Ammonium fixation and availability in some cereal producing soils in Queensland.

Soil Research ◽  
1972 ◽  
Vol 10 (2) ◽  
pp. 197 ◽  
Author(s):  
AS Black ◽  
SA Waring
Keyword(s):  
Nitrate Nitrogen ◽  
Sequential Sampling ◽  
Nitrogen Sources ◽  
Ammonium Nitrogen ◽  
Low Density ◽  
Air Drying ◽  
Ammonium Fixation ◽  
Intensive Cropping ◽  
Almost All ◽  
Pot Culture

Native fixed ammonium nitrogen and fixation of added ammonium nitrogen were studied in 24 Queensland cereal producing soils. The availabiiity of both forms of fixed ammonium nitrogen to wheat was investigated using a montmorillonitic soil under pot culture. Fixation and release of fertilizer ammonium nitrogen were followed in the soil by sequential sampling during crop growth. All soils contained native fixed ammonium nitrogen (6-107 p.p.m. nitrogen, mean 39 p.p.m. nitrogen). Fixation of added ammonium nitrogen was only significant in high clay montmorillonitic soils. Under moist conditions an average of 5% (200 p.p.m. nitrogen added) and 1% (4000 p.p.m. nitrogen added) was fixed. Fixation increased threeto ten-fold following air drying. Intensive cropping only released small but non-significant amounts of native fixed ammonium nitrogen. Of the 15% of added ammonium nitrogen which was fixed, only 50% was released by a single low density cropping causing less nitrogen uptake by wheat tops from ammonium compared with nitrate nitrogen sources. Intensive or successive cropping released almost all recently fixed ammonium nitrogen.

The growth of Luffa aegyptiaca in response to various nitrogen sources and concentrations

1985 ◽  
Vol 63 (12) ◽  
pp. 2283-2287
Author(s):  
Olubukanla T. Okusanya ◽  
Olusola O. Lakanmi
Keyword(s):  
Nitrate Nitrogen ◽  
Nitrogen Concentration ◽  
Nitrogen Sources ◽  
Ammonium Nitrogen ◽  
Lateritic Soil ◽  
Sand Culture ◽  
Growth Media ◽  
Growth Responses ◽  
Poor Growth ◽  
Luffa Aegyptiaca

The growth responses of Luffa aegyptiaca to various nitrogen sources and concentrations were investigated. In sand culture at high concentrations of nitrogen, the species showed equally favourable responses to nitrate nitrogen (KNO3 or Ca(NO3)2), ammonium nitrogen ((NH4)2SO4), and the combination of nitrate and ammonium nitrogen (NH4NO3). There was poor growth in response to NaNO3, CO(NH2)2, and a solution lacking nitrogen. In lateritic soil, the species responded better to ammonium nitrogen and the combination of nitrate and ammonium nitrogen than to nitrate nitrogen. Growth was generally poorer in lateritic soil than in sand. Neither the nitrogen sources nor their concentrations had any significant effect on root weight or the leaf weight ratio. There was a significant decrease in growth as nitrogen concentration decreased in KNO3 and Ca(NO3)2 treatments but it was only at the low concentrations of (NH4)2SO4 and NH4NO3 that growth was significantly reduced. The shoot: root mass ratio decreased as nitrogen concentration decreased. The nature of the growth media and the ecological habit of the species are used to partly explain its responses to different nitrogen sources and concentrations. The possible application of these results to increasing the production of L. aegyptiaca is also discussed.

Structure and chemical composition of yeast chlamydospores of Aureobasidium pullulans

1973 ◽  
Vol 19 (2) ◽  
pp. 163-168 ◽  
Author(s):  
Robert G. Brown ◽  
Louis A. Hanic ◽  
May Hsiao
Keyword(s):  
Cell Walls ◽  
Nitrate Nitrogen ◽  
Nitrogen Nutrition ◽  
Nitrogen Sources ◽  
Dry Weight ◽  
Cell Types ◽  
Ammonium Nitrogen ◽  
Wall Layer ◽  
Outer Cell ◽  
Yeastlike Cells

Cellular form in Aureobasidium pullulons can be partially controlled by nitrogen nutrition. Ammonium nitrogen supports a mixture of filamentous and yeastlike growth, whereas only a few filaments develop on nitrate nitrogen. On nitrate 97% of the cell material consists of a mixture of yeastlike cells and chlamydospores. Chlamydospores are produced on both nitrogen sources; however, with ammonium nitrogen chlamydospores occur in an intercalar position, whereas nitrate nitrogen supports development of chlamydospores as separate structures containing one, two, or occasionally three cells. This mode of production allows separation of yeast chlamydospores from other cell types and subsequent isolation of their cell walls. Yeast chlamydospores and filaments have an electron dense, melanin-rich, granular, outer cell-wall layer which yeastlike cells lack. This granular material is also found in cross walls of filaments and chlamydospores. Glucose is the main component of chlamydospore walls and accounts for 36% of the dry weight. Yeastlike cell walls contain only 13% glucose, but more mannose, galactose, and bound lipid. Most of the glucan portion of chlamydospore walls is insoluble in dilute alkali; methylation analysis indicates that this material contains linear chains of (1 → 3) and (1 → 6) linked glucose. About one residue in five forms a branch point having both (1 → 3) and (1 → 6) linkages.

