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Article

Influence of Slow- or Fast-Release Nitrogen in Xaraés Grass under Tropical Conditions

by
Carlindo S. Rodrigues
1,
Luís H. A. de Matos
2,
Douglas dos S. Pina
2,
Vagner M. Leite
2,
Paula de A. Silva
2,
Robério R. Silva
3,
Taiala C. de J. Pereira
3,
Henry D. R. Alba
2 and
Gleidson G. P. de Carvalho
2,*
1
Federal Institute of Education, Sciences and Technology Baiano, Campus Uruçuca, Uruçuca 45680000, Brazil
2
Department of Animal Science, Universidade Federal da Bahia, Salvador 40170110, Brazil
3
Campus of Itapetinga, State University of Southwest Bahia, Itapetinga 45700000, Brazil
*
Author to whom correspondence should be addressed.
Grasses 2023, 2(1), 47-56; https://doi.org/10.3390/grasses2010005
Submission received: 28 January 2023 / Revised: 2 March 2023 / Accepted: 6 March 2023 / Published: 9 March 2023

Abstract

:
Nitrogen (N) is a nutrient used worldwide in pasture fertilization. However, it is a very volatile element. Furthermore, inappropriate use promotes environmental pollution and economic losses. The present study was carried out to evaluate the effects of the N source on the productivity and N utilization efficiency in Xaraés grass (Brachiaria brizantha cv. Xaraés) under tropical conditions. The randomized complete block design was used in a 3 × 2 × 4 factorial scheme: three seasons (rainy, dry, and transition), two N sources (fast-release = conventional urea, and slow-release = treated urea), and four N doses (0, 80, 160, and 240 kg N/ha/year). Forage accumulation per day differed (p < 0.0001) with the season and N dose. The interaction between those showed a positive linear effect (p < 0.0001) during the rainy season and transition. With increasing N doses, there was a linear increase in annual dry matter production and N accumulation. However, the N utilization efficiency (p < 0.0001) was reduced. Nitrogen sources did not affect forage accumulation and N utilization efficiency. Therefore, it is not recommended to replace fast-release nitrogen fertilization (conventional urea source) with a urease inhibitor (slow-release N source), promoting benefits with lower production costs.

1. Introduction

The Brachiaria brizantha cv. Xaraes is among the most used forages with a high level of technology. Several studies were carried out evaluating the effect of nitrogen fertilization on the accumulation and productivity of this grass [1,2,3,4]; however, studies that evaluate slow- or fast-release N sources to fertilize this grass under tropical conditions are needed. The Xaraés forage is a perennial grass belonging to the Poaceae family, Panicoideae subfamily, and Paniceae tribe. This forage has high vigor and productivity, is resistant to leafhoppers, and can reach up to 1.5 m in height [2,3]. Its cultivation is indicated in tropical climate regions with rainfall above 800 mm per year, and it adapts well to medium fertility soils, producing up to 21 ton/ha of dry matter [4].
Urea [CO(NH2)2] is the most widely used fertilizer in the world because of the high concentration of nitrogen (N) in its composition (46% N) and the lower cost of production compared to other N sources [5,6,7]. However, it also has negative characteristics, such as high hygroscopicity and a high potential for losses by volatilization to the atmosphere in the ammonia (NH3) form [8,9]. These losses can be both an economic problem (because there are fewer nutrients left for plants to take up, which affects performance) and an environmental issue.
An alternative to decrease NH3 losses from urea is to treat the urea with a urease inhibitor. This slows the release of N, increasing absorption efficiency due to reduced NH3 volatilization. Among urease inhibitors, N-(n-butyl) thiophosphoric triamide (NBPT) is the most widely studied and used compound [10,11,12,13]. Although most studies have shown the potential to reduce NH3 losses in different systems from NBPT-treated urea [14,15,16,17,18], the benefits of this compared to untreated urea are less consistent in increasing forage production, with no difference in performance under some conditions [19,20,21].
The observed inconsistencies are probably associated with weather and soil conditions during fertilizer application. Increasing N doses and the application of urea in soils with high humidity and temperature generally cause a greater loss of NH3 [22]. These conditions make the use of urease inhibitors more attractive as a tool to increase N utilization efficiency. Conversely, low temperatures or dry conditions can limit urea hydrolysis and, therefore, NH3 losses [14,23].
Furthermore, in intensively managed pastures, where high doses of N are used, knowledge of the recovery of this nutrient by plants is important to establish strategies aiming for maximum efficiency in the use of N since efficiency is inversely proportional to the doses of N applied [24].
In this regard, there are uncertainties regarding the advantages of using NBPT-treated urea under tropical conditions in order to increase pasture performance and N utilization efficiency. Our hypothesis is that the efficiency in the use of nitrogen of this grass with the application of NBPT-treated urea in tropical conditions could improve its performance. Therefore, this study aimed to evaluate the effects of the N source, fast- or slow-release, on the percentage of dead material, forage accumulation, and N utilization efficiency in Xaraés grass (Brachiaria brizantha cv. Xaraés) under tropical conditions.

