Literature DB >> 25859321

No-tillage and fertilization management on crop yields and nitrate leaching in North China Plain.

Manxiang Huang1, Tao Liang1, Lingqing Wang1, Chenghu Zhou1.   

Abstract

A field experimen class="Chemical">nt was performed from 2003 to 2008 to evaluate the effen class="Chemical">cts of n class="Chemical">tillage system and nitrogen management regimes on crop yields and nitrate leaching from the fluvo-aquic soil with a winter wheat (Triticum aestivum L.)-maize (Zea mays L.) double-cropping system. The tillage systems consisted of conventional tillage (CT) and no-tillage (NT). Three nitrogen management regimes were included: 270 kg N ha(-1) of urea for wheat and 225 kg N ha(-1) of urea for maize (U), 180 kg N ha(-1) of urea and 90 kg N ha(-1) of straw for wheat and 180 kg N of urea and 45 kg N ha(-1) of straw for maize (S), 180 kg N ha(-1) of urea and 90 kg N ha(-1) of manure for wheat and 180 kg N ha(-1) of urea and 45 kg N ha(-1) of manure for maize (M). An array of tension-free pan lysimeters (50 cm × 75 cm) were installed (1.2 m deep) to measure water flow and [Formula: see text]-N movement. No significant effect of the N management regime on yields of winter wheat and maize grain was found in the 5-year rotation. Tillage systems had significant influences on [Formula: see text]-N leaching from the second year and thereafter interacted with N management regimes on [Formula: see text]-N loads during all maize seasons. The average yield-scaled [Formula: see text]-N leaching losses were in order of CTS < NTS< CTU < NTU <CTM < NTM, ranging from 0.88 (CTS) to 6.07 (NTM) kg N Mg(-1) for winter wheat system and from 0.99 (CTS) to 6.27 (NTM) kg N Mg(-1) for summer maize system for 5 rotation years. The results showed that CTS decreased the yield-scaled [Formula: see text]-N leaching losses while sustaining crop grain yields. Considering the lower costs, NTS could be a potential alternative to decrease yield-scaled [Formula: see text]-N leaching losses and improve soil fertility while maintaining crop yield for the winter wheat-maize double-cropping systems in the North China Plain.

Entities:  

Keywords:  Conventional tillage; crop yield; manure; no-tillage; straw; yield-scaled nitrate–nitrogen leaching loss

Year:  2015        PMID: 25859321      PMCID: PMC4377259          DOI: 10.1002/ece3.1420

Source DB:  PubMed          Journal:  Ecol Evol        ISSN: 2045-7758            Impact factor:   2.912


Introduction

n class="Chemical">Numerous studies have demonstrated that no-n class="Chemical">tillage is useful to decrease agriculture production costs, improve soil structure, increase n class="Chemical">organic carbon sequestration, reduce soil erosion (Dabney et al. 2004; Holland 2004), and maintain or increase crop yields (Ehlers and Claupein 1994; Baumhardt and Jones 2002). In contrast to these reports, no-tillage was less successful under conditions of high weed infestation (Soane and Ball 1998) or in heavy clay soils with little or no N fertilization (Rasmussen and Douglas 1992). The effen class="Chemical">ct of no-n class="Chemical">tillage on nitratenitrogen class="Disease">n leaching loss is still a matter of controversy. Generally, no-tillage with surface mulch (crop straw or manure cover) may contribute to an increasing infiltration rate of soils, which may result in an increase in -N leaching loss (Boddy and Baker 1990; Singh and Malhi 2006). On the other hand, some studies have found higher -N leaching rates under CT due to increased N mineralization (Angle et al. 1993; Randall and Iragavarapu, 1995). The reported results of the effects of manure application on nitrate leaching are also inconsistent. Some studies have reported a higher potential risk of nitrate leaching for applications of manure in soils with high levels of soil organic matter (Chambers et al. 2000; Yan et al. 2002; Basso and Ritchie 2005). Zhou et al. (2014) demonstrated the beneficial reduction of nitrate leaching by 36% under synthetic N fertilizer (60% of applied N) plus pig manure (40% of applied N) compared with synthetic N fertilizer treatment in wheatmaize rotation system. The North China Plainpan> (NCP) is an important agronomic and animal husbandry area in China. At present, with an average annual total yield of the crops of winter wheat and summer maize reaching 15t ha−1, the NCP provides nearly 20% of the nation's grains. Since the 1990s, overfertilization has been common with the annual application rate of synthetic N in the NCP ranging from 450 to 800 kg N ha−1 year−1 for the typical winter wheat–summer maize double-cropping systems (Zhang et al. 2007). The intensive conventional tillage with excessive inputs of synthetic nitrogen fertilizer in this area has resulted in the decline of soil fertility and severe environmental pollution, especially -N leaching losses (Gao et al. 1999; Ju et al. 2006). Meanwhile, organic fertilizers (crop straw and manure) are the second N fertilizer resource in the NCP. Farmers have to deal with large quantities of crop straw produced from the double cropping and manure with a substantial amount of straw used for bedding that will have elevated nutrient levels from confined animal excreta (Yue 2009). It has been reported that the average manure N load is 183 kg N ha−1 in the agricultural areas of the NCP (Wu 2005). In general, returning crop straw to the field and manure application can increase soil C sequestration and N input (Baker et al. 2006). Nonetheless, large amounts of manure or crop straw retained on the soil surface can reduce crop yields (Kelley and Sweeney 2005). Especially, straw with a high C: N ratio decreases initial availability of nitrogen due to immobilization (Christensen 1985). Furthermore, there is a higher potential risk of nitrate leaching for excess application of manure (Andraski et al. 2000). Thus, it is necessary to include the N in straw and manure as sources of nutrients to reduce the use of mineral N fertilizer. However, little work has been done on these aspects for this area. An appropriate n class="Chemical">nitrogen manclass="Chemical">pan>agemen class="Chemical">nt regime in combination with a proper n class="Chemical">tillage system is expected to sustain soil fertility and agronomic productivity while decreasing yield-scaled -N leaching (Zhou and Butterbach-Bahl, 2014). It is known that the best management practices (BMPs) for fertilizers can decrease -N leaching losses from fertilized fields while sustaining crop yield. The recommended chemical N rate with appropriate organic fertilizer (straw or manure) rate applied to wheatmaize double-cropping system under no-tillage may be an alternative of the conventional tillage fertilization systems in this region (Hu et al. 2006). A long-term field experiment was initiated in 2003 to investigate the effects of N fertilizer regimes and tillage systems on crop yields and yield-scaled -N leaching in the NCP.

