Nitrogenous fertilizer transformations in the sudan Gezira soil

Summary and Conclusions Direct measurements were made of losses of ammonia during the transformation of urea and ammonium sulphate, surface-applied to alkaline Gezira soil in containers incubated in the field, under different rates of nitrogen application and moisture conditions.The highest rate of ammonia loss occurred during the first week after application with both fertilizers, thereafter decreasing to lower values. The cumulative ammonia loss was higher with higher application of nitrogen. Ammonium sulphate gave consistently higher ammonia losses than urea and losses from open soil system were generally less than from soil in polythene bags.With lowest irrigation level used, ammonia loss attained a sizeable value throughout the incubation period with both fertilizers. With the higher moisture levels, the magnitude of ammonia loss decreased appreciably, much more so with urea than with ammonium sulphate. Induced drying and rewetting prolonged the duration of loss and increased the magnitude of cumulative loss. An appreciable loss of ammonia may take place from fertillzed Gezira Soil under warm conditions, low moisture levels and high fertilizer concentration; this may be the case with patchy fertilizer distribution and frequent light showers during early summer. It is advisable to apply the urea or ammonium sulphate when conditions are most favourable for nitrification.     

Mineralization and gaseous losses of nitrogen from urea and ammonium sulphate in salt-affected soils

Summary An incubation study on mineralization and gaseous losses of nitrogen was conducted on three soils with increasing levels (1.1 to 50 mmhos/cm) of salinity and two levels of urea and ammonium sulphate upto 6 weeks. Mineralization of nitrogen increased with time and decreased with the increase of salinity. It was more from ammonium sulphate than urea, and relatively more from the lower dose. The gaseous losses of NH₄-N increased with salinity. About 35±5 per cent of added N was lost in the gaseous form at maximum (ECe=45 to 50 mmhos/cm) salinity and losses were more from light than heavier soils. Salinity and pH, both were correlated negatively with the N mineralisation and positively with the gaseous losses of ammonia in these salt-affected soils. re]19751105     

Effect of trickle fertigation with three forms of nitrogen on soil pH,levels of extractable nutrients below the emitter and plant growth

The effects of application of nitrogen as calcium nitrate, urea or ammonium sulphate at two rates through the trickle irrigation system on pH and nutrient status of the wetted volume of soil below the emitters and on growth and nutrition of courgette (zucchini) plants (Cucurbita pepo L.) was investigated. Soil acidification, caused by nitrification, occurred to a large extent in the volume of soil immediately below the emitters in the urea and ammonium sulphate treatments. Acidification was greater at the high rate of N addition and more pronounced with ammonium sulphate than urea. A significant amount of applied urea appeared to move through the soil as urea and consequently, at the same rate of N addition, levels of ammonium were lower directly below the emitter and those of nitrate were higher further away from the emitters for the urea than ammonium sulphate treatments. Soil acidification below the emitters resulted in significant decreases in levels of exchangeable Ca, Mg and K and increases in levels of exchangeable Al, EDTA-extractable Fe, Mn, Zn and Cu and bicarbonate-extractable P. Vegetative growth and harvestable yields of courgettes were increased by both irrigation and nitrogen applications. Vegetative growth was generally greater at the low rate of N addition than at the high one and generally followed the order calcium nitrate > urea > ammonium sulphate. However, fruit yields followed the order urea > ammonium sulphate > calcium nitrate and were larger at the high rate of N for urea and ammonium sulphate treatments and unaffected by rate for the calcium nitrate treatments. It is suggested that with fertigation, the form of applied N can have significant physiological effects of plant growth and yields because N may be applied into the root zone on numerous occasions during the growing season.     

Nitrogen transformations in a small mountain stream

Ammonium, urea, and nitrate were added to Bear Brook, a second and third order stream in the Hubbard Brook Experimental Forest, New Hampshire. Removal of ammonium and urea during downstream transport coincided with the release of nitrate. Nitrate removal did not occur when it was added alone or with dissolved organic carbon. Laboratory experiments showed that coarse particulate organic material (detritus) and bryophytes taken from the streambed were active in the removal of ammonium from enriched stream water, and in the release of nitrate upon the addition of ammonium.The patterns of removal and release observed in these experiments suggest a biologically mediated, oxidation process. Budgetary calculations show that the in-stream transformation of nitrogen inputs during summer and autumn could represent 12 to 25 percent of the nitrogen exported as nitrate during winter and spring from heterotrophic streams like Bear Brook. This type of internal cycling affects the timing and form of nitrogen export from small streams draining forested watersheds in the northeastern United States.     

