RESPONSE OF CORN TO NITROGEN IN PREPLANT AND SIDEDRESS APPLICATIONS OF LIQUID DAIRY CATTLE MANURE

1983 ◽  
Vol 63 (2) ◽  
pp. 377-386 ◽  
Author(s):  
E. G. BEAUCHAMP

Two field experiments were conducted, each over a 3-yr period, to compare the availability of N from liquid cattle manure (LCM) with that from urea and anhydrous ammonia to corn. Two times of application (preplant vs. sidedress) and two methods of application (surface vs. injection) of LCM were compared with respect to corn grain yield and soil NO3− concentration during two periods of the growing season. The availability of LCM N was approximately one-half that of fertilizer N. Injection of LCM either before planting or as a sidedressing between the corn plant rows resulted in LCM N being approximately 60% as available as fertilizer N. Application of LCM to the soil surface, as a side dressing resulted in LCM N being approximately one-third as available as anhydrous ammonia N. The data were discussed and interpreted on the basis that manure N is made up of two principal fractions, "organic" and ammoniacal N. The organic N fraction, consisting of all the N other than ammonia, becomes only partly available to the crop through mineralization whereas the ammoniacal N fraction is subject to volatilization if not incorporated into the soil immediately. Soil NO3− concentrations in the June-July period showed the surface preplant LCM N availability to be approximately one-half that of preplant applications of urea. Nitrate concentrations during the September-October period suggested that LCM showed no greater levels of NO3− than urea even at twice the rate of N application. Key words: Corn, nitrogen, preplant and sidedress applications, liquid dairy cattle manure

1996 ◽  
Vol 44 (3) ◽  
pp. 227-239
Author(s):  
H. Biemond ◽  
J. Vos ◽  
P.C. Struik

Four greenhouse and 2 field experiments (the latter on a sandy soil) were carried out with different amounts and dates of N application to analyse the dynamics of dry matter and N accumulation in spinach (cv. Trias). Frequent measurements were carried out on dry matter and N accumulation in leaf blades, petioles and stems. The total accumulation of dry matter and N differed largely among and within experiments. Increasing N application increased yield of dry matter and N accumulation, whereas splitting N applications had much smaller effects. However, the partitioning of dry matter and N proved insensitive to N treatments. Harvest indices for dry matter (about 0.67) or N (about 0.74) of crops at a marketable stage were fairly constant over treatments and experiments. Increasing or splitting the N application affected N accumulation more than dry matter production, resulting in large effects on N concentrations. The lack of variation in response to N for different N regimes facilitates the development of N application techniques aimed at high yield, high quality and reduced emissions. The organic N concentration of leaf blades and petioles decreased with leaf age, although in most experiments this decrease was smaller at higher leaf numbers. The nitrate-N concentration decreased with increasing leaf number at any sampling date; it was higher when N was abundant. High yields in autumn crops were associated with high nitrate concentrations but also with potentially high losses of N.


1982 ◽  
Vol 62 (3) ◽  
pp. 479-486 ◽  
Author(s):  
CAROLINE M. PRESTON

A study of plant uptake, incubation-extraction and acid hydrolysis was carried out on soil samples from a field study using 15N. The samples had varying proportions of residual fertilizer 15N (15Nex) as clay-fixed ammonium and organic N. Availability of 15Nex to plants was positively correlated with percent of 15Nex as clay-fixed ammonium, and negatively correlated with percent of 15Nex as organic N. A similar relationship was noted for recovery of 15Nex in acid hydrolysates. The relationship was reversed for recovery of 15Nex in aqueous extracts following incubation, although this may have been due to lack of removal of N by plant uptake or leaching, and limitation of microbial activity by lack of readily available carbon. This direct comparison of availability of residual fertilizer N as clay-fixed ammonium N and organic N demonstrates that fertilizer N, once incorporated into organic forms, is much less available to plants than fertilizer N in the form of clay-fixed ammonium.


