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Overuse of urea, low nitrogen (N) utilization, and large N losses are common in maize production in North China Plain (NCP). To solve these problems, we conducted two field experiments at Shangzhuang and Quzhou in NCP to test the ability of a newly developed urease inhibitor product Limus® to decrease NH3 volatilization from urea applied to maize. Grain yield, apparent N recovery efficiency (REN) and N balance when using urea applied with or without Limus were also measured over two maize growing seasons. Cumulative NH3 loss in the two weeks following urea application without Limus ranged from 9–108kg N ha−1, while Limus addition significantly decreased NH3 loss by a mean of 84%. Urea with Limus did not significantly increase maize yields (P<0.05) compared with urea alone. However, a significant 11–17% improvement in REN with Limus was observed at QZ. The use of urea-N plus Limus would permit a reduction in N applications of 55–60% compared to farmers’ practice and/or further 20% N saving compared with optimized urea-N rate (150kg N ha−1, based on N requirement by target yield of 7.5 t ha−1), and would achieve the same maize yields but with significantly decreased NH3 loss and increased N utilization.
Ammonia (NH3) is one of the key reactive N (Nr) components and the major alkaline gas in the atmosphere. NH3 directly and/or indirectly contributes to the eutrophication of aquatic ecosystems, soil acidification when nitrified and leached, and the decline in plant biodiversity through its deposition; it also damages human health through secondary aerosol or particle formation (e.g., PM2.5)1,2,3. In China, the total NH3 emission was estimated to be 9.8–20.4 Tg per year in the 2000s, 33–46% of which was derived from N fertilizer application4,5. Another study6 showed that the NH3 loss was up to 3.7 Tg in the North China Plain (NCP) in 2004, of which N fertilizer contributed 54% (and the rest was mainly from animal manures).
Urea accounts for around 60% of total N fertilizer consumption in China, but it has a large potential for NH3 loss, amounting to more than 20% in arable soils with a pH>7 (e.g. those in the NCP)7,8,9. Strategies to decrease NH3 loss from urea-N application to croplands have included the incorporation of surface applied N, deep placement of N fertilizer, and irrigation immediately following N topdressing10,11. However, on smallholder farms, these conservation practices are frequently not used due to labour shortages and delayed irrigation, so NH3 loss is expected to be high. These mitigation practices are even more difficult to apply if the N is applied as a top-dressing or as split applications at selected crop growth stages.
In addition, because of the long-term pressure for food security in China, farmers tend to apply excessive amounts of N fertilizer as an “insurance” to meet crop needs. In the NCP, N recovery efficiency (REN) from urea applied according to farmers’ practice averaged only 15% across 148 on-farm maize experiments12 and 10–19% in a two-year maize based cropping experiment13, suggesting a large opportunity for reducing N losses and improving REN in current urea-N management practices without sacrificing maize yields14.
There is, therefore, a strong demand for options to decrease NH3 losses while achieving higher REN and crop yields. Application of a urease inhibitor could contribute to achieving these objectives, as it should delay urea hydrolysis, decrease NH3 losses and improve N utilization15. A new urease inhibitor product Limus®, as a mixture of 75% N-(n-butyl) thiophosphoric triamide (NBPT) and 25% N-(n-propyl) thiophosphoric triamide (NPPT), was recently developed by BASF SE (a German Company). A laboratory study proved that the mixture of NBPT and NPPT (e.g. 75% vs. 25% or 50% vs. 50%) could achieve better effects in decreasing NH3 loss than single urease inhibitor (NBPT or NPPT)16. Limus product (here referring to plain urea amended with Limus) can be broadcasted on soil surface without extra irrigation or soil incorporation. Recently our previous study demonstrated the positive effects of Limus on decreasing NH3 loss in winter wheat at three locations and improving yield and N utilization with 55% less famer’s N practice under once application in wheat at one of three locations in north and northwest China17. However, the effects of Limus on maize, the largest crop in NCP, were not evaluated under field trials. Considering completely different meteorological (e.g. warm and humid in maize vs. cold and dry in wheat) and soil (e.g. different urease activities) conditions, we hypothesize that the effects of Limus on urease inhibition and NH3 loss mitigation may be lower in maize season than in wheat season. This is because the warm and humid condition will accelerate urea’s hydrolysis and the degradation of Limus.