Materials and Methods

Site description

A field experimen class="Chemical">nt was conducted at Beiqiu (36°56′N, 116°36′E; 30 m above sea level) from October 2003 to September 2008, in Dezhou of Shandong province, China. The area has a semi-arid climate, with a long-term average annual precipitation of 585 mm (1961–2004). About 311-mm precipitation occurs during the rainy months of July–August. The average total precipitation of approximately 150 mm during the winter wheat growth season (mid-October to mid-June) is far less than the water demand of wheat. The soil was the fluvo-aquic soil (Shandong agricultural Department 1986), which was formed from the sediments of the Yellow River. The typical fluvo-aquic soil has a silt loam texture (sand, 13%; silt, 65%; clay, 22%) at 0 to 65 cm depth according to the USDA classification, a pH value of 8.1 to 8.4. The area is representative of the middle–high yield agricultural productivity in the NCP. The selected soil parameters were determined in October 2003 (Table1).
Table 1

Selected soil properties of experiment site.

DepthBD1OM2Total NP2O5K2OpH
cmg cm−3g kg−1H2O
0–101.2212.80.872.0421.98.1
10–201.488.20.631.6221.48.3
20–401.444.80.441.3720.78.4
40–601.563.30.391.3721.98.4

Soil bulk density.

Organic matter.

Selen class="Chemical">cted soil properties of experimen class="Chemical">nt site. Soil bulk density. n class="Chemical">Organic matter.

Field experiment design

The experimen class="Chemical">nt was a randomized, complete-block design with a split-plot arrangemen class="Chemical">nt of tillage systems as a main plot, three nitrogen regimes as subplots, and three replicates. The size of the main plot was 22.5 m × 40 m and that of subplots 6.5 m × 40 m. Summer maize in 2003 was planted without fertilization to make the soil fertility at the site homogeneous. There were two tillage systems: conventional tillage (CT) and no-tillage (NT). The CT consisted of fall plowing two times after maize harvest with a rototiller to a depth of about 0.2 m and harrowing two times to prepare the seedbed for wheat planting. There was no-tillage before maize seeding under CT, which is historically common in the Shandong province. The NT treatment used no soil disturbance except for planting. The practical nitrogen management regimes in local winter wheatmaize production were adopted in this study. The three nitrogen management regimes were as follows: 270 kg N ha−1 year−1 (urea) for wheat and 225 kg N ha−1 year−1 (urea) for maize (U), 180kg N ha−1 year−1 (urea) and 90 kg N ha−1 year−1 (maize straw) for winter wheat and 180 kg N ha−1 year−1 (urea) and 45 kg N ha−1 year−1 (wheat straw) for maize (S), 180 kg N ha−1 year−1 (urea) and 90 kg N ha−1 year−1 (poultry manure) for wheat and 180 kg N ha−1 year−1 urea and 45 kg N ha−1 year−1 (poultry manure) for maize (M). n class="Chemical">Urea for n class="Species">wheat was broadcast on the soil surface manually after rainfall or before irrigation. For U treatmen class="Chemical">nt, the urea (270 kg N ha−1) was in three equal split applications with one-third as basal fertilizer in late October (or early November) and the remaining as supplementary fertilizer in late March (or early April) and May in the following year. For S and M treatments, the amount of urea (180 kg N ha−1) was split into two equal for wheat in late October (or early November) and May in the next year. For CT treatments, urea applied as basal fertilizer for wheat was incorporated with tillage operation in the 20 cm. For maize, urea was manually broadcast on the soil surface after rainfall at early growing period. On average, the poultry manure con class="Chemical">ntainpan>ed 22.5 g kg−1 total class="Chemical">pan> class="Chemical">N, 4.09 g kg−1 alkali-hydrolysis N, 16.1 g kg−1 total P, 12.0 g kg−1 total K, 304 g kg−1 total C. The mean total C and N contents were 411.9 and 7.49 g kg−1 for winter wheat straw and 372.5 and 9.25 g kg−1 for maize straw, respectively. Details of poultry manure and crop straw composition are shown in Table2. Both wheat and maize straws were chopped into 5–8 cm and applied on the surface by hand. For S treatment, the maize straw was applied at 9.7 Mg ha−1 in late March for winter wheat and the wheat straw at 6.0 Mg ha−1 at the early growth period for maize. For M treatment, poultry manure was applied at 4 Mg ha−1 in late March for winter wheat and 2 Mg ha−1 at the early growth period for maize. For U plots, concentrated superphosphate and potassium sulfate were surface-broadcasted to plots at the rates of 120 kg P2O5 ha−1 and 170 kg K2O ha−1 for each crop, respectively. For S plots, 15.5 kg ha−1 (P) and 163.0 kg ha−1 (K) with maize straw were inputs for wheat, and 12 kg ha−1 (P) and 100 kg ha−1 (K) for maize with wheat straw. Therefore, 104.5 kg P ha−1 of concentrated superphosphate was applied to wheat, and 108 kg P ha−1 of concentrated superphosphate and 70 kg K ha−1 of potassium sulfate for maize. For M plots, 64 kg P ha−1 and 48 kg K ha−1 for winter wheat and 32 kg P ha−1 and 24 kg K ha−1 for maize with poultry manure applied were inputs; therefore, 56 kg P ha−1 of concentrated superphosphate and 122 kg K ha−1 of potassium sulfate for winter wheat and 88 kg P ha−1 of concentrated superphosphate and 146 kg K ha−1 of potassium sulfate for maize were applied, respectively.
Table 2

Composition of poultry manure and crop straw.

