The leaching of nitrogen and its uptake by wheat in a soil from southern New South Wales

1965 ◽  
Vol 5 (18) ◽  
pp. 323 ◽  
Author(s):  
RR Storrier
Keyword(s):  
Nitrogen Concentration ◽  
Ammonia Nitrogen ◽  
Mineral Nitrogen ◽  
Low Fertility ◽  
Wheat Crop ◽  
Wagga Wagga ◽  
South Wales ◽  
Nitrogen Deficiencies ◽  
High Concentrations ◽  
Autumn And Winter

The changes in nitrogen concentration in the profile of a red brown earth soil, containing the equivalent of 160 lb mineral nitrogen per acre 18 inches at sowing, and to which ammonium sulphate at 0, 50, 100, and 150 lb nitrogen an acre had been added in early July, were measured for two seasons. A slow rate of nitrification resulted in the presence of high concentrations of residual ammonia-nitrogen 33 months later, equivalent to 55 and 30 per cent of the nitrogen added at the highest rate in fallowed and cropped treatments respectively. This residual ammonia-nitrogen persisted until the spring of the second season, a period of 13 months. Nitrogen was leached into the deeper subsoil, in the autumn and winter, when soil moisture was high and rain frequent. This leached nitrogen was retained in the surface 30 inches of the soil and subsequently taken up by the wheat crop. This uptake was responsible for differences in mineral nitrogen concentration between fallowed and cropped plots of approximately 82 and 96 per cent in the 0-18 inch and 0-30 inch depths respectively. It is suggested that leaching in low fertility soils, following heavy autumn and winter rains, could result in short term nitrogen deficiencies for crops in the Wagga Wagga region.

The availability of mineral nitrogen in a wheat soil from southern New South Wales

1962 ◽  
Vol 2 (6) ◽  
pp. 185 ◽  
Author(s):  
RR Storrier
Keyword(s):  
Nitrogen Uptake ◽  
New South ◽  
New South Wales ◽  
Nitrogen Deficiency ◽  
Ammonia Nitrogen ◽  
Mineral Nitrogen ◽  
Wheat Crop ◽  
Wagga Wagga ◽  
Emergence Period ◽  
South Wales

In a red-brown earth soil from Wagga Wagga the fluctuations in the level of mineral nitrogen (ammonia plus nitrate-nitrogen) and its availability to wheat under growing period rainfalls of 6 inches and 16 inches were studied. Ammonia-nitrogen did not exceed 8 lb nitrogen per acre 6 inches but showed statistically significant short term fluctuations. Mineral nitrogen decreased steadily from the 4-5 leaf stage of plant growth, reaching minimum values in the ear-emergence period when a temporary nitrogen deficiency occurred. Following rainfalls of about one inch or more, conditions favoured biological activity and nitrogen was mineralized, absorbed by the crop and/or leached down the profile. In one season a release of mineral nitrogen about two weeks before flowering contributed an estimated 20-30 per cent of the total nitrogen uptake of the crop. Nitrogen uptake by the wheat crop ceased after flowering and subsequent changes in mineral nitrogen level reflect the net result of mineralization and demineralization processes, and nitrogen uptake by weeds, particularly skeleton weed. Absorption of nitrogen from the profile depended upon seasonal conditions, with the surface 18 inches suppling the greater part of the nitrogen absorbed by the crop. This indicates the need to sample regularly to at least a depth of 18 inches, particularly during the period from 4-5 leaf to flowering, when studying the relation between mineral nitrogen and crop growth. The data suggest that the response of wheat, as measured by grain yield and protein content, to the higher levels of mineral nitrogen in the improved soils of southern New South Wales is determined by soil moisture levels, particularly in the post-flowering period.