Soil Research ◽  
1989 ◽  
Vol 27 (4) ◽  
pp. 685 ◽  
Author(s):  
PE Bacon ◽  
LG Lewin ◽  
JW McGarity ◽  
EH Hoult ◽  
D Alter

The fate of 15N-labelled fertilizer applied to rice (Oryza sativa L) was studied in microplots established within two field experiments comprising a range of stubble levels, stubble management techniques, N application rates and times. The first experiment investigated uptake of soil and fertilizer N in plots where application of 0 or 100 kg N ha-1 to the previous rice crop had produced 11.5 and 16.1 t ha-1 of stubble respectively. The stubble was then treated in one of four ways-burn (no till); burn then cultivated; incorporated in autumn or incorporated at sawing. Microplots within these large plots received 60 kg ha-1 of 5% 15N enriched urea at sowing, just prior to permanent flood (PF), or just after panicle initiation (PI) of the second crop. The second experiment was undertaken within a field in which half of the plots had stubble from the previous three rice crops burned, while the other plots had all stubble incorporated. In the fourth successive rice crop, the two stubble management systems were factorially combined with three N rates (0, 70 or 140 kg N ha-1) and three application times (PF, PI or a 50 : 50 split between PF and PI). Nitrogen uptake and retention in the soil were studied within 15N-labelled microplots established within each of these large plots. Only 4% of the 15N applied at sowing in the first experiment was recovered in the rice crop, while delaying N application to PF or PI increased this to an average of 20% and 44% respectively over the two experiments. The doubling of N application rate doubled fertilizer N uptake and also increased uptake of soil N at maturity by 12 kgN ha-1. Three years of stubble incorporation increased average uptake of fertilizer and soil N in the second experiment by 5 and 12 kg N ha-1 respectively. In both experiments, the soil was the major source of N, contributing 66-96% of total N uptake. On average, in the fourth crop, 20% of fertilizer N was in the grain, 12% in the straw and 3% in the roots, while 23% was located in the top 300 mm of soil. A further 3% was in the soil below 300 mm. The remaining 39% was lost, presumably by denitrification.


1986 ◽  
Vol 66 (4) ◽  
pp. 713-720 ◽  
Author(s):  
E. G. BEAUCHAMP

Three manures were compared with urea as sources of nitrogen for corn (Zea mays L.) on a different field site in each of 3 yr. The manures and their average [Formula: see text]–N:total N ratios were as follows: liquid poultry manure (LPM), 0.89; liquid dairy cattle manure (LCM), 0.53; and solid beef cattle manure (SBM), 0.09. The manures were applied at rates of 100, 200 and 300 kg total N ha−1. An additional LCM treatment of 600 kg total N ha−1 was also included. For comparison with the manures as N sources, urea was applied at rates of 50, 100 and 150 kg N ha−1. The yield response data were examined on the basis of a previously suggested model which predicted that all of the [Formula: see text]–N and part (e.g., 10–20%) of the organic N in manures are available for crop growth in the field. Regression analyses of paired yield data sets of urea and LCM or urea and LPM indicated that only 75–80% of the [Formula: see text]–N fraction applied in these manures was equivalent to urea-N. Thus, it was concluded that the model did not take into account net N immobilization and possibly N losses through denitrification following application. It was concluded also that N release from the organic N fraction of SBM differed substantially from that for the other manures. This conclusion was supported by greenhouse data which indicated that net N immobilization occurred for the first crop shortly after SBM was applied but this was followed by net N mineralization for a second crop as manure decomposition continued. Soil NO3− concentrations in mid-June generally increased with the urea, LPM and LCM sources of N at the higher rates of application in the field. Lower soil NO3− concentrations with SBM reflected the lower availability of N. Key words: Corn, manure N availability, Zea mays L.


