Bulk soil pH and rhizosphere pH of peach trees in calcareous and alkaline soils as affected by the form of nitrogen fertilizers

One-year old nectarine trees [Prunus persica, Batsch var. nectarina (Ait.) Maxim.], cv Nectaross grafted on P.S.B2 peach seedlings [Prunus persica (L.) Batsch] were grown for five months in 4-litre pots filled with two alkaline soils, one of which was also calcareous. Soils were regularly subjected to fertigation with either ammonium sulphate or calcium nitrate providing a total of 550 mg N/tree. Trees were also grown in such soils receiving only deionized water, as controls. Rhizosphere pH, measured by the use of a microelectrode inserted in agar sheet containing a bromocresol purple as pH indicator and placed on selected roots, was decreased by about 2–3 units compared to the bulk soil pH in all treatments. This decrease was slightly less marked when plants were supplied with calcium nitrate rather than ammonium sulphate or control. Measurements conducted during the course of the experiment indicated that ammonium concentration was similar in the solution of soils receiving the two N fertilizers. During the experiment, soil solution nitrate-N averaged 115 mg L^–1 in soil fertilized with calcium nitrate, 68 mg L^–1 in those receiving ammonium sulphate and 1 mg L^–1 in control soils. At the end of the experiment nitrate concentrations were similar in soils receiving the two N sources and bulk soil pH was decreased by about 0.4 units by ammonium sulphate fertigation: these evidences suggest a rapid soil nitriflcation activity of added ammonium. Symptoms of interveinal chlorosis in apical leaves appeared during the course of the experiment in trees planted in the alkaline-calcareous soil when calcium nitrate was added. The slightly higher rhizosphere pH for calcium nitrate-fed plants may have contributed to this. The findings suggest that using ammonium sulphate in a liquid form (e.g. by fertigation) in high-pH soils leads to their acidification and the micronutrient availability may be improved.     

pH changes in the rhizosphere in relation to the pH-buffering of soils

Summary pH values in the rhizosphere of peanut seedlings were measured with Sb micro electrodes in soils with a bulk pH between 3.9 and 7.7. Within 2–2.5 days the roots decreased soil pH to a minimum value which was linearly correlated with short term buffering capacity of the soils as determined by addition of HCl to soil suspensions. The greatest distance from the root surface where pH dropped significantly was found in soils with pH near 6. This maximum distance was also correlated with pH-buffering. The low buffering capacity for soils of pH near 6 seems to be valid for a large number of soils with different properties.     

Effect of pH on nitrogen immobilization in two California soils

Summary The effect of pH on nitrogen immobilization from tagged NH₄Cl and KNO₃ was investigated in two soils. Although the ammonium source was utilized by the soil population preferentially at all pH levels in both soils, there was a marked influence of pH on the quantity immobilized. Nitrogen immobilized from the ammonium source increased, as pH increased, whereas the reverse was true of the nitrate source. These results appear to be related to the physiological acidity or alkalinity of the nitrogen source.Most of the nitrogen incorporated into the organic fraction was present in the amino form.Contribution from the Department of Soils and Plant Nutrition University of California, Davis, and the Department of Vegetable Crops, University of California, Riverside. This work was supported in part by a grant from the National Science Foundation.     

Effect of pH on Na induced Ca deficiency

Although it is well known that high Na concentrations induce Ca deficiency in acidic conditions, the effect of high pH on this competitive mechanism is not so well understood. The effect of Ca activity ratio (CAR) and pH on the Ca uptake of mungbeans (Vigna radiata (L.) Wilczek cv. Emerald) and Rhodes grass (Chloris gayana cv. Pioneer) in Na dominated solution cultures and in soil was investigated. Changes in pH in the alkaline range were shown not to affect the critical CAR of 0.024 (corresponding to 90% relative root length) for mungbeans grown in solution culture. Results from soil grown mungbeans confirmed those from solution culture, with a critical CAR of 0.025. A critical CAR of 0.034 was also established for soil grown Rhodes grass. The similarity of critical values established for mungbeans and Rhodes grass in solution culture and soil justifies the use of both solution culture and soil solution measurement as techniques for studying plant growth and limitations across plant species.     

