Enhancement of cr(lll) phytoaccumulation

Chromium (III) accumulation in high biomass agricultural crops, sunflower (Helianthus annum) and Indian mustard (Brassica juncea) was studied using four soils (pH 4.6 to 7.6) contaminated with different rates of CrCl₃.6H₂O in the presence of synthetic chelate and organic acids. Chromium is essential for normal glucose metabolism in humans and animals, but its contamination and recovery from soils is of environmental concern. Adding ethylenediaminetetraacetic acid (EDTA), citric acid, or oxalic acid to Cr(III)‐contaminated soils significantly increased Cr concentration in plant shoots and roots. Adding Cr(III) complexes of EDTA, citric acid, and oxalic acid to soils dramatically increased (>200‐fold) Cr concentration in shoots and roots. Plant growth was severely decreased but was dependent on soil type, chelate rate, form, and time of chelate application. Chelates and organic acids enhanced Cr(III) accumulation, but its toxic effects were not avoided. Chromium(III) complexes were as toxic to plants as Cr(VI). The phytoaccumulation and recovery of Cr(III) from soils were limited and depended on soil type.     

Studies in manurial values of seaweeds

Summary The effect of applying dry meal of the seaweedPachymenia himantophora to soil has been investigated. The seaweed was found to greatly increase the availability of manganese which became toxic to plant growth on acid soils. The release of manganese appears to be due to altered soil physical conditions causing waterlogging of soils low in calcium.     

Importance of the type of soil for the induction of micronuclei and the growth of primary roots of Vicia faba treated with the herbicides atrazine, glyphosate and maleic hydrazide.

Research was carried out on the genotoxic effects (induction of micronucleated cells in primary root tips) and toxic effects (reduction in primary root growth) in young plants of Vicia faba grown in soils with different organic matter contents and treated with the herbicides atrazine, glyphosate and maleic hydrazide. The data obtained show that the genotoxic effects are noticeably influenced by the interactions between the herbicide and the type of soil in which the Vicia faba have grown. While maleic hydrazide proved to be highly clastogenic for young plants grown in both soils, atrazine was genotoxic only in young plants grown in soil poor in organic matter. Glyphosate did not induce micronuclei under either soil condition, but induced a significant toxic effect.     

Effect of soil acidity, soil strength and macropores on root growth and morphology of perennial grass species differing in acid-soil resistance

It is unclear whether roots of acid-soil resistant plants have significant advantages, compared with acid-soil sensitive genotypes, when growing in high-strength, acid soils or in acid soils where macropores may allow the effects of soil acidity and strength to be avoided. The responses of root growth and morphology to soil acidity, soil strength and macropores by seedlings of five perennial grass genotypes differing in acid-soil resistance were determined, and the interaction of soil acidity and strength for growth and morphology of roots was investigated. Soil acidity and strength altered root length and architecture, root hair development, and deformed the root tip, especially in acid-soil sensitive genotypes. Root length was restricted to some extent by soil acidity in all genotypes, but the adverse impact of soil acidity on root growth by acid-soil resistant genotypes was greater at high levels of soil strength. Roots reacted to soil acidity when growing in macropores, but elongation through high-strength soil was improved. Soil strength can confound the effect of acidity on root growth, with the sensitivity of acid-resistant genotypes being greater in high-strength soils. This highlights the need to select for genotypes that resist both acidity and high soil strength.     

THE EFFECT OF CERTAIN SOIL TREATMENTS ON DIDYMELLA STEM-ROT OF TOMATOES

About 93% of Didymella lycopersici spores were destroyed after 4 weeks incubation in unsterilized soil. A survey of the microflora of glasshouse soil receiving different treatments and inoculated with D. lycopersici showed no clear relation between numbers of any group of organisms and the incidence of stem rot. Sterilized soil was not made toxic to D. lycopersici by the growth of a number of soil microorganisms even after 9 months incubation, but addition of unsterilized soil or of a suspension of unsterilized soil quickly restored toxicity. Direct observations of spores in soil on slides showed that their fate varied with the treatment of the soil before inoculation. With fresh soil or air-dry soil moistened 2 or more days before inoculation, lysis of spores occurred. With air-dry soil moistened and inoculated simultaneously, some spores germinated but growth of germ tubes soon ceased. No direct connexion could be seen between the fate of the spores and soil microorganisms. Addition of glucose to unsterilized soil reduced its toxicity to D. lycopersici. Soils steamed for 1 min. or longer were not toxic to D. lycopersici , but soils steamed for very short periods were as toxic as unsterilized soils although the soil microflora was much reduced.     

