1. Introduction
According to incomplete statistics from the United Nations Educational, Scientific and Cultural Organization (UNESCO) and the Food and Agriculture Organization of the United Nations (FAO), the world’s saline soil area is 9.5438 × 10
8 hm
2 [
1]. China has the third-largest area of saline-alkali land. There are more than 30 million hm
2 of saline-alkali land in China [
2]. Of that total, the saline-alkali land with agricultural development potential accounts for more than 10% of the total cultivated land in China [
3]. Maize is one of the essential food crops in northern China. It is an important feed source for animal husbandry, aquaculture, and other industries [
3]. It can adapt to a certain degree of saline-alkali soil. Planting maize on saline-alkali land needs to meet the nutrition required for its normal growth during its growth period. Still, fertilization will increase the soil salt concentration (Ssc), and that should be considered when determining the fertilization rates on saline-alkali cropland. Rational fertilization to tap the yield potential of maize in saline-alkali soils is vital for stabilizing grain production. However, at present, the results of studies on the interaction between Ssc and nitrogen vary significantly depending on the physical and chemical characteristics of soil in different areas.
Maize is sensitive to salinity stress. The accumulation of soil salinity often decreases maize yield. The presence of soil salinity has a range of physiological effects on plants [
4]. Stomatal conductance (g
s) is a sensitive physiological indicator of plant response to salt [
5]. Moreover, stomatal area and stomatal density can also reflect plants’ response to salinity. Chlorophyll concentration often decreases when plants are grown in saline soils [
6]. Both the osmotic and ionic effects of salt affect plant growth [
5]. The accumulation of salt ions in the cytoplasm of cells can lead to toxic ion effects [
7]. Ions associated with soil salinity can cause an ionic imbalance that reduces the ratio of essential to non-essential nutrients in the soil, thereby reducing nitrogen uptake by plants and negatively interacting with cations and anions [
8,
9]. Some studies have found that microbes can alleviate salt stress. For example, the use of salt-tolerant rhizobia can increase the nutrient uptake (N, P, K) of rapeseed and alleviate the effects of salt stress [
10]. In another study, the authors found growth promoting rhizobacteria limited Na uptake, increased K and Ca uptake, and stimulated nitrogenase activity in both shoots and roots [
11]. Moreover, nitrogen is generally deficient in saline-alkali soils [
12]. Sometimes increasing nitrogen nutrition can alleviate salt stress in plants and promote plant growth [
13]. For example, previous research found that moderate (135 kg ha
−1) and high (180 kg ha
−1) levels of N fertilization could provide the maximum benefit in low- to moderate-salinity and high- or severe-salinity fields, respectively, in the Hetao Irrigation District. [
14]. In another study on maize, the authors found that at the salinity levels of 3.4, 6.7, 9.2, and 12.5 ds m
−1, the nitrogen application of 240 kg N ha
−1 could improve the growth of plants [
15].
It was found by Xie et al., through a comprehensive analysis of data from 571 works in the literature involving two-factor cross-experiments of soil salinity and nitrogen fertilizer, that increasing the nitrogen application rate within the range of 0.18–0.29% salinity can improve crop yield and economic benefits [
16]. In the same study, they also found that above the salinity threshold of 0.35%, soils are not suitable for growing food crops. Machado found that the low water salinity threshold for most fruit crops was between 0.9 and 1.5 ds m
−1, except for pistachios, dates, olives, and figs [
17]. Fertilization combined with drip irrigation can alleviate fruit salt stress, and organic composting has a specific potential to improve soil physical and chemical properties and salt tolerance of fruit crops. The study by Xu et al. found that moderate irrigation and nitrogen application under border irrigation has the advantages of water and fertilizer saving, stable yield, and high light efficiency for maize in salinized farmland [
18]. Liu et al. found that an appropriate soil nitrogen application rate can alleviate the effects of salt stress on plant height, leaf area, and 1000-grain weight of winter wheat [
19]. The effect of relieving salt stress on leaf area was more significant. Song et al. found that nitrogen application can alleviate the inhibitory effect of salinity accumulation on sunflower net photosynthesis and stomatal conductance [
20]. Sunflower dry matter accumulation decreases with increases in soil salinity and increases with increased nitrogen application rates. The above studies researched the effect of fertilization in saline-alkali land on crop growth from different perspectives. They drew valuable research conclusions, but these studies did not explore the internal mechanism of how fertilization alleviates the effect of salt stress on crop physiological functions.
