scholarly journals Nitrogen Uptake Efficiency and Total Soil Nitrogen Accumulation in Long-Term Beef Manure and Inorganic Fertilizer Application

2019 ◽  
Vol 2019 ◽  
pp. 1-6 ◽  
Author(s):  
Peter Omara ◽  
Lawrence Aula ◽  
William R. Raun
Keyword(s):  
Grain Yield ◽  
Soil Nitrogen ◽  
N Uptake ◽  
Inorganic N ◽  
Uptake Efficiency ◽  
N Sources ◽  
Total Soil ◽  
Total Soil Nitrogen ◽  
Amended Soil

Livestock manure is a common soil amendment for crop-livestock production systems. However, the efficiency of crop nitrogen (N) uptake from the manure-amended soil may not equate with that from inorganic N sources. The objective of this paper was to determine the efficiency of N uptake, grain yield, and total soil nitrogen (TSN) accumulation in beef manure-amended soil compared to the inorganic N fertilizer-amended soil. Data (1990–2015) from a long-term continuous winter wheat (Triticum aestivum L.) fertility experiment at Stillwater in Oklahoma, USA, were used in this report. Three of the six “Magruder Plot” treatments used in this study were manure, NPK plus lime (NPKL), and a check (no nutrients applied). Pre-plant N, P, and K were applied annually at 67, 14.6, and 27.8 kg·ha−1, respectively, while beef manure was applied every 4 years at 269 kg N·ha−1. The results indicated that grain N uptake in the manure treatment (48.1 kg·ha−1) was significantly (p<0.05) lower than that in the NPKL treatment (60.2 kg·ha−1). This represents 20.1% efficiency of inorganic N uptake than the manure N uptake. The average grain yield (1990–2015) from the manure and NPKL treatments was 2265.7 and 2510.5 kg·ha−1, respectively, and was not significantly different. There was a trend of TSN increase over the study period for both manure and NPKL treatments. The average TSN from manure and NPKL treatments was 0.92 and 0.91 g·kg−1 soil, respectively, and was not significantly different. While no significant difference between manure and NPKL grain yield was observed, there was a significantly lower uptake efficiency of manure N compared to inorganic N. Furthermore, the low uptake efficiency of the manure N could suggest a potential for environmental pollution. Appropriate timing and application rate of manure N sources could optimize crop use efficiency and limit potential threat to the environment.

The effect of cropping after medic and non-medic pastures on total soil nitrogen, and on the grain yield and nitrogen content of wheat

1980 ◽  
Vol 20 (103) ◽  
pp. 220 ◽  
Author(s):  
CL Tuohey ◽  
AD Robson
Keyword(s):  
Seasonal Variation ◽  
Grain Yield ◽  
Nitrogen Content ◽  
Soil Nitrogen ◽  
Yield Response ◽  
Strongly Correlated ◽  
Nitrogen Response ◽  
Total Soil ◽  
Grain Nitrogen ◽  
Total Soil Nitrogen

The effect of medic and non-medic pastures on grain yield and nitrogen content of wheat was studied over 15 seasons on a friable grey clay in the Wimmera. The effects of length and type of pasture ley on grain yield and nitrogen content were closely related to the effects of these treatments on total soil nitrogen. Grain yield was not increased in any season by increasing total soil nitrogen beyond 0.1 10%. The grain yield response to increased total soil nitrogen varied markedly with seasons and most of the variation could be accounted for by variation in November rainfall; grain yield response was greater in years of higher November rainfall. Grain nitrogen content increased with increasing total soil nitrogen over the range studied (0.078% to 0.1 28%). Seasonal variation in grain nitrogen response to total soil nitrogen was mainly associated with variation in September and November rainfall. Higher September rainfall increased the response and higher November rainfall decreased it. The decline in total soil nitrogen that occurred with cropping was strongly correlated with the level of total soil nitrogen before cropping.