酚顿试剂对竹林土壤中酚类化合物的降解作用

酚类化合物是农业和生态系统中主要的化感物质之一,大量积累在土壤中,抑制作物和林下植物生长,导致农作物减产、连作障碍和自然生态环境破坏。用过氧化氢(H2O2)与硫酸亚铁(Fe2 )所组成的酚顿试剂研究了化学氧化法对化感物质(对香豆酸、对羟基苯甲酸和胡桃醌)、竹林土壤提取物及竹林土壤中对香豆酸的降解作用。过氧化氢与硫酸亚铁的摩尔比为15:1的酚顿试剂,过氧化氢与酚类物质浓度比为8:1时,对酚类物质的降解效率最高。以8×10-3mol/L(0.028%)的H2O2,5.4×10-4mol/L(0.075%)的FeSO4和10-3mol/L的酚类物质组成的反应体系中,反应10min和30min后,对香豆酸的降解率分别为55%和74%;对羟基苯甲酸的降解率在10min时达90%以上;而胡桃醌在10min时已经完全被降解。酚顿试剂处理土壤酚类提取物时,可使其中主要的化感物质对香豆酸降解75%。用含0.1%和1%H2O2的酚顿试剂处理竹(Bambusa chungii)林土壤,土壤对香豆酸的降解率分别为32%和37%。竹林土壤中存在过氧化氢酶和过氧化物酶活性,但没有检测到超氧化物歧化酶活性。土壤中的过氧化氢酶和过氧化物酶可能迅速分解外加的过氧化氢,一方面缩短过氧化氢处理的作用时间和降低降解效率,另一方面可分解过剩的过氧化氢。这说明酚顿试剂是降解土壤和培养液中有害化感物质的有效化学氧化剂。     

Iron toxicity to rice in an acid sulfate soil as influenced by water regimes

Summary The effects of two water regimes: Continuous flooding and flooding with soil drying on iron toxicity to rice in an acid sulfate soil was studied by continuously growing 7 crops of IR-32 rice in pots under the two water treatments. There was no plant growth upto the second crop under both water treatments due to iron toxicity. But there was good growth of rice under the continuous water regime from third cropping onwards, however, there was no growth of rice in the flooding with soil drying treatment even upto the seventh crop due to iron toxicity.The results of the study bring out that keeping an acid sulfate soil flooded for a few weeks and then planting rice when iron in soil solution has dropped below toxicity level may be a possible management practice for lowland rice culture on such soils. Drying and reflooding an acid sulfate soil on the other hand aggravates soil acidity and keeps iron in solution in high amounts to be toxic to rice plant.     

Nodulation and growth ofLablab purpureus (Dolichos lablab) in relation to rhizobium strain,liming and phosphorus

Summary Greenhouse experiments were done with two purposes: (1) to identify strains of rhizobia effective and acid-tolerant in symbiosis withLablab purpureus, and (2) to determine whether soil acidity or the symbiotic condition increased the phosphate requirement for growth.Five rhizobial strains were tested in one neutral soil, two acid soils, and the two acid soils limed to pH 6.6. In the neutral and limed soils, three of the strains were effective (CB1024, CB756, TAL169), but only two strains (CB756, TAL169) remained effective in acid soil.Strain CB756 and plus-N treatments were further compared in a factorial trial involving combinations of five levels of P with lime, no lime and CaCl₂ treatments, applied to an acid soil. Some of the treatments were also applied to plants inoculated with CB1024. Between the N-fertilized and CB756 treatments there was no clear difference in growth response to applied P, and the critical internal concentration of P for 95% of maximal growth was the same (0.22% shoot dry weight). Increasing P beyond levels needed for maximal growth increased nodulation and N concentration in plants inoculated with CB756. It lowered N concentration in N-fertilized plants. There was evidence suggesting that the P requirement of symbiotic plants increased if the soil was acid, or if CB756 were replaced by CB1024 as microsymbiont; but the critical statistical interactions were not significant.     

Cyanuric acid--a s-triazine derivative as a nitrogen source for some soil microorganisms

Cyanuric acid was not toxic for soil microorganisms examined and was even observed to stimulate the growth of Azotobacter in chernozem. Some isolated fungi were capable of cleaving the ring of cyanuric acid. With the use of 15N-labeled cyanuric acid it was found that the nitrogen taken from this compound by Aspergillus minutus and Pseudogymnoascus sp. was incorporated into their proteins. About 70-90% of 15N derived from cyanuric acid was detected in the biomass of the examined fungi. The ability of soil microorganisms to cleave the triazine ring is of importance in the detoxication of soils treated with triazine herbicides.     

