The effect of pellet size on the ammonia loss from urea applied to forest soil

Summary Using diluted phosphoric acid- and glycerol-treated polyurethane plastic foam discs as static ammonia absorbers, the extent of ammonia loss from applied urea was determined on forest soil under field conditions. The investigation, which primarily involved a comparison of urea materials of two different pellet sizes (2–4 mg and 2060 mg urea per pellet, respectively), extended over a period of 28 days. The urea was applied to the soil surface at a rate of 200 kg N per hectare.It was found that the gaseous ammonia loss from the large-pellet urea (tablets) was markedly lower than that from the small-pellet urea during the first two weeks of exposure. On extending the observation period to four weeks, this difference in cumulative ammonia loss decreased successively. After 28 days' exposure, at a daily mean temperature of 13°C, the volatile loss amounted to 20 and 22 per cent, respectively. An addition of 5% (w/w) of a solution of concentrated orthophosphoric acid, or a fine-crystalline ortho-boric acid to the large-pellet urea, resulted in a reduction of the loss to half the value. The possibilities of controlling the ammonia loss from urea by combining the large pellet size with the addition of urease inhibitors are discussed. re]19721012     

Assessment of volatilization loss of ammonia from surface-applied urea on forest soil by N15 recovery

Summary Using vertically isolated micro-plots the isotopic recovery technique was tested for assessing the extent of ammonia volatilization loss from N¹⁵-labelled urea applied on the forest floor (Pinus silvestris L.). The size of the ammonia loss was obtained as a difference between the amounts of labelled urea N added and the amounts of labelled N recovered in the soil profile after 13, 31, and 39 days's exposure, respectively. Urea materials of two different pellet size were used: granulated small pellets (280 pellets per gram) and tablets (2.06 g each). The nitrogen application rate was 200 kg N per hectare. The recovery data for 13 days' exposure indicated a volatilization loss, which for the small pellet urea was 24.9 per cent and for the tabletted urea 12.1 per cent. The corresponding figures for the 31 days' exposure, during which the total amount of precipitation was 14 mm, were 15.1 and 26.9 per cent, respectively. The pattern of labelled N distribution in the soil profile examined showed that during the period of exposure in question a leaching loss of labelled N was rather unlikely. It was demonstrated, furthermore, that nitrogen from the tabletted urea had diffused to a greater depth of the soil than that from the small-pellet urea. Nitrogen from the small-pellet urea was to a large extent recovered in the litter layer. On exposure to heavy rain the tabletted urea was subjected to the highest leaching loss. An addition of 10 per cent (w/w) of metaphosphoric acid or sublimed sulphur to the tabletted urea did not result in any further reduction of the volatilization loss. The merits and limits of the isotopic recovery technique are discussed.     

Water loss from cut grass with special reference to hay-making

Water loss from cut grass was studied to determine factors limiting the drying process. An apparatus, used to measure water loss at 28±1°C from blotting paper and from leaves and stem internodes of cocksfoot, consisted of four channels in which air speed was controlled at 25–80 cm s^-1 and relative humidity at 7–68%. The maximum rate of water loss from wet blotting paper was 10500 mg water dm^-2 h^-1 but from leaves and stem internodes supplied with water it was less than 250 mg dm^-2 h^-1. The rate of loss from both plant specimens and blotting paper was linearly related to the vapour pressure differences between the specimen and the surrounding air but was not increased when air speed was changed from 40 to 80 cm s^-1. Grass specimens supplied with water had lower rates of water loss than wet blotting paper because of tissue resistances which were calculated for (a) untreated leaf and stem specimens, (b) rubbed leaves, (c) cut leaves, (d) leaves exposed to steam for 60 s. Treatments (b)-(d) greatly reduced tissue resistances. The rates of drying of leaves and stem internodes not supplied with water changed only slightly in response to faster air speeds but were significantly increased by treatments (b), (c), (c_s) (split stems), (d) and (e) (exposure to petroleum vapour for 60 s). The most effective treatments trebled the drying rates of leaves and increased the drying rates of stem internodes by 10 times. Reductions in relative humidity had little effect on drying rate following treatments (a), (b), (c) and (d), but when treatments (c_s) and (e) were given, additional significant increases in drying rates were obtained when the relative humidity was reduced. Grass specimens given the most effective treatments and dried under the most favourable conditions did not utilize the full drying capacity of the environment, for the rates of water loss from these specimens were at least three times lower than those from wet blotting paper. The results indicate that high rates of drying could be achieved at 28 ^oC or similar temperatures if practical treatments were developed to remove or greatly reduce the high resistance to water loss in cut grass.     