Nitrogen requirements of the genus Linderina

1970 ◽  
Vol 48 (4) ◽  
pp. 695-698 ◽  
Author(s):  
R. C. Stephen ◽  
Christina Chan
Keyword(s):  
Glutamic Acid ◽  
Organic Nitrogen ◽  
Liquid Culture ◽  
Growth Response ◽  
Nitrate Nitrogen ◽  
Nitrogen Sources ◽  
Ammonium Nitrogen ◽  
Good Growth ◽  
Poor Growth ◽  
Better Than

The influence of different nitrogen sources on the growth of Linderina was examined in liquid culture. Both species of Linderina were unable to assimilate nitrate nitrogen and nitrite seemed to be toxic. Ammonium nitrogen was used but the growth response was considerably lower than that with some organic nitrogen materials. Inclusion in the growth medium of succinic acid as a carbon source failed to improve the assimilation of ammonium.Amino nitrogen as aspartic acid and asparagine gave good growth though not as good as with L- or DL-glutamic acid. The response to DL-glutamic acid was markedly better than to the L-isomer whereas the D-isomer gave relatively poor growth.

scholarly journals Observations on the mobilization of peat nitrogen in incubation experiments

1959 ◽  
Vol 31 (1) ◽  
pp. 268-281
Author(s):  
Jaakko Kivekäs ◽  
Erkki Kivinen
Keyword(s):  
Nitrate Nitrogen ◽  
Ammonium Nitrogen ◽  
The Other ◽  
Incubation Experiments ◽  
Different Types ◽  
Working Out ◽  
Original Amount

60 peat samples from northern Finland representing different types of peat were incubated in a laboratory at a temperature of 17—18° C. The ammonium nitrogen, the nitrate nitrogen and the pH in the samples were determined after one month of incubation as well as after three months of incubation. The results were compared to results from determinations made before incubation. An attempt was made to elucidate the factors that influence the mobilization of nitrogen. On the basis of the above results it is evident that the differences between the various peat types as mobilizers of nitrogen are under these circumstances not very distinct, nor do these differences seem to be dependent on the types of peat. The following facts can, however, be established: In the amounts of ammonium nitrogen an increase takes place in most groups of samples during the first month. This increase is fairly big in the Sphagnum-dominated peats. The increase in ammonium nitrogen continues in the unlimed samples in most peat groups during all three months of incubation. After three months of incubation the amount of ammonium nitrogen in the limed samples is smaller than in the unlimed samples, although it is usually bigger than in the original samples. After the first month of incubation the amounts of nitrate nitrogen in all types of peat have decreased compared to the amounts in the original samples. In the limed samples the decrease is not as great as in the unlimed ones. After three months of incubation the amount of nitrate nitrogen has considerably increased as compared to the amount after one month of incubation. In the limed samples it might to some extent exceed the original amount of nitrate nitrogen, however, this is seldom the case in the unlimed samples. If the results are calculated on the basis of weight unit, it can be stated that the ability to mobilize nitrogen is greater in the Sphagnum peats than in the other peat groups. Working out the results in kg per ha it will be noted that somewhat more nitrogen is mobilized in the Carex-dominated than in the Sphagnum-dominated peats. The results obtained by experiments in the laboratory are not directly applicable to conditions in the field.

RELATIONSHIP OF YIELD AND TOTAL NITROGEN UPTAKE OF BRUSSELS SPROUTS PLANTS GROWN IN THE GREENHOUSE TO AVAILABLE SOIL NITROGEN

1969 ◽  
Vol 49 (3) ◽  
pp. 313-318 ◽  
Author(s):  
D. C. Munro
Keyword(s):  
Total Nitrogen ◽  
Soil Nitrogen ◽  
Nitrogen Uptake ◽  
Nitrate Nitrogen ◽  
Soil Samples ◽  
Moist Soil ◽  
Available Nitrogen ◽  
Air Drying ◽  
Brussels Sprouts ◽  
Relationship Of

Initial nitrate-nitrogen content of the soil gave a correlation coefficient (r) of 0.93 with yields and with total nitrogen uptake of Brussels sprouts plants (Brassica oleracea var. gemmifera DC., Jade Cross). Soil nitrogen extracted with 0.01 M NaHCO3 gave r values of 0.76 with yields and 0.75 with nitrogen uptake. Nitrate incubation results from leached, moist soil samples gave r values of 0.59 with yields and 0.56 with nitrogen uptake. However, air-drying of soil samples prior to leaching and incubation resulted in r values of only 0.15 and 0.11 with yields and nitrogen uptake, respectively. Available nitrogen determined by incubation without previous leaching of the soil samples gave high r values because of the influence of the initial nitrate nitrogen in the soil.