Effects of inoculation of EPS-producing Pantoea agglomerans on wheat rhizosphere aggregation

We investigated plant and soil nitrogen pools and soil processes in monospecific stands of the C₃ sedge Scirpus olneyi and the C₄ grass Spartina patens grown in the field in open top chambers in a brackish marsh on the Chesapeake Bay. Stands of S. olneyi responded to eight years of elevated CO₂, by increased rates of net ecosystem gas exchange and a large stimulation of net ecosystem production. We conducted our study in the summer of 1994 and 1995 when soil cores were collected and aboveground biomass was estimated. Nitrogen concentration in elevated CO₂ treatments was reduced 15% in stems of S. olneyi and 8% in the upper 10 cm of the soil profile. While total plant nitrogen per unit of land area remained the same between treatments, total soil nitrogen showed a non-significant tendency to decrease in the upper 10 cm of the soil profile in elevated CO₂ both years of study. A significant decrease in soil bulk density largely contributed to the observed decrease in soil nitrogen. Exchangeable nitrogen and potential denitrification rates were also reduced in elevated CO₂, but net nitrogen mineralization was unchanged by elevated CO₂ treatment in S. olneyi both years. Plants and soils in a pure stand of the C₄ grass, S. patens, showed none of these effects of elevated CO₂ treatment. Our data provides evidence of changes in nitrogen dynamics of an ecosystem exposed to elevated CO₂ for eight years; however due to the variability in these data, we cannot say if or how these changes are likely to impact the effect of rising CO₂ on primary production or carbon accumulation in this ecosystem in the future.     

pH对不同富集能力植物根际土壤溶液中镉形态的影响

为了解不同p H对土壤溶液中Cd形态分布的影响,采用Visual MINTEQ 3.0模型和阳极溶出伏安法(ASV)研究土壤p H分别为4.0、5.5、7.0和8.5时镉超富集植物东南景天和非富集植物垂盆草根际土壤溶液中Cd的形态分布。模型计算结果表明:随着p H的升高,2种植物土壤溶液中Cd2+的比例均逐渐减小,其中东南景天根际土壤溶液中Cd2+占总溶解性Cd的比例为46.1%~3.2%,垂盆草为60.9%~9.9%;当土壤p H≥5.5时,土壤溶液中Cd形态主要以有机络合态(Cd-DOM)为主;2种植物相比,4个p H水平下垂盆草土壤溶液中Cd2+比例均高于东南景天,但东南景天中有机络合态Cd所占比例较大。基于ASV法的测定结果表明:东南景天土壤溶液中电活性Cd占总溶解性Cd的比例从最小(p H 8.5时)的5.5%到最大(p H 4.0时)的79.6%,而垂盆草的变化范围为11.8%~86.7%;电活性Cd的测定结果与Visual MINTEQ 3.0模型计算结果显著相关(R2=0.80),从而互相验证了实验测量和模拟计算的可靠性。     

Effect of periodate oxidation on the polysaccharide content and microaggregate stability of rhizosphere and non-rhizosphere soils

Summary The relationship between the stability of soil microaggregates in water and the polysaccharide content was examined in rhizosphere and non-rhizosphere samples from a pot experiment using three soils that had grown peas, barley or grasses. The polysaccharide was oxidised and removed using 168h treatment with 0.02M periodate followed by 6h with 0.1M tetraborate. The decrease in polysaccharide content, measured as change in residual reducing sugars, was compared with the stability of soil microaggregates (ca 45m) in water, determined by a turbidimetric method.Total C, N and polysaccharide contents of rhizosphere soils were greater than those for the bulk soil, but the water stability of aggregates was not increased compared to unplanted controls. Periodate oxidation removed a large proportion (59–95%) of the polysaccharide and increased aggregated disruption, but there was no clear relationship between the two measurements. In rhizosphere soil, polysaccharides appreared to make less contribution to aggregate stability than polysaccharide in the bulk soil. The relatively small effect of rhizosphere polysaccharides is probably related to their presence as comparatively massive plant remains and debris; this contrasts with the decomposed and transformed material in the bulk soil.     