2. Material and Methods

2.1. Location of the Experiment and Climatic Conditions

The experiment was carried out from September 2017 to September 2018 on the Talitha farm located in the district of Monte Gordo, Camaçari-BA, Brazil. Located at latitude 12°41′51″ south and longitude 38°19′27″ west, with an altitude of 36 m. The average temperature of the experimental period was about 296.45 Kelvin (K), with an average rainfall of 1466.5 mm. Temperature and precipitation were measured with the help of an environmental thermometer (Sigma Aldrich, São Paulo, Brazil) and a rain gauge (Tecnal, São Paulo, Brazil), respectively.
The soil was evaluated in a commercial laboratory and showed the following chemical and physical characteristics: sandy soil (sand = 894 g/dm3; silt = 18 g/dm3; clay = 88 g/dm3); organic matter (OM) = 21.0 g/dm3; nitrogen (N) = 1.1 g/dm3; pH (H2O) = 5.3; P = 4.0 mg/dm3; K = 0.2 mmolc/dm3; Ca = 13.0 mmolc/dm3; Mg = 7.0 mmolc/dm3; Na = 0.0 mmolc/dm3; Al = 0.0 mmolc/dm3; H + Al = 18.0 mmolc/dm3; Sum of bases (SB) = 20.0 mmolc/dm3; cation exchange capacity (CTC) = 38.0 mmolc/dm3; and base saturation (V) = 53%. The chemical and physical analyses of the soil were carried out in accordance with the methods described by Moniz et al. [25]. During the experimental period, temperature and rainfall were monitored (Figure 1).
Fertilization and planting operations were implemented on 26 June 2016, after preparation and correction of soil acidity. For planting, 15 kg/ha of Brachiaria brizantha cv. Xaraés seeds were used, and 70 kg P2O5/ha (superphosphate), 60 kg KCl/ha (potassium chloride), and 50 kg N/ha (urea) were added throughout the experimental area. Before the beginning of the experimental period, the pasture was managed with a pre-grazing height of 30 cm and a post-grazing height of 15 cm, with dairy cows, for 15 months.
The total experimental area, including corridors, management area, and spacing between plots, was 0.66 hectares and was divided into three blocks, each plot measuring 10 × 10 m, totaling 100 m2. All plots received an application of 30 kg P2O5/ha and 200 kg KCl/ha. The application of N was carried out by the broadcasting method. Superphosphate was applied at a single dose in the first cycle, but KCl and N were divided into 4 applications of equal amounts (beginning and end of the rainy season). The dates of application were the following (day/month/year): first, 2 September 2017; second, 13 September 2017; third, 2 April 2018; and fourth, 24 April 2018.

2.2. Experimental Design

The experimental design used was randomized complete blocks with a 3 × 2 × 4 factorial scheme, referring to: three seasons of the year (rainy, dry, and transition), two N sources (fast-release = conventional urea, and slow-release = NBPT-treated urea), and four N doses (0, 80, 160, and 240 kg N/ha/year), with three replications. The experimental period lasted 380 days, divided into three periods (transition with 123 days, from 2 September 2017 to January 2018; dry season with 97 days, from 4 January 2018 to 11 April 2018; and rainy season with 160 days, from 12 April 2018 to 19 September 2018).

2.3. Grazing Management

Canopy height monitoring began post-grazing, performed three times a week until reaching a pre-grazing height of 30 cm [26,27]. Twelve readings were made for each experimental unit using a dipstick and a radiographic sheet film, according to Pequeno [28]. The pasture defoliation was carried out by adding or removing regulatory animals (mob grazing) [29], simulating a rotational grazing scenario. Three Girolando cows (Bos taurus taurus × Bos taurus indicus) with an average weight of 380 kg were used, using groups of animals for rapid defoliation, with a maximum time of 4 h, for the grass to reach post-grazing height. Prior to grazing, the animals fasted for 12 h on solid feed. This strategy was used to avoid the transfer of N between the animals and the pasture. While the animals were grazing, height measurements were made (30 representative points of the experimental unit) with a ruler and transparency until the canopy reached, on average, 15 cm in height. Nitrogen fertilization was carried out after grazing.