Time of sowing and wheat production in southern NSW

1970 ◽  
Vol 10 (46) ◽  
pp. 604 ◽  
Author(s):  
GD Kohn ◽  
RR Storrier
Keyword(s):  
Soil Moisture ◽  
Grain Yield ◽  
Nitrogen Concentration ◽  
Mineral Nitrogen ◽  
Wagga Wagga ◽  
Grain Protein ◽  
Soil Mineral Nitrogen ◽  
Soil Organic Nitrogen ◽  
South Wales ◽  
Moisture Potential

Wheat (CV. Heron) sown on clover-improved soils at Wagga Wagga, New South Wales, over the period 1961 to 1965 showed a general reduction in yield and an increase in grain protein percentage with delay in sowing. Grain yield decreased by 3.7 per cent for each week's delay in sowing after the end of April and the rate of grain protein increase ranged from 0.09 to 0.56 per cent for each week's delay, depending on seasonal conditions. This grain protein increase was accompanied by a reduced kernel size which resulted in a decrease in grain protein yield of 12.5 lb an acre for each week's delay in sowing. The reduced grain yield with later sowings was associated with less efficient use of soil moisture the post-flowering period. Although the cumulative evapotranspiration of early sown crops was about two inches greater than that for late sown crops in mid-spring, all sowings reduced the soil moisture potential to -15 bars to a depth of four to five feet at maturity. However, the late sown crops matured more rapidly with a reduction in all yield components. Changes in soil mineral nitrogen concentration during the growing season indicated that there Was adequate nitrogen available for all sowings. In two years mineralization of soil organic nitrogen occurred under the crops and contributed significantly to the crops requirement. In a third year mineral nitrogen losses from the soil could not be accounted for by plant uptake.

Fertility investigations on the black earth wheatlands of the Darling Downs, Queensland. III. Mineral nitrogen in the soil and its relation to the wheat crop

1960 ◽  
Vol 11 (1) ◽  
pp. 27 ◽  
Author(s):  
SA Waring ◽  
LJH Teakle
Keyword(s):  
Grain Yield ◽  
Ammonia Nitrogen ◽  
Mean Value ◽  
Mineral Nitrogen ◽  
Wheat Crop ◽  
Nitrogen Accumulation ◽  
A Value ◽  
The Mean ◽  
The One ◽  
Growing Crop

The level of mineral nitrogen in the soil under fallow and crop was measured for the years 1951 to 1953. Relationships of mineral nitrogen at planting to yield and nitrogen content of wheat grain and straw were examined. Values for nitrate nitrogen at the end of the fallow period ranged most commonly from 10 to 20 µg/g in the surface 2 ft and from 0 to 10 µg/g at 2-4 ft. Approximately one-third of the sites showed an increase from the third to the fourth foot. One site showed extremely high values throughout the profile, particularly at 3-4 ft where a value of 127 µg/g was recorded. Values for ammonia nitrogen were most commonly in the range of 0-3 µg/g . Under the growing crop, mineral nitrogen declined for most depths in the period from planting up to September or October, after which there was little further change to harvest. Uptake of mineral nitrogen was normally greatest from the surface 2 ft of soil. Below 3 ft there were two groups of sites. One group showed moderate to high uptake and the second group low uptake. The low uptake in the latter group provides a reason for mineral nitrogen accumulation below 3 ft at some sites. Mineral nitrogen to 4 ft at planting averaged 126 lb/ac, excluding the one site with exceptionally high values. This was double the mean value of 63 lb/ac for nitrogen recovered in grain and straw, for crops planted in May-June. These figures, combined with trends in the soil under crop, suggest that most of the nitrogen used by the crop was derived from that in the soil at planting. Correlations between mineral nitrogen at planting and grain yield were mostly non-significant, suggesting that in general nitrogen was not an important factor limiting yield. Low grain yield and protein percentage were recorded at a number of sites which had been cultivated more than 50 years.

The long term effects of rotation, tillage and stubble management on soil mineral nitrogen supply to wheat

Soil Research ◽  
1992 ◽  
Vol 30 (6) ◽  
pp. 977 ◽  
Author(s):  
DP Heenan ◽  
KY Chan
Keyword(s):  
Soil Nitrogen ◽  
Subterranean Clover ◽  
Mineral Nitrogen ◽  
Wheat Crop ◽  
Wagga Wagga ◽  
Long Term Effects ◽  
Soil Mineral Nitrogen ◽  
Percent Recovery ◽  
Direct Drilling

