Water deficits and hydraulic limits to leaf water supply

Many aspects of plant water use -- particularly in response to soil drought -- may have as their basis the alteration of hydraulic conductance from soil to canopy. The regulation of plant water potential (Psi) by stomatal control and leaf area adjustment may be necessary to maximize water uptake on the one hand, while avoiding loss of hydraulic contact with the soil water on the other. Modelling the changes in hydraulic conductance with pressure gradients in the continuum allows the prediction of water use as a function of soil environment and plant architectural and xylem traits. Large differences in water use between species can be attributed in part to differences in their 'hydraulic equipment' that is presumably optimized for drawing water from a particular temporal and spatial niche in the soil environment. A number of studies have identified hydraulic limits as the cause of partial or complete foliar dieback in response to drought. The interactions between root:shoot ratio, rooting depth, xylem properties, and soil properties in influencing the limits to canopy water supply can be used to predict which combinations should optimize water use in a given circumstance. The hydraulic approach can improve our understanding of the coupling of canopy processes to soil environment, and the adaptive significance of stomatal behaviour.     

Soil conditions and plant growth'

Plants can respond to soil conditions in ways that can not readily be explained in terms of the ability of the roots to take up water and nutrients. Roots may sense difficult conditions in the soil and thence send inhibitory signals to the shoots which harden the plants against the consequences of a deteriorating or restrictive environment, especially if the plants' water supply is at risk. Generally, this behaviour can be interpreted as feedforward responses to the soil becoming too dry or too hard, or to the available soil volume being very small as with bonsai plants, or to roots' becoming infected with pathogens. However, soil that is too soft or in which the roots are forced to grow in very large pores can also induce large conservative responses, the significance of which is unclear. The inhibitory signals may affect stomatal conductance, cell expansion, cell division and the rate of leaf appearance. Their nature is still under debate, and the debate is becoming increasingly complex, which probably signifies that a network of hormonal and other responses is involved in attuning the growth and development of a plant to its environment.     

Magnetic susceptibilities of lake sediment and soils on the shoreline of Lake Naivasha,Kenya

On steep, unvegetated slopes, sands (particle sizes 0.063 to 2 mm) and gravels (2–64 mm) erode from the shoreline of Lake Naivasha (Kenya) and enter the lake basin. This occurred freely where fringing papyrus (Cyperus papyrus) swamp had been cleared in favour of landing jetties or agriculture. Gravel-sized particles have been recovered up to 60 m offshore and sands to 80 m. In an area where papyrus was undisturbed and the swamp margin was 52 m wide, gravel did not enter the lake and sands penetrated to around 35 m. Large particles are much easier to trace to source and to manage than the finer silts and clays (<0.63 m) that form the bulk of Lake Naivasha's sediment. The pattern of mass specific magnetic susceptibilities for the <63 m fraction of lake sediment around the southern shoreline of the lake suggests that fine particles enter open water directly from the shoreline and are not transported from the lake's only perennial inflow, the River Malewa in the north. Such particles originate from a hinterland that supports high intensity horticulture and are therefore a potential source of contamination. Mean ± SD susceptibility (_If) immediately offshore papyrus fringe was 0.49 ± 0.08 × 10^-6 m³ kg^-1 compared with higher values of 1.33 ± 0.14 × 10^-6 m³ kg^-1 where there was no papyrus barrier (P<0.0001). The value for five sites in the middle parts of the lake was 0.45 ± 0.02 × 10^-6 m³ kg^-1 with 1.38 ± 0.10 × 10^-6 m³ kg^-1 near the mouth of the River Malewa. The results of this study are evidence, therefore, that conservation of a continuous papyrus margin of about 50 m width is a priority for intercepting particulate material.     