Poultry manureWinter wheat strawMaize straw
g kg−1
C304 (29.1)1411.9 (46.8)372.5 (38.9)
N22.5 (3.8)7.49 (1.6)9.25 (2.7)
P16.1 (1.9)2.0 (0.3)1.62 (0.5)
K12.0 (2.8)16.7 (1.9)16.8 (4.9)

Numbers in parentheses are the standard errors.

Composition of poultry manure and crop straw. Numbers in parentheses are the standard errors. Seeding for winter class="Chemical">pan> class="Species">wheat and maize was conducted manually under CT and NT systems. Winter wheat was seeded in rows at an interval of 20 cm at a rate of 180 kg ha−1 in mid-October except in 2003. Seeding of wheat was delayed until the 3rd of November by an abnormal precipitation of 166.9 mm in mid-October 2003. Maize was planted in mid-June at the density of 66,400 plants ha−1 in rows at an interval 60 cm. Irrigation water was applied using the surface flooding method with a water meter installed to control the irrigation rate on each plot. Winter wheat was irrigated with 75 mm water on each occasion on March 30, April 29, May 21 and October 15, 2004, and April 6, May 9, and Oct 30, 2005, and March 28, April 15 and October 14, 2006, and April 2 and May 5, 2007, and March 21, 2008. Summer maize was irrigated with 60 mm water on each occasion only on June 20, 2005 and July 30, 2006 (Fig.1). Weeds and insects were chemically controlled, that is herbicide (2, 4-Dichlorophenoxyacetic acid butylate) spraying within 1 week after sowing and insecticide (40% dimethoate, o, o–dimethyl S–[2-(methylamino)–2–oxoethyl] dithiophosphate) in May for winter wheat and late July for maize. Winter wheat was harvested (with DZ Combine harvester) during mid-June and maize in mid-October, with aboveground biomass removed for all treatments. The straws for S plots were conserved for use. The plant samples, comprising separate grain and straw from 2 m2 (1 m × 2 m) sampling area of wheat and 10 plants in the case of maize, were collected from the middle rows of each plot at harvest and were oven-dried at 65°C for 3 days. Grain and straw yields were recorded, and grain data were adjusted to 14% moisture content. The nitrogen content in straw of the subsamples of both wheat and maize and the poultry manure were determined using the micro-kjeldahl method by digesting the samples in H2SO4-H2O2 solution (Bremner and Mulvaney 1982).
Figure 1

Monthly total precipitation (mm), monthly air mean temperature (°C), and monthly total leachate volumes (mm) collected from October 2003 to October 2008. Error bars are the standard errors of the treatment means. Solid arrows denote irrigation. CTU, urea (270 kg N ha−1) for wheat and urea (225 kg N ha−1) for maize with conventional tillage (CT); CTS, urea (180 kg N ha−1) and maize straw (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and wheat straw (45 kg N ha−1) for maize with CT; CTM, urea (180 kg N ha−1) and poultry manure (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and poultry manure (45 kg N ha−1) for maize with CT; NTU, urea (270 kg N ha−1) for wheat and urea (225 kg N ha−1) for maize with no-tillage (NT); NTS, urea (180 kg N ha−1) and maize straw (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and wheat straw (45 kg N ha−1) for maize with NT; NTM, urea (180 kg N ha−1) and poultry manure (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and manure (45 kg N ha−1) for maize with NT.

Mon class="Chemical">nthly total precipitation (mm), monthly air mean temperature (°C), and monthly total leachate volumes (mm) collen class="Chemical">cted from October 2003 to October 2008. Error bars are the standard errors of the treatment means. Solid arrows denote irrigation. CTU, urea (270 kg N ha−1) for wheat and urea (225 kg N ha−1) for maize with conventional tillage (CT); CTS, urea (180 kg N ha−1) and maize straw (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and wheat straw (45 kg N ha−1) for maize with CT; CTM, urea (180 kg N ha−1) and poultry manure (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and poultry manure (45 kg N ha−1) for maize with CT; NTU, urea (270 kg N ha−1) for wheat and urea (225 kg N ha−1) for maize with no-tillage (NT); NTS, urea (180 kg N ha−1) and maize straw (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and wheat straw (45 kg N ha−1) for maize with NT; NTM, urea (180 kg N ha−1) and poultry manure (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and manure (45 kg N ha−1) for maize with NT. Each plot was equipped with a large (0.50 m x 0.75 m) tension-free pan lysimeter in late-August, 2003 for subsurface flow measurements. A lysimeter was inpan>stalled by excavatinpan>g laterally from a trench border of each plot at the depth of 1.2 m. Wiclass="Chemical">pan> class="Chemical">nter wheat and maize roots mainly distribute in the top 0–1.0 m soil layer in the area (Liu et al. 2008; Qi et al. 2012). Therefore, the 1.2-m-deep lysimeter was enough for both winter wheat and maize crops. Lysimeter pan emplacement was made by excavating laterally from a trench a border (none yield row) of each plot at the 1.2 m depth. A lysimeter was inserted into the excavated area so that the pan edge was at least 0.15 m from the trench face. Each lysimeter was filled with coarse sand overlaid by medium-fine sand. The pans were pressed tightly by adjusting the turnbuckles beneath each lysimeter into the roof of the excavated area to ensure contact between the undisturbed soil above and the sand in the lysimeter to establish continuity with the soil profile (Zhu et al. 2002). This prevents wicking of water along the roof and around the lysimeter which was common with open face (empty) tension-free pan lysimeters. The design and installation of the pan lysimeters were similar to those described by Jemison and Fox (1992). Tubes were connected to transport water into buried 20-L storage bottles. All water in each bottle was siphoned out for analysis of nutrient concentrations, and the volume of flow was recorded. Generally, sampling was conducted manually once a week. When amounts of percolate were small, samples from two to four successive sampling times were pooled within a month before -N analyses. After rainfall and irrigation events, samples of percolate were collected the next day when discharge occurred. The subsamples were stored frozen until analysis. Nitrate concentration was determined using a cadmium reduction–diazotization method on a flow-injection analyzer. The -N leaching flux of each single percolation episode was calculated according to Zhou et al. (2014). The amount of seasonal leached -N was calculated as the sum of -N in all samplings within the season. Flow-weighted average concentration values were weighted averages based on total NO3-N transport and total percolation for the corresponding period (Owens et al. 2000). The yield-scale -N leaching loss was defined as the seasonal -N leaching losses from a given treatment divided by the crop yield (kg N Mg−1 grain). Weather data were recorded at the meteorological station located 300 m away from the experimental site.