Effect of brief treatment at alkaline pH on the properties of UDP-glucuronosyltransferase

The kinetic properties of UDP-glucuronosyltransferase were measured after brief treatment of liver microsomes at alkaline pH, followed by assay with p-nitro-phenol as aglycone, at pH 7.5. Enzyme activity increased in a graded fashion as the pH of pretreatment was increased above 8.0, with apparent maximal activation of eight-fold for a pretreatment pH of 11.1. The pH for half maximal activation was 10.6. Brief treatment at alkaline pH prior to assay at pH 7.5 was associated too with a graded conversion of the kinetics of the enzyme from non-Michaelis-Menten to Michaelis-Menten at pH 11.7. Sensitivity to the allosteric modulator, UDP-N-acetylglucosamine decreased as the pH increased. A fifty percent loss of sensitivity to UDP-N-acetylglucosamine-induced activation occurred at pH 10.6. Thus, pretreatment at alkaline pH had irreversible effects on the properties of UDP-glucuronosyltransferase in microsomes. In order to establish the cause for the irreversibility of the changes induced by alkaline pH, microsomes were treated at pH 11.6 prior to purifying UDP-glucuronosyltransferase. Enzyme purified from alkali-treated and untreated microsomes had approximately the same specific activity. More importantly, responses to activation by lipids, and regeneration of allosteric properties were the same for both purified enzymes (from alkali-treated and control microsomes). Pure enzyme was not activated by pretreatment at alkaline pH. We interpret these data to mean that the irreversible effects of alkaline pH on the properties of UDP-glucuronosyltransferase in microsomes were not due to direct effects on the enzyme, but to how the enzyme interacted normally with molecules within the plane of the membrane.     

Effect of alkaline pH on the activity of rat liver phenylalanine hydroxylase

The pH optimum of rat liver phenylalanine hydroxylase is dependent on the structure of the cofactor employed and on the state of activation of the enzyme. The tetrahydrobiopterin-dependent activity of native phenylalanine hydroxylase has a pH optimum of about 8.5. In contrast, the 6,7-dimethyltetrahydropterin-dependent activity is highest at pH 7.0. Activation of phenylalanine hydroxylase either by preincubation with phenylalanine or by limited proteolysis results in a shift of the pH optimum of the tetrahydrobiopterin-dependent activity to pH 7.0. Activation of the enzyme has no effect on the optimal pH of the 6,7-dimethyltetrahydropterin-dependent activity. The different pH optimum of the tetrahydrobiopterin-dependent activity of native phenylalanine hydroxylase is due to a change in the properties of the enzyme when the pH is increased from pH 7 to 9.5. Phenylalanine hydroxylase at alkaline pH appears to be in an altered conformation that is very similar to that of the enzyme which has been activated by preincubation with phenylalanine as determined by changes in the intrinsic protein fluorescence spectrum of the enzyme. Furthermore, phenylalanine hydroxylase which has been preincubated at an alkaline pH in the absence of phenylalanine and subsequently assayed at pH 7.0 in the presence of phenylalanine shows an increase in tetrahydrobiopterin-dependent activity similar to that exhibited by the enzyme which has been activated by preincubation with phenylalanine at neutral pH. Activation of the enzyme also occurs when m-tyrosine or tryptophan replace phenylalanine in the assay mixture. The predominant cause of the increase in activity of the enzyme immediately following preincubation at alkaline pH appears to be the increase in the rate of activation by the amino acid substrate. However, in the absence of substrate activation, phenylalanine hydroxylase preincubated at alkaline pH displays an approximately 2-fold greater intrinsic activity than the native enzyme.     

Phosphorus pools and other soil properties in the rhizosphere of wheat and legumes growing in three soils in monoculture or as a mixture of wheat and legume

Background and aims

Phosphorus and nitrogen availability and forms are affected by soil properties as well as by plant species and further modulated by soil microbes. Additionally, close contact of the roots of two plant species may affect concentrations and forms of N and P. The aim of this study was to assess properties related to N and P cycling in the rhizosphere of wheat and legumes grown in monoculture or in wheat/legume mixtures in three soils differing in pH.

Methods

Faba bean, white lupin and wheat were grown in three soils differing in pH (4.8, 7.5 and 8.8) in monoculture or in mixed culture of wheat and legumes. Rhizosphere soil was collected at flowering and analyzed for P pools by sequential fractionation, available N as well as community structure of bacteria, fungi, ammonia oxidizers, N₂-fixers and P mobilizers by polymerase chain reaction (PCR)—denaturing gradient gel electrophoresis (DGGE).