To systematically evaluate the role of Limus in reducing NH3 volatilization and improving REN and grain yields in maize season, we conducted two typical field experiments over two years at Shangzhuang (SZ) and Quzhou (QZ). We wanted to (1) test our hypothesis (e.g. if Limus shows lower role in mitigating NH3 loss in maize than in wheat) and (2) develop a practical recommendation to minimize NH3 loss and achieve high yields and N utilization in maize in NCP.
After each N application over the two-year trial at each site, NH3 volatilization from urea alone at SZ ranged from 9 to 31kg N ha−1 (accounting for 4–38% of N application) compared to 0 to 2kg N ha−1 (accounting for 0–2% of N application) from urea amended with Limus, while at QZ NH3 loss ranged from 18 to 59kg N ha−1 (accounting for 18–61% of N application) for urea alone compared to 1 to 17kg N ha−1 (accounting for 1–28% of N application) from urea with Limus ((TableTable 2). Compared with Ncon, Nopt significantly (P<0.05) decreased total NH3 loss by up to 2–9kg N ha−1 at SZ and 13–23kg N ha−1 at QZ, while urea amended with Limus significantly decreased NH3 loss by 70–100% at the V3, and 63–100% at the V12 growth stage compared to Nopt at both sites. In contrast, no significant differences in NH3 volatilization were observed between the various Limus treatments (Table 1) at SZ in both years and at QZ in the first year. A significant reduction of total NH3 loss by 14kg N ha−1 (P<0.05) was observed in N80%opt/L-1 compared to Nopt/L and N80%opt/L at QZ in the second year.
At SZ, total cumulative NH3 loss varied from 0 to 37kg N ha−1 (accounting for 0–19% of urea-N) under the different fertilizer treatments, while NH3 loss significantly decreased to almost zero kg N ha−1 (78–100% reduction, P<0.05) when Limus was added. At QZ, Limus addition reduced total NH3 loss by 38–55kg N ha−1 (P<0.05), corresponding to a 65–90% decrease in NH3 loss (Table 2). The greatest decrease in total NH3 losses due to Limus addition occurred in the second year at QZ. At SZ, even though only 5–11kg N ha−1 NH3 was emitted at V12 in the urea-only treatments, urea amended with Limus decreased NH3 volatilization by 5–7kg N ha−1 (P<0.05), corresponding to a 78–100% reduction of NH3 loss.
The dynamics of NH3 fluxes and weather conditions (precipitation, air temperature, relative humidity and wind speed at two heights, etc.) in the two study years at SZ and QZ are shown in Figs 1 and and2,2, respectively. Precipitation events occurred frequently, while the relative humidity ranged from 35–90% (mostly above 55%), and the air temperature mainly around 22–33°C during the different periods of NH3 volatilization at SZ and QZ (Figs 1a’–d’ and 2a’–d’). The daily NH3 emission rates in the two N fertilization events (at V0 or V3 and V12 growth stages) varied between the two study years at SZ (Fig. 1a–d); no NH3 volatilization was detected at V0 in June 2011 (Fig. 1a). At V12 in August 2011 (Fig. 1b), the daily volatilization losses were higher in Ncon and Nopt, in which volatilization peaked at 360 and 300g N ha−1 h−1, respectively, on the first day after surface application of urea. In contrast, urea with Limus (Nopt/L) lost a daily maximum of only about 30g N ha−1 h−1 on the first day after surface application. The NH3 fluxes decreased to 0–50g N ha−1 h−1 on all of the treatments two days later.
Compared with the high NH3 fluxes at SZ after N fertilization at V12 in 2011, maximum volatilization rates were observed with urea alone at V3 in 2012. The highest NH3 fluxes from Ncon and Nopt at SZ occurred from the 3rd to the 10th day after fertilization, while much lower peak fluxes (0–30g N ha−1 h−1) from the Limus treatments (Nopt/L, Nopt/L-1, N80%opt/L-1) were measured on the 4th and 10th days after fertilization at V3 in 2012 (Fig. 1c).