2.4. Forage Accumulation and Production, Regrowth Days, and Dead Material

To evaluate biomass accumulation, two forage samples were taken (at 15 cm and at soil level 0 to 15 cm) in each plot. Each sample measured 0.90 × 0.37 m (0.333 m2); these were weighed and dried at 338.15 K for 72 h. The estimation of the production was made from the evaluations of the forage accumulation dynamics according to Bircham and Hodgson [30]. Forage accumulation (kg DM/ha) was determined by the difference in forage mass (pre-grazing and previous post-grazing) [31]. Annual forage production (kg DM/ha/year) was calculated considering the accumulation of forage from all grazing cycles. The regrowth days were estimated according to the number of days between each grazing cycle, considering the day the animals left the paddock in the previous cycle (post-grazing) until they returned in the following cycle (pre-grazing). After removing the animals (post-grazing), two groups of ten tillers were identified in different areas of the experimental unit (Paddock) [32]. These tillers were randomly identified, and at the end of the grazing cycle (pre-grazing), these were cut close to the soil. Subsequently, the morphological separation and weighing of leaves, stem, and dead material were carried out. Afterward, the samples were dried (338.15 K for 72 h) and stored for further analysis.
Samples were analyzed for N and DM content using the Near Infrared Reflectance Spectroscopy (NIRS) system according to Marten et al. [33]. The reflectance data of the samples, in the wavelength range of 700–2500 nm, were stored in a spectrometer (Unity Scientific SpectraStar™ 2500 170 XL model). The calibration equations for Brachiaria brizantha, 16 peaks were selected (1203, 1349, 1478, 1541, 1595, 554, 1701, 1734, 1781, 1940, 2076, 2118, 2172, 2275, 2319, 2360, and 2500 nm). The equation used to determine DM was (a = mean wavelength of moisture in the sample):
Dry matter = 15.85041 + a1203(−2.21712) + a1349(71.37845) + a1478(−665.545) + a1541(643.2922) + a1595(−300.981) + a1701(1118.107) + a1734(−1089.01) + a1781(360.4243) + a1940(114.9662) + a2076(−972.004) + a2118(962.1933) + a2172(10.17885) + a2275(−335.829) + a2319(−624.293) + a2360(771.3495) + a2500(35.90113)
The nitrogen was determined according to the following equation (b = mean wavelength of nitrogen in the sample):
Nitrogen = −27.6687 + b1203(55.96.28) + b1349(−44.6292) + b1478(−553.552) + b1541(1664.555) + b1595(−1319.18) + b1701(8.4495) + b1734(340.3724) + b1781(−242.333) + b1940(130.4155) + b2076(206.4073) + b2118(−339.165) + b2172(−227.162) + b2275(546.8441) + b2319(505.337) + b2360(−708.738) + b2500(−11.4839)
The values were calculated as percentage of dead material (PDM), using the following equation:
P D M = ( g   d e a d   m a t e r i a l )   /   ( g   l e a f   +   g   s t a l k   +   g   d e a d   m a t e r i a l )   ×   100

2.5. Nitrogen Utilization Efficiency

Nitrogen utilization efficiency was calculated from the difference in forage N content in the pre-grazing and post-grazing period for each grazing cycle. NIRS was used to determine the N content. The N utilization efficiency was performed according to the indices cited by Baligar et al. [34] and adapted for pasture use:
-Nitrogen Efficiency Ratio (NER) = Dry matter production (kg)/N kg of accumulation in forage tissues.
-Agronomic efficiency of applied nitrogen (EAN) = (dry matter production with fertilization (kg) − dry matter production without fertilization (kg))/N dose (kg); kg DM/kg N applied.
-Applied nitrogen recovery efficiency (RNE) = [(N accumulation (kg) with fertilization − N accumulation (kg) without fertilization/N dose applied (kg)] × 100; %.
-Physiological Efficiency (PE) = [dry matter production with fertilization (kg) − dry matter production without fertilization (kg)]/[N accumulation with fertilization (kg) − N accumulation without fertilization (kg)]; kg DM/kg of accumulated N.
The nitrogen content in the roots and in the residue was not determined. The recovery of the N absorbed from the total applied considered only the N absorbed that was in the aerial part of the plants.