Nitrogen application can alleviate the inhibitory effect of soil salinity on the gs value of maize to a certain extent, but in soils with high Ssc, how does the interaction between nitrogen fertilizer and soil salinity regulate the variation in stomatal conductance? What about its deeper physiological mechanism and even molecular regulation mechanism? There are still few related studies on these questions.
There is a large amount of saline-alkali land in the Hetao Irrigation District, which is one of the three super-large irrigation districts in China and the main growing area for maize cultivation. Similar soil salinity composition and concentration ranges were considered in setting up the soil salinity treatments and whether or not to apply nitrogen fertilizer in this study. The research goal was to study the effects of nitrogen fertilization on physiological response of maize to soil salinity. Plant growth and photosynthetic physiological indicators were systematically measured to explain the internal mechanisms of crop physiological response to soil salt concentration and nitrogen from the aspects of leaf anatomy and osmotic regulation, such as stomatal morphology and leaf water potential. Hopefully, this study can provide basic data and a theoretical basis for the study of plant physiological responses to soil salt in saline-alkali areas.
2. Materials and Methods
2.1. Overview of Research Station
The experiment was carried out from April to September 2021 at the Daxing Experimental Station (116.44 E, 39.62 N) of the National Water-Saving Irrigation Beijing Engineering Technology Research Center of the China Water Resources and Hydropower Research Institute. The weather of the station is a warm temperate, semi-humid continental monsoon climate, with annual average, maximum and minimum temperatures of 12.0 °C, 17 °C, and 7 °C, respectively, and average annual rainfall of 540 mm.
2.2. Experimental Design
The soil of the test site was silt loam from the 0–40 cm layer of surface soil of a farm field at the experiment station. The volumetric weight was 1.41 g cm−3, the field capacity was 0.33 cm3 cm−3, the organic mass was 12.17 g kg−1, and the total nitrogen content was 1.00 g kg−1. Available phosphorus and potassium were 16.9 mg kg−1 and 123.6 mg kg−1, respectively. The experimental containers used were polyethylene plastic cuboid flowerpots with a length, width, and height of 34.5 cm × 34.5 cm × 45 cm, respectively. Each pot was filled with 64 kg of soil. Soil water, heat, and salt probes were installed at the depth of 20 cm below the ground surface in each pot. After loading, the soil was watered thoroughly until it was completely saturated and water discharged from the bottom of the basin. After standing for 24 h, the weight of all containers was determined.
The soil salinity concentration in this experiment was set according to the soil salinity composition and concentration in Hetao Irrigation District. According to the weight ratio, three Ssc were set: 0 (S1), 0.1% (S2), and 0.25% (S3). NaCl, CaHCO3, and MgSO4 (Sinopharm Chemical Reagent Co., Ltd, Shanghai, China) were mixed with the mass ratio of 2:2:1 and added to the total weight according to the dry soil weight in the container. The salt was dissolved in water and evenly poured into the container filled with soil.
The base fertilizer was fully dissolved in water according to the set amount of nitrogen fertilizer, and then evenly poured into the container. Two nitrogen application rates were set, namely, no nitrogen application (N0) and nitrogen application (N1). The nitrogen application mode of the N1 treatment is shown in
Table 1, and the total amount of N was 13.2 g per pot. The total amounts of P
2O
5 and K
2O fertilizers (9.49 g, 6.33 g,
Table 1) were the same for all the treatments. Full irrigation was applied with tap water, and the irrigation amount was determined by the weighing method. During the experiment, the soil surface was covered with plastic film to reduce soil evaporation. When filling containers with water after salt application, if there was water drainage, the drained water was collected and added back to the same container with the next irrigation.