The Growth Response of Ecotypes of Holcus lanatus L. from Different Soil Types in Northwestern Europe to Phenolic Acids

Abstract: Phenolics are often discussed in relation to either allelopathy or to herbivory. This work, however, was undertaken to determine if phenolic acids benefit the growth of plants in very acid soils. We here report racial differences in the phenolic acid concentrations of the important plant species found in five sites within Central Scotland which covered a wide range in soil acidity from very acid (organic peats) to mildly acid (calcareous), and describe the racial differences in the growth response of Holcus lanatus L. to phenolic acids with increasing acidity. The total concentrations of phenolic acids in the ecotypes of important species were correlated with the total concentrations found in their respective soils. In general, the most phenolic-rich ecotypes of the five came from the organic acid soils (Flanders Moss [FM] and Sheriffmuir [SMB]). However, with the exception of ferulic acid which was a major component of both acid soils and their associated vegetation, individual simple phenolic acids extracted from either plants or soils were not consistently correlated. The addition of dry plant material collected from the five sites (0.5 g plant material 100 g^-1 soil) to the acid-organic Flanders Moss (FM) soil stimulated the growth of two ecotypes of Holcus (acid-mineral Sheriffmuir [SMM], calcareous Kinloch Rannoch [KR]) but the same litter addition in non-organic, less acidic or calcareous soil inhibited growth of these ecotypes. In hydroponic solutions, growth response of Flanders Moss (FM) and Kinloch Rannoch (KR) to pH and phenolic acid mixtures was interdependent: in acid solutions (pH 4.0) but not at pH 6.5 root elongation rates (RER) of both ecotypes, and shoot elongation rates (SER) of Flanders Moss (FM), increased after treatment with a mixture of seven commonly occurring phenolic acids.     

Abscisic acid concentration,root pH and anatomy do not explain growth differences of chickpea (Cicer arietinum L.) and lupin (Lupinus angustifolius L.) on acid and alkaline soils

The ABA concentrations of leaves, roots, soils and transport fluids of chickpea and lupin plants growing in acid (pH=4.8) and alkaline (pH=8.0) soils and an acid soil with an alkaline subsoil and an alkaline soil with an acid subsoil were measured with the aim of explaining the poor growth of narrow-leafed lupins in alkaline soil. The ABA concentration in the leaves was higher in lupin than chickpea, but did not differ when the plants were grown in alkaline compared to acid soil. The ABA concentration of the roots and xylem sap of lupin did not differ significantly when grown in acid or alkaline soil. Chickpea roots and xylem sap had, however, lower ABA concentrations in acid soil. The ABA concentration in the soil solution was higher in the acid than in the alkaline soil. Roots of lupin and chickpea showed no suberization of the hypodermis or exodermis whether grown aeroponically or hydroponically and the pH of the cytoplasm did not change significantly when root cells of lupin and chickpea were exposed to external pHs of 4.8 or 8.0. The chickpea roots had greater suberization of the endodermal cells adjacent to radial xylem rays and maintained a slightly higher vacuolar pH than lupin in both acid and alkaline external media, but these small differences are insufficient to explain the reductions in lupin growth in alkaline soil.     

Effect of chemical forms of cadmium,zinc, and lead in polluted soils on their uptake by cabbage plants

Sorghum (Sorhum bicolor L. Moench) is an important cereal crop of the world. Performance of sorghum in acid infertile soils that are common to the tropics is rather poor. Research was undertaken in greenhouse and field conditions to evaluate the differences in growth, grain yield, and nutrient efficiency ratio (NER) of sorghum genotypes grown at three levels of Al saturation. The growth of shoots and roots and the grain yields showed significant differences with respect to Al-saturation, genotypes and their interactions. The shoot weights, root weights, and visual scores of the greenhouse study were highly related to grain yields obtained in field. The greenhouse technique adapted in this study appears to be a reliable method for separation of genotypes into Al-tolerant and intolerant types. The NER values helped differentiate genotypes into efficient and inefficient utilizers of the absorbed nutrients. The sorghum entries showed intraspecific genetic diversity in growth and NER values for the essential elements in the presence or absence of toxic levels of Al. We concluded that selection of acid soil tolerant genotypes and further breeding of acid soil (Al) tolerant cultivars is feasible in sorghum.IICA/EMBRAPA/World Bank     

Arbuscular mycorrhizal adaptation,spore germination,root colonization,and host plant growth and mineral acquisition at low pH