Data analysis

Analysis of variance (ANOVA) for split-plot design was performed to determinclass="Chemical">pan>e the significance of differences among the treatments and interactions (Steel and Torrie 1986). In addition, differences for seasonal leachate volumes in millimeters of water depth (mm) among years were also evaluated. Then, multiple comparisons of overall treatment effen class="Chemical">cts and interactions were made with a Fisher's protected least significant difference (LSD) test (p < 0.05). Data on seasonal leachate volumes, -N leaching amounts, crop yields, and cumulate leachate volumes, -N concentration load, and yield-scaled -N leaching losses over 5 year met ANOVA assumptions and were analyzed without transformation.

Results and discussion

Crop yield

The results for crop grain yield for all the treatmen class="Chemical">nts are shown in Tables3 and 4. n class="Chemical">No significant effect on n class="Species">maize grain yield was observed due to tillage or N management regimes for the 5 years. The NT treatments appeared to have higher yields than CT treatments; however, the differences were not significant. Linden et al. (2000) found similar results in a 13-year study conducted on well-drained soils in east-central Minnesota. In that study, NT usually results in equal or greater corn yields than tillage treatments in the first 5 years of the study. However, after year 5, tillage treatments resulted in significantly greater yields than NT treatments. Our result was different from the decreased yield effect of conservation tillage on maize yield due to lower soil organic matter and poorly drained soils in Indiana, USA observed by Griffith et al. (1988). The effect of NT on crop yields varies depending on climate and soil type.
Table 3

Effect of tillage and nitrogen management regimes on summer maize grain yield (kg ha−1).

N regimes
TreatmentUSMMean
2004
CT17257758869387261
NT6859754975237310
Mean705875697230
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2005
CT8298843985518429
NT8312858683508416
Mean830585138450
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2006
CT6527622366446464
NT6660657970476762
Mean659464016845
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2007
CT6265575559145978
NT6445599357946077
Mean635558745854
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2008
CT7688862577628025
NT8027860478018144
Mean785886147781
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2004–2008
CT36,03536,62935,81054,237
NT36,30437,31236,51355,064
Mean36,17036,97036,161
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.

CT, conventional tillage, the soil is tilled with a rototiller in the top soils of 20 cm before winter wheat sowing in autumn. There was no-tillage before maize seeding. NT, no-tillage. U, urea (270 kg N ha−1) for wheat and urea (225 kg N ha−1) for maize. S: urea (180 kg N ha−1) and maize straw (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and wheat straw (45 kg N ha−1) for maize. M: urea (180 kg N ha−1) and poultry manure (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and poultry manure (45 kg N ha−1) for maize.

Table 4

Effect of tillage and nitrogen management regimes on winter wheat grain yield (kg ha−1)

N regimes
TreatmentUSMMean
2003–2004
CT14144380139283958
NT3943377737443821
Mean404337893836
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2004–2005
CT5865581056325769
NT5583547855755546
Mean572456445604
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2005–2006
CT5407506052025223
NT4745485547504783
Mean507649584976
LSD0.05: tillage = 428; N regime = NS; tillage × N = NS.
2006–2007
CT6580644065126511
NT5644513152185331
Mean611257855865
LSD0.05: tillage = 709; N regime = NS; tillage × N = NS.
2007–2008
CT6773658266846680
NT6445601962056223
Mean660963016444
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2003–2008
CT28,76927,69327,95828,140
NT26,36025,26025,49225,704
Mean27,56526,47626,725
LSD0.05: tillage = 1862; N regime = NS; tillage × N = NS.

The treatment details are the same as those in Table3.

Effect of tillage and nitrogen management regimes on summer maize grain yield (kg ha−1). n class="Chemical">CT, conven class="Chemical">ntional tillage, the soil is tilled with a rototiller in the top soils of 20 cm before win class="Chemical">nter wheat sowing in autumn. There was no-tillage before maize seeding. NT, no-tillage. U, urea (270 kg N ha−1) for wheat and urea (225 kg N ha−1) for maize. S: urea (180 kg N ha−1) and maize straw (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and wheat straw (45 kg N ha−1) for maize. M: urea (180 kg N ha−1) and poultry manure (90 kg N ha−1) for wheat and urea (180 kg N ha−1) and poultry manure (45 kg N ha−1) for maize. Effect of tillage and nitrogen management regimes on winter wheat grain yield (kg ha−1) The treatmen class="Chemical">nt details are the same as those in Table3. During the first 2 years of the field experimen class="Chemical">nts, there was inclass="Chemical">pan>significan class="Chemical">nt difference in winter n class="Species">wheat yields among the different treatments. After this initial lag period, the tillage effect was observed in the third and fourth years. The wheat grain yield in the NT treatments was lower by 8.4% in the third year and by 18.1% in fourth year compared with CT treatments, respectively. Tillage in autumn (CT) generally benefits winter wheat roots development in deeper soil profile and absorbs subsoil water in serious dry season in the NCP (Dong et al. 2007). In the fifth year, the wheat grain yield in the NT treatments was also lower than that of the CT treatments, although the difference was insignificant. The higher than average precipitation in April 2007 may offset the shortage of NT on growth of winter wheat, which implies that the effect of NT on yield of winter wheat was affected by the rainfall pattern in dry growing season. There was significan class="Chemical">nt class="Chemical">pan> class="Chemical">tillage effect on cumulative wheat yields (Table4). The NT treatments decreased cumulative wheat yield by 12.2% with annual average of 2.4%. Our results were consistent with other experiments conducted in the NCP, which have demonstrated that compared with traditional tillage farming, NT could reduce winter wheat grain yield (Li et al. 2008; Peng et al. 2011). The negative effects of NT on winter wheat grain yield could be related to the low germination rate and poor plant growth caused by NT (Wuest et al. 2000; Hemmat and Taki 2001). In contrast to our results, conservation tillage's positive effect on rainfed winter wheat yield was observed under the Chinese Loess Plateau climate due to improved soil water storage under monoculture conditions (Su et al. 2007; Wang et al. 2009). n class="Chemical">No significan class="Chemical">nt effect on seasonal n class="Species">maize and winter wheat grain yield or cumulative crop grain yields was observed due to N management regime throughout 5 years (Tables4). Although CTS decreased cumulative wheat yield by 3.7% with annual average of 0.7% compared with CTU, the difference was insignificant. These results suggest that there is greater potential to decrease the rates of urea application (33.3% reduction for wheat and 20% for maize) while sustaining crop grain yields by adopting S and M regimes in place of the U regime in the area studied.