The maize variety was Jintian 8 (seed cultivated in Inner Mongolia that is suitable for growth and development in saline-alkali soil). Two locations were selected for sowing in the container: 4–6 seeds were buried in each location, and two plants were fixed in each container. Maize was sown on 2021.5.15 and harvested on 2021.9.25. The planting rate was 100%, and the maize was harvested in the R5 stage.
2.3. Observation Items and Methods
The following parameters were regularly measured: (1) dynamic changes in soil water and salt content in the root layer of each treatment and each growth period; (2) the crop growth index, physiological index, and biomass of each treatment.
2.3.1. Meteorological Elements and Soil Water and Salt Dynamics
The meteorological data were collected by an automated weather station (Hobo, Onset., Cape Cod, MA, USA) at the station every 15 min, including solar radiation, temperature, humidity, wind speed, precipitation, etc.
An EC5 probe (METER Group Inc., Pullman, WA, USA) was used to monitor soil moisture content. The salt content of the soil was measured as the electrical conductivity (EC) with a salt probe and automatically collected by a data logger (Zl6, METER Group Inc., Pullman, WA, USA). The probes were buried at a depth of 20 cm from the soil surface when the pots were filled. EC values of S1, S2 and S3 were 1.9 ds m−1, 3.21 ds m−1, 5.6 ds m−1, respectively.
2.3.2. Growth Index
Plant height was measured with a tape from the soil surface to the top of the maize plant at the stages of twelfth leaf (V12) and tasseling (VT). At the same time, stem diameter was measured by averaging the long axis width and short axis width of maize stalk with a vernier caliper at the height of 20 cm from the ground surface. Leaf area was also measured at the stages of V12 and VT. Using a tape measure, we measured the leaf length from the position where the leaf was connected with the stem to the leaf tip, and the leaf width as the width at the middle of the leaf, and obtained the regression equation of maize area through the grid method, y = 0.75×, and then measured the actual leaf area of maize plants in each treatment according to the regression equation.
2.3.3. Chlorophyll Content SPAD
A SPAD-502 chlorophyll meter (SPAD-502 plus, Konica Minolta Holdings, Inc., Chiyoda-ku, Tokyo, Japan) was used to measure the SPAD value at eight positions evenly distributed on the middle part of leaves.
2.3.4. Leaf Water Potential
Leaf water potential was measured by the PMS 600 Portable Plant Water Potential Cavitation Pressure Chamber (Particle Measuring Systems, Boulder, CO, USA). Leaf water potential was measured by the pressure chamber, as follows. Remove the leaf from the plant with scissors, tear a part of the leaf along the main vein at the incision site, move the leaf into the pressure chamber, extend the leaf main vein incision at the air chamber cover so that the veins can be seen. Close the air cover chamber and open the intake valve to increase the pressure in the pressure chamber. When tiny water droplets appear at the incision, stop the pressure immediately and read the pressure value. At this time, the negative number of the pressure value is the leaf water potential.
2.3.5. Gas Exchange, A-Ci Response Curve
The LI-6800 photosynthetic measurement system (Li-Cor Inc., Lincoln, NE, USA) was used to measure the gas exchange during the day. The measured parameters included g
s, A, and intercellular CO
2 concentration (Ci). Intrinsic water use efficiency, WUE
in, was calculated with Equation (1) [
21]:
where:
A—net photosynthetic rate, µmol m−2 s−1;
gs—stomatal conductance, mol m−2 s−1.
