# Influence of Controlled Drainage on the Groundwater Nitrogen and Phosphorus Concentration at Jointing-Booting Stage of Wheat

Authors: Jin-tao Cui; Guang-cheng Shao; Shuang-en Yu; Xi Cheng
Journal: Journal of Chemistry
 (2016)

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## Abstract

The effect of controlled drainage on nitrogen (N) and phosphorus (P) emission at jointing-booting stage of winter wheat was studied in 2007-2008. The conventional subsurface drainage was taken as the control (T5). The groundwater depth was naturally drained to 400 mm and 800 mm below the soil surface within 3 days at the jointing-booting stage, after the water level was kept at 100 mm for 1 day (T1, T2) and 3 days (T3, T4) from the soil surface. Results showed that controlled drainage could significantly reduce the concentration of P and N in groundwater. Compared to T5, the four controlled treatments could significantly decrease the concentration of TP,N
H
4
+-N, and N
O
3
--N. The highest concentration reduction for TP and N
O
3
--N was observed under T4 and T1, which reached 64.9% and 73.2%, respectively. As for the concentration of N
H
4
+-N, the highest reduction was obtained under T2. The change of TP concentration was significantly affected by the interaction of submergence time and drain depth, while the influence of controlled drainage on N
H
4
+-N concentration was not significant. The submergence time, drain depth, and the interaction of submergence time and drain depth had significant effect on the change of concentration of N
O
3
--N.


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## Body

## 1. Introduction

Since the irrational irrigation and drainage and excessive fertilization on the farmland, large amounts of nitrogen and phosphorus had been lost from farmland by ways of runoff and leakage. This is an important reason for the eutrophication of water body in recent years [1–4]. In southern China, winter wheat often receives high amount of N fertilizer which combined with shallow root system and drainage poses a high risk of N leaching losses. High N leaching losses from wheat have been reported in several studies from China [5]. The soils used for winter wheat in southern China show low P sorption capacity and shallow groundwater level; P leaching losses from wheat may also be high. Drainage is an important measure to allow timely field operation and protect wheat field from waterlogging. However, irrational drainage shortens the residence time of water in the biologically active unsaturated zone and substantially alters the water regime. Attempts to reduce nutrient losses in drainage water have led to the development of controlled drainage (CD). Controlled drainage aimed to maintain a higher depth of water and captured more drainage water than traditional drainage in the field [6, 7]. Results showed that controlled drainage could reduce drainage quantity [8]. Moreover, the concentration of N and P in drainage water could be decreased, especially in surface runoff. These studies further stressed the importance of controlled drainage in decreasing the loss of N and P from field [9, 10]. Yin et al. [11–13] showed that surface controlled drainage measures could effectively reduce the concentration of nitrogen in the drainage and the drainage outflow volumes. At the same time, the multiobjective controlled drainage model was developed for storm drainage and reducing nitrogen and phosphorus loss [14]. Qiao et al. [15] showed that, under shallow-irrigation and deep-sluice model, the drainage flow of controlled drainage decreases 7.6% compared with uncontrolled drainage. Wesström and Messing [10] reported 79% and 94% reductions in drain outflows for successive years following controlled drainage implementation. Field experiment and modeling with DRAINMOD by Wang et al. [16] showed that the proposed model was effective for predicting the surface runoff, subsurface drainage, and nitrate loss.The researches on the changes of N and P concentration in groundwater of wheat field which focus on the whole growth period have been reported frequently [17–19]. However, as for one growth stage, especially the jointing-booting stage, which is a critical period of wheat growth, the related research is rare. Here, we presented field measurements of N and P from the groundwater of wheat field under controlled drainage in southern China in 2007-2008. The main objective is to gain an insight into the concentration of P and N change under controlled drainage at the jointing-booting stage. Besides, controlled drainage whether to further take advantage of the interactive effect of submergence duration combined with drainage depth should be confirmed and further studied. Therefore, this study can provide basis for reasonable drainage scheme about winter wheat field and an effective option for mitigating environmental pollution.