Further observations on Potamodiscus Gerloff =Pinaciophora Greeff, with special reference to Alaska and arctic Canada

Pinaciophora spiculata sp. nov. is described on the basis of two complete periplasts collected in arctic Canada at—l°C in 1973. One has been tested for silicon by means of X-ray microanalysis with strongly positive results. The species possesses dimorphic scales, the spicular scales and exceptionally small plate-scales being equally diagnostic. The circumstances under which the name has already appeared in the literature are explained. In addition, the known ranges of two other taxa are extended by broken periplasts recovered from other arctic or subarctic areas, notably P. denticulata Thomsen (plate scales only) formerly known from Peru and now from South Alaska (at Homer) while the type species of the genus ( Poturnodiscus kalbei Gerloff 1968= Pinaciophora fluivatilis Greeff 1875) is demonstrated both from South Alaska and from beneath sea ice in North Alaska, in both localities possibly introduced into the sea by freshwater drainage.     

Further observations on the genus Pappomonas Manton et Oates with special reference to P. virgulosa sp. nov. from West Greenland

Electron microscopy of dried preparations of Arctic nanoplankton has permitted a second species of the recently erected genus Pappomonas Manton et Oates to be described and named. P. virgulosa sp. nov. is characterised by coccolith appendages composed of a central shaft ending in a cluster of four finger-like rods. There are also calcified plates of characteristic construction, without appendages. Detailed observations on the coccoliths, especially on the shapes and arrangement of component calcite crystallites and the presence of unmineralised components, have permitted further comparisons to be made with equivalent structures in Papposphaera lepida Tangen, recently investigated in the southern hemisphere, as well as with Pappomonas flabellifera Manton et Oates. As a working hypothesis, an interpretation of coccolith morphology in all three taxa has been formulated in terms of known structural components of uncalcified scales in Chrysochromulina spp. The need for fuller information on certain details, notably the coccolith bases in Pappomonas spp. is stressed.     

Patterns of ammonia volatilization from a forest soil

Summary Ammonia volatilization from urea-treated soils was estimated under field and laboratory conditions. Acid-washed filter papers were hung in the air in a spruce stand treated with N and P fertilizers in a factorial design. In the laboratory, moss sods were incubated to quantify ammonia volatilization.Ammonia volatilization increased with the level of N applied and more ammonia was absorbed by filter papers at 0.6 m above the ground than those at 1.2 m. Maximum rates of ammonia volatilization in urea-treated plots were observed between the third and fourth day after fertilizer application and similar absorption patterns were observed in areas not treated with urea. It is, therefore, suggested that ammonia volatilized from urea-treated plots can move to untreated areas. Addition of P along with urea significantly reduced ammonia volatilization under field conditions.Laboratory experiments showed that addition of urea to moss sods increased the pH of the organic layer from about 3.6 to 8.8. Sphagnum moss sods volatilized more ammonia (about 1.7 per cent of the added material) than feather moss sods (about 0.8 per cent). At higher incubation temperatures, however, the rate of ammonia volatilization decreased in sphagnum moss sods but increased in feather moss sods.     

Further observations on Calliacantha Leadbeater Choanoflagellata), with special reference to C. simplex sp. nov. from many parts of the world.

C. simplex is a new species with an unusually wide geographical range, occurring at sea temperatures as varied as 0 degrees C under ice at Pt Barrow or -1 degrees C in arctic Canada, to 22 degrees C on the equator at the Galapagos Islands. The morphology and range of variation are illustrated by means of light microscopy, transmission electron microscopy and scanning electron microscopy applied to dry whole mounts prepared in situ from freshly-gathered wild material. Among the diagnostic structural features, special interest attaches to the position of the anterior transverse costa which is located unusually far back in comparison with other members of the genus; it is also shown to be within and not outside the ring of four longitudinal costae building up the lorica chamber, although this feature can only be ascertained by scanning. The differences between this species and C. natans (type species of the genus) are shown to be greater and to involve more characters than could previously have been recognized, and some possible functional implications are discussed in a preliminary way.     

