# The Effects of Controlled Drainage on N Concentration and Loss in Paddy Field

Authors: Bin Lu; Guangcheng Shao; Shuang’en Yu; Shiqiang Wu; Xinghua Xie
Journal: Journal of Chemistry
 (2016)

---

## Abstract

To relieve the situation of the agricultural nonpoint pollution (NPS) in south and east China, paddy field controlled drainage (PFCD) is applied as an important and efficient approach to agricultural water management. A series of PFCD tests at four major growth stages of rice were conducted by use of 18 lysimeters. Concentration of ammonia nitrogen (N
H
4
+-N) and nitrate nitrogen (N
O
3
--N) in surface and subsurface paddy water was observed. The results indicated that the concentration of N
H
4
+-N and N
O
3
--N in paddy water declined with the persistence of a waterlogged condition. Compared to traditional drainage, PFCD reduced N loss in surface water by 95.6%, 78.7%, 59.6%, and 87.4% at the stage of tillering, jointing-booting, heading-flowering, and milking, respectively. It should be noted that loads of N losses in surface water increased on the fourth day after waterlogging at the jointing-booting and milking stage, and surface water exhibited higher N concentration on the first day after waterlogging at each stage. Therefore, paddy field surface water drainage should be avoided in these periods.


---

## Body

## 1. Introduction

Field drainage is widely known as an essential measure to ensure that crops achieve high and steady production. However, unreasonable field irrigation and drainage management present several problems as well. For example, excess drainage leads to the mass flow of agriculture pollution into rivers and lakes. Furthermore, nitrogen (N) and phosphorus (P) runoff and drainage from paddy fields are major sources of nonpoint source pollution (NPS) in south and east China [1–3]. In several major lakes such as Taihu Lake, Dianchi Lake, and Chaohu Lake, eutrophication has become increasingly severe [4–7]. With regard to problems of water shortage and water environment deterioration, controlled drainage (CD) has been identified as an efficient approach to agricultural water management in humid and arid regions [8–10].Paddy field controlled drainage (PFCD) is a highly efficient drainage pattern that uses the institution of outfall to control field water discharge and elevate the level of farm ditch, as well as achieving water saving and pollution reduction [11, 12]. This pattern is different from the conventional pattern of paddy field drainage. Industry practice shows that paddy fields can retard and store floodwater during major flood periods. Furthermore, paddy fields not only save irrigation water and improve the utilization of rainwater but also alleviate the region pressure of flood protection [10, 11].Controlled drainage, which is also called drainage water management (DWM), has been used for several years in North Carolina, Florida, and other locations [9, 13]. In the controlled drainage situation, the flow lines are shallower than in the uncontrolled system, and the water table is maintained at a shallower depth by a control structure which reduces deep percolation below the root zone by reducing hydraulic gradients and increases capillary upflow as evapotranspiration depletes soil water in the root zone [8]. Numerous studies have shown that CD could reduce annual transport of total N in the field by 40%–50% and total P by 35%–45% [14–17]. Annual CD could reduce approximately 30%–60% of water volume compared with conventional drainage [18–20]. One the one hand, CD can reduce total leaching rate from less water drainage; on the other hand, the rise of subsurface water level can prompt soil denitrification, which then decreases the concentration of nitrate nitrogen.The PFCD technology was discovered by Chinese scholars in the 1990s, and several experimental studies and field practices have been conducted constantly in rice-planting regions. Zhang et al. [21] studied the transport and loss of nitrogen in a drainage paddy field. Luo et al. [22] and Jia et al. [23] conducted field experiments on the effects of drainage control on salt and water balance in the Yinnan irrigation district. Xiao et al. [24, 25] examined the changes in N and P of flooded paddy water systems and obtained the optimal drainage time at each stage of growth. All the results concluded that PFCD plays a significant role in water conservation and nonpoint source pollution reduction.Two important factors for PFCD are surface water level and waterlogging duration. When the paddy surface water level is too deep or when the duration of waterlogging is too long, a waterlogged disaster can occur, which may then cause plant growth retardation and yield reduction. On the contrary, pollution reduction and water conservation cannot be achieved when waterlogging duration is too short. To achieve comprehensive benefits from environment and economic resources, we must assess surface water depth, flooding time, leakage intensity, and other factors [26, 27].This study emphasized the environmental benefits of deliberate water resources utilization. The paper showed dynamic changes in N concentration in surface and subsurface paddy water, analyzed the effects of leakage intensity and N leaching, calculated loads of N losses through surface drainage, and demonstrated the effects of pollution reduction and water saving through PFCD.