## 2. Materials and Methods

### 2.1. Experimental Site and the Soil Properties

The experiment was carried out in specially designed experimental tanks at the Key Laboratory of Efficient Irrigation-Drainage and Agricultural Soil-Water Environment in Southern China, Ministry of Education (31°57′N, 118°50′E), during the winter wheat growing seasons of 2007-2008. The study area has a subtropical monsoon climate with average annual air temperature of 15.4°C and mean annual evaporation of 900 mm. The average annual precipitation is 1,051 mm, where more than 60% of precipitation falls in the rainy season and the precipitation is concentrated in the months of May–September. The frost-free period is 220 days per year.There were 15 fixed tanks, and each of them was 2 m wide, 2.5 m long, and 2 m high container constructed from concrete block and sealed with a waterproof paint. Figure1 was the schematic diagram of a setup for maintaining ponding water depth. Groundwater level was changed by raising or lowering the height of the finger of electromagnetic valve relative to the bottom of each tank. When ponding water depth lowered to lower limit of designed water level, irrigation water was added until water table reached upper limit of designed water level with autoirrigation system (vice versa).Figure 1
Schematic diagram of the experimental setup placed in the tank.The soil texture of the experimental tanks in the plowed layer was clay, with pH value of 7.78, organic matter of 2.40%, total phosphorus of 0.32 g·kg−1, available phosphorus of 53.63 mg·kg−1, total nitrogen of 0.67 g·kg−1, and available nitrogen of 12.5 mg·kg−1. The saturated soil water contents (m·m−1) for the layer of 0–30 cm were 30.4%, and field water-holding rate was 26.5%.


### 2.2. Experimental Design and Management

Five treatments were used to evaluate the effect of controlled drainage at jointing-booting stage on the change of N and P concentration, as shown in Table1. The control (T5) was the conventional subsurface drainage, where the relative soil water content was maintained at 70–80% and the groundwater level was kept below −600 mm at the tillering stage, −800 mm at the jointing-booting stage, and −1,000 mm at the onset of flowering. The water depth of control treatments was kept 100 mm from the soil surface at other treatments. The water layer above the soil was maintained for 1 day, and then it was drained to −400 mm (T1) and −800 mm (T2) below the surface within 3 days at the jointing-booting stage. The water layer above the soil was maintained for 3 days, and then it was drained to −400 mm (T3) and −800 mm (T4) below the surface within 3 days at the jointing-booting stage. Except at the jointing-booting stage, the water level of treatments was the same as T5 at other growth stages. These treatments were arranged in a randomized complete block design with three replications and means were compared with a Least Squares Means procedure.Table 1
Design of controlled drainage scheduling.
Treatments
Tillering stage/mm
Jointing-booting stage
Panicle initiation stage/mm
Milky stage/mm
T1
≤−600
100 mm (1 d) (3 d-400)
≤−1000
≤−1000
T2
≤−600
100 mm (1 d) (3 d-800)
≤−1000
≤−1000
T3
≤−600
100 mm (3 d) (3 d-400)
≤−1000
≤−1000
T4
≤−600
100 mm (3 d) (3 d-800)
≤−1000
≤−1000
T5
≤−600
≤−800
≤−1000
≤−1000
Note:I mm(K d) (M d −J mm): I mm fixed water level was kept with duration of K day at Jointing-booting stages from the soil surface and drained to −J mm in M days. <−N mm: −N mm was the upper limit of groundwater level, if groundwater level exceeded the value and drainage would be conducted. T1, T2, T3, and T4 denote different controlled treatments at jointing-booting stage; T5 as the control indicates conventional subsurface drainage.Yangmai 14, hybrid wheat currently used in local production, was grown in the experiment tanks at the rate of 150 kg·ha−1 on 12 November in 2007. Applications of fertilizer (N : P2O5 : K2O, 15 : 10 : 15) at the rate of 1500 kg·ha−1 in the form of compound fertilizer were applied in tanks evenly. Each treatment includes the same agronomic measures except irrigation and drainage.According to the growth characteristics of winter wheat and combined with observations of physiological and ecological in the testing process, the growth stages of wheat were divided into four stages (Table2).Table 2
Division of growth stages of winter wheat in 2007-2008.
Stages
Tillering stage
Jointing-booting stage
Panicle initiation stage
Milky stage
Starting date
February 11
March 26
April 17
May 1
End date
March 25
April 16
April 30
May 25


### 2.3. Sample Collection and Measurement

Water treatment was started on April 3 in 2008. During the controlled drainage period, water samples were collected in the polyethylene bottle for four times, at the beginning and end of the submergence and drainage. The subsurface water was collected by the underground drainage pipe. The sampled water was analyzed for total phosphorus (TP), ammonium nitrogen (N
H
4
+-N), and nitrate nitrogen (N
O
3
--N) through the use of a Shimadzu UV-2800 spectrophotometer. Spectrophotometric determination of molybdenum and antimony with potassium sulfa was used to measure the concentration of total phosphorus (TP). In addition, spectrophotometric determination of the reagent of flocculation and precipitation and the ultraviolet spectrophotometry were used to analyze ammonium nitrogen (N
H
4
+-N) and nitrate nitrogen (N
O
3
--N) content in water test, respectively.


