most dominant form of Zn, contributing about 55% to total Zn, whereas nonspecifically adsorbed exchangeable Zn was the most important fraction of Zn contributing to DTPA Zn.     

Phosphorus Fertilizer Requirements and Nutrient Uptake of Irrigated Dry‐Season Cotton Grown on Virgin Soil in Tropical Australia

Abstract

Considerable amounts of phosphorus (P) fertilizer will be required on soils in the proposed Ord Stage II area of northwestern Australia if a sustainable dry‐season, cotton‐production system is to be established, because in their virgin state, the soils are known to be inherently low in P. This study aimed to determine P‐fertilizer requirements on these soils to optimize cotton yield as well as nutrient uptake. Five rates of P fertilizer were applied to soil recently cleared of trees and prepared for irrigation. In the second year, these same rates were imposed over the trial. It was concluded that the application of 60 kg ha^?1 of P was sufficient to allow maximum yield and quality for dry‐season cotton grown in the first season on virgin soils in the Ord River Irrigation Area (ORIA), and a total of 80 kg ha^?1 of P was required when cotton was grown over two seasons.     

Growth,Mineral Composition,and Biochemical Changes of Broad Bean as Affected by Sodium Chloride and Zinc Levels and Sources

Plants grown in salt‐affected soils may suffer from limited available water, ion toxicity, and essential plant nutrient deficiency, leading to reduced growth. The present experiment was initiated to evaluate how salinity and soil zinc (Zn) fertilization would affects growth and chemical and biochemical composition of broad bean grown in a calcareous soil low in available Zn. The broad bean was subjected to five sodium chloride (NaCl) levels (0, 10, 20, 30, and 40 m mol kg^?1 soil) and three Zn rates [0, 5, and 10 mg kg^?1 as Zn sulfate (ZnSO₄) or Zn ethylenediaminetetraaceticacid (EDTA)] under greenhouse conditions. The experiment was arranged in a factorial manner in a completely randomized design with three replications. Sodium chloride significantly decreased shoot dry weight, leaf area, and chlorophyll concentration, whereas Zn treatment strongly increased these plant growth parameters. The suppressing effect of soil salinity on the shoot dry weight and leaf area were alleviated by soil Zn fertilization, but the stimulating effect became less pronounced at higher NaCl levels. Moreover, rice seedlings treated with ZnSO₄ produced more shoot dry weight and had greater leaf area and chlorophyll concentration than those treated with Zn EDTA. In the present study, plant chloride and sodium accumulations were significantly increased and those of potassium (K), calcium (Ca), and magnesium (Mg) strongly decreased as NaCl concentrations in the soil were increased. Moreover, changes in rice shoot Cl^?, Na⁺, and K⁺ concentrations were primarily affected by the changes in NaCl rate and to a lesser degree were related to Zn levels. The concentrations of Cl^? and Na⁺ associated with 50% shoot growth suppression were greater with Zn‐treated plants than untreated ones, suggesting that Zn fertilization might increase the plant tolerance to high Cl^? and Na⁺ accumulations in rice shoot. Zinc application markedly increased Zn concentration of broad bean shoots, whereas plants grown on NaCl‐treated soil contained significantly less Zn than those grown on NaCl‐untreated soil. Our study showed a consistent increase in praline content and a significant decrease in reducing sugar concentration with increasing salinity and Zn rates. However, Zn‐treated broad bean contained less proline and reducing sugars than Zn‐untreated plants, and the depressing impact of applied Zn as Zn EDTA on reducing sugar concentration was greater than that of ZnSO₄. In conclusion, it appears that when broad bean is to be grown in salt‐affected soils, it is highly advisable to supply plants with adequate available Zn.     

Influence of Aggregate Size,Electrolyte Concentration,and Sodium Adsorption Ratio on Crack Parameters of a Vertisol

Shrinking–swelling and crack formation influence soil physical behavior and productivity. Soil factors affecting crack formation and dimensions are clay content and mineralogy, aggregate stability as well as total concentration (C_t), and sodium adsorption ratio (SAR) of soil solution. Tillage intensity, which determines aggregate size, may also play a significant role in crack formation and dimensions. In the present work, total length, mean width, total area, and cover percentage of cracks were studied, under laboratory conditions, in beds of two aggregate sizes (<1 and 2–1 mm) of a Vertisol. The beds were saturated, equilibrated with sodium chloride (NaCl)/calcium chloride (CaCl₂) solutions of C_t 2, 5, 10, 20, and 30 mmol/L and SARs 0, 2, 5, 10, and 20 (mmol/L)^1/2, and allowed to air‐dry. After air‐drying, pictures of the samples were taken and used for the calculation of crack parameters by a scanning program. The results showed that aggregate size was the dominant factor determining the crack parameters: the cracks formed in beds of aggregates <1 mm were wider and of a smaller total length, total area, and cover percentage (p < 0.05) than those cracks formed in beds of aggregates 2–1 mm in size. It was also determined that changes of C_t resulted in a greater influence on crack characteristics than changes of SAR in the equilibrating solutions.     

Alfalfa Responses to Combined Use of Lime and Limiting Nutrients on an Acidic Soil

An on-farm field experiment was conducted on an acidic soil to investigate the effects of combined use of lime and deficient nutrients on herbage yield of alfalfa (Medicago sativa L.). Omitting lime and limiting nutrients led to elevated concentrations of aluminium (Al), iron (Fe), and manganese (Mn) in alfalfa leaves and stems and caused severe reductions in herbage yield of alfalfa. Combined use of lime (2 t ha^?1) and nutrients [phosphorus (P): 20 kg ha^?1, sulfur (S): 20 kg ha^?1, zinc (Zn): 4 kg ha^?1, and boron (B): 2 kg ha^?1] had the maximum increase in groundcover, root biomass, nodulation, leaf retention, leaf-to-stem ratio, herbage yield, crude protein, and nutrient composition of alfalfa. These beneficial effects were due to raised soil pH; improved calcium (Ca), P, S, Zn, and B nutrition; and reduced Al, Mn, and Fe toxicity. Aluminium and all the nutrients except copper (Cu) were more concentrated in alfalfa leaves than stems.