Percolation

The mon class="Chemical">nthly total percolation was showed inpan> Figure1. There were only two drainpan>age episodes inpan> the autumn of 5 win class="Chemical">nter wheat seasons, one in October 2004 and the other one in October 2006 after irrigation. Generally, no measurable percolation occurred from October to the February of the subsequent year due to dry and freezing weather conditions during the experiment period. Most of percolation occurred as a consequence of successive episodes of irrigation or heavy rainfall from March to September, especially during rainy summer, which agrees with the results reported in other studies (Huang et al. 2011; Zhou et al. 2012). The seasonal leachate volumes were differen class="Chemical">nt among years due to rainfall (Tables6). The total leachate volumes during maize seasons varied from the lowest amount in year 2006 to the highest amount in year 2004 (Table6), corresponding to total precipitation during maize seasons of a minimum of 242 mm in 2006 to a maximum of 654 mm in 2004 (Fig.1), respectively.
Table 6

Effect of tillage and nitrogen management regimes on leachate volumes (mm) during summer maize seasons

N regimes
TreatmentUSMMean
2004
CT1155.8a2169.0a157.8a160.9
NT165.4a170.3a170.9a168.9
Mean160.6169.7164.4
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2005
CT95.1b94.3b92.7b94.1
NT105.3b110.9b109.3b108.5
Mean100.2102.6100.9
LSD0.05: tillage = 5.2; N regime = NS; tillage × N = NS.
2006
CT28.4e28.3d27.2d27.9
NT30.1d30.8d31.9c31
Mean29.229.629.6
LSD0.05: tillage = 2.5; N regime = NS; tillage × N = NS.
2007
CT64.7c59.1c60.4c61.3
NT78c78.3c76.7d77.6
Mean71.468.668.5
LSD0.05: tillage = 12.7; N regime = NS; tillage × N = NS.
2008
CT53.1d52.9c54c53.2
NT80c79.5c78.9c79.5
Mean66.46766.3
LSD0.05: tillage = 6.0; N regime = NS; tillage × N = NS.

The treatment details are the same as those in Table3.

For the same treatment in a column, different letters indicate significant difference between years at P < 0.05.

Effect of tillage and nitrogen management regimes on leachate volumes (mm) during winter wheat seasons. The treatmen class="Chemical">nt details are the same as those in Table3. For the same treatmen class="Chemical">nt within a column, differen class="Chemical">nt letters indicate significant difference between years at P < 0.05. Effect of tillage and nitrogen management regimes on leachate volumes (mm) during summer maize seasons The treatmen class="Chemical">nt details are the same as those in Table3. For the same treatmen class="Chemical">nt in a column, differen class="Chemical">nt letters indicate significant difference between years at P < 0.05. The effen class="Chemical">ct of n class="Chemical">N managemen class="Chemical">nt regime on leachate volume was insignificant throughout the 5-year rotation (Tables7). The tillage effects on leachate volumes were insignificant for the first three cropping seasons (P > 0.05). Thereafter, tillage significantly affected seasonal leachate volumes (Tables6).
Table 7

Effect of tillage and N management regimes on -N leaching (kg -N ha−1) during winter wheat seasons

N regimes
TreatmentUSMMean
2003–2004
CT13.21.78.44.4
NT3.92.712.56.4
Mean3.62.2104
LSD0.05: tillage = NS; N regime = 1.8; tillage × N = NS.
2004–2005
CT3.11.313.35.9
NT3.91.816.87.5
Mean3.51.615.0
LSD0.05: tillage = 0.6; N regime = 1.9; tillage × N = NS.
2005–2006
CT25.312.847.228.4
NT31.518.860.737.0
Mean28.415.854.0
LSD0.05: tillage = 10; N regime = 4.1; tillage × N = NS.
2006–2007
CT2.20.58.63.8
NT5.11.717.28.0
Mean3.71.112.9
LSD0.05: tillage = 4.1; N regime = 4.4; tillage × N = NS.
2007–2008
CT13.78.134.718.8
NT27.610.447.328.4
Mean20.69.341.0
LSD0.05: tillage = NS; N regime = 4.7; tillage × N = 6.7.

The treatment details are the same as those in Table3.

Effect of tillage and N management regimes on -N leaching (kg -N ha−1) during winter wheat seasons The treatmen class="Chemical">nt details are the same as those in Table3. There were about 100 mm of the 5-year cumulative leachate volumes for n class="Chemical">NT subplots more than n class="Chemical">CT subplots (Table7), which could be related to improved pathways for water percolation and the mechanical delay of runoff by rough surface to increase more n class="Chemical">water moving into the soil matrix during rain-runoff events in NT plots (Wilson et al. 2004). The temporal lag effect of NT system on water percolation observed in this study reflected the changes of soil hydraulic properties under NT treatment, which may be a very slow process. Higher biological activity, increased soil organic matter due to the retention of organic material as crop residues and manure on the soil surface, and reduced soil disturbance under NT plots lead to a more stable soil pore system (Six et al. 2002). An improved soil structure and continuous soil pores enable higher infiltration and ultimately increased available water for winter wheat production (Thierfelder and Wall 2009; Liu and Luo 2011).