Wheat was grown as a monoculture or in rotation with lupin or subterranean clover in a long-term rotation, stubble and tillage experiment established in 1979, on a red earth (Gn 2 . 12) at Wagga Wagga, N.S.W. The effect of rotation, tillage and stubble management on the supply of soil nitrogen, and amounts leached were studied by in situ sequential soil sampling during the wheat phase of the rotation in years 10 and 11. Of the rotations, grazed subterranean clover-wheat accumulated higher mineral nitrogen levels during the wheat phase than a lupin-wheat rotation, which in turn produced higher levels than wheat-wheat. The mean seasonal total of net soil nitrogen mineralized (0-15 cm) was 239 kg N ha-1 for subterranean clover-wheat, 165 kg N ha-1 for lupin-wheat and 99.5 kg N ha-1 for wheat-wheat. In a lupin-wheat rotation, retention of stubble increased the net amount of nitrogen mineralized in both seasons. Direct drilling also increased net mineralization in 1990 but the results were inconsistent in 1989. Losses from the surface 15 cm were closely related to the amounts mineralized, with the highest recorded in subterranean clover-wheat rotations. Percent recovery of soil mineralized nitrogen by the above-ground wheat crop following lupin ranged from 57% to 83%, with both direct drilling and stubble retention reducing recovery. While total plant uptake of nitrogen in a wheat-wheat rotation was low, percent recovery was high (77%), compared with that in a subterranean clover-wheat rotation (60%).

Mineral nitrogen fluctuations in soils under improved pasture in Southern New South Wales

1962 ◽  
Vol 13 (6) ◽  
pp. 1059 ◽  
Author(s):  
JR Simpson
Keyword(s):  
New South ◽  
New South Wales ◽  
Heavy Rain ◽  
Early Spring ◽  
Mineral Nitrogen ◽  
Nitrate Accumulation ◽  
South Wales ◽  
Native Pasture ◽  
Autumn And Winter ◽  
Improved Pasture

Soils under improved pasture on the Southern Tableland of New South Wales accumulated nitrate in substantial quantities during the summer and autumn. In this respect they behaved quite unlike the pasture soils which have been studied in most of the earlier literature, and they resembled cultivated fallow soils, which usually accumulate nitrate at the same time of the year. The nitrate was produced mainly in the top inch of soil; ammonium also accumulated under certain conditions. The precise sequence of climatic events, particularly the period of drying between consecutive wettings, was of primary importance in the nitrate accumulation. The nitrate produced during summer and early autumn disappeared from the topsoil after heavy rain in autumn and winter. The seasons could therefore be distinguished as a nitrogen-rich summer and autumn, a nitrogen-depleting winter, and a nitrogen-poor early spring, with an increasing supply of mineral nitrogen during late spring. No appreciable fluctuations in mineral nitrogen were found in soils resown directly from native pasture with less than 0.10% total nitrogen at 0-2 in.

Screening and Characterization of a Bacterium Capable of Simultaneous Heterotrophic Nitrification and Aerobic Denitrification at High Concentrations of Ammonia-Nitrogen

2014 ◽  
Vol 665 ◽  
pp. 487-490
Author(s):  
Te Wang ◽  
Zhao Xia Liu ◽  
Mei Juan Wu ◽  
Fu Hui Kang ◽  
Qing Chen ◽  
...  
Keyword(s):  
16S Rdna ◽  
Ammonia Nitrogen ◽  
Heterotrophic Nitrification ◽  
Denitrification Rate ◽  
Aerobic Denitrification ◽  
Optimal Conditions ◽  
Carbon And Nitrogen ◽  
Mass Ratios ◽  
High Concentrations ◽  
Denitrification Process

