Interaction of iron chelate and nitrogen fixation in peanuts grown on calcareous soil

The interaction of iron (Fe) nutrition and nitrogen (N₂) fixation was examined in peanuts grown in the field for two growing seasons. The treatments were: a) inoculated with Rhizobium, not fertilized with N, b) uninoculated, fertilized with N, and c) uninoculated not fertilized with N. These treatments were tested with or without Fe chelate application. Inoculated peanuts produced up to 42% higher N yield than the uninoculated, non‐fertilized plants. Moderately chlorotic peanuts fertilized with Fe did not increase significantly their yield but had bigger nodules than peanuts not fertilized with Fe. There were no interactions between Fe and N treatments, indicating that both nutrients were important for growth and for N₂ fixation. Remedy of Fe chlorosis on calcareous soils with FeEDDHA will not reduce N₂ fixation.     

Effect of nitrogen and phosphorus on zinc nutrition of corn in a calcareous soil

Different factors affect zinc (Zn) nutrition of plants, among which pH and phosphorus (P) have been studied widely but nitrogen (N) has not received much attention. The present experiment was designed to study the effect of N and P on growth and Zn nutrition of corn (Zea mays L.) in a highly calcareous soil of Iran. The experiment was a 3x3x2 factorial in randomized complete blocks with three replications which was conducted in greenhouse for eight weeks. Treatments consisted of three levels of N (0,75, and 150 mg/kg), three levels of P (0, 50, and 100 mg/kg), and two levels of Zn (0 and 20 mg/kg). Application of N increased dry matter (DM), N concentration and uptake, Zn concentration and uptake, and N: P and N: Zn ratios of plant tops; but it decreased P concentration and uptake and P: Zn ratio. Application of P increased DM, P concentration and uptake, N uptake, and P: Zn and N: Zn ratios; but it decreased N and Zn concentrations and N: P ratio. Dry matter and Zn concentration and uptake increased but P: Zn and N: Zn ratios decreased following the application of Zn. Multiple regression equations obtained showed the influence of N application on increasing Zn concentration and uptake and lowering the P: Zn ratio of plant tops. It was concluded that N application improves Zn nutrition of corn in highly calcareous soils by increasing plant Zn concentration and uptake and decreasing P concentration. This lowers the P: Zn ratio of plant tops to a more optimum range for plant growth.     

Responses of earlirose rice to iron,zinc, and BPDS when grown on calcareous soil

Abstract

The Earlirose cultivar of rice (Oryza sativa L.) grown in calcareous Hacienda loam soil was extremely Fe deficient. The Fe deficiency was corrected by premixing 40 ppm Fe (as FeSO₄) into the soil before transplanting plants. The Fe deficiency appeared to be induced by high plant levels of Cu and Mn. Addition of Zn (40 ppm as ZnSO₄) intensified the Fe deficiency. The Fe addition did not overcome the effect of the Zn. BPDS (bathophenanthroline disulfonate), a chelator of Fe⁺⁺, had little effect on the results.     

Copper and zinc uptake by celery plants grown on acidic soil amended with biosolids

For trace elements, such as copper (Cu) and zinc (Zn), the bioavailability of these elements, Cu and Zn, in biosolids is important because both are essential elements and both are potential contaminants when biosolids are land applied. A greenhouse study was conducted in factorial experiment based on a completely randomized design (CRD) with four replications on a soil treated with four rates of Cu (0, 50, 100, and 150 mg/kg) and four rates of Zn (0, 150, 300, and 450 mg/kg) on celery plants to investigate the distribution and mobility of these elements as well as growth and antioxidant changes of celery. The results of antioxidant changes were inconclusive due to irregular changes with Zn and Cu applications. However, generally the results show that Cu did not affect superoxide dismutase (SOD) or peroxidase (POD) activities in most of the treatments. On the other hand, Zn stimulated SOD and POD activities in most of the treatments. The photosynthesis rate decreased with the applications of Cu and Zn at the rates above 100 and 300 mg/kg and increased in low Cu concentration (50 mg/kg) compared to S (soil without biosolid).     