2.6. Statistical Analysis

The variables of accumulation, percentage of dead material, and days of regrowth were subjected to analysis of variance using the PROC MIXED of SAS (Statistical Analysis System-version 9.2 for Windows®) as described by the model below:
Yijkl = µ + Bi +Sj + dk + (S × D)jk + eijk +Pl + (S × P)jl + (D × P)kl + (S × D × P)jkl + εijkl
where Yijkl = observed value; μ = overall mean; Bi = random effect of the blocks; Sj = fixed effect of N source; Dk = fixed effect of N dose; (S × D)jk = interaction effect of source×dose; eijk = random error associated with source and dose of N; Pl = fixed effect of the season of the year; (S × P)jl = interaction effect of source×season; (D × P)jL = interaction effect of dose×season; (S × D × P)jkl = interaction effect of source×dose×season; εijkl = random error associated with the season effect.
The efficiency of utilization variables was subjected to analysis of variance using SAS PROC MIXED (Statistical Analysis System-version 9.2) as described in the model:
Yijk = µ + Bi + Sj + dk + (S × D)jk + eijk
where Yijk = observed value; μ = overall mean; Bi = random effect of the blocks; Sj = fixed effect of N source; Dk = fixed effect of N dose; (S × D)jk = interaction effect of source × dose; eijk = random error associated with source and dose of N.
The results for the quantitative factors (dose) were evaluated by regression analysis, and for qualitative factors (source and season), the Tukey test both considered a 5% probability to type I error.

3. Results

The nitrogen source did not affect the production parameters (p > 0.05) and percentage of dead material (p = 0.789). Furthermore, in the interactions with season and/or dose, the nitrogen source did not promote (p > 0.05) significant effects (Table 1). The effects of the season, the dose, and the interaction of these on pasture production are shown in Table 2.
Forage accumulation was higher in the transition season compared to the other seasons when the N dose was 80 and 240 kg/ha/year (p < 0.0001) and similar to N doses of 0 and 160 kg/ha/year (Table 2). The rainy season promoted a greater accumulation of forage compared to the dry season, regardless of the N dose (p < 0.0001). The N dose promoted a linear increase in forage accumulation in the rainy (p < 0.0001) and transition (p < 0.0001) seasons. In the dry season, the N dose did not affect (p > 0.05) forage accumulation (Table 2).
The dry season presented the highest percentage of dead material (p < 0.0001) independent of the N dose. Regarding the dose of N, the percentage of dead material decreased linearly in inverse relation to the increase in the dose of N in the rainy and transition (p < 0.0001) seasons (Table 2).
Regrowth days were higher in the dry season compared to the rainy season; the transition season showed the lowest values compared to the other seasons (p < 0.0001), regardless of the N dose. Considering the N dose, a quadratic regression of regrowth days was observed in the rainy (p = 0.0046) and transition (p < 0.0001) seasons, with an estimated minimum dose of 184.5 and 214.3 kg N corresponding to 22.6 and 27.6 regrowth days, respectively. During the dry season, the N dose promoted an increasing linear effect (p = 0.0017) on regrowth days (Table 2).
The nitrogen utilization efficiency parameters were affected by the N dose (kg/ha/year), except for the applied nitrogen recovery efficiency (p = 0.4831). On the other hand, the different sources of nitrogen release did not affect (p > 0.05) the nitrogen utilization efficiency parameters (Table 3).
Forage production (p < 0.0001) and N accumulation (p < 0.0001) showed an increasing linear effect in relation to higher N doses applied. The nitrogen utilization efficiency (p = 0.0292), the agronomic efficiency of the applied nitrogen (p = 0.0013), and the physiological efficiency (p = 0.0121) showed a decreasing linear effect contrary to the increase in the applied N dose (Table 3).

4. Discussion

The controlled release and constant availability of nutrients in the soil over time are desirable characteristics of fertilizers [7]. However, under the experimental conditions presented here, the results showed that fertilization with NBPT-treated urea (slow-release N) had no effect on the growth response or N utilization efficiencies of Brachiaria brizantha cv. Xaraés when compared to the use of conventional urea (fast-release N).