EFFECTS OF pH AND NITROGEN SOURCES ON GROWTH OF MICROCYSTIS AERUGINOSA KÜTZ.

1962 ◽  
Vol 8 (1) ◽  
pp. 1-11 ◽  
Author(s):  
Jack McLachlan ◽  
P. R. Gorham
Keyword(s):  
Growth Inhibition ◽  
Microcystis Aeruginosa ◽  
Nitrate Nitrogen ◽  
Nitrogen Sources ◽  
Cesium Chloride ◽  
Potassium Nitrate ◽  
Degree Of Ionization ◽  
Ph Values ◽  
Effects Of Ph ◽  
Ph Range

Microcystis aeruginosa Kütz. (strain NRC-1) grew equally well throughout the pH range 6.5 to 10 when provided with suitable media. Toxicity of tris(hydroxymethyl)aminomethane (TRIS) towards the alga was found to decrease as the pH decreased and could be correlated with the degree of ionization of the TRIS molecule. Other organic buffers examined were either toxic at all concentrations and pH values tested or promoted lysis. When TRIS was used as a buffer, higher concentrations of cesium chloride and potassium nitrate were tolerated without growth inhibition at pH 6.5 than at 7.5. In the presence of TRIS, Microcystis grew equally well with nitrate, ammonium, or urea as nitrogen sources. Eight out of 20 amino compounds examined served as nitrogen sources in TRIS-buffered medium, but growth was poorer than with nitrate nitrogen.

EFFECT OF AMMONIUM NITROGEN AND AMINO ACIDS ON PERITHECIAL FORMATION OF VENTURIA INAEQUALIS

1971 ◽  
Vol 51 (1) ◽  
pp. 29-33 ◽  
Author(s):  
R. G. ROSS ◽  
FRANCES D. J. BREMNER
Keyword(s):  
Amino Acids ◽  
Ammonium Carbonate ◽  
Venturia Inaequalis ◽  
Amino Nitrogen ◽  
Basal Medium ◽  
Nitrogen Sources ◽  
Ammonium Nitrogen ◽  
Racemic Mixture ◽  
Appreciable Change ◽  
The Media

Perithecia of Venturia inaequalis did not form in a basal medium to which was added ammonium sulfate, chloride, phosphate or tartrate as the sole sources of nitrogen, when the pH of the medium was allowed to fall to inhibitory levels. Perithecia formed with these ammonium salts as nitrogen sources when calcium carbonate was added to control the pH. With ammonium carbonate and oxalate there was no appreciable change in pH, and perithecia formed with these salts as nitrogen sources. Perithecia did not form in media with leucine as a nitrogen source. Formation of perithecia with other amino acids depended on the concentration of amino-nitrogen in the media. A substance toxic to perithecial formation may form in cultures containing leucine; if so, it is produced in different amounts by the two isomers and the racemic mixture of this amino acid.

The effects of ammonium and nitrate nitrogen on the growth of perennial rye grass

1936 ◽  
Vol 26 (2) ◽  
pp. 249-257 ◽  
Author(s):  
A. H. Lewis
Keyword(s):  
Nitrogen Content ◽  
Nitrate Nitrogen ◽  
Ammonium Nitrogen ◽  
Early Stages ◽  
Rye Grass

The results show clearly a more rapid and greater uptake of ammonium than of nitrate nitrogen by perennial rye grass grown in a sand-bentonite medium of pH 7·61. The extent to which the extra uptake with added ammonia was reflected in increased yields was dependent upon the age of the grass.Except in the very early stages the percentage nitrogen content of the herbage was higher where nitrate nitrogen was applied than where ammonium nitrogen was applied. This indicates that any nitrate absorbed by the plant was less, efficient in increasing yields than was ammonium nitrogen.The percentage P205 content of the grass was higher where the nitrogen was applied in the ammoniacal form than where it was applied as nitrate, and it appears that this greater P205 uptake with ammonium nitrogen resulted in increased growth.

Influence of Photochemical Reactions on the Content and Transformation of Mineral Nitrogen in Sod-Podzol Soil

2018 ◽  
Vol 781 ◽  
pp. 195-199
Author(s):  
Sergey Novoselov
Keyword(s):  
Nitrate Nitrogen ◽  
Ammonium Nitrogen ◽  
Photochemical Reactions ◽  
Mineral Nitrogen ◽  
Light Energy ◽  
Second Stage ◽  
Humus Substances ◽  
Microbiological Oxidation ◽  
Two Stages

The article discusses the photochemical effects of sunlight on the soil. Under the influence of light energy the amount of mineral and easy hydrolysable nitrogen, as well as labile humus substances increased in the soil. The photochemical destruction of humus substances was accompanied by an increase in their mobility and loss of colour. The article shows that the process of mineral nitrogen formation in the soil during the photochemical destruction of humus substances has two stages. The first stage includes photochemical reactions with the formation of ammonium nitrogen. The second stage is the microbiological oxidation of ammonium nitrogen to the nitrate nitrogen.

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