## 2. Materials and Methods

### 2.1. Experimental Site

This study was conducted in an experimental field at water-saving and agroecological experimental plot located in Jiangning Campus of Hohai University, Jiangsu Province of China (Nanjing, latitude 31°57′N, longitude 118°50′E, 144 m above sea level). The region has a subtropical humid monsoon climate zone, with an average annual evaporation of 900 mm and yearly average temperature of 15.7°C, and the maximum and minimum air temperatures are 43.0°C and −14.0°C, respectively. The mean annual rainfall is 1021 mm of which more than 60% of precipitation falls in the rainy season and the precipitation is concentrated in May to September. The number of frost-free days is 237 per year. The temperature, precipitation, and evaporation were recorded daily by an automatic weather station (ICT, Australia) in the experimental plot.The area has been 5 years of rice-wheat rotation system. The soil in the area is a typical permeable paddy soil. The topsoil was 0–30 cm in lysimeter with pH value of 6.97, soil bulk density was 1.46 g/cm3, soil porosity was 44.97%, and field capacity was 25.28%. Characteristics of topsoil are shown in Table 1. There are 32 fixed lysimeter test-pits (28 with closed concrete bottom, 4 without bottom) with specifications for the length × width × depth = 2.5 m × 2 m × 2 m in the experimental field. Those lysimeters layouts were divided into two groups of 16 each. We only employed 18 of them in this research, shown in Figure 1(a). Underground gallery and drainage system are built between the two groups, and a mobile canopy is equipped on the ground.Table 1
Physical and chemical characteristics of topsoil (0–30 cm layer) in lysimeters.
θ
n
ρ
b
Porosity
pH
Organic matter
Total N
Available N
Total P
Available P
(%)
(g/cm3)
(%)
(—)
(g/kg)
(g/kg)
(mg/kg)
(g/kg)
(mg/kg)
25.28
1.46
44.97
6.97
21.88
0.9048
27.65
0.32
12.5
Note:θ
n and ρ
b represent field moisture capacity and soil bulk density, respectively.Figure 1
(a) Schematic diagram of irrigation-drainage system (IDS) and test-pits distribution. Water was supplied from an underground reservoir to every test-pit through pipelines. (b) Underground gallery and drainage system. (c) Lysimeter test-pits. Inside the yellow box is the electromagnetic flow valve device.An integrated irrigation-drainage system (IDS) was installed at the experimental field. For the irrigation system, water was supplied from an underground reservoir to every test-pit through pipelines, and the accuracy of irrigation water volume is controlled by a computer by controlling the electromagnetic flow valves (see Figures1(a) and 1(c)). Water table was changed by raising or lowing the height of a float valve for each treatment. When the ponded water depth dropped to the lower water level, irrigation water was added with auto-irrigation system until the upper water level limit was reached. For details of water table control structures, see Figure  1 in [28]. The drainage system is located in subsurface below the ground path in the middle of the test-pits (see Figures 1(a) and 1(b)). Groundwater in the test-pits can be discharged through artificial drainage, which can control drainage time and water volume and facilitate collection of groundwater samples.