### 2.4. Statistical Analysis

Data were analyzed using multivariate analysis of variance (MANOVA) procedure of SPSS software Version 22.0. Treatment means were separated by least significant difference (LSD) test at the 0.05 probability level.


## 2.1. Experimental Site and the Soil Properties

The experiment was carried out in specially designed experimental tanks at the Key Laboratory of Efficient Irrigation-Drainage and Agricultural Soil-Water Environment in Southern China, Ministry of Education (31°57′N, 118°50′E), during the winter wheat growing seasons of 2007-2008. The study area has a subtropical monsoon climate with average annual air temperature of 15.4°C and mean annual evaporation of 900 mm. The average annual precipitation is 1,051 mm, where more than 60% of precipitation falls in the rainy season and the precipitation is concentrated in the months of May–September. The frost-free period is 220 days per year.There were 15 fixed tanks, and each of them was 2 m wide, 2.5 m long, and 2 m high container constructed from concrete block and sealed with a waterproof paint. Figure1 was the schematic diagram of a setup for maintaining ponding water depth. Groundwater level was changed by raising or lowering the height of the finger of electromagnetic valve relative to the bottom of each tank. When ponding water depth lowered to lower limit of designed water level, irrigation water was added until water table reached upper limit of designed water level with autoirrigation system (vice versa).Figure 1
Schematic diagram of the experimental setup placed in the tank.The soil texture of the experimental tanks in the plowed layer was clay, with pH value of 7.78, organic matter of 2.40%, total phosphorus of 0.32 g·kg−1, available phosphorus of 53.63 mg·kg−1, total nitrogen of 0.67 g·kg−1, and available nitrogen of 12.5 mg·kg−1. The saturated soil water contents (m·m−1) for the layer of 0–30 cm were 30.4%, and field water-holding rate was 26.5%.


## 2.2. Experimental Design and Management

Five treatments were used to evaluate the effect of controlled drainage at jointing-booting stage on the change of N and P concentration, as shown in Table1. The control (T5) was the conventional subsurface drainage, where the relative soil water content was maintained at 70–80% and the groundwater level was kept below −600 mm at the tillering stage, −800 mm at the jointing-booting stage, and −1,000 mm at the onset of flowering. The water depth of control treatments was kept 100 mm from the soil surface at other treatments. The water layer above the soil was maintained for 1 day, and then it was drained to −400 mm (T1) and −800 mm (T2) below the surface within 3 days at the jointing-booting stage. The water layer above the soil was maintained for 3 days, and then it was drained to −400 mm (T3) and −800 mm (T4) below the surface within 3 days at the jointing-booting stage. Except at the jointing-booting stage, the water level of treatments was the same as T5 at other growth stages. These treatments were arranged in a randomized complete block design with three replications and means were compared with a Least Squares Means procedure.Table 1
Design of controlled drainage scheduling.
Treatments
Tillering stage/mm
Jointing-booting stage
Panicle initiation stage/mm
Milky stage/mm
T1
≤−600
100 mm (1 d) (3 d-400)
≤−1000
≤−1000
T2
≤−600
100 mm (1 d) (3 d-800)
≤−1000
≤−1000
T3
≤−600
100 mm (3 d) (3 d-400)
≤−1000
≤−1000
T4
≤−600
100 mm (3 d) (3 d-800)
≤−1000
≤−1000
T5
≤−600
≤−800
≤−1000
≤−1000
Note:I mm(K d) (M d −J mm): I mm fixed water level was kept with duration of K day at Jointing-booting stages from the soil surface and drained to −J mm in M days. <−N mm: −N mm was the upper limit of groundwater level, if groundwater level exceeded the value and drainage would be conducted. T1, T2, T3, and T4 denote different controlled treatments at jointing-booting stage; T5 as the control indicates conventional subsurface drainage.Yangmai 14, hybrid wheat currently used in local production, was grown in the experiment tanks at the rate of 150 kg·ha−1 on 12 November in 2007. Applications of fertilizer (N : P2O5 : K2O, 15 : 10 : 15) at the rate of 1500 kg·ha−1 in the form of compound fertilizer were applied in tanks evenly. Each treatment includes the same agronomic measures except irrigation and drainage.According to the growth characteristics of winter wheat and combined with observations of physiological and ecological in the testing process, the growth stages of wheat were divided into four stages (Table2).Table 2
Division of growth stages of winter wheat in 2007-2008.
Stages
Tillering stage
Jointing-booting stage
Panicle initiation stage
Milky stage
Starting date
February 11
March 26
April 17
May 1
End date
March 25
April 16
April 30
May 25