Effects of zinc complexes on the distribution of zinc in calcareous soil and zinc uptake by maize

The movement and availability of Zn from six organic Zn sources in a Typic Xerorthent (calcareous) soil were compared by incubation, column assay, and in a greenhouse study with maize (Zea mays L.). Zinc soil behavior was studied by sequential, diethylenetriaminepentaacetate, and Mehlich-3 extractions. In the incubation experiment, the differences in Zn concentration observed in the water soluble plus exchangeable fraction strongly correlated with Zn uptake by plants in the greenhouse experiment. Zinc applied to the surface of soil columns scarcely moved into deeper layers except for Zn-ethylenediaminetetraacetate (EDTA) that showed the greatest distribution of labile Zn throughout the soil and the highest proportion of leaching of the applied Zn. In the upper part of the column, changes in the chemical forms of all treatments occurred and an increase in organically complexed and amorphous Fe oxide-bound fractions was detected. However, the water soluble plus exchangeable fraction was not detected. The same results were obtained at the end of the greenhouse experiment. Significant increases were found in plant dry matter yield and Zn concentration as compared with the control treatment without Zn addition. Increasing Zn rate in the soil increased dry matter yield in all cases but Zn concentration in the plant increased only with Zn-EDTA and Zn-ethylenediaminedi-o-hydroxyphenyl-acetate (EDDHA) fertilizers. Higher Zn concentration in plants (50.9 mg kg(-)(1)) occurred when 20 mg Zn kg(-)(1) was added to the soil as Zn-EDTA. The relative effectiveness of the different Zn carriers in increasing Zn uptake was in the order: Zn-EDTA > Zn-EDDHA > Zn-heptagluconate >/= Zn-phenolate approximately Zn-polyflavonoid approximately Zn-lignosulfonate.     

Influence of compost of sewage sludge and low-quality water on pesticide uptake by tomato plants grown in an iron mine soil

Purpose

In mine soils, especially from arid or semiarid areas, the use of low-quality water for irrigation is a usual practice. Therefore to fill this gap, different experiments have been carried out to evaluate the effect of compost, pesticide and wastewater on the growth of tomato plants in a mine soil located at an iron extraction area.

Materials and methods

Soils proceeded from Alquife mine wastes whose most outstanding characteristics are alkaline conditions, low organic matter and electrical conductivity and high As concentration. The compost of sewage sludge (CSL) used to amend this soil had a slightly acid pH (6.8), EC 3.0?±?0.07 dS m^-1 (1/10 ratio, m/V) and 10 % organic carbon (OC) content. Irrigation was performed with distilled water (DW) or wastewater (WW) and two pesticides, the insecticide thiacloprid and the fungicide fenarimol, were applied to the soil. Tomato was grown directly from seeds on each pot. Four treatments with addition of pesticides were considered. For comparison purposes, two additional treatments without pesticides were also included.

Results and discussion

Addition of compost of sewage sludge led to a significant and sustained increase of soil OC content and dehydrogenase activity, while irrigation with wastewater had a slight or negligible effect on both properties. The plant species responded negatively to wastewater irrigation when this practice was undertaken with the application of both pesticides. No detectable amounts of thiacloprid, a relatively unstable and polar insecticide, were found in soil. The concentration of fenarimol in soil was higher after amendment with compost, but was not modified by irrigation with wastewater. In tomato shoots, the amounts of both pesticides were inversely correlated with final soil organic carbon, indicating that this soil property is relevant for their plant uptake. Besides, fenarimol concentrations in the soil and the tomato shoots were inversely related (r?=??0.836).

Conclusions

Tomato was not able to grow healthy in Alquife mine soil without compost addition. The irrigation with wastewater only reduced plant growth when used in combination with pesticides. Uptake of both pesticides by tomato plants was negligible according to the low bioaccumulation factor values, but was almost doubled for wastewater irrigation. Caution should be taken with the use of treated wastewater, because it may reduce plant growth in tomato that is a species sensitive to salinity.