### 2.2. Experimental Design

The variety of rice used in the 2010 experiment was Japonica riceYangjing 4038. To perform paddy field water level management under different flooding conditions, we designed a series of tests at the four major stages of rice growth (tillering, jointing and booting, heading and flowering, and milky stage, in such order). The paddy field water levels, rice growth stages, and controlled drainage periods are summarized in Table 2.Table 2
Design of PFCD water level and controlled periods in 2010.
Growth stage
Tillering stage
Jointing-booting stage
Heading-flowering stage
Milking stage
Growth date (month/day)
Jul 05~Aug 05
Aug 06~Aug 26
Aug 27~Sep 09
Sep 10~Sep 22
Control date (month/day)
Jul 19~Jul 28
Aug 14~Aug 23
Aug 30~Sep 08
Sep 12~Sep 21
Surface water level or subsurface water table depth (mm)
W1
120 (2 mm/d)
−300~30
−300~30
−300~30
W2
120 (4 mm/d)
−300~30
−300~30
−300~30
W3
−200~20
250 (2 mm/d)
−300~30
−300~30
W4
−200~20
250 (4 mm/d)
−300~30
−300~30
W5
−200~20
−300~30
250 (2 mm/d)
−300~30
W6
−200~20
−300~30
250 (4 mm/d)
−300~30
W7
−200~20
−300~30
−300~30
250 (2 mm/d)
W8
−200~20
−300~30
−300~30
250 (4 mm/d)
CK
−200~20
−300~30
−300~30
−300~30
Note: bold types indicate paddy field controlled drainage treatments at different stages, the left numeral is paddy water level, and the numeral in parentheses is drainage intensity under control. Minus sign represents subsurface water table depth.Eight waterlogging and controlled drainage treatments (W1–W8) and one treatment for comparison (CK) were used in the experiment, each with two reduplications. Waterlogging treatments were performed in lysimeters with a closed bottom, whereas comparative treatments were performed in lysimeters without a bottom. Two leakage rates (2 mm/d and 4 mm/d) were designed under the same flooding condition in each stage. The paddy field waterlogging process was simulated after one occurrence of intensive rainfall in different periods. The irrigation program used on comparative treatments was based on controlled irrigation, which is an irrigation program for water saving [28, 29].Agricultural fertilization was conducted three times during the period of rice growth. The fertilizers applied were base fertilizer (date: June 28, type: compound fertilizer, amount: 1200 kg/ha), tillering fertilizer (date: July 5, type: urea, amount: 130 kg/ha), and panicle fertilizer (date: August 6, type: urea, amount: 130 kg/ha), in this specific order. All other recommended cultivated practices for achieving maximum grain yield were followed.


### 2.3. Sampling and Data Analysis

Water samples were collected four times during flooding period at each stage, according to the following sequence which was the 1st, 4th, 7th, and 10th day after being controlled. Surface water was collected by 50 ml syringe and saved in polyethylene bottle, without disturbing soil and selecting randomly. Water samples were analyzed for ammonium nitrogen (N
H
4
+-N) and nitrate nitrogen (N
O
3
--N) using a Shimadzu UV-2800 spectrophotometer. N
H
4
+-N was determined by Nessler’s reagent colorimetric method (GB7479-87). N
O
3
--N was determined by the ultraviolet spectrophotometry method (HJ/T 346-2007).The N losses via subsurface drainage were calculated by multiplying the N concentrations (bothN
H
4
+-N and N
O
3
--N) in the water samples and the volume of the drainage, and surface water N loads were calculated using N concentration and surface water volume also. One-way ANOVA was used to detect the effect from N concentration to N leaching. Statistical analyses of the data were performed using SPSS.


## 2.1. Experimental Site

This study was conducted in an experimental field at water-saving and agroecological experimental plot located in Jiangning Campus of Hohai University, Jiangsu Province of China (Nanjing, latitude 31°57′N, longitude 118°50′E, 144 m above sea level). The region has a subtropical humid monsoon climate zone, with an average annual evaporation of 900 mm and yearly average temperature of 15.7°C, and the maximum and minimum air temperatures are 43.0°C and −14.0°C, respectively. The mean annual rainfall is 1021 mm of which more than 60% of precipitation falls in the rainy season and the precipitation is concentrated in May to September. The number of frost-free days is 237 per year. The temperature, precipitation, and evaporation were recorded daily by an automatic weather station (ICT, Australia) in the experimental plot.The area has been 5 years of rice-wheat rotation system. The soil in the area is a typical permeable paddy soil. The topsoil was 0–30 cm in lysimeter with pH value of 6.97, soil bulk density was 1.46 g/cm3, soil porosity was 44.97%, and field capacity was 25.28%. Characteristics of topsoil are shown in Table 1. There are 32 fixed lysimeter test-pits (28 with closed concrete bottom, 4 without bottom) with specifications for the length × width × depth = 2.5 m × 2 m × 2 m in the experimental field. Those lysimeters layouts were divided into two groups of 16 each. We only employed 18 of them in this research, shown in Figure 1(a). Underground gallery and drainage system are built between the two groups, and a mobile canopy is equipped on the ground.Table 1
Physical and chemical characteristics of topsoil (0–30 cm layer) in lysimeters.
θ
n
ρ
b
Porosity
pH
Organic matter
Total N
Available N
Total P
Available P
(%)
(g/cm3)
(%)
(—)
(g/kg)
(g/kg)
(mg/kg)
(g/kg)
(mg/kg)
25.28
1.46
44.97
6.97
21.88
0.9048
27.65
0.32
12.5
Note:θ
n and ρ
b represent field moisture capacity and soil bulk density, respectively.Figure 1
(a) Schematic diagram of irrigation-drainage system (IDS) and test-pits distribution. Water was supplied from an underground reservoir to every test-pit through pipelines. (b) Underground gallery and drainage system. (c) Lysimeter test-pits. Inside the yellow box is the electromagnetic flow valve device.An integrated irrigation-drainage system (IDS) was installed at the experimental field. For the irrigation system, water was supplied from an underground reservoir to every test-pit through pipelines, and the accuracy of irrigation water volume is controlled by a computer by controlling the electromagnetic flow valves (see Figures1(a) and 1(c)). Water table was changed by raising or lowing the height of a float valve for each treatment. When the ponded water depth dropped to the lower water level, irrigation water was added with auto-irrigation system until the upper water level limit was reached. For details of water table control structures, see Figure  1 in [28]. The drainage system is located in subsurface below the ground path in the middle of the test-pits (see Figures 1(a) and 1(b)). Groundwater in the test-pits can be discharged through artificial drainage, which can control drainage time and water volume and facilitate collection of groundwater samples.