Long-term effectiveness of vivianite in reducing iron chlorosis in olive trees

Iron (Fe) chlorosis is common in olive (Olea europaea L.) trees growing on highly calcareous soils in Southern Spain, where generally causes reduction in yield, size and commercial value of the olives. The objective of this research was to study the effectiveness of synthetic vivianite (Fe₃(PO₄)₂H₂O) to reduce Fe chlorosis in olive. Experiments were established in three orchards with cultivars `Hojiblanco', `Manzanillo', and `Picual'. The design was a randomised block design with two or three treatments (control with no Fe fertiliser and vivianite at one or two rates). A vivianite suspension (0.05 kg dm<sup>–3</sup> water) was injected into the soil at 10–20 points around the tree at the depth of maximum root density (25–35 cm). The rates (and times of application) were 0.5 and 1 kg tree<sup>–1</sup> for `Hojiblanco' (March 1997), 1 kg tree^–1 for `Manzanillo' (March 1998), and 2 kg tree<sup>–1</sup> for `Picual' (March 1998). The leaf chlorophyll content index (CCI) was estimated on the youngest expanded leaves by means of a Minolta apparatus (SPAD units). The colour index of the olives was estimated by visual comparison with a scale ranging from 1 (pale yellow) to 8 (normal green). For the period studied (July 1997–November 1999), the CCI of fertilised trees was, in general, significantly higher than that of control trees, and so was the case with the olive colour index. Olive yield, measured in the experimental fields with `Hojiblanco' (in 1999) and `Manzanillo' (in 1998 and 1999), was higher for the fertilised than for the control trees but differences were only significant in 1999. These results suggest that vivianite is effective to reduce Fe chlorosis for more than two seasons. Such effectiveness is probably due to the poorly crystalline Fe(III) oxides (which are good sources of Fe to plants) that result from the slow oxidation and incongruent dissolution of vivianite.     

Cadmium removal capacities of filamentous soil fungi isolated from industrially polluted sediments,in La Plata (Argentina)

Aspergillus terreus, Cladosporium cladosporioides, Fusarium oxysporum, Gliocladium roseum, Penicillium spp., Talaromyces helicus and Trichoderma koningii were isolated from heavily polluted streams near an industrial area in La Plata, Argentina. The fungi were obtained from sediments with 0.25–0.50 mg Cd/l and they were isolated in cadmium-basal medium. They were then cultivated to evaluate their Cd detoxification abilities. The biomass developed in static assays represented 5–53% of the yield of stirred cultures, for the different fungal species, although the cadmium absorption were similar in both cases. These soil fungi represented 50% of the total isolates and their mycelial growth was conspicuous in these polluted sediments. Although bacteria have been mentioned as active microorganisms against heavy metals, the mycelial fungi were able to develop a significantly higher mass to sequestrate more metals. Thus, they could be used in remediation biotechnology to improve the Cd detoxification of chronically contaminated habitats.     

Physical education - new technologies for mapping plant genomes

Locating DNA sequences to specific chromosomal segments is essential for associating genes with phenotypes. It is routinely achieved by segregation analysis using meiotic mapping populations that have also been used to collect phenotypic information. However, meiotic mapping is struggling to cope with the shear volume of sequences emerging from high-throughput (HTP) gene-discovery programs. We describe two approaches, Radiation Hybrid and ‘HAPPY’ mapping, which, in conjunction with meiotic mapping, represent valuable HTP tools in the quest to link genes to phenotypes.     

不测土条件下半定量施肥原理和模型评述

1　不测土条件下半定量推荐施肥的需求矿质营养学说是施肥最基本原理 ,它的诞生标志着人类主动施肥时期的开始。从早期的定性施肥阶段 ,发展到今天的定量施肥阶段 ,如何确定施肥量一直是施肥技术的核心和难点。测土是定量施肥或精确施肥的前提。然而 ,测土本身存在各种偏差或精度、测土需要费用 ,本文仅对代表性的不测土施肥模型及其原理进行评述。即使有了土壤有效养分的测定结果 ,如何将其转化为一季内土壤提供的养分量一直是个理论难题 ,特别是Ｎ素土壤供应量更为难测或难以估算。因此 ,如何在使用定量施肥模型的同时 ,而又将土壤养分因…     

Cultivar-Specific Carbohydrate-Binding Properties of Lectins from Broad-Bean Seeds