Nitrate–nitrogen concentration and leaching

Leaching n class="Chemical">-N concentrations displayed strong variation within sampling dates and significantly different between treatments (Fig.2). Generally, the -N concentrations in leachate had higher levels after fertilizer application in April and late July/early August followed irrigation or rainfall. The -N concentrations in leachate in 2003–2004 rotational year were relative lower likely due to no fertilization of NPK during maize season in 2003 and dilution of abundant percolation during 2004 summer seasons. Manure application even significantly raised the -N concentration under the M plots from the first winter wheat season compared to the other treatments (P < 0.05). The highest concentration of -N in leachate was measured in the manure plot while the lowest values were always observed in the S plot for both tillage systems (Table7). The influences of application of both straw and poultry manure on the concentration of NO3-N in leachate were different. Studies found that there were more subject to leaching from manure N sources than those from inorganic N sources and inverse for S treatment (Bergström and Kirchmann 1999; Thomsen 2005). The NO3-N concentration values of the leachate were relative lower under the CT than those of the NT (Table7). This may be related to reduced crop uptake of due to undeveloped crop roots in subsurface under NT conditions (Qin et al. 2004) and more coming from mineralization of organic N accumulated in soil surface of NT plots (Thomsen and SØrensen 2005).
Figure 2

The NO3-N concentration (mg L−1) in leachate from lysimeters under different treatments by collection date, November 2003 to October 2008. Error bars are the standard errors of the treatment means. Solid arrows denote urea application, and short dash dot arrows denote straw or manure application. The treatment details are the same as those in Figure1.

The n class="Chemical">NO3-N concen class="Chemical">ntration (mg L−1) in leachate from lysimeters under different treatmen class="Chemical">nts by collection date, November 2003 to October 2008. Error bars are the standard errors of the treatment means. Solid arrows denote urea application, and short dash dot arrows denote straw or manure application. The treatment details are the same as those in Figure1. There was significan class="Chemical">nt iclass="Chemical">pan> class="Chemical">nteraction between tillage and N management regimes on -N concentration in leachate (Table7). Flow-weighted average -N concentration (FWC) across the 5 years for CTS was the lowest with 9.6 mg/L across the 5-year rotation, which was lower than the EPA critical level of 10 mg/L, followed by NTS. FWC of NTM was the highest with 52.8 mg/L, followed by CTM treatment. n class="Chemical">Nitrate N leakage generally occurred after n class="Chemical">N fertilizer application following irrigation or/and rainfall during spring and summer in our experiment. There were only two episodes of n class="Chemical">nitrate N losses occurring from late autumn through overwinter months across 5 rotation years (Figs.2). Field observation in the NCP ever illustrated that no leaking occurred under the irrigation amount of 75 mm during winter wheat season assuming 1 m as the root zone (Yuan et al. 1995). n class="Chemical">N managemen class="Chemical">nt regimes had significant influences on n class="Chemical">-N leaching during all seasons (Tables9). The -N leaching for S treatments was relatively low, while the highest was found for treatments of M. Compared with U plots, the total amount of -N leaching from S treatments over 5 years was lower by 55.9% and greater by 85% for M treatments (Table7). It is understood that the C:N ratios of organic materials applied in field are the major factors determining the immobilization and subsequent mineralization and release of N in response to organic material inputs (Whitmore 1996). Generally, the C:N ratios > 30 are conducive to N immobilization and < 20 for net N mineralization. While the N input rate in three N management regimes was equal in our study, C input and the C:N ratios were different. The yearly total C input in S treatment was 14.2 Mg ha−1 with C:N ratios of 55.0 for wheat straw and 40.3 for maize straw. For M treatment, the yearly total C input was 6 Mg ha−1 with the C: N ratio of 13.5. Christensen (1985) reported N immobilization of 1–3 kg per Mg straw in straw application field. Murphy et al. (2000) found that both soluble organic and mineral N pools were smaller in the soil amended with maize residues (C:N = 108:1) due to immobilization. Poudel et al. (2002) reported high rates of N mineralization and increased soil microbial activity in manure application soil. Therefore, it is most likely to immobilize N and lower the level of nitrate leaching in S plots while there was high rate of N mineralization and leaching in M plots.
Table 9

Effect of tillage and nitrogen management regimes on cumulative leachate volumes (mm), -N leachate loss (kg -N ha−1) and flow-weighted average -N concentration (mg L−1) for 5 year

N regimes
TreatmentUSMMean
Leachate volumes (mm)
CT1615632615621
NT711724722719
Mean663678669
LSD0.05: tillage = 8; N regime = NS; tillage × N = NS.
Concentration (mg L−1)
CT23.39.643.725.6
NT29.313.052.831.7
Mean26.311.348.3
LSD0.05: tillage = 1.79; N regime = 1.09; tillage × N = 1.54.
NO3-N leaching (kg NO3-N ha−1)
CT143.960.7269.3157.9
NT208.294.8381.9228.3
Mean176.177.7325.7
LSD0.05: tillage = 12.9; N regime = 9.5; tillage × N = 13.5.

The treatment details are the same as those in Table3.

Effect of tillage and N management regimes on -N leaching (kg -N ha−1) during maize seasons. The treatmen class="Chemical">nt details are the same as those in Table3. Effect of tillage and nitrogen management regimes on cumulative leachate volumes (mm), -N leachate loss (kg -N ha−1) and flow-weighted average -N concentration (mg L−1) for 5 year The treatmen class="Chemical">nt details are the same as those in Table3. n class="Chemical">NT had significan class="Chemical">nt influences on -N leaching from the second year (Tables9). The total amoun class="Chemical">nt of -N leaching from NT system over 5 years was greater by 44.6% compared to that from CT system (Table7), which may be due to more percolate volumes and increased potential for transport of to groundwater under NT compared to CT (Bronick and Lal 2005). The n class="Chemical">tillage system and n class="Chemical">N management regimes interaction on leaching was significant (Tables9). From the second year, tillage systems interacted with N management regimes on -N loads for maize seasons (Table9). Interactive effect of tillage and N management regimes on -N leaching was also observed in 2007/2008 for wheat season. This was probably due to enhanced soil water percolation by adequate rainfall of 100.6 mm in April 2007 in comparison with the 44-year average of 34 mm in the same period (Fig.1). For the 5-year cumulative -N leaching, the highest losses were measured in the treatments NTM and CTM, followed by NTU and CTU, and then by NTS and CTS (Table7). As mentioned above, there were higher macropores and biochannels and more in the manure application soil under NT condition, which might cause more water and movement under NTM plots. Averagely, the leaching loss rates of N applied ranged from 2.5% (CTS) to 15.4% (NTM), which were lower than the average level of 19.1% derived from the values of 22% and 15% of applied N to wheat and maize systems worldwide (Zhou and Butterbach-Bahl 2014). In contrast to our results, some studies (Zavattaro et al. 2012; Zhou et al. 2014) reported that manure application and NT decreased -N leaching. They attributed the decreasing of -N leaching to increased immobilization of nitrogen under manure surface application and incorporation into soil and higher level of ammonia losses (30% of N applied) from surface applied urea under NT system. In our experiment, fertilizer including urea and manure or crop straw is surface applied, which decreased immobilization of nitrogen. Moreover, the ammonia loss rates are about 3–8% of N applied at the rates of 120–360 kg N ha−1 of urea (Wang et al. 2002) and 19.5% under poultry application at the rate of 24 Mg N ha−1 (Li et al. 2009). Therefore, surface application increased the amount of N sensitive to leaching loss from manure treatment in our experiment.