## 2.2. Experimental Design

The variety of rice used in the 2010 experiment was Japonica riceYangjing 4038. To perform paddy field water level management under different flooding conditions, we designed a series of tests at the four major stages of rice growth (tillering, jointing and booting, heading and flowering, and milky stage, in such order). The paddy field water levels, rice growth stages, and controlled drainage periods are summarized in Table 2.Table 2
Design of PFCD water level and controlled periods in 2010.
Growth stage
Tillering stage
Jointing-booting stage
Heading-flowering stage
Milking stage
Growth date (month/day)
Jul 05~Aug 05
Aug 06~Aug 26
Aug 27~Sep 09
Sep 10~Sep 22
Control date (month/day)
Jul 19~Jul 28
Aug 14~Aug 23
Aug 30~Sep 08
Sep 12~Sep 21
Surface water level or subsurface water table depth (mm)
W1
120 (2 mm/d)
−300~30
−300~30
−300~30
W2
120 (4 mm/d)
−300~30
−300~30
−300~30
W3
−200~20
250 (2 mm/d)
−300~30
−300~30
W4
−200~20
250 (4 mm/d)
−300~30
−300~30
W5
−200~20
−300~30
250 (2 mm/d)
−300~30
W6
−200~20
−300~30
250 (4 mm/d)
−300~30
W7
−200~20
−300~30
−300~30
250 (2 mm/d)
W8
−200~20
−300~30
−300~30
250 (4 mm/d)
CK
−200~20
−300~30
−300~30
−300~30
Note: bold types indicate paddy field controlled drainage treatments at different stages, the left numeral is paddy water level, and the numeral in parentheses is drainage intensity under control. Minus sign represents subsurface water table depth.Eight waterlogging and controlled drainage treatments (W1–W8) and one treatment for comparison (CK) were used in the experiment, each with two reduplications. Waterlogging treatments were performed in lysimeters with a closed bottom, whereas comparative treatments were performed in lysimeters without a bottom. Two leakage rates (2 mm/d and 4 mm/d) were designed under the same flooding condition in each stage. The paddy field waterlogging process was simulated after one occurrence of intensive rainfall in different periods. The irrigation program used on comparative treatments was based on controlled irrigation, which is an irrigation program for water saving [28, 29].Agricultural fertilization was conducted three times during the period of rice growth. The fertilizers applied were base fertilizer (date: June 28, type: compound fertilizer, amount: 1200 kg/ha), tillering fertilizer (date: July 5, type: urea, amount: 130 kg/ha), and panicle fertilizer (date: August 6, type: urea, amount: 130 kg/ha), in this specific order. All other recommended cultivated practices for achieving maximum grain yield were followed.


## 2.3. Sampling and Data Analysis

Water samples were collected four times during flooding period at each stage, according to the following sequence which was the 1st, 4th, 7th, and 10th day after being controlled. Surface water was collected by 50 ml syringe and saved in polyethylene bottle, without disturbing soil and selecting randomly. Water samples were analyzed for ammonium nitrogen (N
H
4
+-N) and nitrate nitrogen (N
O
3
--N) using a Shimadzu UV-2800 spectrophotometer. N
H
4
+-N was determined by Nessler’s reagent colorimetric method (GB7479-87). N
O
3
--N was determined by the ultraviolet spectrophotometry method (HJ/T 346-2007).The N losses via subsurface drainage were calculated by multiplying the N concentrations (bothN
H
4
+-N and N
O
3
--N) in the water samples and the volume of the drainage, and surface water N loads were calculated using N concentration and surface water volume also. One-way ANOVA was used to detect the effect from N concentration to N leaching. Statistical analyses of the data were performed using SPSS.