Volatilization of ammonia from submerged tropical soils

Summary A laboratory study was made of the losses of nitrogen through ammonia volatilization from four flooded, tropical soils. The soils used varied considerably in pH, organic matter content, and cation exchange capacity. Losses were measured from the unamended soils, and from ammonium sulphate and urea-treated soils. Two rates of nitrogen application (approximately 50 and 200 kg/ha N) and two methods of application (simulated field broadcast and fertilizer incorporation) of the nitrogen were used. Losses of ammonia were detected for each of the unamended soils, including an acid sulphate soil of pH 3.6. Increased application of both ammonium sulphate and urea resulted in increased losses of ammonia through volatilization. Incorporation of the nitrogen into the mud of the flooded soils significantly decreased losses due to volatilization. It was concluded that the initial or ‘aerobic’ pH of the soils was the soil characteristic most closely related to the magnitude of losses due to volatilization.     

Urea Uptake and Carbon Fixation by Marine Pelagic Bacteria and Archaea during the Arctic Summer and Winter Seasons

How Arctic climate change might translate into alterations of biogeochemical cycles of carbon (C) and nitrogen (N) with respect to inorganic and organic N utilization is not well understood. This study combined ¹⁵N uptake rate measurements for ammonium, nitrate, and urea with ¹⁵N- and ¹³C-based DNA stable-isotope probing (SIP). The objective was to identify active bacterial and archeal plankton and their role in N and C uptake during the Arctic summer and winter seasons. We hypothesized that bacteria and archaea would successfully compete for nitrate and urea during the Arctic winter but not during the summer, when phytoplankton dominate the uptake of these nitrogen sources. Samples were collected at a coastal station near Barrow, AK, during August and January. During both seasons, ammonium uptake rates were greater than those for nitrate or urea, and nitrate uptake rates remained lower than those for ammonium or urea. SIP experiments indicated a strong seasonal shift of bacterial and archaeal N utilization from ammonium during the summer to urea during the winter but did not support a similar seasonal pattern of nitrate utilization. Analysis of 16S rRNA gene sequences obtained from each SIP fraction implicated marine group I Crenarchaeota (MGIC) as well as Betaproteobacteria, Firmicutes, SAR11, and SAR324 in N uptake from urea during the winter. Similarly, ¹³C SIP data suggested dark carbon fixation for MGIC, as well as for several proteobacterial lineages and the Firmicutes. These data are consistent with urea-fueled nitrification by polar archaea and bacteria, which may be advantageous under dark conditions.     

The effect of intermittent flooding on the growth and yield of wetland rice and nitrogen-loss mechanism with surface applied and deep placed urea

Summary Wetland rice was cultivated in pots of puddled soil under continuous and intermittent flooding conditions. The soil was either fertilized with the surface application of prilled urea in three split doses or once with urea supergranules applied at different soil levels.The grain yield, fertilizer efficiency and percent nitrogen recovery by the grains were increased by deep placement of urea supergranules independent of the water regime. Grain yield was always lower with intermittent flooding, particularly when the plants were fertilized with the surface application of prilled urea.Nitrogen loss by ammonia volatilization, measured in a closed cuvette system, was reduced from 24% with the surface application of urea prills and 20% with surface application of urea supergranules to approximately 2% with deep placement of urea supergranules. Intermittent flooding created conditions which promoted additional nitrogen loss by nitrification and denitrification processes. The total nitrogen loss, measured in an open cuvette system, was about 38% with the surface application of urea supergranules, whereas this loss was reduced to 10% with deep placement of urea supergranules. Furthermore, deep placement of urea fertilizer reduced the nitrogen loss irrespective of water regime.     