1993 ◽  
Vol 41 (3) ◽  
pp. 179-203
Author(s):  
P.J.A.G. Deenen ◽  
E.A. Lantinga

The effects of fertilizer N application on herbage intake and animal performance under continuous grazing management with dairy cows, and on herbage accumulation under a weekly and an approximately 4-weekly cutting regime were studied in 1986-1988 in resown Lolium perenne cv. Wendy grassland on a silty loam soil in Oostelijk Flevoland, Netherlands. 250-700 kg N/ha was applied annually under grazing and from 0 to 700 kg N/ha was applied under cutting. At an assumed marginal profitability of 7.5 kVEM per kg N applied the optimum N application rate was on average 511 and 308 kg/ha per year for 4-weekly cutting and continuous grazing, respectively (1 kVEM = 6.9 MJ Net Energy for lactation). However, especially under grazing, there was a great variation in response to N between years which could be related to soil N availability, length of the growing season and sward quality. Throughout the experimental period the mean tiller density in the grazed swards was hardly affected by the level of N application. However, there were temporary differences in openness of the sward which increased with the level of N application, leading to a loss of productivity as a result of impeded N uptake. Herbage N was poorly converted into animal products. The average efficiency of use of ingested N at 250 kg N was 23%. Higher rates of fertilizer N decreased N use efficiency (19% at 700 kg N/ha per year) but markedly increased N excreted per ha.


Agriculture ◽  
2021 ◽  
Vol 11 (8) ◽  
pp. 752
Author(s):  
Aliasghar Montazar ◽  
Daniel Geisseler ◽  
Michael Cahn

Nitrogen (N) and irrigation water must be effectively used in mineral soils to produce carrots with high yield and minimal environmental impact. This study attempts to identify optimal N and irrigation management practices for low desert carrot production in California by investigating consumptive water use and N uptake and removal rates in fresh market and processing carrots. Field experiments were conducted at the University of California Desert Research and Extension Center and nine farmer fields during two growing seasons. The actual evapotranspiration (ETa) was measured using the residual energy balance method with a combination of surface renewal and eddy covariance equipment. Crop canopy coverage, actual soil nitrate-N from multiple depths as well as total N percentage, dry matter, and fresh biomass in roots and tops were measured over the growing seasons. The length of the crop season had a wide range amongst the experimental sites: from a 128-day period in a processing carrot field to as long as 193 days in a fresh market carrot field. The seasonal ETa varied between 305.8 mm at a silty loam furrow irrigated processing carrot field and 486.2 mm at a sandy clay loam sprinkler irrigated fresh market field. The total N accumulated at harvest ranged between 205.4 kg ha−1 (nearly 52% in roots) and 350.5 kg ha−1 (nearly 64% in roots). While the mean value of nitrogen removed by carrot roots varied from 1.24 to 1.73 kg N/Mg carrot roots, it appears that more N was applied than was removed by carrot roots at all sites. Within the range of N application rates examined at the experimental sites, there was no significant relationship between carrot fresh root yield and N application rate, although the results suggested a positive effect of N application on carrot yield. Sufficient soil N availability over the growing season and the lack of significant yield response to N application illuminated that optimal N rates are likely less than the total amounts of N applied at most sites.


2018 ◽  
Vol 61 (4) ◽  
pp. 1365-1377
Author(s):  
Lijun Guo ◽  
Jiusheng Li ◽  
Yanfeng Li ◽  
Di Xu

Abstract. Field experiments on maize ( L.) under surface drip irrigation were carried out during two consecutive growing seasons to examine the influence of water quality (groundwater and secondary sewage effluent) and nitrogen (N) application rate on growth and yield, N agronomic efficiency, and N availability of effluent. Pot experiments were conducted using the 15N isotope tracer method and the fertilizer equivalence (FE) approach to provide direct evidence of the effluent N availability derived from the field experiments. Four N application rates ranging from 0 to 180 kg ha-1 for field experiments and from 0 to 2.64 g pot-1 (0 to 210 kg ha-1 equivalent) for pot experiments were investigated with secondary sewage effluent (SW) and groundwater (GW). Results showed that either irrigation with sewage effluent or increasing N application rates from 0 to 120 kg ha-1 were conducive to increasing maize productivity. Nonetheless, SW irrigation reduced the agronomic efficiency of applied N compared to GW irrigation supplemented with fertilizers, suggesting greater potential N losses under SW irrigation. Effluent N that was absorbed by maize was negatively correlated to increasing N application rates. On average, the N contained in effluent was only 51% to 69% as available as an equivalent application rate of urea N in improving maize production. The organic N fraction of effluent (20%) and higher potential N losses from SW irrigation primarily explained the lower effluent N availability in comparison to fertilizer urea. Overall results recommended an economic and ecological N application rate of 107 kg ha-1 for maize under drip irrigation when applying SW, with an approximate 14% urea N reduction to attain a satisfactory yield in comparison to GW irrigation. Keywords: Agronomic efficiency, Fertilizer equivalence approach, Isotope tracer method, Secondary treated wastewater.