## 3. Results

### 3.1. Dynamic Changes ofNH
4
+-N and NO
3
--N Concentration

#### 3.1.1.NH
4
+-N and NO
3
--N in Surface Water

Figure2 shows the dynamic changes of N
H
4
+-N and N
O
3
--N concentration in surface water of paddy field under controlled drainage. Overall, a declining tendency was observed in the concentration levels of N
H
4
+-N and N
O
3
--N, except that the N
O
3
--N concentration was increased during the tillering stage, whereas N
H
4
+-N was increased later in the heading and flowering stage (September 5–8) and early in the milky stage (September 12–15).Figure 2
Dynamic changes ofN
H
4
+-N and N
O
3
--N concentration in surface water. (a) Tillering stage. (b) Jointing-booting stage. (c) Heading-flowering stage. (d) Milking stage.
(a)
(b)
(c)
(d)N concentration was relatively higher on the first day after waterlogging. On the 10th day, theN
H
4
+-N concentration for W1, W2, W3, W4, W7, and W8 was reduced to 68.3%, 67.4%, 38.2%, 44.4%, 55.0%, and 62.7%, respectively. The N
O
3
--N concentration for W3, W4, W5, W6, W7, and W8 was reduced to 69.4%, 73.7%, 66.7%, 67.6%, 71.3%, and 74.6%, respectively.


#### 3.1.2.NH
4
+-N and NO
3
--N in Subsurface Water

Figure3 presents the dynamic changes in N
H
4
+-N and N
O
3
--N concentration in subsurface water of paddy field under controlled drainage. The trend of subsurface N
H
4
+-N concentration variety corresponded with surface water concentration. Compared with the concentration on the first day after paddy field waterlogging, the N
H
4
+-N concentration on the 10th day for W1, W2, W3, W4, W7, and W8 was reduced to 64.6%, 58.4%, 25.4%, 28.4%, 79.4%, and 55.4%, respectively.Figure 3
Dynamic changes ofN
H
4
+-N and N
O
3
--N concentration in subsurface water. (a) Tillering stage. (b) Jointing-booting stage. (c) Heading-flowering stage. (d) Milking stage.
(a)
(b)
(c)
(d)A remarkable downtrend ofN
O
3
--N concentration was observed at the jointing and booting stage. The N
O
3
--N concentration on the 10th day for W3 and W4 was reduced to 45.5% and 37.4%, respectively, compared with that on the first day. N
O
3
--N concentration was relatively higher at the tillering stage, mainly because of nitrification by residual N in soil. Meanwhile, the change in N
O
3
--N concentration was smaller in other stages.


### 3.2. Effect from Drainage Intensity to N Leaching

The amount of paddy N leaching during the control period is shown in Table3. The amount of N leaching under 4 mm/d leakage intensity was remarkable about two times larger than that under the 2 mm/d treatment. The highest amount of N
H
4
+-N and N
O
3
--N leaching was observed at the milking and tillering stages, respectively.Table 3
N leaching amount of controlled drainage paddy field under two leakage intensity conditions.
Growth stage
Tillering stage
Jointing-booting stage
Heading-flowering stage
Milking stage
Leakage intensity
2 mm/d
4 mm/d
2 mm/d
4 mm/d
2 mm/d
4 mm/d
2 mm/d
4 mm/d
N
H
4
+-N (g⋅ha−2)
134.93
261.84
86.25
208.33
79.35
206.97
185.13
359.58
N
O
3
--N (g⋅ha−2)
108.6
229.16
49.96
124.16
19.76
42.05
21.27
49.93Results of ANOVA for N concentration through leaching under two leakage intensities are shown in Table4. All the Sig values (p) were larger than 0.05. Results show that the difference between the two conditions was not significant.Table 4
ANOVA results for N concentration through leaching under two leakage intensity conditions.
Factors
Tillering stage
Jointing-booting stage
Heading-flowering stage
Milking stage
F
Sig
F
Sig
F
Sig
F
Sig
N
H
4
+-N
0.007
0.938
3.573
0.108
3.703
0.103
0.004
0.950
N
O
3
--N
0.246
0.638
1.533
0.262
0.127
0.734
2.118
0.196