A bacterium capable of simultaneous heterotrophic nitrification and aerobic denitrification at high concentrations of ammonia-nitrogen was screened and identified and the denitrification property was investigated in this paper. The strain was isolated from aeration tank of wastewater disposed by activated sludge and analyzed and identified by 16S rDNA. The effects of different carbon sources and carbon and nitrogen mass ratios on denitrification rate were studied. The changes of various forms of ammonia-nitrogens during the simultaneous heterotrophic nitrification and aerobic denitrification process were characterized. A strain capable of simultaneous heterotrophic nitrification and aerobic denitrification at 600 mg/L nitrogen concentration has been isolated and screened. Comparison of its 16S rDNA sequence showed 100% similarity to Bacillus licheniformis strain Lr124/6. The strain was named as Bacillus sp. A22. The optimal conditions for degradation of ammonia-nitrogen by Bacillus sp. A22 were trisodium citrate as carbon source and carbon and nitrogen mass ratios of 10. The denitrification rate was 98.2% after 96 h of culture under the optimal conditions and there was hardly any intermediates accumulation in the denitrification process. It has practical applications that the denitrification can be performed efficiently at high concentrations of ammonia-nitrogen by method of simultaneous heterotrophic nitrification and aerobic denitrification by Bacillus sp. A22 in nitrogen purification treatment of wastewater with high concentrations of ammonia-nitrogen.

Digestibility, nitrogen retention and plasma metabolite concentrations in steers offered whole crop wheat silage-based rations

1997 ◽  
Vol 1997 ◽  
pp. 132-132
Author(s):  
A.P. Moloney ◽  
P. O'Kiely
Keyword(s):  
Protein Concentration ◽  
Nitrogen Concentration ◽  
Nitrogen Retention ◽  
Wheat Crop ◽  
Moisture Concentration ◽  
Protein Nitrogen ◽  
Urea Treatment ◽  
Plasma Metabolite ◽  
Carbohydrate Supplement

The yield of dry matter (DM) in a mature wheat crop can equal that obtained from three cuts of grass. Ensiled mature whole crop wheat is however characterised by a lower digestibility and lower crude protein concentration than good quality grass silage. Addition of urea at ensiling has been shown to increase the digestibility and the non-protein nitrogen concentration of whole crop wheat silage. The objectives of this study were to determine (i) the effect of urea-treatment on the in vivo digestibility of wheat of relatively high moisture concentration and (ii) the effects of the provision of a rapidly fermentable carbohydrate supplement on nitrogen metabolism in steers fed these silages.

scholarly journals Mycelial biomass cultivation of Lentinus crinitus

2020 ◽  
Vol 36 (6) ◽  
Author(s):  
Itaruã Machri Colla ◽  
Olavo Bilac Quaresma de Oliveira Filho ◽  
Janyeli Dorini Silva de Freitas ◽  
Míria Benetati Delgado Bertéli ◽  
Giani Andrea Linde ◽  
...  
Keyword(s):  
Soybean Meal ◽  
Nitrogen Concentration ◽  
Fungal Growth ◽  
Malt Extract ◽  
Biomass Growth ◽  
Mycelial Biomass ◽  
Protein Nitrogen ◽  
Temperature Growth ◽  
Nitrogen Concentrations ◽  
High Concentrations

Lentinus crinitus is a medicinal basidiomycete, little studied regarding the basic cultivation conditions, which is used in bioremediation and consumed by native Indians from the Brazilian Amazon. Also, it produces a fungal secondary metabolite panepoxydone that has been described as an essential regulator of the inflammatory and immune response. This study aimed to evaluate basic conditions of temperature, pH, and nitrogen concentration and source in the cultivation of L. crinitus mycelial biomass. In order to evaluate fungal growth temperature, 2% malt extract agar (MEA) medium, pH 5.5, was utilized from 19 to 40 °C. For pH, MEA had pH adjusted from 2 to 11 and cultivated at 28 °C. Urea or soybean meal was added to MEA to obtain final concentration from 0.5 and 16 g/L of nitrogen, pH of 5.5, cultivated at 28 °C. The best temperature growth varies from 31 to 34 ºC and the optimal one is 32.7º C, and the best pH ranges from 4.5 to 6.5 and the optimal one is 6.1. Protein or non-protein nitrogen concentration is inversely proportional to the mycelial biomass growth. Nitrogen concentrations of 2.0 g/L soybean meal and urea inhibit mycelial biomass growth in 11% and 12%, respectively, but high concentrations of 16.0 g/L nitrogen inhibit the growth in 46% and 95%, respectively. The fungus is robust and grows under extreme conditions of temperature and pH, but smaller adaptation with increasing nitrogen concentrations in the cultivation medium, mainly non-protein nitrogen.

Sign in / Sign up

Export Citation Format

Share Document