     

Prediction of residual effects of zinc sulfate on growth and zinc uptake of corn plants using three zinc soil tests

Abstract

A significant portion of chemical zinc (Zn) fertilizers applied to calcareous soils is not absorbed by the first crop and may, therefore, affect the growth and chemical composition of the subsequent crops. This is called the residual effect of Zn. Soil tests may be used to predict such effects. The present experiment was conducted to study the residual effects of zinc sulfate (ZnSO₄) on the second crop of corn (Zea mays L.) grown on selected highly calcareous soils of Iran and to compare the suitability of three soil tests for prediction of the effects. Twenty highly calcareous soils of southern Iran (16–58% calcium carbonate equivalent; pH 7.9–8.5), previously treated with three levels of Zn (0, 10, and 20 mg Zn/kg as ZnSO₄) and under one crop of corn, was used in greenhouse to grow a second crop of corn without additional Zn fertilizer but with uniform application of nitrogen (N), phosphorus (P), and iron (Fe). Soils were sampled before the second crop and extracted with three Zn extradants, DTPA, EDTA‐(NH₄)₂CO₃, and EDTA. Dry weight of plant tops and Zn concentration and uptake after eight weeks under the greenhouse conditions were used as the plant responses to residual Zn. Statistical analyses including F‐test and multiple regression equations showed that the overall effect of previously‐applied Zn on dry matter was nonsignificant, but Zn concentration and uptake were significantly increased. The three soil tests predicted the Zn concentration and uptake equally well. Moreover, DTPA and EDTA soil tests could predict the dry matter of plants at the highest level of previuosly‐applied Zn (20 mg Zn/kg), especially when selected chemical properties of soil, namely, calcium carbonate equivalent or organic matter content, were considered in the regression equations.     

Co-application of sugarcane bagasse biochar,farmyard manure and mineral nitrogen improved growth indices of corn grown in alkaline calcareous soil

Abstract

Soil quality and crop productivity can be improved by the combined soil application of organic amendments and synthetic fertilizers. We evaluated the sole and combined effects of sugarcane-bagasse biochar (SBB), farmyard manure (FYM) and nitrogen (N) fertilizer on soil properties and corn yield traits. Three N fertilizer rates (0, 50 and 100% of recommended) were used with or without the organic amendments. We observed significant increases in soil nitrate-N (at vegetative and reproductive phases), ammonical-N and microbial-biomass-N contents in responses to a co-application of 0.5% SBB, 0.5% FYM and 100% N fertilizer (p?≤?0.05). While the same co-application also resulted in the most significant soil organic carbon value, the maximum soil microbial biomass carbon was observed when 0.5% SBB and 0.5% FYM combination was applied along with 50% N fertilizer (p?≤?0.05). Plant growth indices—shoot length and, fresh and dry weights of shoot and root were also recorded to be the highest where the same organic amendments were applied in addition to a 50% or 100% mineral N fertilizer (p?≤?0.05). Combined application of the organic amendments effectively improved soil CEC compared to those in responses to individual applications of SBB and FYM (p?≤?0.05). Conclusively, for increasing the corn yield and improving the soil quality, the co-application of 0.5% SBB and 0.5% FYM was more effective than any of the individual 1% applications; Additions of 50% and 100% mineral N to the organic combination were equally useful for increasing the grain yield.     

Effects of solid phase from pig slurry on iron,copper, zinc,and manganese content of soil and wheat plants

A two‐year lysimeter experiment was conducted using winter wheat plants on two texturally contrasting soils (soil A and soil B). The main objective of this study was to evaluate the influence of increasing doses (5, 10, 15, 20, and 251 ha^‐1) of solid phase from pig slurry (SP) on soil extractable copper (Cu), zinc (Zn), iron (Fe), and manganese (Mn) and on wheat micronutrients composition and uptake. As the control, a basic dressing of NPK fertilizer was applied. Results showed that increasing additions of SP significantly enhanced extractable Cu, Zn, Fe, and Mn content on the topsoil for both soils tested. In addition, a significant increase was detected for extractable Cu, Zn, and Mn content with increasing application rates of SP for subsoil A, but no significant differences were detected for subsoil B. A significant increase in the contents of Fe, Mn, and Zn in the plants as well as total uptakes were observed from increasing doses of SP. Copper content in the plants was not significantly affected. Finally, a strong pH effect was exerted in the Mn and Zn uptake by the plants.     