### 3.3. Effect of Pollution Reduction

Surface water N loads and emission reduction of N under different flooding times are shown in Figures4 and 5. N loads in surface paddy water declined along with the persistence of waterlogging duration. Compared with traditional drainage (drainage immediately after waterlogging), PFCD (10 d) reduced N loss in surface water by 95.6%, 78.7%, 59.6%, and 87.4% at each of the four stages, in this particular order.Figure 4
Loads of N in surface water and accumulated water consumption. (a) Tillering stage. (b) Jointing-booting stage. (c) Heading-flowering stage. (d) Milking stage. The accumulated water consumption was measured by water decrease depth.
(a)
(b)
(c)
(d)Figure 5
N emission reductions of PFCD treatments.


## 3.1. Dynamic Changes ofNH
4
+-N and NO
3
--N Concentration

### 3.1.1.NH
4
+-N and NO
3
--N in Surface Water

Figure2 shows the dynamic changes of N
H
4
+-N and N
O
3
--N concentration in surface water of paddy field under controlled drainage. Overall, a declining tendency was observed in the concentration levels of N
H
4
+-N and N
O
3
--N, except that the N
O
3
--N concentration was increased during the tillering stage, whereas N
H
4
+-N was increased later in the heading and flowering stage (September 5–8) and early in the milky stage (September 12–15).Figure 2
Dynamic changes ofN
H
4
+-N and N
O
3
--N concentration in surface water. (a) Tillering stage. (b) Jointing-booting stage. (c) Heading-flowering stage. (d) Milking stage.
(a)
(b)
(c)
(d)N concentration was relatively higher on the first day after waterlogging. On the 10th day, theN
H
4
+-N concentration for W1, W2, W3, W4, W7, and W8 was reduced to 68.3%, 67.4%, 38.2%, 44.4%, 55.0%, and 62.7%, respectively. The N
O
3
--N concentration for W3, W4, W5, W6, W7, and W8 was reduced to 69.4%, 73.7%, 66.7%, 67.6%, 71.3%, and 74.6%, respectively.


### 3.1.2.NH
4
+-N and NO
3
--N in Subsurface Water

Figure3 presents the dynamic changes in N
H
4
+-N and N
O
3
--N concentration in subsurface water of paddy field under controlled drainage. The trend of subsurface N
H
4
+-N concentration variety corresponded with surface water concentration. Compared with the concentration on the first day after paddy field waterlogging, the N
H
4
+-N concentration on the 10th day for W1, W2, W3, W4, W7, and W8 was reduced to 64.6%, 58.4%, 25.4%, 28.4%, 79.4%, and 55.4%, respectively.Figure 3
Dynamic changes ofN
H
4
+-N and N
O
3
--N concentration in subsurface water. (a) Tillering stage. (b) Jointing-booting stage. (c) Heading-flowering stage. (d) Milking stage.
(a)
(b)
(c)
(d)A remarkable downtrend ofN
O
3
--N concentration was observed at the jointing and booting stage. The N
O
3
--N concentration on the 10th day for W3 and W4 was reduced to 45.5% and 37.4%, respectively, compared with that on the first day. N
O
3
--N concentration was relatively higher at the tillering stage, mainly because of nitrification by residual N in soil. Meanwhile, the change in N
O
3
--N concentration was smaller in other stages.


## 3.1.1.NH
4
+-N and NO
3
--N in Surface Water

Figure2 shows the dynamic changes of N
H
4
+-N and N
O
3
--N concentration in surface water of paddy field under controlled drainage. Overall, a declining tendency was observed in the concentration levels of N
H
4
+-N and N
O
3
--N, except that the N
O
3
--N concentration was increased during the tillering stage, whereas N
H
4
+-N was increased later in the heading and flowering stage (September 5–8) and early in the milky stage (September 12–15).Figure 2
Dynamic changes ofN
H
4
+-N and N
O
3
--N concentration in surface water. (a) Tillering stage. (b) Jointing-booting stage. (c) Heading-flowering stage. (d) Milking stage.
(a)
(b)
(c)
(d)N concentration was relatively higher on the first day after waterlogging. On the 10th day, theN
H
4
+-N concentration for W1, W2, W3, W4, W7, and W8 was reduced to 68.3%, 67.4%, 38.2%, 44.4%, 55.0%, and 62.7%, respectively. The N
O
3
--N concentration for W3, W4, W5, W6, W7, and W8 was reduced to 69.4%, 73.7%, 66.7%, 67.6%, 71.3%, and 74.6%, respectively.