Nitrogen nutrition of ginger (Zingiber officinale)

Summary Two fertilizer experiments were conducted in the field at Beerwah, South-East Queensland. In the first experiment leaf nitrogen concentrations, and the yield of ginger shoots and rhizomes at early and late harvests increased both with the total amount of nitrogen applied up to the highest level studied (336 kg N/ha as ammonium nitrate) and with the number of applications making up the total. At all levels of nitrogen application the apparent recovery of fertilizer nitrogen increased in the order 1 application <2 applications <4 applications. At 33.6 kg N/ha there appeared to be no advantage in dividing the total N applied into more than 4 applications but the data suggested higher recoveries of nitrogen with 8 applications at 112 kg N/ha and 336 kg N/ha. In the second experiment, ammonium nitrate, urea, and ammonium sulphate were found to be equally effective as nitrogen fertilizers for ginger when applied at equal rates of nitrogen per hectare. However, in terms of cost effectiveness they rated in the order urea > ammonium nitrate > ammonium sulphate.All three nitrogen sources acidified the soil, the decrease in soil pH during the growing season increasing with increasing rate of application. In Experiment 1 split applications, which increased the recovery of applied nitrogen in the crop, also increased the extent of acidification. In Experiment 2 ammonium sulphate tended to be more strongly acidifying than the other fertilizers but the difference was statistically significant only at the highest rate of nitrogen application. Because of the strong effects of nitrogen supply on both yield and soil pH, the highest yields were associated with end-of-season pH values below 5.0.     

The simple open soil method of measuring urea volatilisation losses

Summary A simple technique of estimating ammonia volatilisation loss from urea applied to soil is described. The soil is incubated with urea, after which hydrochloric acid is added to prevent loss of N from the hydrolysed urea during drying of the soil. The volatilisation loss is estimated by difference between the N recovered from the soil and the urea applied. Recovery studies of urea hydrolysis on 3 Malaysian soils show that the hydrolysis products, consisting of ammonium N and any unreacted urea, can be quantitatively recovered from the soil by this technique, with average recoveries of 95%–97%. A cross-check by 9 laboratories indicated good accuracy and precision in the method. When the open soil method was compared with the direct measurement of ammonia loss in simple volatilisation chambers, it gave much higher results suggesting that the closed system of trapping tended to underestimate volatilisation losses during urea hydrolysis.     

The role of nitrogen in promoting the toxic cyanophyte Cylindrospermopsis raciborskii in a subtropical water reservoir

1. The relative contribution of dissolved and atmospheric nitrogen to promoting dominance of the toxic nitrogen‐fixing cyanobacterium, Cylindrospermopsis raciborskii was examined in a subtropical water reservoir, North Pine Reservoir. 2. A combination of process studies in situ and analysis of historical water quality data suggests that nitrogen fixation was not the principal mechanism for acquiring nitrogen and unlikely to be the mechanism whereby C. raciborskii gains a competitive advantage. Ammonium was the preferred nitrogen source, followed by nitrate then nitrogen fixation. 3. Ammonium uptake rates in the euphotic zone were higher in the summer and autumn months compared with winter and spring coinciding with lower ammonium concentrations. Nitrate uptake rates did not appear to vary seasonally and were lower than those for ammonium in the summer, but similar in winter. Nitrate concentrations were higher in winter than summer and generally higher than ammonium concentrations. 4. Ammonium and nitrate uptake rates were similar at light intensities between 10% and 100% of surface light, contrasting with primary productivity which peaked between about 10 to 20% of surface light. Thus the phytoplankton population was adapted to low light conditions but remained able to utilise dissolved inorganic nitrogen over a wide range of light conditions. 5. The ammonium pool in the surface waters was relatively small compared with the phytoplankton uptake rates, and ammonium must therefore be rapidly recycled through the food web over periods of less than 1 h. Short‐term depletion may result, during which time the higher concentrations of nitrate are likely to provide a supplementary supply of nitrogen. 6. The dominance of C. raciborskii in this reservoir is more likely to be due to a superior ability to scavenge and store the low concentrations of phosphate, and a superior adaptation to the low light conditions exacerbated by artificial mixing.     

Nitrogen balance sheet of (NH4)2SO4-gypsum pellets and mixtures and ureaformaldehyde applied to corn in pots of sand

Summary A comparison of ammonium sulphate added to sand pots in different ways and ureaformaldehyde as sources of N to corn plants was carried out. The results showed that nitrogen utilization by plants from ammonium sulphategypsum pellets was greater than its utilization when ammonium sulphate was mixed with gypsum or when the pellets were ground or from ureaformaldehyde. The leached nitrogen from the pellets, ammonium sulphate applied in 3 portions and ureaformaldehyde was not significantly different and was lower than other ammonium sulphate treatments. The nitrogen remaining in pots fertilized by ureaformaldehyde was much greater than the corresponding amount in the case of all ammonium sulphate treatments. Gaseous loss of nitrogen took place in all nitrogen treatments with the loss from ammonium sulphate-gypsum pellets being the lowest.Incubation in sand of ureaformaldehyde, urea, and ammonium sulphate was carried out to understand better the growth conditions of corn fertilized by ureaformaldehyde. In the case of ureaformaldehyde- and urea-sand systems, the pH increased, NO₂ ^– accumulated and considerable loss of nitrogen took place. The pH, the NO₂ ^– accumulation and the loss of N tended to decrease with gypsum increments. re]19720801     