## 2.3. Sample Collection and Measurement

Water treatment was started on April 3 in 2008. During the controlled drainage period, water samples were collected in the polyethylene bottle for four times, at the beginning and end of the submergence and drainage. The subsurface water was collected by the underground drainage pipe. The sampled water was analyzed for total phosphorus (TP), ammonium nitrogen (N
H
4
+-N), and nitrate nitrogen (N
O
3
--N) through the use of a Shimadzu UV-2800 spectrophotometer. Spectrophotometric determination of molybdenum and antimony with potassium sulfa was used to measure the concentration of total phosphorus (TP). In addition, spectrophotometric determination of the reagent of flocculation and precipitation and the ultraviolet spectrophotometry were used to analyze ammonium nitrogen (N
H
4
+-N) and nitrate nitrogen (N
O
3
--N) content in water test, respectively.


## 2.4. Statistical Analysis

Data were analyzed using multivariate analysis of variance (MANOVA) procedure of SPSS software Version 22.0. Treatment means were separated by least significant difference (LSD) test at the 0.05 probability level.


## 3. Results

### 3.1. The Change of Concentration of TP

Compared to T5, the CD treatments had significant impacts on the change of the concentration of TP (p
≤
0.05). The reduction of concentration of TP under T4 registered the highest percentage (64.9%), while the lowest (4.6%) was T5 (Figure 2). The average change of TP concentration under T1 and T3 (37.2%) was closed to the average value under T2 and T4 (39.5%). Similarly, compared with the average change value of T1 and T2, the average value of T3 and T4 was high 9%. Furthermore, although the same fixed water level under T1 and T2 was kept for same day, the change of concentration of TP under T1 was almost 400% higher than T2 due to different drainage depth, and the concentration change decreased as the depth increases. On the contrary, the change of percentage increased as the depth increases under T3 and T4. The MANOVA indicated submergence duration and drainage depth had insignificant effect on the change of concentration of total phosphorus; however, the interaction of submergence duration and drainage depth had significant effect (Table 3).Table 3
MANOVA results for the change of concentration of TP,N
H
4
+-N, and N
O
3
--N.
MANOVA results (p values)
TP
N
H
4
+-N
N
O
3
--N
Submergence time
0.073 ns
0.008∗
0.028∗
Drainage depth
0.092 ns
0.000∗
0.002∗
Submergence time × drainage depth
0.000∗
0.354 ns
0.000∗
Note: the values of TP,N
H
4
+-N, and N
O
3
--N concentration are means of 3 replications. Significant differences for submergence duration, drainage depth, and submergence duration × drainage depth are indicated with asterisks (∗) for α
<
0.05; ns: not significant.Figure 2
The change of the concentration of TP under controlled drainage at jointing-booting stage. The initial and final concentrations are the TP concentration in groundwater at the beginning of submergence and end of drainage, respectively. Vertical bars represent ± standard error (SE) of the mean.


### 3.2. The Change of Concentration ofN
H
4
+-N

Figure3 showed the change of concentration of N
H
4
+-N from the beginning to the end of five treatments. Submergence duration and drainage depth both had significant effect on the change of concentration of N
H
4
+-N (Table 3). Compared with the control, CD treatments had significant impacts on the concentration of N
H
4
+-N (p
≤
0.05). The N
H
4
+-N concentration for T1, T2, T3, T4, and T5 was reduced by 12.9%, 23.1%, 8.1%, 20.6%, and 2.9%, respectively. Table 3 indicated that the interaction between submergence duration and drainage depth did not significantly affect the change of the concentration of N
H
4
+-N (p
≤
0.05).Figure 3
The change of the concentration ofN
H
4
+-N under controlled drainage at jointing-booting stage. The initial and final concentrations are the N
H
4
+-N concentration in groundwater at the beginning of submergence and end of drainage, respectively. Vertical bars represent ± standard error (SE) of the mean.


