ALBERT

Notes: [Auszug] The procedure employed was to measure the reac tion rates for a series of different sector speeds as in the normal rotating-sector method1, but the rates were obtained from the expansion/time plots as in the dilatometric non-stationary state method6 instead of the usual contraction/time curves. By ...

Notes: [Auszug] Fig. 1. Dilatometer and vacuum jacket. Constriction at A is sealed when dilatometer has been filled with monomer Fig. 2. The variation of volume with time immediately following the commencement of irradiation of vinyl acetate photosensitized with 1.1' azo-ftis-cg/c/ohexane carbonitrile at 25 C. ...

Notes: We investigated the influence of root border cells on the colonisation of seedling Zea mays roots by Pseudomonas fluorescens SBW25 in sandy loam soil packed at two dry bulk densities. Numbers of colony forming units (CFU) were counted on sequential sections of root for intact and decapped inoculated roots grown in loose (1.0 mg m−3) and compacted (1.3 mg m−3) soil. After two days of root growth, the numbers of P. fluorescens (CFU cm−1) were highest on the section of root just below the seed with progressively fewer bacteria near the tip, irrespective of density. The decapped roots had significantly more colonies of P. fluorescens at the tip compared with the intact roots: approximately 100-fold more in the loose and 30-fold more in the compact soil. In addition, confocal images of the root tips grown in agar showed that P. fluorescens could only be detected on the tips of the decapped roots. These results indicated that border cells, and their associated mucilage, prevented complete colonization of the root tip by the biocontrol agent P. fluorescens, possibly by acting as a disposable surface or sheath around the cap.

Notes: [Auszug] In a study of the effect of ferric chloride in dimethylformamide solution on photosensitized vinyl polymerization, we have found the system much more complex. First, ferric chloride has a high extinction coefficient (5 x 103 l.mole?1cm?1) at 3650 Å, and consequently, except at very low ...

Notes: Abstract. Hard-setting soils are widespread in dry regions. Their properties are described and a physical explanation for hard-setting behaviour is given. The limitations on soil management and physical fertility caused by hard-setting depend on timing of rainfall or irrigation with respect to cultivations and crop development, and much research is needed to quantify reductions in crop yield imposed by these limitations.

Notes: Roots grow thicker in compacted soil, even though it requires greater force for a large object to penetrate soil than it does for a small one. We examined the advantage of thickening in terms of the stresses around a root penetrating with constant shape, rather than the stresses around an expanding cylinder or sphere, as has been studied previously. We combined experiments and simulations of the stresses around roots growing in compacted soils. We measured the diameter of pea roots growing in sandy loam and clay loam at four different densities, and the critical-state properties of the soils. At a penetration resistance of about 1 MPa the diameter of the roots in the sandy loam was about 40% greater than that at 0.7 MPa, and at 2 MPa it was about 60% greater. In the clay loam, there was less thickening – about 10% greater at 1 MPa and about 20% greater at 1.5 MPa. The maximum axial stresses were predicted using a critical-state finite-element model to be at the very tip of the root cap. When there was friction between the root and the soil, shear stresses were predicted with smaller values at the tip than just behind the tip. When the interface between the soil and the root was assumed to be frictionless, there were by definition no shear stresses. In the frictionless case the advantage of root thickening on relieving peak stress at the root tip was diminished. The axial and shear stresses were predicted to be smaller in the clay loam than in the sandy loam and may explain why the roots did not thicken in this soil although its resistance to penetration was similar. Our results suggest that the local values of axial and shear stresses experienced by the root near its tip may be as important in constraining root growth as the total penetration resistance.