氮锌配施对石灰性土壤锌形态及肥效的影响

通过分析石灰性土壤上施用锌肥后土壤中锌的形态变化,研究锌肥的有效性及后效,为指导合理施用锌肥提供理论依据。结果表明在潜在性缺锌的石灰性土壤施锌肥没有明显的增产效果,可增加小麦籽粒锌含量,但不同基因型反应差异很大;土壤中的锌主要以矿物态存在,占全锌91.5%~97.6%,其次为松结有机态锌(1.34%~5.53%)、碳酸盐结合态锌(0.47%~1.55%);施入土壤中的锌增加了交换态、松结有机态、碳酸盐结合态、氧化锰结合态锌含量,但大部分转化为矿物态;种植小麦可以使土壤中的锌向有效态转化;施氮增加了小麦对锌的吸收,也增加了锌矿化的比例;主成分分析结果表明,交换态、松结有机态和碳酸盐结合态均能不同程度反映土壤锌的有效性,石灰性土壤中碳酸盐结合态和有机结合态锌含量占有较为可观的比例,因此增加这两种形态储备容量是调节和控制土壤锌营养状况的重要措施。     

Calcium,magnesium, and potassium uptake by crested wheatgrass grown on calcareous soils

Abstract

Forage intake with potassium/(calcium + magnesium) [K/(Mg + Ca)] values in excess of 2.2 are associated with grass tetany and Mg deficiencies in ruminants. This study was conducted to determine the degree to which forage K and Mg concentrations and K/(Ca + Mg) ratios could be predicted from soil bicarbonate (HCO₃) extractable phosphate‐phosphorus (PO₄‐P), and saturation extract Ca, Mg, K, sodium (Na), and nitrate‐nitrogen (NO₃‐N) concentrations. Crested wheatgrass (Agropyron spp) strains and cultivars representing four ploidy levels were grown in the greenhouse on eight calcareous soils with different saturation extract Ca, Mg, K and K/Mg ratios. The plants were harvested three times. Soil solution K/(Ca + Mg) and K/Mg ratios were the only measured soil parameters that showed a consistent correlation with plant K/(Ca + Mg) ratios. Bicarbonate extractable soil P was positively related to plant P and K uptake in the first harvest, but was not related in the second and third harvests nor was soil P related to plant Ca or Mg content. There was a tendency for the higher ploidy level entries to have higher plant K/(Ca + Mg) ratios. It was concluded that soil K/(Ca + Mg) ratios can be used to predict relative forage K/(Ca + Mg) ratios for grasses grown under similar conditions.     

Influence of nitrogen and elemental‐sulfur fertilization on sulfur oxidation and mineralization in relation to soil moisture on a calcareous soil of the Inner Mongolia steppe of China

Grassland‐livestock farming is the main agricultural activity in the Inner Mongolia steppe of China. It has been estimated that more than 80% of the grasslands suffer from sulfur (S) deficiency in this region. In an incubation study and a greenhouse experiment with alfalfa, the influence of soil moisture (40% and 70% water‐holding capacity, WHC), nitrogen (0 and 200 mg N (kg soil)^–1 as NH₄NO₃), and elemental sulfur (eS; 0 and 300 mg S (kg soil)^–1) amendments on the apparent eS oxidation, eS‐oxidation rate, net S‐mineralization rate, and S uptake of alfalfa were studied. After 28 d of incubation, the eS‐oxidation rate was four times higher at 70% than at 40% WHC if no N was applied. With N application, soil moisture had only minor effects on eS oxidation during the whole incubation period. In the greenhouse experiment, lower values for eS‐oxidation rate and net S‐mineralization rate were found if no N was applied. Application of N and eS significantly increased alfalfa growth and S uptake. The results of both experiments suggest that combined N and eS applications are the best way to alleviate S deficiency on these calcareous soils.     