Results

Soil type was the major factor determining plant growth, rhizosphere nutrient dynamics and microbial community structure. Among the crop species, only faba bean had a significant effect on nitrification potential activity (PNA) in all three soils with lower activity compared to the unplanted soil. Soil type and plant spieces affected the community composition of ammonia-oxidizing archaea (AOB), ammonia-oxidizing archaea (AOA), N₂-fixers (nifH), P mobilizers (ALP gene) and fungi, but not that of bacteria. Among the microbial groups, the AOA and nifH community composition were most strongly affected by crop species, cropping system and soil type, suggesting that these groups are quite sensitive to environmental conditions. All plants depleted some labile as well as non-labile P pools whereas the less labile organic P pools (NaOH extractable P pools, acid extractable P pools) accumulated in the rhizosphere of legumes. The pattern of depletion and accumulation of some P pools differed between monoculture and mixed culture as well as among soils.

Conclusions

Plant growth and rhizosphere properties were mainly affected by soil type, but also by crop species whereas cropping system had the least effect. Wheat and the legumes depleted less labile inorganic P pools in some soils whereas less labile organic P pools (NaOH extractable P, acid extractable P) accumulated in the rhizosphere of legumes.     

Evaluating the effect of increased rates of rhizobial inoculation on grain legume productivity

Intrinsic promiscuity in cowpea and bean enables plants to nodulate with native rhizobia, though sometimes ineffective rhizobia may occupy nodules, resulting in poor response to inoculation. Field trials were conducted from 2014 to 2017 in Marondera, Natural Region II, Zimbabwe, to determine the effect of increasing inoculation rates on legume growth parameters, nitrogen uptake and grain productivity. Treatments included an un-inoculated control and inoculant rates of ×1 (standard), ×2, ×3, ×4, ×5, ×7 and ×10 for both cowpea (rhizobia - inoculant-strain-MAR 1510) and bean (rhizobia-inoculant-strain-CIAT 899). Biomass productivity ranged from 2.05 (×2) - 2.94 t ha^?1 (×4) and 1.10 (×10) – 1.95 t ha^?1 (×4) for cowpea and bean, respectively. Nitrogen uptake increased with increasing inoculation rates reaching up to 57.56 kg N ha^?1 for bean (×4) and 100.20 kg N ha^?1 for cowpea (×3). The uninoculated control was not significantly different from the standard, {(×1); 1 g inoculant 500 g seed^?1} treatment, for cowpea nodule weight and grain productivity. The highest cowpea and bean nodule weights were recorded from the ×3 and ×4 treatments, respectively, in the first season. Cowpea grain yield significantly varied across treatments, ranging between 0.63 and 1.55 t ha^?1 with the ×3 recording the highest yield. The “×4” treatment recorded the highest bean grain productivity reaching up to 0.88 t ha^?1. It can be concluded that, increasing rhizobia cells concentration per unit seed up to ×3 (cowpea) and ×4 (bean) improves response to inoculation and grain productivity suggesting a need to change product formulation or increase inoculation rate.     

Aluminium speciation and phytotoxicity in alkaline soils

Aim

Highly alkaline soils (pH?>?9.0) may adversely affect agricultural crop productivity. Problems encountered include poor structure and nutrient deficiency. Research based on solution cultures suggests that aluminium (Al) phytotoxicity may occur in soils with pH?>?9.0, but little research has been undertaken on actual soils under controlled conditions. The nature of the Al species responsible and the pH regime of the soils when this occurs are unknown.

Methods

The charge and species of Al responsible for this toxicity was investigated using Zeta Potential measurement, Nuclear Magnetic Resonance (NMR) spectroscopy, Al precipitation characteristics and electrical conductivity as a function of pH. An anion exchange resin was used to evaluate Al availability to plants at alkaline pH. To verify Al phytotoxicity, a pot experiment was performed with plants grown at near neutral and high pH, with and without Al.

Results

The anionic aluminate species of aluminium was ubiquitous at highly alkaline pH, and was the dominant charged species at pH 9.2. Aluminium was phytotoxic at high pH, significantly reducing the stem and root development of field pea test plants over and above that caused by alkalinity alone. The effects of both alkalinity in general and aluminium in particular became noticeable at pH 9.0 and debilitating at pH?>?9.2.