Arbuscular mycorrhizal (AM) fungi colonize plant roots and often enhance host plant growth and mineral acquisition, particularly for plants grown under low nutrient and mineral stress conditions. Information about AM fungi and mycorrhizal ( +AM) host plant responses at low pH ( < 5) is limited. Acaulospora are widely reported in acid soil, and Gigaspora sp. appear to be more common in acid soils than Glomus sp. Spores of some AM fungi are more tolerant to acid conditions and high Al than others; t Acaulospora sp., Gigaspora sp., and Glomus manihotis are particularly tolerant. Root colonization is generally less in low than in high pH soils. Percentage root colonization is generally not related to dry matter (DM) produced. Maximum enhancement of plant growth in acid soil varies with AM fungal isolate and soil pH, indicating adaptation of AM isolates to edaphic conditions. Acquisition of many mineral nutrients other than P and Zn is enhanced by +AM plants in acid soil, and the minerals whose concentration is enhanced are those commonly deficient in acid soils (Ca, Mg, and K). Some AM fungal isolates are effective in overcoming soil acidity factors, especially Al toxicity, that restrict plant growth at low pH.     

施用尿素引起红壤pH及铝活性的短期变化

酸性红壤在我国南方广泛分布,其酸性是限制大多数作物生长的一个主要环境胁迫因子,主要原因是低pH条件下土壤中Al的溶解所导致的毒性.对3种红壤施用不同浓度的尿素,其pH值在短期内都随着施入尿素浓度的增大而急剧上升,交换性Al随着施用尿素浓度的增大而急剧下降.交换性Al含量与土壤pH值变化呈显著负相关.动态试验表明,pH值上升的现象是短期的,pH值在达最大值后缓慢下降,下降幅度最大的阶段在第2～4周.短期内,施用尿素能显著降低酸性土壤对玉米的铝毒效应.     

Oxidation of pipecolic acid in soils and in rhizosphere soil of different plants

Soil respiration was proportional to its total carbon content. Maximum respiratory activity occurred in garden soil, followed in descending order by chernozem soil, brown soil, and sand. The oxidation of pipecolic acid, as studied by the Warburg manometric technique, in different rhizosphere soils from four crops 7, 13 and 20 days after planting as well as from one crop grown in different soils, was consistently in all cases faster than that by the corresponding non-rhizosphere soils. The curves of the rate of oxygen consumption during pipecolic acid oxidation, by garden soil (whether rhizosphere or non-rhizosphere soil) as well as by chernozem rhizosphere soil of different plants at the three stages of plant growth studied contained two peaks (two phases), whereas in non-rhizosphere chernozem soil as well as in brown soil and sand (whether affected or not affected by plant roots) only one peak was attained in the curves of the rate of oxygen uptake. The rapidity with which pipecolic acid was oxidized in the rhizosphere soil differed from plant to plant and at different phases of plant growth, and also with the type of soil used for plant growing. The extent of pipecolic acid oxidation after the first and second (if it occurred) phases did not differ in the different soils, both rhizosphere and non-rhizosphere soil, but the rate of oxygen uptake was higher in rhizosphere than in the corresponding non-rhizosphere soil. During the first phase, oxygen uptake accounted for slightly less than one-third of the total amount of oxygen required for complete oxidation of the added pipecolic acid. About two-thirds of that total amount were taken up during the both phases of oxidation.     

Preface

Biological properties of soil are not only essential for the maintenance of soil fertility and the sustainability of the plant-soil ecosystems, but also indicators of land reclamation of contaminated or disturbed soils. This experiment involves two plants (barley and field pea) growing in four soils with different hydrocarbon contents. The objective was to study the effect of hydrocarbons on plant growth and microbial activity, and to evaluate the acid phosphatase activity as an indicator of reclamation of hydrocarbon-contaminated soils. Barley root mass decreased with the increase of the hydrocarbon content but field pea roots were not sensitive to the hydrocarbon content in this experiment. The hydrocarbon contamination reduced the plant growth but increased the microbial activity. The acid phosphatase activity was controlled by both plant root production and microbial activity, therefore it was not a good indicator of the reclamation of oil-contaminated soils.     

Interactions of calcium sulfite with soils and plants

CaSO₃ is a by-product formed by several of the processes used for scrubbing SO₂ from flue gas produced by coal-burning power generators. Using CaSO₃ to improve the calcium status of acid soils would be a beneficial alternative to disposal in landfills. CaSO₃ has biocidal properties and is used as a disinfectant and food and drink preservative. It is important to evaluate under what conditions application to soils would not harm plant growth. Laboratory experiments confirmed that two transformations of CaSO₃ occurred in soil systems: (1) decomposition to produce SO₂ gas, and (2) oxidation to calcium sulfate. Conversion to SO₂ occurred in solution and soil at low pH, and acid soils treated with CaSO₃ were initially toxic to seedling root growth. The degree of toxicity was time-dependent, with reduction in toxicity occurring as CaSO₃ oxidized to calcium sulfate. Soil reaction also influenced toxicity, and at soil pH levels above 6, little seedling toxicity was evident.     