UAN氮溶液对潮土上玉米生长和氮素吸收的作用效果

为探究UAN氮溶液在潮土上对玉米生长和氮素吸收的作用效果,采用盆栽试验,研究UAN氮溶液对玉米收获期干物质积累、氮磷钾吸收量和土壤氮磷钾养分状况及pH值的影响。结果表明,等氮量的UAN氮溶液和尿素均促进了玉米的生长和对氮磷钾的吸收,两者的氮肥利用率无显著差异,分别为65.35%和64.76%。与全量UAN氮溶液相比,减施UAN氮溶液20%使玉米的生物量减少14.71%,植株中氮、磷、钾的养分吸收量分别降低24.27%、18.65%、10.47%。在低肥力潮土上,等氮量的UAN氮溶液和尿素对玉米的生长和氮素吸收的效果相当;减施UAN氮溶液20%影响玉米的生长和氮素的吸收,而氮肥利用率无明显变化。     

Effect of phosphate dissolving bacteria on P-uptake by barley plants grown in a salt affected calcareous soil

In a pot experiment the effect of inoculation of a salt affected calcareous soil with phosphate dissolving bacteria (PDB) on dehydrogenase activity and P-uptake by barley plants was investigated. Four levels of artificial salinity were used, i. e., 0.2, 0.4, 0.8 and 1.2 % total soluble salts. Inoculation increased PDB in all treatments, but it did not affect the microbial activity in the soil as represented by dehydrogenase activity. The higher the salt level the lower the counts of PDB and dehydrogenase activity in the soil. A positive significant difference was recorded in P-uptake as a result of inoculation and a negative one as a result of increasing salinity.     

营养型土壤改良剂对酸性土壤中钾的调节及玉米吸钾量的影响

营养型土壤改良剂(以下简称改良剂)施入三种不同肥力水平的土壤进行恒温培养试验和盆栽试验,测定土壤有效钾的含量、盆栽试验玉米的生物量和钾吸收量。结果表明:对于有效钾含量高的土壤,改良剂能促进钾的缓效化,有利于土壤钾的保蓄,防止土壤钾的淋失;对于有效钾含量较低的土壤,改良剂可以活化土壤中的钾,提高土壤钾的有效性;不同肥力水平的土壤,改良剂都能促进玉米对钾的吸收,有利于提高钾肥的吸收利用效率。     

土壤压实对土壤物理性质及小麦氮磷钾吸收的影响

为了研究土壤压实对土壤物理性质以及小麦养分吸收情况的影响,在2006和2007年进行了两轮田间试验.试验中,先用旋耕机对田块进行旋耕,耕深10cm,然后使用手扶式、轮式、履带式拖拉机在旋耕后的田块中通过1次(T1)、2次(T2)、4次(T3)以对土壤进行压实处理,对照组(T4)不作任何压实处理.压实处理后再次对土壤表层进行浅旋耕,耕深5 cm,耕后用播种机进行小麦播种,小麦品种为南京-601.试验结果发现,次表层土壤的压实处理显著影响次表层土壤的容重,孔隙度,小麦蛋白质含量以及植物中N、P、K的含量.除次表层的土壤容重在T3组中最大,T4组中最小外,其他参数值在T4组中最大,T3组中最小.并且,随着次表层土壤压实程度的增加,几乎所有的参数(土壤容重除外)都有所减少.不过,与第一年相比,参数值在第二年略有增加.总之,土壤压实严重破坏土壤结构,不利于小麦对养分的吸收.     