水氮互作对冬小麦田氨挥发损失和产量的影响

2015-2017年利用水肥渗漏研究池,以‘石麦15’(SM15)为材料,采用随机区组设计,设置2个氮肥类型(尿素和有机肥牛粪)、2个施氮水平(180和90 kg·hm^-2)、2个灌溉水平(500和250 mm)进行试验,探讨水、氮及其互作对冬小麦田土壤氨挥发损失量和籽粒产量的影响.结果表明: 施肥以后土壤氨挥发持续7 d左右.2015-2016年施肥后各处理土壤氨挥发损失总量为13.36～46.04 kg·hm^-2,氨挥发氮肥损失率为8.9%～41.1%,2016-2017年各处理土壤氨挥发损失总量为14.78～52.99 kg·hm^-2,氨挥发氮肥损失率为9.2%～45.8%;两年试验内氨挥发损失量最多的处理为W₂U₁(施尿素N 180 kg·hm^-2,灌溉量250 mm),氨挥发损失率最高的处理为W₂U₂(施尿素N 90 kg·hm^-2,灌溉量250 mm),合理的水氮管理可以显著降低土壤氨挥发损失率,施用尿素造成的土壤氨挥发损失为有机肥的2～3倍.两年试验均以W₁M₁(施牛粪N 180 kg·hm^-2,灌溉量500 mm)的小麦产量最高,灌溉量、肥料类型和施氮量互作对冬小麦产量影响极显著.综合氨挥发损失量和冬小麦籽粒产量,本试验条件下,水氮互作效应显著,冬小麦生育期内总灌溉量500 mm、施有机肥180 kg·hm^-2时冬小麦季土壤氨挥发损失率较低,产量最高,施用有机肥的增产效果优于尿素,可作为黄淮海地区冬小麦实际生产中增产增效的水肥优化管理方式.     

SEASONAL VARIATIONS IN TOTAL NITROGEN,CARBON AND AMINO ACIDS IN MACROCYSTIS INTEGRIFOLIA AND NEREOCYSTIS LUETKEANA (PHAEOPHYTA)1

Seasonal variations in tissue nitrogen, carbon, amino acids and ammonium were determined for the brown algae Macrocystis integrifolia Bory and Nereocystis luetkeana (Mertens) Pastels and Ruprecht, For M. integrifolia, the proportions of tissue nitrogen and carbon in blades, bulbs and stipes were also determined. The composition of the two algae in terms of the above constituents was similar. In addition, ammonium, nitrogen and protein-bound amino acids showed distinct seasonal trends with high values during the winter and low levels during the summer. The range for nitrogen was 0.8–3.0% and for proteins 7.6–11.7% of dry weight. In contrast, carbon content and C/N ratio showed the reverse trend with higher values during the summer and lower values during the winter. The range for carbon was 19–31% of dry weight, and the C/N ratio showed a range of 9–37. The free amino acids did not show any specific seasonably. Tissue nitrogen and carbon showed higher values in the blades than in the bulbs and stipes.     

Autotrophic ammonia oxidation at low pH through urea hydrolysis.

Ammonia oxidation in laboratory liquid batch cultures of autotrophic ammonia oxidizers rarely occurs at pH values less than 7, due to ionization of ammonia and the requirement for ammonium transport rather than diffusion of ammonia. Nevertheless, there is strong evidence for autotrophic nitrification in acid soils, which may be carried out by ammonia oxidizers capable of using urea as a source of ammonia. To determine the mechanism of urea-linked ammonia oxidation, a ureolytic autotrophic ammonia oxidizer, Nitrosospira sp. strain NPAV, was grown in liquid batch culture at a range of pH values with either ammonium or urea as the sole nitrogen source. Growth and nitrite production from ammonium did not occur at pH values below 7. Growth on urea occurred at pH values in the range 4 to 7.5 but ceased when urea hydrolysis was complete, even though ammonia, released during urea hydrolysis, remained in the medium. The results support a mechanism whereby urea enters the cells by diffusion and intracellular urea hydrolysis and ammonia oxidation occur independently of extracellular pH in the range 4 to 7.5. A proportion of the ammonia produced during this process diffuses from the cell and is not subsequently available for growth if the extracellular pH is less than 7. Ureolysis therefore provides a mechanism for nitrification in acid soils, but a proportion of the ammonium produced is likely to be released from the cell and may be used by other soil organisms.     