At QZ, the daily NH3 volatilization rates (Fig. 2a–d) were approx. 3 times higher than those at SZ (Fig. 1a–d) over the two-years. Fluxes at QZ were higher in the Ncon and Nopt treatments, peaking at 400–800 and 200–700g N ha−1 h−1, respectively, during the first 3 days after urea application. Thereafter, they quickly decreased to 0–200g N ha−1 h−1 for both Ncon and Nopt (Fig. 2a–d). In contrast, NH3 fluxes in the urea with Limus treatments (Nopt/L, N80%opt/L, N80%opt/L-1) were only 0–150g N ha−1 h−1 after application. Generally, similar maximum NH3 fluxes (600–800gN ha−1 h−1) at QZ were measured at each fertilization event in spite of slightly different patterns of flux. Following N fertilization at V3 and V12, NH3 volatilization was only detected for 5–7 days during the first year (Fig. 2a–b), while the volatilization period lasted longer (up to 12 days) in the second year (Fig. 2b–c).
Lower grain dry matter (DM) yields (2.9–6.3 t DM ha−1 with no N) were found at SZ compared with those at QZ (4.5–7.5 t DM ha−1 with no N) (Fig. 3). At SZ, the grain yields ranged from 5.5 to 7.7 t DM ha−1 during the first and second years under different N application treatments, while the grain yields ranged from 9.0 to 10.1 t DM ha−1 d at QZ site. Totally, N fertilizer application significantly (p<0.05) improved maize grain yield by 93–135% (1st year) and 21–33% (2nd year) but no statistically significant differences (P>0.05) were observed between N treatments. Even the most efficient (in terms of REN) treatment N80%opt/L obtained maize yields similar to the other N treatments at both sites.
The REN (N recovery efficiency, an indicator of N use efficiency) was between 30% (Ncon) and 52% (Nopt & Nopt/L-1) in the first year, and 19% (Ncon) to 39% (N80%opt/L-1) in the second year at SZ (Fig. 3). In contrast, the REN was consistently higher (ranging from 1 to 26%) at QZ than at SZ across all N treatments during both years on average. The REN was lower in Ncon than in the Nopt treatments because of the greater amount of N applied to Ncon at both sites. No significant differences between optimized N fertilization (±Limus) were found at SZ, but the use of Limus (Nopt/L) at QZ led to an average REN increase by 17% and 11% when compared to Nopt in the 1st and 2nd years, respectively. Also REN in the N80%opt/L treatment was 23% (P<0.05) higher than in Nopt in the first year at QZ but, on average across the two years and two sites, applying N80%opt/L-1 did not result in significant differences in REN (ranging from 39 to 60%) compared with Nopt (ranging from 31 to 53%).
Nitrogen balances are shown in Table 3. The “other N loss” in Table 3 comprises all N loss pathways other than NH3 volatilization (e.g., nitrification/denitrification, N leaching) as well as possible errors. Relatively low mineral N (Nmin) in the 0–1m soil profiles before sowing was observed at both SZ (68kgN ha−1) and QZ (35kgN ha−1) in the first year, while relatively high Nmin before sowing was measured on each plot at both SZ (62 to 220kgN ha−1) and QZ (59 to 120kgN ha−1) in the second year (Table 3). Apparent N mineralization based on an N balance in N0 was 33kgN ha−1 at SZ, and 57kgN ha−1 at QZ during two years on average.