### 3.3. The Change of Concentration ofN
O
3
--N

The change of the concentration of theN
O
3
--N in groundwater under CD treatments was shown in Figure 4. The concentration of N
O
3
--N under CD treatments declined after submergence. There are significant differences between CD treatments and the control for the decreased percentage of concentration of the N
O
3
--N. It indicated that the combination of submergence duration and drainage depth both had a significant effect on the concentration of the N
O
3
--N (p
≤
0.05). The decreased percentage of the concentration N
O
3
--N under T1 reached the maximum (73.2%) among five treatments, while the smallest decreased percentage (31.6%) was obtained under T3. As was seen from Table 3, submergence duration, drainage depth, and the interaction between submergence duration and drainage depth had significant influence on the change of concentration of N
O
3
--N.Figure 4
The change of the concentration ofN
O
3
--N under controlled drainage at jointing-booting stage. The initial and final concentrations are the N
O
3
--N concentration in groundwater at the beginning of submergence and end of drainage, respectively. Vertical bars represent ± standard error (SE) of the mean.


## 3.1. The Change of Concentration of TP

Compared to T5, the CD treatments had significant impacts on the change of the concentration of TP (p
≤
0.05). The reduction of concentration of TP under T4 registered the highest percentage (64.9%), while the lowest (4.6%) was T5 (Figure 2). The average change of TP concentration under T1 and T3 (37.2%) was closed to the average value under T2 and T4 (39.5%). Similarly, compared with the average change value of T1 and T2, the average value of T3 and T4 was high 9%. Furthermore, although the same fixed water level under T1 and T2 was kept for same day, the change of concentration of TP under T1 was almost 400% higher than T2 due to different drainage depth, and the concentration change decreased as the depth increases. On the contrary, the change of percentage increased as the depth increases under T3 and T4. The MANOVA indicated submergence duration and drainage depth had insignificant effect on the change of concentration of total phosphorus; however, the interaction of submergence duration and drainage depth had significant effect (Table 3).Table 3
MANOVA results for the change of concentration of TP,N
H
4
+-N, and N
O
3
--N.
MANOVA results (p values)
TP
N
H
4
+-N
N
O
3
--N
Submergence time
0.073 ns
0.008∗
0.028∗
Drainage depth
0.092 ns
0.000∗
0.002∗
Submergence time × drainage depth
0.000∗
0.354 ns
0.000∗
Note: the values of TP,N
H
4
+-N, and N
O
3
--N concentration are means of 3 replications. Significant differences for submergence duration, drainage depth, and submergence duration × drainage depth are indicated with asterisks (∗) for α
<
0.05; ns: not significant.Figure 2
The change of the concentration of TP under controlled drainage at jointing-booting stage. The initial and final concentrations are the TP concentration in groundwater at the beginning of submergence and end of drainage, respectively. Vertical bars represent ± standard error (SE) of the mean.


## 3.2. The Change of Concentration ofN
H
4
+-N

Figure3 showed the change of concentration of N
H
4
+-N from the beginning to the end of five treatments. Submergence duration and drainage depth both had significant effect on the change of concentration of N
H
4
+-N (Table 3). Compared with the control, CD treatments had significant impacts on the concentration of N
H
4
+-N (p
≤
0.05). The N
H
4
+-N concentration for T1, T2, T3, T4, and T5 was reduced by 12.9%, 23.1%, 8.1%, 20.6%, and 2.9%, respectively. Table 3 indicated that the interaction between submergence duration and drainage depth did not significantly affect the change of the concentration of N
H
4
+-N (p
≤
0.05).Figure 3
The change of the concentration ofN
H
4
+-N under controlled drainage at jointing-booting stage. The initial and final concentrations are the N
H
4
+-N concentration in groundwater at the beginning of submergence and end of drainage, respectively. Vertical bars represent ± standard error (SE) of the mean.