Ammonium and urea removal by Spirulina platensis

Different concentrations either of ammonium chloride or urea were used in batch and fed-batch cultivations of Spirulina platensis to evaluate the possibility of substituting nitrate by cheaper reduced nitrogen sources in wastewaters biotreatment. The maximum nitrogen concentration able to sustain the batch growth of this microalga without inhibition was 1.7 mM in both cases. Ammonium chloride was limiting for the growth at lower concentrations, whereas inhibition took place at higher levels. This inhibition effect was less marked with urea, likely because the enzymatic hydrolysis of this compound by urease controlled the ammonia transfer into the cell. Fed-batch experiments carried out by pulse-feeding either ammonium or urea proved that the use of these compounds as nitrogen sources can sustain the long term-cultivation of S. platensis, provided that the conditions for their feeding are accurately optimized.     

Effect of nitrogen sources on oxidoreductive enzymes and ethanol production during D-xylose fermentation by Candida shehatae.

The effect on D-xylose utilization and the corresponding xylitol and ethanol production by Candida shehatae (ATCC 22984) were examined with different nitrogen sources. These included organic (urea, asparagine, and peptone) and inorganic (ammonium chloride, ammonium nitrate, ammonium sulphate, and potassium nitrate) sources. Candida shehatae did not grow on potassium nitrate. Improved ethanol production (Y(p/s), yield coefficient (grams product/grams substrate), 0.34) was observed when organic nitrogen sources were used. Correspondingly, the xylitol production was also higher with organic sources. Ammonium sulphate showed the highest ethanol:xylitol ratio (11.0) among all the nitrogen sources tested. The ratio of NADH- to NADPH-linked D-xylose reductase (EC 1.1.1.21) appeared to be rate limiting during ethanologenesis of D-xylose. The levels of xylitol dehydrogenase (EC 1.1.1.9) were also elevated in the presence of organic nitrogen sources. These results may be useful in the optimization of alcohol production by C. shehatae during continuous fermentation of D-xylose.     

Nitrogen excretion and changes in blood components during emersion of the subtidal spider crab Maia squinado (L.)

Survival ability of Maia squinado to emersion and subsequent reimmersion was determined in winter and summer conditions. Male spider crabs were less tolerant of emersion than females. Emersion (up to 24 h in summer and to 48 h in winter) induced a marked reduction of nitrogen excretion, especially ammonia excretion. Increase in blood ammonia content was rapid and very high in summer (1750 micromol l(-1)), but non-lethal levels. Estimation of the body ammonia overload showed that only 30% of unexcreted ammonia accumulated in blood. The ammonia release at reimmersion indicated that ammonia also accumulated in other body compartments. Increase in blood urate content, which indirectly reduces ammonia production, was similar at both seasons. Emersed M. squinado was rapidly resorting to anaerobic metabolism, especially in summer when its blood haemocyanin content is low. A strong hyperglycemia was developed in the first 12 h of emersion at both seasons. Mortality occurring beyond 24 h of reimmersion, when the body ammonia overload is cancelled and the recovery of most of blood components is achieved, remains unexplained.     

Protein synthesis, RNA concentrations, nitrogen excretion, and metabolism vary seasonally in the Antarctic holothurian Heterocucumis steineni (Ludwig 1898)