A-Ci response curves were measured once at the V12 stage. The A-Ci response data were gathered using the auto program with a portable photosynthesis system (Li-6800, Li-COR Inc., Lincoln, NE, USA). The A-Ci curves were measured from 9:00 to 14:00 with the photosynthetic active radiation (PAR) of 1800 μmol m
−2 s
−1 and the temperature of 25 °C. The carbon dioxide concentrations in the leaf chamber were set to 400, 300, 200, 150, 100, 80, 40, 400, 400, 600, 800, 1000, 1200, and 1500 μmol mol
−1, a total of 14 values. The A-Ci curve fitting utility model [
22] was used to determine the values of V
pmax and V
cmax.
2.3.6. Stomatal Morphology Index
Nail polish was applied to the middle, suitable part of the most developed leaf at the top of each sample. After formation, the film was peeled off and placed into a slide. The stomatal morphological parameters were photographed by Motic Panthera (Motic China Group Co., LTD, Xiamen, China), which were: the length of the stomata long axis, the short axis length of stomata, and stomatal density (the number of pores in the visible area divided by the visible area). The length and width of the stomata were measured by Motic Panthera software 1.0.23. (Motic China Group Co., LTD, Xiamen, China). The area of pores was calculated by using the elliptic area calculation formula. Estimation of theoretical maximum stomatal conductance (g
smax) [
23]:
where:
d—diffusion coefficient of water vapor in air (24.9 × 10−6 m−2 s−1);
SD—stomatal density (mm−2);
amax—pore area (mm2);
v—molar volume of air (22.4 × 10−3 m3 mol−1, 25 °C, 101.3 Mpa);
PD—stomatal depth, assumed to be equal to stomatal guard width (um).
2.4. Data Processing Methods
The experimental data obtained were processed by SPSS statistical analysis software, and significant differences in the data were tested with Tukey’s HSD method for multiple comparisons (p < 0.05 significant level). SPSS 25.0 software was used for data univariate analysis, paired analysis, variance analysis, and linear regression analysis. The Origin software was used for graphing.
4. Discussion
Clarifying the physiological response mechanism of maize after nitrogen application under soil salt stress is necessary to alleviate soil salt stress and stabilize grain production [
5,
24,
25]. Previous studies focused on how to select crop varieties with solid salt and alkali resistance or management measures such as leaching soil salt and alkali to improve maize biomass and yield. There are few studies on improving maize biomass, yield, and water use efficiency from the perspective of leaf photosynthetic physiology and biochemistry.
In this study, we evaluated the effects of salinity and nitrogen fertilizers on maize growth and physiological indexes. We found that the leaf area, plant height, stem diameter, and SPAD of maize decreased with increases in Ssc (
Figure 1,
Figure 2,
Figure 3 and
Figure 4). Our conclusion is similar to that of Nathan E. G. Smith et al., namely, that plant biomass, height and SPAD decrease with increasing salinity [
26]. Plant growth responds to salinity in two phases: a rapid, osmotic phase that inhibits growth of young leaves, and a slower, ionic phase that accelerates senescence of mature leaves [
5]. The osmosis of salt and the toxic ion effect are the main reasons for the growth decline. The application of NH4
+ can help provide favorable ion homeostasis [
14]. Many permeable substances contain the element N. Therefore, nitrogen application can alleviate the effects of salt stress on leaf area, plant height and stem diameter. In the N1 treatment in our study with nitrogen application under the same salt treatment, all indexes except leaf area were significantly higher than those of the N0 treatment (
Figure 1,
Figure 2 and
Figure 3). However, nitrogen application under the high salt S3 treatment reduced leaf area. The application of nitrogen fertilizer in a certain range can alleviate the stress effect of salt on maize growth indicators. Similar results were obtained by Xu et al. They found that applying nitrogen fertilizer at 281.18 kg hm
−2 and 229.4 kg hm
−2 had the best effect on the biomass of maize when the soil salt concentration was 0.247 and 0.839 g kg
−1, respectively [
18].