## 3.3. The Change of Concentration ofN
O
3
--N

The change of the concentration of theN
O
3
--N in groundwater under CD treatments was shown in Figure 4. The concentration of N
O
3
--N under CD treatments declined after submergence. There are significant differences between CD treatments and the control for the decreased percentage of concentration of the N
O
3
--N. It indicated that the combination of submergence duration and drainage depth both had a significant effect on the concentration of the N
O
3
--N (p
≤
0.05). The decreased percentage of the concentration N
O
3
--N under T1 reached the maximum (73.2%) among five treatments, while the smallest decreased percentage (31.6%) was obtained under T3. As was seen from Table 3, submergence duration, drainage depth, and the interaction between submergence duration and drainage depth had significant influence on the change of concentration of N
O
3
--N.Figure 4
The change of the concentration ofN
O
3
--N under controlled drainage at jointing-booting stage. The initial and final concentrations are the N
O
3
--N concentration in groundwater at the beginning of submergence and end of drainage, respectively. Vertical bars represent ± standard error (SE) of the mean.


## 4. Discussion

The jointing-booting stage was a key period during the period of winter wheat growth, because the dry matter accumulation mainly occurred at this stage [20, 21]. The vegetative and reproductive growth of wheat developed simultaneously, and then physiological metabolism was rapid at this stage, which led to the great demand for nitrogen and phosphorus. In this experiment, the concentration of N and P in underground water was obviously decreased by controlled treatments at jointing-booting stage. The decrease of TP concentration in groundwater was mainly through the fixation of soil particles and the absorption of wheat during the submergence [22]. The absorption was affected by submergence duration and the groundwater depth, which led to the reduction of TP concentration among the controlled treatments. This was consistent with the research of Yin et al. [23], in which the TP concentration in groundwater was significantly decreased by almost 50% under the condition of controlled drainage.The major nitrogen treatment mechanisms of wheat included sedimentation, chemical adsorption, microbial interactions with nitrogen, and plant uptake [24–27]. The sedimentation and chemical adsorption were both dependent on duration and soil style. As for the microorganisms, the biological nitrogen transition included a two-opposite process: nitrification and denitrification. Nitrification implied a chemolithoautotrophic oxidation of ammonia to nitrate under strict aerobic conditions. The nitrification process highly demanded oxygen. Under controlled drainage condition, the biological denitrification mechanism made use of nitrate as the terminal electron acceptor in low-oxygen environments [28]. This led to the result that the change of concentration of N
O
3
--N was higher than that of N
H
4
+-N. As was shown in Figures 3 and 4, N
H
4
+-N was the major component of N in runoff water after submergence. Similarly, Shao et al. [27] also found that the concentration of N
H
4
+-N was more than six times as much as N
O
3
--N during the submergence.The growth condition of wheat was an important factor in the reduction of nitrogen in groundwater. The winter wheat was more influenced byN
O
3
--N than N
H
4
+-N [29], which was another reason why the concentration of N
O
3
--N was lower than that of N
H
4
+-N. When shorter duration of submergence was kept, the concentration of N
H
4
+-N and N
O
3
--N tended to favor salient reduction. This was because of the stronger root respiration which affected the absorption and utilization of nutrients [30, 31]. This also explained why the emission reduction was lower under T3 than the other CD treatments. Similar results were also reported under the controlled drainage condition in southern China [32].This study only investigated the change of TP,N
H
4
+-N, and N
O
3
--N concentration at joint booting stage of wheat, under the controlled drainage treatments. It did not investigate the effect of controlled drainage on the amount of water discharge and concentration varying with time after submergence withdrawal. More research needs to be carried out in the future to define these relationships.


## 5. Conclusion

In southern China, traditional drainage might be considered as an efficient mean to rapidly eliminate excess water on the farmland. Nevertheless, this treatment might lead to large amounts of nitrogen and phosphorus loss from farmland and exacerbating water eutrophication. Controlled drainage as an effective drainage method could significantly reduce the concentration of nitrate-nitrogen, ammonium nitrogen, and total phosphorus in groundwater wheat field. Compared with the conventional subsurface drainage, controlled drainage reduced highest the concentration of TP,N
H
4
+-N, and N
O
3
--N losses in groundwater by 64.9% (T4), 23.1% (T2), and 73.2% (T1), respectively. Results of MAOVA for the change of TP concentration showed that the interaction of submergence time and drain depth was significant, while the influence of controlled drainage on N
H
4
+-N concentration was not significant. The submergence time, drain depth, and the interaction of submergence time and drain depth had significant effect on the change of concentration of N
O
3
--N. Therefore, the intensity of controlled drainage must be considered particularly, including submergence duration and drainage depth, in order to obtain the greater reduction effect and the normal growth of wheat at the later stage.



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*Source: 5280194-2016-08-18.xml*