4.1. Forage Accumulation and Production

At the soil level, urea is separated from N-(n-butyl) thiophosphoric triamide (NBPT), the latter being the true inhibitor of urease activity [35,36], reducing the overall nitrogen loss rate as NH3 [13,37,38]. NBPT-treated urea reduces NH3 loss by approximately 53% [6]. However, the degradation of NBPT-treated urea in tropical climates is affected by temperature, soil type, and soil pH [39]. Linquist et al. [40], studying different N sources, including NBPT, found no differences in yield or N use in soils with pH < 6.0.
Under tropical climate conditions, temperature and humidity influence the increased degradation of NBPT-treated urea [36,41]. This may explain the similar results between treatments in the rainy and transition seasons. Furthermore, NBPT decreases its activity when it comes into contact with organic residues since these increase urease activity [42]. On the other hand, pasture residues affect the activity of NBPT-treated urea when the NBPT content is 530 mg/kg [43]. The slow-release N source used in this experiment contains 530 mg NBPT/kg; therefore, probably under tropical conditions, it is necessary to increase the amount to be used to observe significant results.
During the rainy and transition seasons, forage accumulation linearly increased at 0.305 kg DM/ha per day for each kg of N applied. The management of the entrance and exit of the meadow was carried out to avoid the excessive accumulation of stems. Therefore, increasing N doses promoted greater forage accumulation [44,45,46]. The increase in forage accumulation and the reduction of regrowth time resulted from the adequate management of the pasture during the rainy and transition seasons. However, in the dry season, probably due to water stress, canopy growth was slower, independent of the source and release rate of N.
Forage development is directly influenced by temperature, light, humidity, and soil nutrients [47]. During the rainy season, with lower temperatures and low light index, the growth rate is slower, requiring a gradual release of N for its optimization. Therefore, the slow-release N source could show a better result than conventional urea, considering that soils with high moisture and low temperatures generally promote an increase in nitrogen losses as NH3 [22].
The accumulation of forage as a function of the nitrogen rate corresponds to the increase in productivity from higher rates of appearance and elongation of leaves [2,48], thus reducing the rate of senescence and the accumulation of dead material. The positive effects of nitrogen fertilization on dry matter production after each cut or grazing were corroborated by Germano et al. [49].
Based on the observed results, we could affirm that in tropical climates, the activity of NBPT was reduced in concentrations of 530 mg/kg; consequently, nitrogen is lost mainly through volatilization rather than being taken up by the plant. For this reason, forage production and accumulation were not significantly different between nitrogen sources (NBPT-treated urea and urea) used as fertilizers for Xaraes grass, which is in contrast to our hypothesis.

4.2. Nitrogen Utilization Efficiency

Although the results of the different N sources on the increase in pasture yield were diverse [50,51], dry matter production and related nitrogen use efficiencies did not differ for the main effects of conventional urea and NBPT-treated urea in the current study. This knowledge is important for formulating strategies to maximize use efficiency, minimize environmental impact [24], and increase aboveground nitrogen accumulation with increasing N application rates [50,51].
On the other hand, the increase in N dose promotes lower utilization and physiological efficiencies, resulting in lower agronomic N efficiency. Three classes of NER are defined: low (<15 kg DM/kg N), moderate (15 to 45 kg DM/kg N), and high (>45 kg DM/kg N). In the current study, the N utilization efficiency was considered high, ranging from 67.7 to 80.4 kg DM/kg N applied. It is believed that the reduction in the mentioned efficiencies is not linked to N losses but is related to the so-called “excessive consumption”, where plants absorb the nutrient in excess of metabolic need and accumulate it in organelles, as well as in mitochondria, chloroplasts, and especially in vacuoles [52].
Our hypothesis was that the efficiency in the use of nitrogen of this grass with the application of NBPT-treated urea in tropical conditions could improve the performance of the Xaraes grass. However, probably due to climatic conditions, nitrogen use was generally similar between N sources, which decreased the chances that NBPT-treated urea would promote higher N-use efficiencies compared to urea without urease inhibitor treatment.