Impact of lupins, grazed or ungrazed subterranean clover,stubble retention, and lime on soil nitrogen supplyand wheat nitrogen uptake, grain yields, and grain protein

1998 ◽  
Vol 49 (3) ◽  
pp. 487 ◽  
Author(s):  
W. J. McGhie ◽  
D. P. Heenan ◽  
D. Collins
Keyword(s):  
Grain Yield ◽  
Soil Nitrogen ◽  
N Uptake ◽  
Subterranean Clover ◽  
Growing Season ◽  
Grain Protein ◽  
Soil N ◽  
Grain Yields ◽  
Total Soil ◽  
Total Soil N

Soil nitrogen (N), N uptake, and wheat production in relation to rotation with wheat, lupin,or subterranean clover, mulched or grazed, were examined on a red earth at Wagga Wagga, New South Wales. Data over 4 years (1992{95) are presented from a long-term trial commenced in 1979. The effects of the various rotations on wheat productivity changed with seasonal rainfall duringthe wheat and the previous legume growing year. Generally, low rainfall (1991 and 1994) during thelegume growing season resulted in lower N uptake, grain protein, and grain yield by wheat grown ina following season. The addition of N fertiliser (100 kg N/ha) to continuous wheat increased soil N supply, N uptake, grain yield, and grain protein. Yields from continuously cropped wheat fertilisedwith N were usually lower than those after a lupin growing season, although total soil N levels weresimilar. Subterranean clover produced higher total soil N and grain protein than lupin but yields werenormally less. Lodging and take-all diseases were higher after a growing season with subterraneanclover than after lupins and most likely reduced grain yields. Grazing, as opposed to mowing andmulching subterranean clover, increased soil total N, grain protein, and usually soil mineral N, butnot grain yield. The addition of lime at 1·5 t/ha raised the soil pH(CaCl2) (0-10 cm) of the mostacidified treatment, continuously cropped wheat fertilised with N, from 4·04 to a mean of 4·7, andincreased yields and N uptake in 1993 and 1995.

A Long-Term Rotational and Manurial Trial in Uganda

1976 ◽  
Vol 12 (3) ◽  
pp. 305-317 ◽  
Author(s):  
A. R. McWalter ◽  
R. H. Wimble
Keyword(s):  
Soil Nitrogen ◽  
Negative Curvature ◽  
Finger Millet ◽  
Critical Level ◽  
Farmyard Manure ◽  
Partial Explanation ◽  
Total Soil ◽  
Yield Trends ◽  
Total Soil Nitrogen

Mean yields and average trends with time are given for cotton, finger millet and groundnuts grown in a rotational experiment during the period 1936–64. The experiment, which ran for five cycles, involved a five-year rotation with three different resting periods, five types of resting cover, and farmyard manure at three levels. Yield trends differed from crop to crop, and a critical level of total soil nitrogen is suggested in partial explanation. Responses to farmyard manure in most crops increased over die years, with increasingly marked negative curvature in a pattern that showed most strongly in cotton crops immediately following the application of manure.

scholarly journals Influence of No-Tillage on Soil Organic Carbon, Total Soil Nitrogen, and Winter Wheat (Triticum aestivum L.) Grain Yield

2019 ◽  
Vol 2019 ◽  
pp. 1-9
Author(s):  
Peter Omara ◽  
Lawrence Aula ◽  
Elizabeth M. Eickhoff ◽  
Jagmandeep S. Dhillon ◽  
Tyler Lynch ◽  
...  
Keyword(s):  
Triticum Aestivum ◽  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Grain Yield ◽  
Soil Nitrogen ◽  
No Tillage ◽  
Wheat Grain ◽  
N Rates ◽  
Total Soil Nitrogen