Effect of manganese and soil pH on the iron content of crops grown on podzol soils

In a greenhouse study on three podzol soils with pH values of 5.4–5.6, liming to pH 7.6 or higher decreased the Fe concentration of pea plant tissues from 47 to 42 ppm. In the case of barley, liming the soil increased the mean tissue Fe concentration from 104 to 119 ppm at pH 7.6 and to 107 ppm at pH 7.7. Field experiments on wheat, oats, alfalfa, and timothy showed that Mn applied to the soil or as foliar spray did not affect the Fe concentration of cereal or forage plant tissues. Liming did not affect the Fe concentration of cereal kernels but on a few locations it increased the Fe concentration of the boot stage tissue. The Fe concentration in oats was higher than that in wheat. Based on the results of a survey, it was found that forage legumes contained more Fe than did timothy. The survey also showed that a few Fe values in timothy and cereals would be considered low, although Fe deficiency has not been experienced in this region. A number of the samples would be in the deficiency range from the animal nutrition standpoint.     

Effect of varied soil nitrogen supply on growth and nutrient uptake of young Norway spruce plants grown in a shaded environment

To understand the effect of increased soil N supply on tree growth and nutrient uptake, three-year-old Norway spruce seedlings were grown in pots on low-nutrient mineral forest soil supplemented with N in mineral or organic form. Outdoor shaded growth conditions were used, to test the hypothesis that shaded plants are particularly susceptible to high soil N supply. Plants were harvested eleven months after planting. Shoot growth was not affected by the N supply, but N concentrations in needles and roots were increased in plants supplied with mineral N (150 or 300 mg N [kg soil]^—1). Root growth was drastically reduced and root/shoot ratios were decreased in plants with higher N uptake. A high supply of mineral N to soil also decreased the concentrations of other essential elements (P, K) in the needles and thus had effects on plant growth which may impair the stress resistance of trees. Organic N in the form of keratin (150 mg N [kg soil]^—1) did not influence plant growth significantly. The adverse effects of high mineral N supply were particularly pronounced under shaded conditions in comparison to results from other experiments using higher light intensity and temperature conditions.     

Effects of sulfur,zinc, iron,copper, manganese,and boron applications on sunflower yield and plant nutrient concentration

Abstract

Sulfur, zinc, iron, copper, manganese, and boron application did not affect the seed yield or oil percentage of sunflower (Hilianthus annuus L.) on both dryland and irrigated soils in North Dakota in 1981. Field averages indicated significant Zn, Mn, and B uptake by sunflower at the 12‐leaf stage as a result of fertilization with these elements. Increased Zn uptake was also observed in the uppermost mature leaf at anthesis from zinc fertilization.

Although sunflower yield from boron fertilization was not significantly different from the check, a trend was observed in which boron fertilization seemed to decrease sunflower yield. Sunflower yields from the boron treatment were the lowest out of seven treatments in three out of four fields. Also, sunflower yield from the boron treatment was significantly lower than both iron and sulfur treatments when all fields were combined.     

Phosphorus requirement of corn and sunflower grown on calcareous soils of Pakistan

Abstract

Determining phosphorus (P) fertilizer requirement through sorption isotherms is considered more accurate than conventional soil testing. Phosphorus sorption isotherms were constructed by using the Missa (Typic Ustochrept), Gujranwala (Udic Haplustalf), Abbotabad (Aquic Entrochrept), and Rasulpur (Ustochreptic Camborthid) soil series which varied in their calcium carbonate (CaCO₃) and clay contents. Quantities of fertilizer‐P (mg P/kg soil) required to adjust the standard soil solution P concentration (0.2 mg P/L) were: Missa, 83; Gujranwala, 51; Abbotabad, 50; and Rasulpur, 8. Langmuir model conformed better with the adsorption data than Freundlich model and indicated that the order of maximum adsorption capacity (b) was: Missa > Abbotabad = Gujranwala > Rasulpur. The P sorption curves were used to develop the soil solution P concentration in the Gujranwala and Missa soils varying from native to 0.5 mg P/L. Soil solution P requirement of corn and sunflower for near‐maximum (95%) biomass production was approximately the same, 0.32 mg P/L. Internal P requirement in whole shoots (≤30 cm tall) were 0. 29% for corn and 0.39% for sunflower.