Physical factors influencing decomposition of organic materials in soil aggregates

Glucose or starch labelled with ¹⁴C was mixed thoroughly into slurried soils. Aggregates of different sizes were obtained from the soils as they dried. The labelled substrates were considered to be distributed in both micro- and macropores in the aggregates. Control samples (labelled substrates in macropores only) were prepared by adding the labelled carbohydrates after the formation of the aggregates. The various samples were sterilized by γ-irradiation and stored at ?15°C.Samples were wetted to about ?20kPa, inoculated with soil organisms, and incubated for 4 weeks at 28°C in closed systems, which enabled regular measurement of ¹⁴CO₂ released.Based on the ¹⁴CO₂ released, it was concluded that starch was protected from microbial attack when present in micropores in aggregates made from fine sandy loam.After incubation samples were dried and rewetted. The flush of ¹⁴CO₂ released was twice as big for samples containing labelled starch compared with glucose, showing that disruption of aggregates, containing residual starch, and rearrangements of soil components are as important as chemical and biological factors in causing the flush of CO₂ resulting from wetting a soil. Mechanical disruption of the aggregates resulted in a similar flush of ¹⁴CO₂.     

Soil and erosion features of the central plateau region of Tigrai,Ethiopia

The results of reconnaissance soil surveys covering 6,000 km² are used to describe the Central Plateau region, which lies at elevations of 2,000 to 2,800 m in northern Ethiopia. Landform and soil sequences on calcareous shales, dolerites and sandstones are described, in which the principal soil units are Lithosols, Luvisols, Cambisols, Arenosols and Vertisols. Detailed morphological and analytical data are presented for a profile representative of arable soils in each sequence.Small-scale subsistence cultivation of cereals is the dominant land use; all land which is physically cultivable is at present cultivated. Settlement patterns are closely related to soil type, nucleated settlement occurring on fine textured soils but dispersed settlement on coarser textured and more freely draining soils.Erosion and soil moisture features of the three landforms described were investigated and compared. Empirical methods and suspended sediment measurements indicate high rates of regional soil loss (17–33 t ha^?1 yr^?1), accounted for by seasonally high rates of rainfall erosivity, steep terrain and poor land use. The recent development of gully erosion is seen to be linked to the disintegration of waterfall tufas. Application of the universal soil loss equation to arable lands indicates potential annual soil losses in the range of 400 t ha^?1 on Vertisols to 200 t ha^?1 on Cambisols: differences in rates are ascribed principally to differences in crop planting dates, which affect the degree of vegetative protection during periods of high rainfall erosivity.Soil moisture is shown to be in the available range for less than three months in the year. The time at which moisture in the profile enters the available range differed between the three soils monitored and was found to be closely related to the crop planting date, thus indirectly affecting the erosion hazard.     

Effect of infection of seminal and nodal roots by the take-all fungus on tiller numbers and shoot weight of wheat

A simple technique is described for the separation of seminal and nodal roots of wheat grown in pots. The effect of infection of either of the root-systems of wheat by the take-all fungus on tiller numbers and shoot weight was investigated using a variation of the technique. Both root systems were necrosed by the introduced inoculum of the pathogen to which they were exposed when they were about 7 days old. Although infection of either of the root systems resulted in significant reduction of tiller numbers, only infection of nodal roots caused significant reduction of shoot weight.     

Effects of organic amendments on evolution of ethylene and other hydrocarbons from soil

Evolution of C₂H₄ from soils under anaerobic conditions was stimulated by amendment with cereal straw, but hay had little effect. Temporary restoration of aerobic conditions resulted in large increases in C₃ and C₄ hydrocarbons, with both straw and hay amendments. Several known products of the fermentative degradation of carbohydrate increased the evolution of hydrocarbons under anaerobic, and to a greater extent, under aerobic conditions. In particular, ethanol and butyric acid promoted the formation of C₂H₄ and propylene, respectively. The association between degradation products and C₂H₄ suggests that both may be implicated when root growth is adversely affected by the anaerobic decomposition of plant residues.     

An outbreak of botulism in gulls on the Firth of Forth,Scotland

The first recorded outbreak of type C botulism in gulls (Larus spp.) in Britain is described. Between June and October 1975, at least 2080 gulls died around the Firth of Forth. The hot dry summer favoured the proliferation of the causative organism, Clostridium botulinum. A definite source of the botulism was not found but prompt removal of the carcases and covering the pools where Cl. botulinum was growing appeared to reduce the mortality. Immunity acquired during widespread exposure to the disease in 1975 may have prevented the reappearance of botulism during the similar climatic conditions in 1976.     

Laboratory study of phosphorus forms and test procedures on soils under aerobic and anaerobic conditions

The inorganic forms of phosphorus in nine samples of surface soils from the Nainital Tarai of India were determined by a series of extractions with different reagents after incubation for 45 days under aerobic or anaerobic conditions. The forms of phosphorus in samples incubated under aerobic conditions and the pH range of 7.2–8.5 indicated that the soils had been subject to slight chemical weathering. Anaerobic incubation to simulate conditions in lowland rice paddies converted part of the inorganic phosphorus into more labile forms, based on changes in amounts of isotopically exchangeable phosphorus. Amounts of the element converted to more labile forms differed among the nine soil samples.A better correlation was found between amounts of phosphorus extracted by 0.5M NaHCO³ (Olsen's method) than by 0.03N NH₄F in 0.25N HCl (Bray's method) and the isotopically exchangeable phosphorus. The better correlation suggests that the bicarbonate extraction would be the better method for estimating “availablelrd phosphorus in soils of lowland rice paddies. Recalibration of the test prior to such use seems desirable to allow for increases in amounts of phosphorus in labile forms after soils have been shifted from aerobic to anaerobic conditions.     

Management of radioactive waste

The safe management of the solid radioactive waste material generated by the various operations that make up the rapidly growing nuclear electric power industry, the nuclear reactors themselves, and the plants which provide new fuel for these reactors and process the spent fuel which results from reactor operations are discussed.     

THE VISUAL ESTIMATION OF PASTURE AVAILABILITY USING STANDARD PASTURE CORES

A coring technique (6), that may be used for estimating the mean amount of herbage on closely grazed pastures, has been adapted to include visual scoring. Two methods are described, both of which use sets of pasture cores from the sward as reference standards. The observers score the herbage on view at random sites against the standards. In the first method the scores are converted to herbage yields directly by reference to the yields of the standards. In the second method a double sampling regression technique is used and the set of standards is used as a visual guide only.