Yield-scaled basis NO3−-N leaching losses

n class="Chemical">Nitrogen managemen class="Chemical">nt regimes had significant influences on yield-scaled n class="Chemical">-N leaching during all seasons (Tables11). The values for S treatments were lowest, while the highest was found for the M treatment. NT significantly increased yield-scaled -N leaching losses from the second year and had interaction with N management regimes from 2006 to 2008 maize season (Table11).
Table 11

Effect of tillage and N management regimes on yield-scaled -N leaching (kg -N Mg−1 grain) during maize seasons.

N regimes
TreatmentUSMMean
2004
CT11.870.463.491.94
NT2.250.713.532.16
Mean2.060.583.51
LSD0.05: tillage = NS; N regime = 0.43; tillage × N = NS.
2005
CT4.812.526.194.51
NT6.243.759.226.41
Mean5.533.147.71
LSD0.05: tillage = 0.60; N regime = 0.91; tillage × N = NS.
2006
CT0.960.271.831.02
NT1.780.352.331.49
Mean1.370.312.08
LSD0.05: tillage = 0.15; N regime = 0.16; tillage × N = 0.22.
2007
CT3.040.556.673.41
NT4.341.2110.765.44
Mean3.690.888.81
LSD0.05: tillage = 0.63; N regime = 0.88; tillage × N = 1.24.
2008
CT2.480.823.712.34
NT3.721.445.963.71
Mean3.101.134.83
LSD0.05: tillage = 0.89; N regime = 0.40; tillage × N = 0.57.
2004–2008
CT2.690.994.392.69
NT3.751.596.233.86
Mean3.221.295.31
LSD0.05: tillage = 0.18; N regime = 0.18; tillage × N = 0.25.

The treatment details are the same as those in Table3.

Effect of tillage and N management regimes on yield-scaled -N leaching (kg -N Mg−1 grain) during winter wheat seasons. The treatmen class="Chemical">nt details are the same as those in Table3. Effect of tillage and N management regimes on yield-scaled -N leaching (kg -N Mg−1 grain) during maize seasons. The treatmen class="Chemical">nt details are the same as those in Table3. The yield-scaled -N leaching losses ranged from 0.08 to 12.8 kg n class="Chemical">N Mg−1 (mean: 2.78 kg N Mg−1) and 0.27 to 10.76 kg n class="Chemical">N Mg−1 (mean: 3.24 kg N Mg−1) for winter wheat and maize systems, respectively, which were within the scope of 0.3 to 15.1 kg N Mg−1 and 0.3 to 25.6 kg N Mg−1 for wheat and maize systems reported by Zhou et al. (2014). On average, the rather low values in CTS (0.08–2.53 kg N Mg−1, mean: 0.90 kg N Mg−1) and the rather higher values in NTM (3.05–12.80 kg N Mg−1, mean: 6.0 kg N Mg−1) were observed in winter wheat system. Similarly, the rather low levels in CTS (0.27–2.52 kg N Mg−1, mean: 0.92 kg N Mg−1) and the rather higher levels in NTM (2.33–10.76 kg N Mg−1, mean: 6.36 kg N Mg−1) in maize system were observed. Obviously, the yield-scaled -N leaching losses for CTS were lower than the value of 3.47 to 6.71 kg N Mg−1 for wheat system with N fertilization rate being in the ranges of > 250 kg N ha−1 and 2.82 to 6.18 kg N Mg−1 for maize system with N fertilization rate being in the ranges of 200 to 300 kg N ha−1 reported by Zhou et al. (2014). The n class="Chemical">tillage and n class="Chemical">N management regimes had markedly influences on the average yield-scaled -N leaching losses across 5 years (Tables11). Under winter wheat system, the average yield-scaled -N leaching losses for CTS were significantly lower compared to CTU, while the value for NTS was lower than that of CTU, but the difference was not significant. Under maize system, CTS and NTS significantly decreased the average yield-scaled -N leaching losses as compared to CTU. These showed that accepting yield losses of 0.7% for CTS and 2.4% for NTS compared to CTU would decrease the -N leaching losses per kg wheat yield to a certain extent. In the maize systems, both CTS and NTS not only decreased -N leaching losses but also maintained cumulative maize yields. The highest amoun class="Chemical">nt of yield-scaled n class="Chemical">nitrate leaching from the manure treatments could be attributed to high mineralization rate of organic N and mismatch between manure application and crop take-up in M treatments. These processes in the NCP are not clear, and further research is needed to assess factors influencing yield-scaled -N leaching from manure application in wheatmaize doubling system and to improve fertilization management. On the other hand, although organic source as poultry manure can still have environmental impact and caution needs to be taken, straw returned with decreased mineral N fertilizer treatment (CTS and NTS) is a promising alternative with regard to yield-scaled -N leaching while increasing soil organic matter inputs in wheatmaize double-cropping system. It is noteworthy that we discussed only the combined effen class="Chemical">cts of n class="Chemical">tillage systems and N management regimes on crop yields and yield-scaled -N leaching losses. Crop yield is one of the main financial components of farming. Farmers focus on the balance between costs and income. In recent years, fertilizers and land preparation have now become the higher direct cost in the winter wheat/maize double-cropping system in the NCP (Kang 2012). In spite of marginal reduction of wheat yield calculated as above, the decreased urea inputs (90 kg N ha−1 for winter wheat, 45 kg ha−1 for maize, respectively), together with the decreased costs of land preparation with no-tillage, make it feasible for farmers to implement the NTS and NTM treatments. Provided with significantly (P < 0.01) lower -N losses than those of the CTU treatment over the 5 years, the NTS treatment also proved to be a potential alternative of the CTU treatment which is currently the most common management practices in the NCP. Economic analysis is needed in further study.

