EFFECT OF AMMONIUM NITROGEN AND NITRATE NITROGEN, SEPARATELY AND IN COMBINATION, ON THE GROWTH OF THE HIGHBUSH BLUEBERRY

1967 ◽  
Vol 47 (5) ◽  
pp. 555-562 ◽  
Author(s):  
L. R. Townsend
Keyword(s):  
Nitrate Nitrogen ◽  
Ammonium Nitrogen ◽  
Sand Culture ◽  
Highbush Blueberry ◽  
Culture Study ◽  
Nutrient Levels ◽  
Leaves And Roots

A greenhouse sand-culture study with two sands revealed that growth was significantly better with ammonium nitrogen, or ammonium nitrogen plus nitrate nitrogen, than with nitrate nitrogen. Roots of plants receiving NO3-N were dark brown or black, whereas roots of those receiving NH4-N or NH4-N + NO3-N were light brown. Nutrient levels in leaves and roots were significantly affected by the form of applied N. Plants receiving NH4-N had significantly higher leaf levels of N, P and Fe and significantly lower levels of K, Ca, Mg, Mn and Al than did plants receiving NO3-N. Levels in plants receiving NH4-N + NO3-N were generally intermediate. Effluent pH from NH4-N or NH4-N + NO3-N plants decreased during growth, but pH of effluents from NO3-N plants increased.

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.

INFLUENCE OF FORM OF NITROGEN AND pH ON GROWTH AND NUTRIENT LEVELS IN THE LEAVES AND ROOTS OF THE LOWBUSH BLUEBERRY

1969 ◽  
Vol 49 (3) ◽  
pp. 333-338 ◽  
Author(s):  
L. R. Townsend
Keyword(s):  
Culture Study ◽  
Vaccinium Angustifolium ◽  
Water Culture ◽  
Nutrient Levels ◽  
Lowbush Blueberry ◽  
Independent Form ◽  
Effects Of Ph ◽  
Leaves And Roots

In a water culture study with lowbush blueberry (Vaccinium angustifolium Ait.), growth was significantly better at pH 4.5 than at pH 6.0 (22.9 g new growth per plant compared with 9.6 g) and with NH4-N than with NO3-N (21.9 g compared with 10.7 g). The absence of a significant pH × form of N interaction suggested that the effects of pH and form of N were independent. Form of N and pH also affected the levels of various nutrients in the leaves and roots.

scholarly journals Mineral Composition of Young Rabbiteye and Southern Highbush Blueberry Exposed to Salinity and Supplemental Calcium

1994 ◽  
Vol 119 (2) ◽  
pp. 229-236 ◽  
Author(s):  
Glenn C. Wright ◽  
Kim D. Patten ◽  
Malcolm C. Drew
Keyword(s):  
Calcium Supplementation ◽  
Dry Weight ◽  
Sand Culture ◽  
Nutrient Concentrations ◽  
Highbush Blueberry ◽  
Vaccinium Ashei ◽  
Supplemental Calcium ◽  
Total Plant ◽  
Leaves And Roots ◽  
Southern Highbush

`Tifblue' and `Brightwell' rabbiteye blueberry (Vaccinium ashei Reade) and `Sharpblue' southern highbush blueberry (primarily V. corymbosum) were treated with 0, 25, and 100 mm Na+ as Na2SO4 or NaCl, and 0, 1, 3, and 10 mm supplemental Ca2+ in sand culture in the greenhouse. For rabbiteye plants salinized with Na2SO4, leaf Na+ concentrations increased 54-fold and the percentage of total plant Na+ found in the leaves increased from 9% to 63% with increasing external Na+. Calcium supplementation reduced the Na+ concentrations in leaves by up to 20%. Leaf Ca2+ concentrations increased with Ca2+ supplementation, but accounted for a decreasing percentage of the total Ca2+ found in the plant, since root Ca2+ concentrations were much higher. Root Na+ concentrations increased with increasing Na+ treatments to a smaller extent than in the leaves and were also reduced by Ca2+ supplements. Potassium concentrations in leaves and roots decreased with increasing Na+ treatment levels, particularly in roots, where K+ concentration was about half at 100 mm Na+ (as Na2SO4.) Leaf Na+ concentrations were up to two times greater when Na was supplied as NaCl compared to Na2SO4. For plants salinized with NaCl, leaf Na+ levels increased to 1.1% and did not decrease when supplemental Ca2+ was applied. Leaf Cl- concentrations also increased greatly with NaCl, reaching >1.0% (dry weight basis.). Root Cl- concentrations also increased with increasing salinity and were not affected by Ca2+ supplements. Ca2+ supplementation led only to a greater Ca2+ concentration in leaves and roots, but this did not alter Na+ concentrations. Nutrient concentrations in `Sharpblue' leaves, stems, and roots were greater than those of the rabbiteye cultivars, but were influenced by salinity and Ca2+ in essentially the same way. Excess Na+, Cl-, or both, together with lowered K+, were likely the cause of extensive leaf necrosis and may be indicative of a lack of a mechanism to control Na+ influx into blueberry leaves.

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.

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.