At SZ, the residual soil Nmin at harvest in Ncon was 212 and 337kgN ha−1 during the first and second years, respectively. These values were significantly higher than those in the optimized urea±Limus treatments (72–162kgN ha−1) during both years. The apparent N loss based on an N balance in Ncon at SZ was 28 and 83kgN ha−1 during the first and second years, but only 16–44kgN ha−1 in the optimized urea±Limus treatments (Table 3). At QZ, the highest residual Nmin was measured in Ncon (averaging 107kgN ha−1), while the amounts were about 67% less in the Nopt treatment (averaging 34kgN ha−1) and 56% lower in the urea with Limus (Nopt/L, Nopt/L-1, N80%opt/L-1) treatments (averaging 47kgN ha−1). Likewise, the highest mean apparent N loss of 118kgN ha−1 occurred in Ncon, followed by 75kgN ha−1 in Nopt, and 40kgN ha−1 in Nopt/L, NoptL-1, and N80%opt/L-1. As a whole, both the highest residual soil Nmin and apparent N losses were in Ncon plots at both sites. Relatively low apparent N loss was observed for treatments with Limus compared to Nopt. Moreover, the proportions of residual soil Nmin to apparent N losses differed at SZ and QZ: residual soil Nmin accounted for 80% of the N surplus (76 to 85%) at SZ but only 49% (40 to 58%) at QZ. Compared with the 1st year, the N surplus under farmers’ practice (Ncon) increased by 87 (at QZ) and 180 (at SZ) kg N ha−1, while only by 45 (at QZ) and 69 (at SZ) kg N ha−1 with optimized N fertilization (Nopt, Nopt/L) in the 2nd year.
Our research confirmed that conventional urea application to maize caused large NH3 losses (average 10–36% of urea-N applied) in the NCP. Similar research by Su et al.9 found NH3 losses of up to 26–33% of surface-applied urea at the V3 and V10 growth stages of maize production in the NCP. Optimized urea amended with Limus significantly decreased NH3 losses by a mean of 84% and improved REN in some cases, consistent with our previous results in winter wheat (e.g. a mean of 83% in NH3 loss mitigation)17. Our results deny our prior hypothesis that Limus may have lower role in mitigating NH3 loss and improving REN. We expect that the trade-offs between meteorological conditions (warm and humid in maize vs. cold and dry in wheat) and NH3 volatilization processes (high flux with short volatilization period in maize vs. low flux with long volatilization period in wheat) could explain why Limus effects on maize (the present study) are comparable to that on wheat17. In addition, the inhibition period of up to 14 days allowed sufficient time for rain to leach the urea into the subsoil and so prevent further NH3 losses (Figs 1 and and22).
The dynamics of NH3 fluxes were mostly determined by the weather (e.g., precipitation, air temperature and wind speed) after N application (Figs 1 and and2).2). At SZ, for example, NH3 loss was only detected during the V3 growth stage in 2012, when initial environmental conditions (2–4mm light precipitation and 60–78% relative humidity) were favorable for NH3 volatilization. In contrast, the low relative humidity (35–50%) and soil moisture content, together with a heavy rainfall (60mm) on the 6th day after N top dressing during the V0 growth stage in 2011 were unfavorable for NH3 volatilization. The magnitude of NH3 losses was largely influenced by small temporal differences in the weather and initial soil moisture content18,19. Some farmers in China broadcast N fertilizer after precipitation. This would further increase NH3 volatilization risk because high air humidity or limited rainfall provide adequate moisture for urea hydrolysis and cause the desorption of ammoniacal N from the soil20,21. In contrast, heavy rainfall effectively mitigates NH3 losses by leaching unhydrolized urea into the soil profile where it will be retained11,22. This was clearly demonstrated during the two maize growing seasons at QZ (Fig. 2a–d). Here moist initial soil conditions favoured rapid urea hydrolysis and promoted the initial NH3 loss. However, the high NH3 fluxes then rapidly decreased and stopped after precipitation (15–23mm). In the NCP, we find that NH3 volatilization will not be inhibited unless the daily precipitation is ≥7mm (Figs 1a’–d’ and 2a’–d’).