Conclusions

This study demonstrated that the influence of n class="Chemical">tillage on crop yield depended onpan> crop type under the semihumid temperate climate of the n class="Chemical">NCP. The effect of n class="Chemical">tillage on maize crop yields was insignificant throughout the 5-year rotation, while NT decreased wheat grain yield only for 2 of 5 seasons. However, similar crop yields between nitrogen management regimes on winter wheat and maize crop yields for the 5 rotation years suggest that it may be possible to decrease the rates of urea application while sustaining crop grain yields by adopting S and M regimes in place of the U regime in the area studied. The n class="Chemical">tillage and n class="Chemical">N management regimes had significan class="Chemical">nt effect on the yield-scaled -N leaching losses with CTS and NTS being lowest and NTM and CTM being highest in wheat and maize system, respectively. Thus, CTS minimized -N leaching without losing production compared to CTU, and NTS may be a potential alternative to decrease yield-scaled -N leaching losses but not lower crop yield for the wheatmaize double-cropping systems in the NCP.
Table 5

Effect of tillage and nitrogen management regimes on leachate volumes (mm) during winter wheat seasons.

N regimes
TreatmentUSMMean
2003–2004
CT130.6b231.2b28.8b30.2
NT30.7c30.4c30.9b30.7
Mean30.730.829.9
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2004–2005
CT30.8b30.9b28.5b30.1
NT32.6b31.7bc32.4b32.2
Mean31.631.330.5
LSD0.05: tillage = NS; N regime = NS; tillage × N = NS.
2005–2006
CT57.1a56.3a54.1a55.8
NT61.2a62.3a63.2a62.2
Mean59.159.358.7
LSD0.05: tillage = 2.8; N regime = NS; tillage × N = NS.
2006–2007
CT17.7c20.7c24.5b21
NT33.2b34.1b32.9b33.5
Mean25.527.428.8
LSD0.05: tillage = 3.2; N regime = NS; tillage × N = NS.
2007–2008
CT53.1a58.7a56.6a56.1
NT63.8a63.4a63.9a63.7
Mean58.461.160.2
LSD0.05: tillage = 5.2; N regime = NS; tillage × N = NS.

The treatment details are the same as those in Table3.

For the same treatment within a column, different letters indicate significant difference between years at P < 0.05.

Table 8

Effect of tillage and N management regimes on -N leaching (kg -N ha−1) during maize seasons.

N regimes
TreatmentUSMMean
2004
CT113.43.42413.6
NT15.15.326.515.6
Mean14.24.425.3
LSD0.05: tillage = NS; N regime = 2.3; tillage × N = NS.
2005
CT39.020.952.937.6
NT51.532.176.653.4
Mean45.326.564.7
LSD0.05: tillage = 3.7; N regime = 3.9; tillage × N = 5.5.
2006
CT6.31.612.26.7
NT11.82.316.510.2
Mean9.02.014.3
LSD0.05: tillage = 1.1; N regime = 1.7; tillage × N = 2.4.
2007
CT18.83.239.620.5
NT27.97.361.732.3
Mean23.45.250.7
LSD0.05: tillage = 8.6; N regime = 4.3; tillage × N = 6.1.
2008
CT19728.518.2
NT29.812.446.329.5
Mean24.49.737.4
LSD0.05: tillage = 4.2; N regime = 1.2; tillage × N = 1.7.

The treatment details are the same as those in Table3.

Table 10

Effect of tillage and N management regimes on yield-scaled -N leaching (kg -N Mg−1 grain) during winter wheat seasons.

N regimes
TreatmentUSMMean
2003–2004
CT10.780.442.141.12
NT1.000.713.351.69
Mean0.890.582.74
LSD0.05: tillage = NS; N regime = 0.54; tillage × N = NS.
2004–2005
CT0.530.232.341.03
NT0.710.333.051.36
Mean0.620.282.69
LSD0.05: tillage = 0.6; N regime = 0.36; tillage × N = NS.
2005–2006
CT4.692.539.085.43
NT6.643.8712.807.77
Mean5.663.2010.94
LSD0.05: tillage = 0.76; N regime = 1.01; tillage × N = NS.
2006–2007
CT0.340.081.310.58
NT0.920.333.211.49
Mean0.630.202.26
LSD0.05: tillage = 0.63; N regime = 0.59; tillage × N = 0.83.
2007–2008
CT2.011.235.202.81
NT4.311.737.614.55
Mean3.161.486.41
LSD0.05: tillage = 2.17; N regime = 0.73; tillage × N = 1.03.
2003–2008
CT1.650.884.012.18
NT2.741.406.073.40
Mean2.191.145.04
LSD0.05: tillage = 0.63; N regime = 0.30; tillage × N = 0.42.

The treatment details are the same as those in Table3.

  2 in total

1.  Nitrogen balance and groundwater nitrate contamination: comparison among three intensive cropping systems on the North China Plain.

Authors:  X T Ju; C L Kou; F S Zhang; P Christie
Journal:  Environ Pollut       Date:  2005-12-20       Impact factor: 8.071

2.  Nitrate leaching, direct and indirect nitrous oxide fluxes from sloping cropland in the purple soil area, southwestern China.

Authors:  Minghua Zhou; Bo Zhu; Klaus Butterbach-Bahl; Tao Wang; Jessica Bergmann; Nicolas Brüggemann; Zhenhua Wang; Taikui Li; Fuhong Kuang
Journal:  Environ Pollut       Date:  2011-12-23       Impact factor: 8.071

  2 in total

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