Aluminum concentration was about three times greater in the lower leaves than in upper leaves. Lower leaves also had much greater concentrations of Ca, Mg, K, S, Fe, Mn, Cu, and B compared with upper leaves. In contrast, P and Zn concentrations were greater in the upper leaves than in lower leaves. Results suggest that the combined use of lime and all the limiting nutrients may realize potential beneficial effects of alfalfa on acidic soils where more than one essential nutrient is deficient. This may increase growth potential, nitrogen contributions, and groundcover by alfalfa and reduce soil erosion and runoff.     

Zinc Release Characteristics from Calcareous Soils using Diethylenetriaminepentaacetic Acid and Other Organic Acids

Adsorption and desorption reactions of zinc (Zn) in soils control its availability to plants. In the present investigation, time-dependent Zn release was evaluated using three organic acids [diethylenetriaminepentaacetic acid (DTPA), citric acid, and maleic acid] to depict the Zn fraction controlling Zn release rate from slightly calcareous to calcareous soils. Eight surface and two subsoil samples of selected soil series varied in their physicochemical properties, amount of Zn held in different chemical pools, and Zn-retention capacities (21–61%). Each soil was extracted for a total period of 24 h at 1:10 soil/extractant suspension ratio using 0.005 M DTPA. The time-dependent parabolic diffusion model best described the Zn release in six consecutive extractions. Soils differed in cumulative Zn extracted (1.09–3.81 mg kg^?1 soil) and Zn release rate. Under similar conditions, three soils differing in Zn-retention capacities were also extracted with five different concentrations (0.01–0.0001 M) of citric and maleic acids. Although both maleic and citric acids released soil Zn at greater rates and in greater amounts than DTPA, maleic acid was more efficient. Soil Zn bound to amorphous iron (Fe) + manganese (Mn) oxides was the main Zn pool that controlled Zn release characteristics.     

Effects of Long-Term Inorganic and Organic Fertilization on Soil Micronutrient Status

Soil micronutrients were studied on loess soil with an 18-year long-term experiment. The results indicated that total soil iron and copper contents were similar under all treatments, but total soil manganese and zinc contents were significantly greater at the surface soil in the fertilized plots than in the controls, and total manganese contents were significantly greater in the whole soil profile under manure plus inorganic fertilizers than under controls. Generally, application of inorganic fertilizers had no effects on available soil micronutrient contents. The straw plus inorganic fertilizers significantly increased available manganese content at surface soil and available iron in subsurface soils. However, manure plus inorganic fertilizers significantly augmented soil-available iron contents throughout the profile, and raised available manganese, copper, and zinc contents, respectively, at surface soil relative to controls. The results suggest that long-term input of organic amendments alter the properties of soil and increase its plant-available micronutrient contents.     

The influence op soil treatments on elemental composition of corn and on zinc soil tests on two Missouri soils

Abstract

Corn (Zea mays L) was grown at three locations on soil treated with Zn at two levels of soil fertility. Corn leaves were sampled at 2 stages of growth and analyzed for several elements. Yields were measured and soils were analyzed for O.lN HCl and DTPA extractable Zn and by standard testing methods for other components.

Zinc at 10 and 20 lb/A did not affect corn grain yields. The Zn treatments significantly increased leaf Zn concentrations. The influence of leaf sampling time differed between locations. The DTPA and O.lN HCl extractable soil Zn both reflected the Zn soil treatments. The DTPA appeared to extract a more soluble component of soil Zn which became more un‐extractable with time. In general, the extractable soil Zn was poorly correlated with Zn concentrations in the corn leaves. Under the conditions of the experiment the soil Zn levels as measured by the 2 extractants were a poor predictor of plant Zn when soil Zn levels were adequate.     

Micronutrient topdressing of alfalfa (medicago sativa L.) on a udollic albaqualf

Abstract

An established stand of alfalfa (Medicago sativa L.) was topdressed with two rates each of borax, zinc sulfate, and copper sulfate at two levels of applied P and K. Yields and plant composition were determined at five harvests over two seasons. Treatments were not effective in increasing yields but topdressing with B and Zn increased the concentration of these elements in the plant tissue. The Cu concentration in alfalfa tissue was not affected by topdressing with copper sulfate. Phosphorus application rates of about four times removal rates were needed to maintain the Bray 2 soil test level of the soil.     

Triticale,wheat, and rye growth rates and mineral accumulation at various growth stages

Abstract

Cultivars of triticale, wheat, and rye were grown with different N‐fertilizer rates and sampled at various maturity stages in 1975 to 1977. ‘6TA 131’ triticale, ‘Arthur’ wheat, and ‘Abruzzi’ rye were used as checks. Increasing N fertilizer rates increased dry matter and N accumulation in the above‐ground plant parts. However, after flowering losses of dry matter and N from the plants increased with N fertilizer rates. Triticale and rye generally absorbed more N from the soil than wheat. Triticale and wheat straw had higher P concentrations than rye. The head/straw concentration ratios were: triticale and rye>wheat for P, wheat>triticale and rye for K while Ca and Mg ratios were triticale>wheat>rye.