No-tillage (NT) can improve soil properties and crop yield. However, there are contrasting reports on its benefits compared to conventional tillage (CT). Dataset (2003–2018) from long-term continuous winter wheat (Triticum aestivum L.) experiments 222 (E222) at Stillwater and 502 (E502) at Lahoma in Oklahoma, USA, established in 1969 and 1970, respectively, was used. Both experiments were managed under CT until 2010 and changed to NT in 2011. In each tillage system, treatments included nitrogen (N) rates at E222 (0, 45, 90, and 135 kg·N·ha−1) and E502 (0, 22.5, 45, 67, 90, and 112 kg·N·ha−1). The objective was to determine the change in wheat grain yield, soil organic carbon (SOC), and total soil nitrogen (TSN) associated with the change to NT. Grain yield was recorded, and postharvest soil samples taken from 0–15 cm were analyzed for TSN and SOC. Average TSN and SOC under NT were significantly above those under CT at both locations while grain yield differences were inconsistent. Under both tillage systems, grain yield, TSN, and SOC increased with N rates. At E222, grain yield, TSN, and SOC under NT were 23%, 17%, and 29%, respectively, more than recorded under CT. At E502, grain yield was lower under NT than CT by 14% while TSN and SOC were higher by 11% and 13%, respectively. Averaged over experimental locations, wheat grain yield, TSN, and SOC were 5%, 14%, and 21%, respectively, higher under NT compared to CT. Therefore, NT positively influenced grain yield, TSN, and SOC and is likely a sustainable long-term strategy for improving soil quality and crop productivity in a continuous monocropping system.

Effect of Prescribed Burning of Forest Litter on Total Soil Nitrogen

1962 ◽  
Vol 26 (2) ◽  
pp. 200-202 ◽  
Author(s):  
J. O. Klemmedson ◽  
A. M. Schultz ◽  
H. Jenny ◽  
H. H. Biswell
Keyword(s):  
Soil Nitrogen ◽  
Prescribed Burning ◽  
Forest Litter ◽  
Total Soil ◽  
Total Soil Nitrogen

The effects of some grazed tropical grass-legume mixtures and nitrogen fertilized grass on total soil nitrogen, organic carbon, and subsequent yields of Sorghum vulgaris

1967 ◽  
Vol 7 (24) ◽  
pp. 66 ◽  
Author(s):  
RJ Jones
Keyword(s):  
Organic Carbon ◽  
Soil Nitrogen ◽  
Crop Yields ◽  
Low Fertility ◽  
Apparent Lack ◽  
Carbon And Nitrogen ◽  
Total Soil ◽  
Significant Difference ◽  
Nitrogen Treatments ◽  
Total Soil Nitrogen

Mixtures of some tropical legumes and Paspalum plicatulum (Michx) cv. Hartley, and stands of P. plicatulum were fertilized with urea at 100 and 200 lb nitrogen an acre a year, and were intermittently grazed by cattle over a period of four years. Soil analyses for organic carbon and for total soil nitrogen in the fourth year of the pasture phase revealed large treatment effects in three of the five replicates. These three replicates which were on a podsolic soil were lower in fertility than the remaining two on a latosolic soil. Soil nitrogen at the 0-3 inch depth in the high nitrogen treatment, and in two Phaseolus atropurpureus D.C. treatments was significantly higher than the control (P<0.05). Organic carbon at the 0-3 inch depth was significantly higher than the control (P<0.05) in the nitrogen treatments and in one of the P. atropurpureus treatments. For both soil nitrogen and organic carbon the Lotononis bainesii Bak. treatment did not differ from the control. There was no significant difference between treatments for soil nitrogen or organic carbon at the 3-6 inch depth though trends were similar to those at 0-3 inches. Organic carbon and nitrogen were closely correlated for all treatments at both depths, and there were no significant differences in the C : N ratio in any treatment. Yields of sorghum grown as a test crop after the pastures were significantly correlated with soil nitrogen values in the three low fertility replicates. A high correlation (r = +0.976) also existed between yields of nitrogen obtained in the pasture phase and test crop yields of nitrogen for all treatments except L. bainesii. Reasons for the apparent lack of improvement in soil nitrogen and carbon on the higher fertility replicates and for the poor test crop yields following L. bainesii are discussed.