Lectins were isolated and purified from three broad bean (Vicia faba L.) cultivars differing in the effectiveness of their symbiosis with root nodule bacteria (Rhizobium leguminosarum bv. viciae). From seeds of symbiotically effective cvs. Aushra and Daiva, we isolated only one lectin from each cultivar, whereas two lectins, Yu-1 and Yu-2, were isolated from seeds of symbiotically ineffective cv. Yugeva. Lectins from cvs. Aushra and Daiva were more active than lectins from cv. Yugeva and exhibited similar carbohydrate specificity. Methyl--D-mannopyranoside and trehalose were the most potent inhibitors of their hemagglutination activity. Lectin Yu-1 resembled them in its carbohydrate-binding properties. However, D-mannose, trehalose, and melecitose were its most effective inhibitors. Lectin Yu-2 differed substantially from these lectins. It exhibited an affinity for D-glucuronic acid, D-glucosamine, and 2-deoxy-D-glucose. In addition, it could interact with carbohydrates of the galactose family (2-deoxy-D-galactose, D-galactosamine, and lactose) and also with D-xylose and 2-deoxy-D-talose. Thus, lectins from cvs. Aushra and Daiva and also Yu-1 can be considered D-mannose/D-glucose-specific lectins, whereas Yu-2 lectin exhibited a combined carbohydrate specificity. The affinity of Yu-1 and Yu-2 lectins for their natural receptors, exopolysaccharides and lipopolysaccharides of broad-bean nodule bacteria, was twice as low as that of lectins from cvs. Aushra and Daiva. We believe that properties of seed lectins are an important cultivar-specific trait that determines host-plant (broad beans) specificity during the establishment of legume–rhizobia symbiosis.     

A research on the microfungal flora of somegreenhouse soils in the vicinity of LapsekiÇanakkale,Turkey

Qualitative and quantitative distributions of microfungal flora of the some greenhouse soils in the vicinity of Lapseki, Canakkale were studied. A total of 25 soil samples were collected from 10 cm depth in five greenhouses. Using soil dilution technique, 128 different microfungal isolates were obtained Isolates collected belonged to Oomycetes (1), Zygomycetes (7), Ascomycetes (9) and 96 belonging to the Deuteromycetes Fifteen isolates were classified as Mycelia Sterilia. The genera of microfungi most abundant in the greenhouse soils were Aspergillus, Penicillium, Geomyces, Exophiala and Fusarium. Qualitative and quantitative distributions of the Aspergillus were higher than those of the other genera. It was found that the maximum value was in greenhouse 5 and the minimum value was in greenhouse 4. The solarization method was the most effective in reducing fungal numbers.     

The development of potential screens based on shoot calcium and iron concentrations for the evaluation of tolerance in Egyptian genotypes of white lupin (Lupinus albus L.) to limed soils

European cultivars of white lupin (Lupinus albus L.) grow poorly in limed or calcareous soils. However, Egyptian genotypes are grown successfully in highly calcareous soil and show no stress symptoms. To examine their physiological responses to alkaline soil and develop potential screens for tolerance, three experiments were conducted in limed and non-limed (neutral pH) soil. Measurements included net CO2 uptake, and the partitioning of Fe2+ and Fe3+ and soluble and insoluble Ca in stem and leaf tissue. Intolerant plants showed clear symptoms of stress, whereas stress in the Egyptian genotypes and in L pilosus Murr. (a tolerant species) was less marked. Only the intolerant plants became chlorotic and this contributed to their reduced net CO2 uptake in the limed soil. In contrast, Egyptian genotypes and L pilosus showed no change in net CO2 uptake between the soils. The partitioning of Ca and Fe either resulted from the stress responses, or was itself a stress response. L pilosus and some Egyptian genotypes differed in soluble Ca concentrations compared with the intolerant cultivars, although no significant difference was apparent in the Ca partitioning of the Egyptian genotype Giza 1. In a limed soil, Giza 1 maintained its stem Fe3+ concentration at a level comparable with that of plants grown in non-limed soil, whereas stem [Fe3+] of an intolerant genotype increased. Gizal increased the percentage of plant Fe that was Fe2+ in its leaf tissue under these conditions; that of the intolerant genotype was reduced. The potential tolerance of the Egyptian genotypes through these mechanisms and the possibility of nutritional-based screens are discussed.