Laboratory measurements and simulations of ammonia volatilization from urea applied to calcareous Chinese loess soils

Ammonia volatilization is the major pathway for mineral nitrogen loss in the calcareous soils of the Chinese loess plateau, with maximum losses reaching 50% of the fertilizer-N applied. A volatilization-diffusion experiment was carried out in the laboratory using a forced-draft system and soil columns of 15.5 cm depth. Urea was surface applied at rates of 210 kg N ha^-1 to a soil with 10% CaCO₃ and a pH of 7.7. The amount of ammonia volatilized as well as the concentration profiles of ammoniacal-nitrogen and soil pH in the upper 50 mm of the soil columns after 4, 7 and 10 days were measured and subsequently modelled. The mechanistic model of Rachhpal-Singh and Nye, originally developed for neutral, non-calcareous soils, was modified to include the pH-buffering action of the soil carbonates. Model parameters were independently determined or taken from the literature. Measured and predicted cumulative NH₃ losses agreed very well in the first 10 days following fertilizer application. However, in contrast to the simulations, NH₃-volatilization was still proceeding in the experiment even after 13 days, with cumulative losses reaching 60% of the applied N. In addition to the high initial soil pH, the low bulk density and high volumetric air content of the soil columns used for the experiment proved decisive for the high rates of ammonia volatilization, provoking a strong increase in the amount of ammoniacal-N diffusing towards the soil surface as gaseous NH₃. The simulations showed that due to the high soil pH, the buffering action of the soil carbonates played a comparatively smaller role.     

土壤盐渍化对尿素与磷酸脲氨挥发的影响

氨挥发是肥料氮素损失的重要途径之一,肥料类型、土壤类型、肥料用量以及土壤全盐量均影响氨挥发损失率及挥发特征。本文采用通气法测定了磷酸脲和尿素两种肥料六个施肥量处理分别施入六个不同盐渍化程度（1.7、9.9、16.4、23.2、29.1、37.9 g/kg）的土壤后氨挥发累积状况和动力学特性,以及土壤氨挥发累积量与土壤电导值之间的相关性。结果表明：（1）在土壤总盐介于1.66 -37.9 g/kg的范围内,随着土壤含盐量增加,尿素与磷酸脲处理的氨挥发累积量显著增加;土壤含盐量对氨挥发速率有显著的促进作用。（2）各处理二次线性函数拟合的二项式系数a均为负值,表明：在不同盐渍化条件下肥料的挥发速率是随着时间增长而降低的;一次线性函数和Elovich 方程的斜率a随土壤含盐量增加而增大,表明：土壤盐渍化将加剧土壤的氨挥发速率。（3）土壤氨挥发累积量与电导值拟合结果符合logistic方程（︱R︱分别为0.9732,0.9815,0.965,0.9182,0.9817,0.9971︱R︱>r0.01=0.9172, n=6）,氨挥发累积量随土壤电导值呈“S”型增长。     

Calanoid copepods from South Georgia,with special reference to size dimorphism within the genus Pseudoboeckella

Summary Three species of calanoid copepods, Boeckella michaelseni, Parabroteas sarsii and Pseudoboeckella poppei were recorded from 6 freshwater localities in the Husvik area, South Georgia. Of the latter species two distinct size morphs occurred, with no overlap in size even in closely situated populations. The large morph was recorded in lakes, the small was found in ponds. The small morph did not coexist with the large predatory P. sarsii, and we suggest predation pressure from this species as the major cause for the observed distribution of these morphs. The pronounced size segregation as well as small morphological dissimilarities suggest that these morphs are reproductively isolated. While the large morphotype corresponds to that of P. poppei, the taxonomic affinities of the small morph are uncertain.     

Further segregation analysis of the fragile X syndrome with special reference to transmitting males

Summary A new series of 96 pedigrees with the fra(X) syndrome was analysed using complex segregation analysis with pointers, defining affection as any degree of mental impairment. These families were found to exhibit the same segregation pattern as the first series of 110 pedigrees (Sherman et al. 1984). The best estimate for penetrance of mental impairment in males was 79% and in females was 35% for the combined data. Again, there was little evidence for sporadic cases among affected males.Many more intellectually normal transmitting males have been observed since the existence of such males and the concomitant need to investigate the paternal side of pedigrees was recognized. On further investigation of all 206 pedigrees from the old and new data sets, the sibships of nonexpressing males appeared to be different from those of expressing males. Our analysis, using mental impairment as the phenotype, suggested that obligate carrier mothers and daughters of intellectually normal transmitting males are rarely, if ever, mentally impaired and that the sibs of transmitting males are much less likely to be retarded than the sibs of mentally impaired males. Though mothers and daughters of transmitting males are similar in phenotype, the expression of the gene in their offspring appears to be different: the penetrance of mental impairment is higher in offspring of intellectually normal daughters of transmitting males than in offspring of intellectually normal mothers of transmitting males. The implications of these observations for genetic counseling and for genetic models of the fra(X) syndrome are discussed.