## 3.1.2.NH
4
+-N and NO
3
--N in Subsurface Water

Figure3 presents the dynamic changes in N
H
4
+-N and N
O
3
--N concentration in subsurface water of paddy field under controlled drainage. The trend of subsurface N
H
4
+-N concentration variety corresponded with surface water concentration. Compared with the concentration on the first day after paddy field waterlogging, the N
H
4
+-N concentration on the 10th day for W1, W2, W3, W4, W7, and W8 was reduced to 64.6%, 58.4%, 25.4%, 28.4%, 79.4%, and 55.4%, respectively.Figure 3
Dynamic changes ofN
H
4
+-N and N
O
3
--N concentration in subsurface water. (a) Tillering stage. (b) Jointing-booting stage. (c) Heading-flowering stage. (d) Milking stage.
(a)
(b)
(c)
(d)A remarkable downtrend ofN
O
3
--N concentration was observed at the jointing and booting stage. The N
O
3
--N concentration on the 10th day for W3 and W4 was reduced to 45.5% and 37.4%, respectively, compared with that on the first day. N
O
3
--N concentration was relatively higher at the tillering stage, mainly because of nitrification by residual N in soil. Meanwhile, the change in N
O
3
--N concentration was smaller in other stages.


## 3.2. Effect from Drainage Intensity to N Leaching

The amount of paddy N leaching during the control period is shown in Table3. The amount of N leaching under 4 mm/d leakage intensity was remarkable about two times larger than that under the 2 mm/d treatment. The highest amount of N
H
4
+-N and N
O
3
--N leaching was observed at the milking and tillering stages, respectively.Table 3
N leaching amount of controlled drainage paddy field under two leakage intensity conditions.
Growth stage
Tillering stage
Jointing-booting stage
Heading-flowering stage
Milking stage
Leakage intensity
2 mm/d
4 mm/d
2 mm/d
4 mm/d
2 mm/d
4 mm/d
2 mm/d
4 mm/d
N
H
4
+-N (g⋅ha−2)
134.93
261.84
86.25
208.33
79.35
206.97
185.13
359.58
N
O
3
--N (g⋅ha−2)
108.6
229.16
49.96
124.16
19.76
42.05
21.27
49.93Results of ANOVA for N concentration through leaching under two leakage intensities are shown in Table4. All the Sig values (p) were larger than 0.05. Results show that the difference between the two conditions was not significant.Table 4
ANOVA results for N concentration through leaching under two leakage intensity conditions.
Factors
Tillering stage
Jointing-booting stage
Heading-flowering stage
Milking stage
F
Sig
F
Sig
F
Sig
F
Sig
N
H
4
+-N
0.007
0.938
3.573
0.108
3.703
0.103
0.004
0.950
N
O
3
--N
0.246
0.638
1.533
0.262
0.127
0.734
2.118
0.196


## 3.3. Effect of Pollution Reduction

Surface water N loads and emission reduction of N under different flooding times are shown in Figures4 and 5. N loads in surface paddy water declined along with the persistence of waterlogging duration. Compared with traditional drainage (drainage immediately after waterlogging), PFCD (10 d) reduced N loss in surface water by 95.6%, 78.7%, 59.6%, and 87.4% at each of the four stages, in this particular order.Figure 4
Loads of N in surface water and accumulated water consumption. (a) Tillering stage. (b) Jointing-booting stage. (c) Heading-flowering stage. (d) Milking stage. The accumulated water consumption was measured by water decrease depth.
(a)
(b)
(c)
(d)Figure 5
N emission reductions of PFCD treatments.