5. Conclusions

The NBPT-treated urea in grass pastures Brachiaria brizantha cv. Xaraés managed with pre- and post-grazing heights of 30 and 15 cm had no effect on forage accumulation and N utilization efficiencies. However, the nitrogen application as fertilizer, regardless of the release rate, provides an increase in forage accumulation in a shorter regrowth period and a reduction in the percentage of material up to a rate of 240 kg N/ha/year during the rainy season and the transition. It is necessary to evaluate the use of the NBPT-treated urea in concentrations of NBPT higher than 500 mg/kg in Brachiaria brizantha cv. Xaraés grass in tropical conditions.

Author Contributions

Conceptualization, L.H.A.d.M.; C.S.R.; T.C.d.J.P.; H.D.R.A.; methodology, L.H.A.d.M.; D.d.S.P.; V.M.L.; R.R.S.; formal analysis, L.H.A.d.M.; investigation, L.H.A.d.M.; P.d.A.S.; resources, G.G.P.d.C.; data curation, L.H.A.d.M.; T.C.d.J.P.; H.D.R.A.; writing—original draft preparation, L.H.A.d.M.; writing—review and editing, T.C.d.J.P.; H.D.R.A.; visualization, C.S.R.; D.d.S.P.; supervision, G.G.P.d.C.; project administration, C.S.R.; G.G.P.d.C. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not Applicable.

Data Availability Statement

The data used to generate the results in the paper are not available.

Acknowledgments

The authors thank “Conselho Nacional de Desenvolvimento Científico e Tecnológico–CNPq” and “Coordenação de Aperfeiçoamento de Pessoal de Nível Superior–CAPES” for the scholarships awarded.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. Precipitation rate and average monthly temperature (Kelvin degrees) from September-2017 to September-2018. T. max., T. min., and T. mean are the maximum, minimum, and mean temperatures, respectively.
Figure 1. Precipitation rate and average monthly temperature (Kelvin degrees) from September-2017 to September-2018. T. max., T. min., and T. mean are the maximum, minimum, and mean temperatures, respectively.
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Table 1. Production of Brachiaria brizantha cv. Xaraés grass in response to different seasons, N sources, and N dose.
Table 1. Production of Brachiaria brizantha cv. Xaraés grass in response to different seasons, N sources, and N dose.
ItemSourceSeasonDose (kg/ha/year)SEM
NBPTUreaRainyDryTransition080160240
Regrowth days50.4150.6033.1894.0424.2954.2050.4648.9148.430.55
Forage accumulation (kg DM/ha/day)52.3551.4559.1911.8984.6234.2948.7951.3573.153.11
Percentage of dead material29.5429.6917.1351.2720.4533.2630.2427.6927.282.58
p-Value
Source (S)Season (P)Dose (D)S × DS × PP × DS × P × D
Regrowth days0.6535<0.0001<0.00010.70240.0720<0.00010.0534
Forage accumulation 0.7892<0.0001<0.00010.46540.7050<0.00010.8505
Percentage of dead material0.8723<0.0001<0.00010.95450.1204<0.00010.3441
NBPT: N-(n-butyl) thiophosphoric triamide-treated urea; Urea: Conventional urea; SEM, Standard error of the mean.
Table 2. Production of Brachiaria brizantha cv. Xaraés grass in response to different seasons and N dose.
Table 2. Production of Brachiaria brizantha cv. Xaraés grass in response to different seasons and N dose.
SeasonDose (kg/ha/year)SEMp-Value
080160240LinearQuadratic
Forage accumulation per day (kg DM/ha/day)
Rainy42.1 a53.6 b63.4 a77.7 b5.33<0.0001 10.1147
Dry11.7 b13.7 c10.5 b11.6 c0.470.89390.9295
Transition49.1 a79.1 a80.1 a130.1 a11.90<0.0001 20.8033
p-Value<0.0001<0.0001<0.0001<0.0001
Percentage of dead material
Rainy24.5 b15.0 c16.0 b13.1 b1.78<0.0001 30.0784
Dry46.8 a54.5 a50.1 a53.7 a1.250.18330.2580
Transition28.6 b21.3 b17.0 b15.0 b2.12<0.0001 40.1605
p-Value<0.0001<0.0001<0.0001<0.0001
Regrowth days
Rainy41.6 b32.4 b29.8 b28.9 b2.05<0.00010.0046 5
Dry91.7 a94.3 a95.2 a95.0 a0.570.0017 60.0629
Transition29.3 c24.7 c21.7 c21.4 c1.30<0.0001<0.0001 7
p-Value<0.0001<0.0001<0.0001<0.0001
SEM, Standard error of the mean; N, nitrogen; DM, Dry Matter. Mean values followed by different letters, in the same column, are significantly different at 5% probability by Tukey’s test. Regression equations: 1 Ŷ = 0.1457x + 41.704 R2 = 0.99; 2 Ŷ = 0.3051x + 48.009 R2 = 0.88; 3 Ŷ = 0.0135x + 92.418 R2 = 0.74; 4 Ŷ = 0.0002x2 − 0.0738x + 29.378 R2 = 0.99; 5 Ŷ = 0.0003x2 − 0.1287x + 41.355 R2 = 0.99; 6 Ŷ = −0.0561x + 27.177 R2 = 0.93; 7 Ŷ = 0.0003x2 − 0.1286x + 41.346 R2 = 0.98.
Table 3. Nitrogen utilization efficiency in Brachiaria brizantha cv. Xaraés grass in response to different sources and doses (kg/ha/year) of nitrogen.
Table 3. Nitrogen utilization efficiency in Brachiaria brizantha cv. Xaraés grass in response to different sources and doses (kg/ha/year) of nitrogen.
Source (S)Dose (D)SEMp-Value
SourceDoseS × D
ItemUreaNBPT080160240LinearQuadratic
FP15,37415,504982515,05016,66720,217830.300.89050.0001 10.38330.8726
NA205.6212.0125.9184.2226.3298.910.880.57780.0001 20.53890.8205
NER76.974.680.481.573.667.72.450.89640.0292 30.16490.8731
EAN50.350.6-65.342.843.35.460.96030.0013 40.13760.8321
RNE66.575.9-76.464.273.06.580.2801--0.4840
PE78.265.4-90.365.959.34.990.06950.0121 50.15210.0619
NBPT: N-(n-butyl) thiophosphoric triamide-treated urea; Urea: Conventional urea; SEM, Standard error of the mean; FP, Forage production (kg DM/ha/year); NA, Nitrogen accumulation (kg N/ha/year); NER, Nutrient efficiency ratio (kg DM production/N kg of accumulation in forage tissues); EAN, Agronomic efficiency of applied nitrogen (kg DM/N kg rate); RNE, Applied Nitrogen Recovery Efficiency; PE, Physiological efficiency (kg DM/kg accumulated N). Regression equations: 1 Ŷ = 40.993x + 10521 R2 = 0.96; 2 Ŷ = 0.7014x + 124.66 R2 = 0.99; 3 Ŷ = −0.0575x + 82.7 R2 = 0.85; 4 Ŷ = −0.11x + 72.467 R2 = 0.73; 5 Ŷ = −0.155x + 102.83 R2 = 0.90.
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Rodrigues, C.S.; Matos, L.H.A.d.; Pina, D.d.S.; Leite, V.M.; Silva, P.d.A.; Silva, R.R.; Pereira, T.C.d.J.; Alba, H.D.R.; Carvalho, G.G.P.d. Influence of Slow- or Fast-Release Nitrogen in Xaraés Grass under Tropical Conditions. Grasses 2023, 2, 47-56. https://doi.org/10.3390/grasses2010005