Seasonal changes in protein and nitrogen metabolism have not previously been reported in any Antarctic suspension-feeding species that ceases feeding for extended periods in winter. To provide comparison with data reported on Nacella concinna, a species that continues to feed in winter, we have measured feeding activity; oxygen consumption; ammonia, urea, and fluorescamine-positive substance (FPS) excretion; O : N ratios; body wall protein synthesis; RNA to protein ratios; and RNA activity at three times during the year in an Antarctic suspension-feeding holothurian. Feeding activity ceased for 4 mo during winter, and oxygen consumption rates decreased from 8.79+/-0.43 micro mol h(-1) to 4.48+/-0.34 micro mol h(-1). Ammonia excretion also decreased during winter from 2,600+/-177 nmol N h(-1) to 974+/-70 nmol N h(-1), but urea excretion rates increased from 178+/-36 nmol N h(-1) to 281+/-110 nmol N h(-1), while FPS excretion rates remained unchanged throughout the year with a seasonal mean of 88+/-13 nmol N h(-1). Oxygen to nitrogen ratios ranged between 6 and 10, suggesting that proteins were used as the primary metabolic substrate. Body wall protein synthesis rates decreased from 0.35%+/-0.03% d(-1) in summer to 0.23% d(-1) in winter, while RNA to protein ratios decreased from 33.10+/-1.0 microg RNA mg(-1) protein in summer to 27.88+/-1.3 microg RNA mg(-1) protein in winter, and RNA activity was very low, ranging between 0.11+/-0.01 mg protein mg(-1) RNA d(-1) in summer and 0.06+/-0.01 mg protein mg(-1) RNA d(-1) in winter. Heterocucumis steineni shows a larger seasonal decrease in oxygen consumption and ammonia excretion between February (summer) and July (winter) than N. concinna, while the proportional decrease in protein synthesis rates is similar in both species.     

Diel patterns of nitrogen excretion, plasma constituents, and behavior in the gulf toadfish (Opsanus beta) in laboratory versus outdoor mesocosm settings

Nitrogen excretion by the gulf toadfish (Opsanus beta) is of interest because of its high proportion of urea excretion compared with that of other teleosts. To better understand the factors influencing the timing of nitrogen excretion, the ratio of excreted urea∶ammonia, and the effector molecules regulating these processes, gulf toadfish were subjected to a series of experiments that moved them progressively from internal laboratory to outdoor mesocosm settings while assessing their behavior, nitrogen excretion patterns, levels of plasma hormones/effectors, and other parameters. In confined flux chambers in both laboratory and outdoor settings, toadfish nitrogen excretion was largely observed as urea pulses, with no apparent diel patterns to the pulses. Unrestrained toadfish in mesocosms exhibited distinctly nocturnal behavior, remaining exclusively in shelters during the day but taking several forays out into the mesocosm at night. In contrast to nitrogen excretion patterns in chambers, urea and ammonia were coexcreted in mesocosms and ratios for urea∶ammonia were very close to 1∶1 for both fed and fasted toadfish. The majority of measured excretion (and corresponding declines in plasma urea levels) occurred during two distinct periods of pulsing during daylight hours (0600-1000 and 1600-1800 hours). The declines in plasma urea associated with excretion were preceded by/coincided with declines in plasma cortisol. No day/night or hourly patterns in plasma serotonin (5-hydroxytryptamine [5-HT]) were observed, but there was a strong positive correlation among all samples between plasma urea and 5-HT. There was also a negative correlation between plasma cortisol and 5-HT. As expected for a nocturnally active species, plasma melatonin was significantly lower in daylight hours. A variety of enzyme activities (glutamine synthetase, glutaminase) and mRNA levels (glutamine synthetase, urea transporter, and Rhesus proteins) showed no significant variation over a diel cycle. Unlike prior laboratory studies, our results show that gulf toadfish in a natural setting have a distinctly diurnal pattern of nitrogen excretion and that ammonia and urea are coexcreted. The decline in plasma cortisol associated with urea pulses noted in prior laboratory studies was not as evident in the natural setting.     

Nitrogen and Carbohydrate Metabolism of Japanese Mint as Affected by Phosphorus Deficiency and Seasonal Variations

The paper presents effects of phosphorus deficiency and seasonal variations on nitrogen and carbohydrate metabolism of Japanese mint (Mentha arvensis L. var. piperascens, Holmes). Mint plants were grown in sand cultures under full nutrition and under phosphorus deficiency conditions during winter and summer. Various nitrogen and sugar fractions were determined in the component parts at specified periods of growth stages. Phosphorus deficiency disturbed the nitrogen metabolism at the stages for amide and amino acid formation, which resulted in an accumulation of carbohydrates. The content of total soluble and total nitrogen was higher and that of insoluble nitrogen was lower in summer as compared with winter plants. Of the soluble fractions, the ammonia, amide and nitrate nitrogen were higher and the ‘rest’ nitrogen lower in winter plants. Nitrate formed the highest bulk of the pool of soluble nitrogen in winter, whereas in summer ‘rest’ nitrogen was most abundant. The content of total sugar in winter plants far exceeded that of summer plants, which was wholly due to increase in sucrose content. Glucose was the predominant reducing sugar in both seasons. However, the summer plants were richer in glucose than those from the winter.