Notes: Friction accounts for a large proportion of the resistance to a penetrometer probe, often much more so than to a plant root. The contribution of frictional resistance to penetrometer resistance was investigated in five soils with texture ranging from sandy loam to silty clay. The effect on penetration resistance of rotating the conical tip of the probe was studied in both intact cores of undisturbed field soil, and in cores remoulded from sieved soil. Rotation altered the orientation of the vector of frictional resistance towards a direction perpendicular to the probe axis, and so decreased the component of frictional resistance that opposed the axial penetration of the probe. The decrease in friction was greater for probes with a semiangle of 5° than those with a 30° semiangle and was more than half of the total resistance to a nonrotating probe in 15 out of the 16 cases studied. A theoretical treatment of the effect of rotation period on probe resistance showed good agreement with the experimental results. The penetration resistance of a metal probe is related to that of a root in terms of frictional resistance and factors such as the penetration rate. When all frictional resistance was subtracted from the resistance measured to the penetration of a 5 semiangle probe, the remaining resistance was similar to that measured for roots growing in the same soil.

Notes: The production of exudates by plant roots and microbes in the rhizosphere, together with intense wetting and drying cycles due to evapotranspiration, stimulate changes in soil structure. We have attempted to separate these two processes using an experimental model with bacterial exopolysaccharides (dextran and xanthan) and root mucilage analogues (polygalacturonic acid, PGA), and up to 10 cycles of wetting and drying. To characterize the soil structure, tensile strength, water sorptivity and ethanol sorptivity of the amended soils were measured, and thin sections were made. Xanthan and PGA induced greater tensile strength of the amended soil, suggesting that they increased the bond energy between particles. Porosity increased with each cycle of wetting and drying, and this increase was less pronounced for the PGA 2 g l−1 than for the xanthan and dextran. This suggests that PGA stabilized the soil against the disruptive effect caused by the wetting and drying. The PGA was the only polysaccharide that influenced water sorptivity and repellency, resulting in slower wetting of the treated soil. Wetting and drying led to an increase of the sorptivity and a decrease of the repellency for all treatments with the exception of the PGA-amended soils. The PGA may therefore stabilize the soil structure in the rhizosphere by increasing the strength of bonds between particles and decreasing the wetting rate.〈section xml:id="abs1-2"〉〈title type="main"〉Influence de mucilages racinaire et microbiens modèles sur la structure du sol et le transport d'eau〈section xml:id="abs1-3"〉〈title type="main"〉RésuméLa production d'exsudats par les plantes et les microbes de la rhizosphère ainsi que les cycles d'humectation–dessiccation très intense due à l'évapotranspiration, entraînent des modifications de la structure du sol. Notre objectif a été de séparer ces deux processus en utilisant un modèle expérimental avec des polysaccharides bactériens (dextran et xanthan) et un analogue d'exsudat racinaire (acide polygalacturonique, APG), et jusqu'à dix cycles d'humectation et dessiccation. Afin de caractériser la structure du sol, la résistance en traction ainsi que l'infiltration de l'eau et de l'éthanol dans le sol amendé par les différents polymères ont été mesurés, et des lames minces ont été réalisées. Le xanthan et l'APG ont provoqué la plus forte augmentation de la résistance en traction, ce qui serait attribuable à une plus grande énergie de liaison entre les particules de sol. La porosité a augmenté avec chaque cycle d'humectation–dessiccation pour tous les traitements et cette augmentation a été moins prononcée pour l'APG 2 g l−1 par rapport au xanthan et au dextran. Cela suggère que l'APG a stabilisé le sol contre la déstructuration provoquée par les cycles d'humectation–dessiccation. L'APG a été le seul polysaccharide qui a influencé– dans le sens d'une diminution – l'infiltration de l'eau dans le sol amendé. Les cycles d'humectation–dessiccation ont entraîné une augmentation de l'infiltration de l'eau dans le sol amendé par les différents polymères à l'exception de l'APG. Ce dernier stabiliserait donc la structure du sol dans la rhizosphère en augmentant la force de liaison entre les particules et en diminuant la vitesse d'humectation du sol.

Notes: A technique is described for non-destructive observations and analysis of root growth in granular media, using time-lapse video in conjunction with a pressure cell. The pressure cell consists of one half of a traditional triaxial cell with a flat clear perspex front allowing growth of the root to be monitored using a video camera. The cell is connected to an external pressure supply, which is used to regulate precisely the confining pressure, and hence, the physical impedance to root growth. Preliminary results of the growth of root axes and the emergence of laterals of peas over a range of physical impedances are presented to illustrate the potential of this technique in studying root growth.