Soil aluminium effects on uptake,influx, and transport of nutrients in sorghum genotypes

Sorghum [Sorghum bicolor (L.) Moench] is the fifth most important cereal crop of the world. In South America, it is grown mainly on acid soils, and its production on these soils is limited by deficient levels of available P, Ca, Mg, and micronutrients, and toxic levels of Al and Mn. A greenhouse experiment was undertaken to evaluate the genotypic differences in sorghum for uptake (U), inhibition (IH), influx (IN) into roots, and transport (TR) to shoot for nutrients at three levels of soil Al saturation (2, 41, 64%). Overall shoot nutrient U, IN, and TR showed a significant inverse correlation with soil Al saturation and shoot Al concentration, and a significant positive correlation with shoot and root dry weight. The nutrient uptake parameters differentiated genotypes into most and least efficient categories at various levels of soil Al saturation. The nutrient uptake parameters showed significant differences with respect to soil Al saturation, genotypes, and their interactions. In the current study, Al tolerant genotypes recorded higher IN and TR for P, K, Ca, Mg, Zn, and Fe than Al-sensitive genotypes. Therefore, these U, IN, and TR traits could be used in selection of sorghum plants adaptable to acid soils. Sorghum genotypes used in this study showed intraspecific genetic diversity in U, IN, and TR for essential nutrients. It was concluded that selection of acid soil tolerant genotypes and further breeding of acid (Al) tolerant sorghum cultivars are feasible.IICA/EMBRAPA/World BankIICA/EMBRAPA/World BankIICA/EMBRAPA/World Bank     

Comparative toxicity of nanoparticulate CuO and ZnO to soil bacterial communities

The increasing industrial application of metal oxide Engineered Nano-Particles (ENPs) is likely to increase their environmental release to soils. While the potential of metal oxide ENPs as environmental toxicants has been shown, lack of suitable control treatments have compromised the power of many previous assessments. We evaluated the ecotoxicity of ENP (nano) forms of Zn and Cu oxides in two different soils by measuring their ability to inhibit bacterial growth. We could show a direct acute toxicity of nano-CuO acting on soil bacteria while the macroparticulate (bulk) form of CuO was not toxic. In comparison, CuSO(4) was more toxic than either oxide form. Unlike Cu, all forms of Zn were toxic to soil bacteria, and the bulk-ZnO was more toxic than the nano-ZnO. The ZnSO(4) addition was not consistently more toxic than the oxide forms. Consistently, we found a tight link between the dissolved concentration of metal in solution and the inhibition of bacterial growth. The inconsistent toxicological response between soils could be explained by different resulting concentrations of metals in soil solution. Our findings suggested that the principal mechanism of toxicity was dissolution of metal oxides and sulphates into a metal ion form known to be highly toxic to bacteria, and not a direct effect of nano-sized particles acting on bacteria. We propose that integrated efforts toward directly assessing bioavailable metal concentrations are more valuable than spending resources to reassess ecotoxicology of ENPs separately from general metal toxicity.     

Effect of the chemical and physical condition of the soil on Verticillium wilt of antirrhinum

Summary In vitro study showed thatVerticillium dahliae Kleb. grew well in a wide range of acid and alkaline media (viz. pH 3.5 to 10.5). The best growth of the fungus was observed in pH 5.5. Soil pH 3.5 was toxic for growing antirrhinum seedlings. Development of Verticillium wilt of antirrhinum was affected by soil pH. The severity of the disease was greater in alkaline soil conditions compared with acid conditions. Soil of pH 3.5 gave very good control of the symptom expression by the infected plants. Rhizosphere analysis results showed that fungal population with the exception ofPenicillium spp., was drastically reduced in the rhizosphere of the plants grown in acid soil. Although the overall population of fungi was reduced in theV. dahliae infected antirrhinum rhizosphere in acid soil, the population ofPenicillium spp. markedly increased. The antagonistic activity of thePenicillium spp. in the rhizosphere might also have reduced the disease severity. Since the seedlings did not grow properly in very dry and very wet soil, rhizosphere analysis of these soils was not possible. Disease severity was much less in wet soil compared with plants grown in medium moisture level and dry soil, but the plant growth was very poor. Dedicated to the memory of the late Prof. H. K. Baruah from whom I had the inspiration for research