## 4. Discussion

The results indicated that N concentration in surface water decreased effectively when proper subsurface drainage rate in the paddy field is maintained in the waterlogging condition. This condition is caused by several processes. The reasons for the decline inN
H
4
+-N concentration include volatilization, nitrification, soil adsorption, crop absorption, and migration into depth. Meanwhile, the reasons for the decline in N
O
3
--N concentration include denitrification, crop absorption, leaching loss, and migration into depth [30–34]. Nitrification and denitrification are two important mechanisms of nitrogen transform and N2O emissions from fields. Many factors regulate these processes, particularly soil water content and temperature, microorganism types, and PH, and so on. Subsurface environment affects the activity of soil bacteria significantly. The mechanisms of temperature and soil water regime effects should be studied specifically.N concentration was relatively higher on the first day after waterlogging. This phenomenon was caused by N released from surface soil, which is disturbed by water-drop splash from irrigation or rainfall.N
H
4
+-N concentration was later increased at the heading and flowering stage (September 5–8) and in the early days at the milky stage (September 12–15). This phenomenon can explain the organic nitrogen released from the paddy field, which was accelerated by scorching weather. N
O
3
--N concentration was lower at the tillering stage, where the urea may still be in a hydrolytic status, and a cumulative process occurs for N
H
4
+-N to nitrify into N
O
3
--N.Generally,N
O
3
--N was relatively stable and was found to migrate into aquifer heavily. N
H
4
+-N was difficult to remove from underground and its conversion process into soil was complicated. The underground environment in the paddy field under controlled drainage was highly complex because it involved the effects of soil, moisture, crop, microorganism, and fertilizer. Therefore, the mechanism of N migration and transformation requires further research.Results of ANOVA for subsurface water N concentration showed that the difference between the two drainage intensities was not significant. Wesström et al. [35] compared the conventional drainage system and controlled drainage strategies through a field experiment in Southern Sweden, and the experiment results showed that the N and P losses in controlled drainage were lower than those in conventional drainage, but N and P concentrations in subsurface drainage water were revealed to have no significant differences between the two drainage systems. Such results were similar to ours, although the conditions we compared were both under a controlled drainage system. This suggests that the N concentrations were similar under two leakage conditions. N loss through drainage increases as runoff volume increases. Furthermore, we consider drainage water volume as the main factor that affects N leaching amount.As mentioned, a mass of N wound was released from surface soil, which was disturbed by irrigation or rainfall on the first day after waterlogging. Thus, we should not discharge the surface water immediately after paddy flooding. In our tests, the loads of N losses on the fourth day after waterlogging were increased at the jointing-booting and milking stages. Surface drainage should be avoided in these conditions as well.On the contrary, several disadvantages are caused by prolonged waterlogging. Waterlogging duration has remarkable effects on crop yield. For instance, when the surface water level is too high in the tillering stage, it will cause the number of tillers to reduce and lead directly to reducing the rice yield in the late stage. So, paddy water should be drained at an appropriate time. Rice plant manifests root hypoxia when it lives in the field without leakage or without being in deep water for a long time. This condition goes against the physiological metabolism of the rice plant and therefore disrupts photosynthesis, eventually causing plant growth retardation and yield reduction. These adverse effects can be reduced by enhancing field leakage, which can increase soil ventilation volume.Paddy field controlled drainage can effectively save irrigation water and decrease nitrogen pollution emission. However, many issues require further study, such as how rice yield losses can be minimized on the basis of water saving and pollution reduction. Such a problem must be assessed comprehensively from the perspectives of surface water depth, flooding stage and time of duration, leakage intensity, and other factors. More tests need to be carried out in the future to provide a basis for decision-making. We can determine the optimal drainage time through the multiobjective analysis method.


## 5. Conclusions

By analyzing N concentration and calculating the amount of N leaching and loads of N losses, we can summarize the main conclusions of this experimental study as follows:(1)
TheN
H
4
+-N and N
O
3
--N concentrations in paddy water declined along with the prolongation of waterlogging duration. Surface water was found to have higher N concentration on the first day after paddy field waterlogging at each stage, and loads of N losses increased on the fourth day at the jointing-booting and milking stages. Thus, surface drainage should be avoided in these two conditions.
(2)
The amount of N leaching under 4 mm/d leakage intensity was approximately two times larger than that under the 2 mm/d treatment. Results of ANOVA for N concentration through leaching under the two leakage intensities showed that the difference between such intensity levels was not significant. Therefore, the main factor that affects N leaching amount is seepage water volume.
(3)
Loads of N losses in surface paddy water declined with the continuation of waterlogging duration. Compared with traditional drainage, controlled drainage reduced N loss in surface water by 95.6%, 78.7%, 59.6%, and 87.4% at each of the four stages.



---

*Source: 1073691-2016-04-03.xml*