We also found that the soil salinity stress with each treatment had a significant effect on the water potential of maize leaves (
Figure 5). The higher the Ssc, the lower the Ψ, and the worse the ability of maize to absorb water from the soil. Liao et al. found that leaf osmotic adjustment was a key physiological trait under water and salt stress. Mild water-salt stress can increase osmotic regulation and water resistance [
27]. The conclusion was similar to that of our study, which found that nitrogen fertilization alleviates the effect of salt stress on leaf water potential caused by the S1, S2 and S3 treatments (
Figure 5). Previous studies have shown that water or salt stress will change the coupling relationship between grain yield and water use and change the proportion of photosynthetic maize products allocated to reproductive organs [
28,
29,
30,
31]. In this study, with the increase in soil salt content, the dry matter mass of maize in each treatment showed a significant downward trend. Under the S2 treatment, compared with no nitrogen application, the nitrogen application increased the dry maize matter. Nitrogen application reduced the dry matter mass of maize under S1 and S3 treatments. It can be seen that with the increase in Ssc, the dry matter weight of maize showed a significant downward trend. Under the S2 treatment, nitrogen application significantly increased the dry matter weight. Under S1, S2, and S3 treatments, nitrogen application increased the dry matter (
Figure 3b).
RuBP carboxylase and PEP carboxylase are key enzymes in the photosynthetic carbon cycle [
32]. The values of V
cmax and V
pmax after nitrogen application were higher than those with no nitrogen application, indicating that within the range of salt treatment concentration set in this experiment (
Figure 7), the nitrogen application could alleviate the inhibitory effect of soil salt on the carboxylation of Rubisco and PEP protease in maize. Additionally, after nitrogen application, V
pmax, and V
cmax values decreased more than before nitrogen application among the three soil salinity treatments. With the increase in Ssc, the difference in V
pmax before and after nitrogen application first decreased and then increased, and the difference in V
cmax gradually decreased. The alleviating effect of nitrogen application on RuBP carboxylase activity decreased, and the alleviating effect on PEP carboxylase activity increased first, then decreased, and then increased again.
It was also found that with the increase in Ssc, A, g
s, stomatal width, a
max, stomatal circumference, g
smax, stomatal density (SD) and other parameters all showed a downward trend; however, the SD increased. Previous research has shown that salt reduces A and g
s in plants [
5]. Through regression analysis, Liao and others found that the decreases in A and g
s were related to the decreases in leaf water potential and leaf nitrogen content under water and salt stress [
27]. Nitrogen is a component of many permeable solutes, proteins, and membranes to maintain cell swelling [
33,
34]. Ssc can result in an imbalance of solute water potential and an inability to maintain cell swelling. Therefore, the stomatal width, g
smax, and a
max. will decrease. However, after nitrogen application, cell expansion will be restored, so nitrogen application will relieve the stress from salt on stomatal width, g
smax and a
max. Under S1 and S2 salinity treatments, nitrogen application alleviated the stress effect of soil salinity on the above indicators. However, under S3 treatment, g
s, a
max and g
smax of maize leaves all decreased after nitrogen application (
Figure 6 and
Figure 8). This may be because when nitrogen is applied at a high Ssc, the SPAC water transport system is stressed. It is difficult for the root system to absorb enough water to meet the needs of plants, resulting in a decrease in leaf water potential and cell water content, which will have a negative impact on the leaves, resulting in the decrease in air pore conductivity and net photosynthetic rate, which is similar to the conclusions of Munns [
5] and Tardieu [
24]. In this study, under N0 and N1 treatments, the WUE
in increased with the increase in Ssc. Under the same soil salinity treatment, each value after nitrogen application was higher than that with no nitrogen application (
Figure 6).
The purpose of the evolution of stomata to adapt to the environment is to achieve greater water use and photosynthetic productivity [
35]. Higher stomatal conductance and photosynthesis lead to more water utilization and carbon-organic synthesis, which are converted to biomass [
36,
37]. At the same time, maize adapts to stress through its own osmotic regulation ability [
38]. In this study, how maize copes with the stress of nitrogen application in high-salt soil through osmotic regulation and its own physiological regulation system, thus maintaining higher WUE
in, is still unclear. We will carry out further research in the future.