Additionally, the NH3 flux from urea at QZ was about 3 times higher than that at SZ over the two seasons (Figs 1a–d). This can partly be explained by the much higher urease activity in the QZ soil (13.0μgN g−1 soil h−1 or 29.3kgN ha−1 h−1) than the SZ soil (4.2μgN g−1 soil h−1 or 9.5kgN ha−1 h−1). High soil urease activity was reported to have a close positive relationship with the timing of urea hydrolysis as well as NH3 loss23,24. Nevertheless at SZ, NH3 loss still amounted to 31% of the urea-N applied (75kgN ha−1) during the V3 growth stage in 2012 (Table 2). This confirms that urea hydrolysis-induced NH3 volatilization is mostly dependent upon meteorological (e.g. amount of precipitation and wind speed) and soil (e.g. soil humidity and soil temperature) conditions15,18. In the current study, we found that the NH3 loss rates in maize seasons (2012/13) were nearly 20% higher than those in the previous winter wheat season (2011/12) at QZ with same amount of urea17. One factor that possibly influenced the different losses was air-soil temperature since the higher temperature in the summer maize growing season may have increased microbial activity and hydrolysis of urea fertilizers, also more NH3 in gaseous phase and less in solution phase at higher temperature15,23.
Considering the high potential for NH3 loss in the NCP, with most soils at pH>7.5, we expected that Limus will be very effective in decreasing NH3 emissions in this region. Our two-year experimental data confirm this role of Limus at both SZ and QZ sites in NCP.
Some previous reports have shown that the use of a urease inhibitor could increase the yields of crops25,26, while others did not show any significant yield increases27,28,29. A meta-analysis conducted by Abalos et al.30 found that urease inhibitors had a positive effect on crop yield (10%) and N use efficiency (12%), but their effectiveness was dependent on environmental and management factors. Our study clearly demonstrates a significant effect of Limus on mitigating NH3 volatilization but no significant effect on yield. During our first study year (2011 at SZ and 2012 at QZ), the initial soil Nmin contents were low (35–68kgN ha−1) because of previous N depletion (Table 3). However, grain yields were maintained under treatments of urea with Limus (Nopt/L-1 & N80%opt/L-1) applied only once at V0 or V3 (Fig. 3). High NH3 losses of 42–55kgN ha−1 (accounting for 20–28% of total N applied) were measured at QZ during the first maize season (2012) in the absence of Limus but, unexpectedly, maize grain yield was not improved by using Limus despite initial soil Nmin contents being less than half of those at SZ. However, the REN of urea with Limus (Nopt/L & N80%opt/L) significantly increased by about 20% and 33% compared to Nopt (53%) and Ncon (40%), respectively, and there was an increase in maize N uptake. During the 2nd study year, the sum of inputs to soil mineral N (including initial soil Nmin, N fertilizer, plus contributions from N mineralization) increased to a mean of 363kgN ha−1 at SZ and 324kgN ha−1 at QZ, respectively (Table 3). Therefore at both sites, despite the NH3 loss of 28–37kgN ha−1 at SZ and 86–109kgN ha−1 at QZ, there was still more than sufficient soil Nmin available to meet crop requirements without the use of Limus. However, residual mineral N contents were approx. 30kgN ha−1 higher (ranging from 11 to 52kgN ha−1) in treatments with Limus (Nopt/L), compared to Nopt treatments (Table 3), showing the N conserving effect of Limus and so the need to apply less N fertilizer to the following crop.