scholarly journals Spatial variability of total soil nitrogen and sulphur content at two conventionally managed fields

2008 ◽  
Vol 54 (No. 10) ◽  
pp. 413-419 ◽  
Author(s):  
V. Vaněk ◽  
J. Balík ◽  
J. Šilha ◽  
J. Černý
Keyword(s):  
Spatial Variability ◽  
Crop Yield ◽  
Soil Nitrogen ◽  
Coefficient Of Variation ◽  
Sulphur Content ◽  
N Content ◽  
Total N ◽  
Total Soil ◽  
Positive Correlations ◽  
Total Soil Nitrogen

Spatial variability of total soil nitrogen and sulphur content has been observed in two plots (I – 54 ha and II – 32 ha). Soil samples were taken from the topsoil in a regular grid, which was localised by GPS (individual sampling points were 80 m apart); subsequently total soil N and S contents were analysed. The average N content in plot I was 0.16%; in plot II it was 0.12%. The content of S in plots I and II was 0.09% and 0.08%, respectively. Spatial variability of total N differed in separate parts of the plots. A higher variability was recorded in plot I, where the coefficient of variation (<I>CV</I>) was 15.7%, whereas in plot II it was only 11.1%. However, sulphur showed only little variability, and thus its coefficient of variation was low (2.5 a 2.3% in plots I and II, respectively). A positive and mostly conclusive relationship has been observed between the N content of soil and the crop yield. This effect was more significant in plot II. The S content in soil showed no correlation with yield. Furthermore, positive correlations were observed between field altitude, soil moisture and crop yield in both plots.

Herbage production and the accumulation of soil nitrogen under irrigated pastures on the Riverine Plain

1974 ◽  
Vol 14 (66) ◽  
pp. 49 ◽  
Author(s):  
CR Kleinig ◽  
JC Noble ◽  
AJ Rixon
Keyword(s):  
Perennial Ryegrass ◽  
Soil Nitrogen ◽  
White Clover ◽  
Accumulation Rate ◽  
Total Yield ◽  
Subterranean Clover ◽  
Nitrogen Accumulation ◽  
Total Soil ◽  
Total Soil Nitrogen ◽  
Applied Nitrogen

Herbage yield, herbage nitrogen, and soil nitrogen accumulation were followed over a five-year period (1958-63) under irrigated annual and perennial pastures established initially with different clovergrass proportions. Species sown in the annual pasture treatments were subterranean clover (Trifolium subterraneum cv. Tallarook) and annual ryegrass (Lolium rigidum cv. Wimmera). Those used in the perennial mixtures were white clover (T. repens cv. Irrigation) and perennial ryegrass (L. perenne cv. Victorian). In the treatments sown to annual or perennial ryegrass only, nitrogenous fertilizer as urea was applied annually at four rates. Total soil nitrogen (mat + 0-91 cm of soil) after five years did not differ significantly for annual pasture and bare ground. In contrast, total soil nitrogen under all perennial pasture treatments, particularly those with a white clover component, was significantly greater than for bare soil (5365 cf. 4181 kg ha-1). Where white clover was sown, nitrogen accumulated at the rate of 258 kg ha-1 per annum compared with 101 kg ha-1 per annum under subterranean clover, the latter barely matching the accumulation rate under perennial ryegrass sown alone without applied nitrogen (105 kg N ha-1 p.a.). Nitrogen accumulation (soil plus mat) was related to both legume and non-legume nitrogen. Perennial pasture, particularly if white clover was present, generally outyielded annual pasture. The total yield of white clover over five years was 29,970 kg ha-1 compared with 11,614 kg ha-1 for subterranean clover. Annual and perennial ryegrasses showed similar yield responses to applied nitrogen. Irrespective of the rate of urea application, nitrogen recovery was low (21-23 per cent).

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