AMA Style

Rodrigues CS, Matos LHAd, Pina DdS, Leite VM, Silva PdA, Silva RR, Pereira TCdJ, Alba HDR, Carvalho GGPd. Influence of Slow- or Fast-Release Nitrogen in Xaraés Grass under Tropical Conditions. Grasses. 2023; 2(1):47-56. https://doi.org/10.3390/grasses2010005

Chicago/Turabian Style

Rodrigues, Carlindo S., Luís H. A. de Matos, Douglas dos S. Pina, Vagner M. Leite, Paula de A. Silva, Robério R. Silva, Taiala C. de J. Pereira, Henry D. R. Alba, and Gleidson G. P. de Carvalho. 2023. "Influence of Slow- or Fast-Release Nitrogen in Xaraés Grass under Tropical Conditions" Grasses 2, no. 1: 47-56. https://doi.org/10.3390/grasses2010005

APA Style

Rodrigues, C. S., Matos, L. H. A. d., Pina, D. d. S., Leite, V. M., Silva, P. d. A., Silva, R. R., Pereira, T. C. d. J., Alba, H. D. R., & Carvalho, G. G. P. d. (2023). Influence of Slow- or Fast-Release Nitrogen in Xaraés Grass under Tropical Conditions. Grasses, 2(1), 47-56. https://doi.org/10.3390/grasses2010005

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