Research has shown that continually increasing the amount of N applied does not produce a sustained increase in crop productivity due to diminishing returns31. In our experiments, compared with the optimized urea-N treatments, grain yield was not significantly increased by the larger amounts that farmers applied (Ncon), while the REN of Ncon was significantly reduced to 30% at SZ and 40% at QZ in the 1st year and 19% at SZ and 31% at QZ in the 2nd year. Previous observations indicated that REN in the NCP has decreased to <20% under current farming N practice12, because of excessive N fertilizer use by farmers, which is substantially less than the 30–35% achieved in the 1980s in China10. As a consequence, the various N loss pathways including N leaching, NH3 volatilization, and N2O emission5,13 cause environmental pollution, such as enhanced N deposition3, pollution haze32, increased greenhouse gas emissions33, and soil acidification34. These problems have become increasingly serious in rapidly developing nations and their consequences are important on a global scale1,35. In addition, the excessive application of N fertilizer has been shown to lead to the accumulation of nitrate N in the soils of the NCP12. We found that the residual nitrate N retained in the 0–1m soil profile after harvest ranged from 203kgN ha−1 to 310kgN ha−1 at SZ after the 2-year study. After harvesting maize, Ju et al.36 reported nitrate N to be 275kgN ha−1 in the top 0.9m soil layer and 213kgN ha−1 in the 0.9–1.8m soil layer in Shandong province in the NCP, which was a potential threat to shallow groundwater quality through nitrate N leaching. Over-application of urea-N is common in Chinese intensively managed croplands due to the low economic penalties associated with yield losses and the relatively low price of urea fertilizer37. The optimized urea treatment with or without Limus maintained yields and achieved higher REN values (51% with urea alone and 62% with urea with Limus at QZ, and 41% and 42% at SZ, respectively). This and the much smaller applications of N fertilizer (by about 48% compared to farmer’s practice) led to less Nr losses and a smaller residual soil Nmin. A further 20% reduction in optimized N rate by using urea plus Limus (N80%opt/L-1: 120kgN ha−1, applied at V0 or V3) shows that Limus can maintain maize yields at a mean of approx. 6.5 t DM ha−1 at SZ and 9.6 t DM ha−1 at QZ while increasing the REN to an average of 41% at SZ and 55% at QZ, and at the same time saving labour. The once application practice of urea with Limus (e.g. N80%opt/L-1) should be consistent to Chinese smallholder farmers’ requirement: fertilization as simple as possible.
Although these practices represent a large step forward, increasing rather than merely maintaining crop yields remains a fundamental challenge. New research should quantify the economics (especially the environmental benefit of NH3 reduction) of using a urease inhibitor (e.g. Limus) across a range of soils, management, and climate variables.
The North China Plain (NCP) is the main maize (and wheat) production region in China, accounting for 39% of total national maize production13. The climate conditions are sub-humid continental. Mean annual rainfall is 500–700mm, with ~70% of precipitation occurring during the maize growing season. The field experiments were conducted for two consecutive years at two typical sites in the NCP: (1) Shangzhuang (SZ, 40°05′ N and 116°12′ E) in Beijing, during the 2011 and 2012 maize seasons; (2) Quzhou (QZ, 36°58′ N and 115°12′ E) in Hebei, during the 2012 and 2013 maize seasons. The soil types of SZ and QZ are fluvo-aquic soil and alluvial soil, respectively. Both soils are of calcareous loamy and silty texture and representative of the NCP. The initial soil pH at both (1:2.5 soil water ratio) was 7.9~8.0 and total N content 0.6~0.7gkg−1. Urease activity was 4.2μgN g−1 soil h−1 and 13.0μgN g−1 soil h−1 before seeding in the SZ and QZ soils, respectively. And soil organic matter content was 9.7 and 12.0gkg−1 in the SZ and QZ soils.
Before planting, phosphorus (calcium superphosphate, 60kg P2O5 ha−1) and potassium (potassium sulphate, 60kg K2O ha−1) fertilizers were applied to the plots, according to local mechanical tillage practices. Table 1 shows the detailed information on the N and Limus treatments at the sites, and there were six N treatments at each of the two maize experiments. All of the urea and urea plus Limus were surface applied in a randomized block design to four replicate plots of 30–40m2. Five of the six treatments were the same at both sites: N0, no N fertilizer; Ncon, conventional urea (270–300kgN ha−1); Nopt, optimized urea (150kgN ha−1); Nopt/L, optimized urea amended with Limus (150kgN ha−1), applied at two doses differently (SZ) or equally (QZ) at V0 (seeding, only at SZ in 2011) or V3 (three-expanded leaves) and V12 (twelve-expanded leaves) growth stages for Ncon, Nopt and Nopt/L; N80%opt/L-1, 80% of optimized urea amended with Limus (120kgN ha−1) applied only once at V0 or V3 stage. The additional treatment was Nopt/L-1 at SZ, which was optimized urea amended with Limus (150kgN ha−1) applied only once at V0 or V3, or at QZ, N80%opt/L which was optimized urea amended with Limus (120kgN ha−1) applied half at V3 and half at V12. The amount of optimized urea N was based on previous research on N fertilizer recommendations38,39. V3 and V12 were two key stages of maize for N topdressing. The maize variety Xianyu 335 was used at SZ at sowing densities of 60,000 and 70,000 seeds ha−1 in the first and second years, respectively. The maize variety at QZ was Zhengdan 958 sown at 90,000 seeds ha−1, based on local practice. Maize crop management (e.g. applications of pesticide and herbicide) was conducted according to traditional local practices at each site. Before the experiment, the winter wheat and summer maize rotation had been planted for at least one year without fertilizer inputs. No irrigation water was supplied for maize production at each site.