Runoff characteristics of nutrients in the forest streams in Hyogo Prefecture, Japan

2001 ◽  
Vol 44 (7) ◽  
pp. 151-156 ◽  
Author(s):  
S. Umemoto ◽  
Y. Komai ◽  
T. Inoue
Keyword(s):  
Total Nitrogen ◽  
Total Phosphorus ◽  
Suspended Solids ◽  
Nitrate Nitrogen ◽  
Ammonium Nitrogen ◽  
Stream Flows ◽  
The Difference ◽  
Hyogo Prefecture ◽  
Forest Streams ◽  
Precipitation Events

Nutrients and other pollutant runoffs from streams in artificial forest areas in central Hyogo Prefecture in southwest Japan have been investigated to estimate pollutant loads since 1995. The orthophosphate and ammonium nitrogen contents were usually low and constant during the investigation. When the flowrates of the streams were normal, the concentrations of suspended solids, CODMn, TOC and total phosphorus were very low, and did not change much. However, when stream flows were increased by rainstorms or other precipitation, higher concentrations of these parameters occurred. Otherwise, the average concentrations of nitrate nitrogen and total nitrogen were 0.26 mg/l and 0.31 mg/l, respectively, and they were often increased by precipitation events. They changed at the same time because the ratio of nitrate nitrogen per total nitrogen was high, about 80%. The fluctuation of concentrations of total phosphorus was similar to SS concentrations, which suggested that phosphorus was discharged in the types of suspended solids from forest areas. The specific loads of the nutrients and some other pollutants did not differ among the three watersheds investigated. However, the difference among them between fine days and rainy days was fairly large. It was presumed that pollutant runoff from forest areas is strongly dependent on precipitation events.

scholarly journals Effects of Grazing Pattern on Ecosystem Respiration and Methane Flux in a Sown Pasture in Inner Mongolia, China

Atmosphere ◽  
2018 ◽  
Vol 10 (1) ◽  
pp. 5
Author(s):  
Baoling Mei ◽  
Hongyu Yue ◽  
Xunhua Zheng ◽  
William McDowell ◽  
Qingshan Zhao ◽  
...  
Keyword(s):  
Soil Moisture ◽  
Organic Carbon ◽  
Dissolved Organic Carbon ◽  
Soil Temperature ◽  
Inner Mongolia ◽  
Nitrate Nitrogen ◽  
Ecosystem Respiration ◽  
Ammonium Nitrogen ◽  
Agricultural Practice ◽  
Ch4 Flux

The establishment of sown pasture is an important agricultural practice in many landscapes. Although both native grassland and sown pasture play a key role in the global carbon cycle, due to lack of data and field experiments, our understanding of grassland CH4 fluxes and CO2 emissions remains limited, especially when it comes to sown pasture. We measured ecosystem respiration and CH4 fluxes in response to a variety of potential drivers (soil temperature, soil moisture, ammonium nitrogen, nitrate nitrogen and dissolved organic carbon) in CG (continuous grazing), RG (rotational grazing) and UG (ungrazed) plots in sown grassland for one year in Inner Mongolia. Fluxes of CH4 and ecosystem respiration were measured using static opaque chambers and gas chromatography. Grazing significantly reduced ecosystem respiration (p < 0.01), and grazing pattern significantly influenced respiration in CG and RG plots (p < 0.01). We find that the sown grassland is a net sink for atmospheric CH4. No influence of grazing pattern was observed on CH4 flux in CG, RG and UG (p > 0.05). Soil temperature is the most important factor influencing ecosystem respiration and CH4 flux in the sown grassland, with soil moisture playing a secondary role to soil temperature. Variation in levels of ammonium nitrogen, nitrate nitrogen and dissolved organic carbon had little influence on ecosystem respiration or CH4 flux (except in UG plots). The values obtained for ecosystem respiration of grasslands have a large uncertainty range, which may be due to spatial variability as well as differences in research methods. Mean CH4 fluxes measured only during the growing season were much higher than the annual mean CH4 fluxes.

scholarly journals The effect of pulverising aeration on changes in the oxygen and nitrogen concentrations in water of Lake Starzyc

2015 ◽  
Vol 25 (1) ◽  
pp. 31-36 ◽  
Author(s):  
Piotr Wesołowski ◽  
Adam Brysiewicz
Keyword(s):  
Dissolved Oxygen ◽  
Nitrate Nitrogen ◽  
Ecological Status ◽  
Ammonium Nitrogen ◽  
Abiotic Conditions ◽  
The Third ◽  
Long Period ◽  
Nitrogen Concentrations ◽  
Bottom Waters ◽  
Restoration Measures

Abstract Due to poor ecological status of Lake Starzyc, lake restoration measures were undertaken in 2003 to improve aerobic conditions of near-bottom waters and to decrease phosphorus concentrations. To do this, a wind-driven pulverising aerator was installed in the lake. The aim of this study was to analyse variability of oxygen and nitrogen concentrations in lake water near the aerator in the third year of its operation and later on in the three-year-long period of the years 2008–2010. It was found that concentrations of ammonium-nitrogen, nitrate-nitrogen and dissolved oxygen near the aerator did not differ from those in sites 4 and 5, which evidenced similar abiotic conditions in analysed waters. Higher concentrations of dissolved oxygen and lower concentrations of nitrate-nitrogen were found in the years 2008–2010 than in 2005.

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