Conclusion

As this corresponds to the pH where aluminate becomes dominant, it is probably responsible for the phytotoxicity.     

环境条件对不同品种小麦缺Mn的影响

在温室和网室中进行盆栽试验 ,研究不同环境条件和杂草对冬小麦缺Mn的影响 ,同时探讨不同小麦品种对缺Mn的耐性 ,发现生长在温室中的小麦其缺Mn症尤为严重 ,而从网室转移到温室的小麦因苗期在网室中受降雨渍水影响吸收了较多Mn2 ,缺Mn症就较轻 ,表明环境因子中降雨是影响小麦Mn营养的一个重要因素 ;供试的 3个品种中 331 7较耐缺Mn ,其Mn的吸收量明显高于敏感品种 .此外 ,试验还发现与小麦伴生的杂草麦麦草对Mn吸收能力强 ,是小麦根际Mn营养的有力争夺者 .     

Plant and rhizosphere processes involved in phytoremediation of metal-contaminated soils

This paper reviews the recent advances in understanding of metal removal from contaminated soils, using either hyperaccumulator plants, or high biomass crop species after soil treatment with chelating compounds. Progress has been made at the physiology and molecular level regarding Zn and Ni uptake and translocation in some hyperaccumulators. It is also known that natural hyperaccumulators do not use rhizosphere acidification to enhance their metal uptake. Recently, it has been found that some natural hyperaccumulators proliferate their roots positively in patches of high metal availability. In contrast, non-accumulators actively avoid these areas, and this is one of the mechanisms by which hyperaccumulators absorb more metals when grown in the same soil. However, there are few studies on the exudation and persistence of natural chelating compounds by these plants. It is thought that rhizosphere microorganisms are not important for the hyperaccumulation of metals from soil. Applications of chelates have been shown to induce large accumulations of metals like Pb, U and Au in the shoots of non-hyperaccumulators, by increasing metal solubility and root to shoot translocation. The efficiency of metal uptake does vary with soil properties, and a full understanding of the relative importance of mass flow and diffusion in the presence and absence of artificial chelates is not available. To successfully manipulate and optimise future phytoextraction technologies, it is argued that a fully combined understanding of soil supply and plant uptake is needed.     

Effect of pH on Mn absorption by barley genotypes in a chelate-buffered nutrient solution

A new chelate-buffering technique was used to investigate the effect of pH (6.00, 6.85 and 7.70) on manganese (Mn) absorption from nutrient solution by three genotypes of barley plants differeing in Mn efficiency. The nutrient composition was adjusted such that the calculated activities of Mn²⁺, Zn²⁺, Cu²⁺ and Ni²⁺ were similar in each pH, thus eliminating any effect of the pH treatment on Mn²⁺ supply. Increasing pH from 6.00 to 7.70 increased the rate of Mn absorption and decreased the external Mn requirement for optimal growth rate. With increasing pH, Mn concentrations in roots rose markedly, and were higher than those in shoots at pH 7.70. Genotypic differences in Mn concentration of roots appeared only at higher pH. We suggest that higher Mn concentration in roots of inefficient plants may be related to Mn immobilisation in roots, and this may be a factor in the mechanism of Mn efficiency.     

pH对土壤中土著快、慢生大豆根瘤菌结瘤的影响

1　引　　言土壤 ｐＨ对根瘤菌结瘤的影响一直是微生物学和微生物生态学研究的内容之一[4] .在对大豆根瘤菌的研究中 ,早期的研究主要集中于生长慢、产碱的大豆慢生根瘤菌 (Ｂｒａｄｙｒｈｉｚｏｂｉｕｍｊａｐｏｎｉｃｕｍ) [1,2 ] .1982年 ,Ｋｅｙｓｅｒ等[3] 报道了一类生长快、产酸的大豆根瘤菌 ,并命名为费氏中华根瘤菌 (Ｓｉｎｏｒｈｚｏｂｉｕｍ ｆｒｅｄｉ ｉ) .由于它们在生理特性方面存在着明显的差异 ,其结瘤能力以及环境的生物、物理和化学等因素对结瘤的影响一直受到广泛的重视 .本文研究了偏酸、偏碱的 ｐＨ对费氏中华根瘤菌…