A calibrated Dräger-Tube Method (DTM) was adopted to measure NH3 loss, which is a dynamic chamber technique adjusted to actual meteorological conditions (e.g., temperature, wind speed) by an empirical calibration equation8. The calibrated DTM has been shown to be well-suited for NH3 measurements in multi-plot trials, and has been widely used around the world40,41,42. Briefly, four chambers (total surface area approx. 400cm2) were gently pressed about 2cm into the soil, and connected to a Teflon tube, a Dräger NH3 indicator tube, and a hand pump to detect the NH3 concentration. The primary NH3 flux was converted into the ambient NH3 flux using a calibration equation that included outside temperature and wind speed (at 0.2m and 2m height). The NH3 indicator tubes and pump were supplied by Drägerwerk AG, Lübeck, Germany. More details of the calibrated DTM method are presented in40,43, where the comparison of the DTM with NH3 volatilization observed from micrometeorological measurements showed very good agreement, especially for surface applied and evenly distributed N fertilizers.
The maize plants were harvested manually and aboveground crop residues, except stubble, were removed from each plot at maturity during the two maize cropping seasons. The plant samples (including grains, cobs and straws) from six maize plants per plot were oven-dried at 65°C to a constant weight. For determination of above-ground N uptake, plant samples were digested by H2SO4-H2O2 solution and N concentrations in grain and straw analyzed by the micro-Kjeldahl method.
Soils were sampled with an auger to 1m before planting and after harvest, taking five cores per plot in 20-cm increments (i.e. 0–20, 20–40, 40–60, 60–80 and 80–100cm). The fresh soil samples were extracted with a 1:10 ratio of soil to 0.01molL−1 CaCl2 and analyzed for NO3−-N and NH4+-N by an AA3 continuous flow analyzer (Bran+Luebbe GmbH, Norderstedt, Germany).
The REN was calculated using the following equation: REN=(crop N uptake in applied N plot-crop N uptake in N0 plot)/applied fertilizer N×100 and indicates the percentage of fertilizer N recovered in aboveground plant biomass44.
where the initial soil Nmin and residual soil Nmin were the mineral N content within the top 1m of soil before planting and after harvest, respectively.
One-way analysis of variance was performed on NH3 loss, grain yield, REN and other related parameters using the SPASS 17.0 statistical software. Significant differences among means were identified using Duncan’s test at P<0.05.
How to cite this article: Li, Q. et al. A new urease-inhibiting formulation decreases ammonia volatilization and improves maize nitrogen utilization in North China Plain. Sci. Rep. 7, 43853; doi: 10.1038/srep43853 (2017).
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This study was financially supported by the National Natural Science Foundation of China (41425007, 31421092) and the BASF SE, Ludwigshafen, Germany. The authors specially thank Prof. Volker Römheld (who passed away on 27 November 2013) for promoting the Sino-German cooperation during his life.
Dr Qianqian Li’s work has partly been funded by BASF SE. About the trial design, Prof. Xuejun Liu consulted for Drs. Gregor Pasda, Wolfram Zerulla and Alexander H. Wissemeier who work in BASF SE as staff. Dr Marco Roelcke, Profs. Keith Goulding, Xinping Chen and Fusuo Zhang declare no potential conflict of interest.
Author Contributions X.J.L., G.P., W.Z. and A.H.W. designed the experiments. Q.Q.L. and X.Q.C. performed the experiments. Q.Q.L. and X.J.L. analyzed data and wrote the paper. X.J.L., M.R., X.P.C., K.G. and F.S.Z. discussed and contributed to interpretation of the manuscript.