1998 ◽  
Vol 78 (4) ◽  
pp. 597-605 ◽  
Author(s):  
Thi Sen Tran ◽  
Marcel Giroux

From an environmental standpoint, it is important to follow the fate of applied fertilizer N in soil–plant system. In this study, field experiments were conducted at two sites (Du Contour and Sainte-Rosalie series) in the Saint-Hyacinthe region in 1989 and 1990, and at four sites (Le Bras-I, -II, -III and Fourchette series) at Saint-Lambert-de-Lauzon in 1989, 1990 and 1991. The site and year combinations represented a range of different climatic conditions. The 15N-labelled fertilizer as 15NH415NO3 was spread on microplot at 180 kg N ha−1 rate, just before corn seeding. The recovery of fertilizer N (NREC) of grain and silage corn (Zea may L.) varied from 47 to 51%. At harvest, the amount of residual mineral N (soil and fertilizer) in soil profile (0–90 cm) ranged from 55 kg N ha−1 in a wet growing season to 176 kg N ha−1 in a dry growing season. The NREC in the mineral pool varied from 1.4% in wet growing season, especially on sandy soil, to 20.6% under dry conditions. The NREC recovered in the organic and fixed pools was 16.3, 24.6 and 38.9% of applied rate on the sandy soil, silt loam soil and clay loam soil, respectively. This pool was immobilized in soil profile and less subjected to significant loss overwinter than the mineral pool. The annual loss of fertilizer N varied from 13.6% on Sainte-Rosalie soil, having high N immobilization capacity, to 44.1% on Le Bras-II. These results shown that under the humid conditions found in Quebec, application of fertilizer N exceeding the optimum N rate will contribute to environmental pollution risk especially on permeable soils or soils having low N fixation and immobilization capacity. Key words: Fertilizer N loss, 15N-fertilizer, corn, mineral N, organic N


1997 ◽  
Vol 77 (2) ◽  
pp. 179-186 ◽  
Author(s):  
R. Lessard ◽  
P. Rochette ◽  
E. G. Gregorich ◽  
R. L. Desjardins ◽  
E. Pattey

Dairy cows and heifers in Québec and Ontario produce 19 Mt of manure annually. Most of this manure is applied to soils and may influence the atmospheric loading of greenhouse gases such as CH4 In this study, soil surface CH4 fluxes were measured 36 times during the snow-free season of 1993, and 28 times in 1994, on plots fertilized with organic or inorganic-N. In 1993, stockpiled dairy cattle manure was applied at rates of 0, 56 and 112 Mg ha−1 In 1994, the treatments were: zero N, 100 Mg ha−1 of stockpiled dairy cattle manure, 100 Mg ha−1 of composted dairy cattle manure and 200 kg N ha−1 as ammonium nitrate. Methane fluxes (−0.012 to 0.004 mg m−2 h−1) were usually higher (less negative) on manured than on unmanured plots, but the differences were not statistically significant. No significant effect of mineral-N fertilization was observed as the ammonium nitrate treatment showed uptake rates similar to those of the control. In 1993, episodic above-ambient CH4 concentrations were measured at 0.15 m (8 ppmv) and 0.05 m (2.7 ppmv) using stationary air probes, but were not associated with significant CH4 emissions at the soil surface. This observation suggested that CH4 produced in the soil was oxidized by methane-consuming organisms as it diffused towards the surface. Methane concentrations in soil air were higher in manured than in unmanured plots during most of the 1994 snow-free season, but were similar late in the season when soluble organic C concentrations in the manured plots returned to levels measured in the control plots early in the season. The results of this study indicate that the application of quantities up to 100 Mg ha−1 of dairy cattle manure to a soil under maize is not likely to have a large impact on the net exchange of CH4 between the soil and the atmosphere in central Canada. Key words: Methane, greenhouse gases


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