Abstract
Introduction:
Straw return has been widely recognized as an important carbon (C) enhancement measure in agroecosystems, but the C-phosphorus (P) interactions and their effects on plants in saline soils are still unclear.
Methods:
In this study, we investigated the effects of straw return and three P application levels, no P fertilizer (Non-P), a conventional application rate of P fertilizer (CP), and a high application rate of P fertilizer (HP), on maize growth and soil C and P fractions through a pot experiment.
Results and discussion:
The results revealed that the dry matter weight of maize plant was no difference between the two straw return levels and was 15.36% higher under HP treatments than under Non-P treatments. Plant nutrient accumulations were enhanced by straw addition and increased with increasing P application rate. Straw application reduced the activities of peroxidase (POD), superoxide dismutase (SOD), catalase, and the content of malondialdehyde (MDA) in maize plants by 31.69%, 38.99%, 45.96% and 27.04%, respectively. P application decreased SOD, POD activities and MDA content in the absence of straw. The contents of easily oxidized organic carbon (EOC), particulate organic carbon (POC) and the ratio of POC/SOC in straw-added soils were 10.23%, 17.00% and 7.27% higher, respectively, than those in straw-absent soils. Compared with Non-P treatments, HP treatments led to an increase of 12.05%, 23.04% in EOC, POC contents respectively, while a decrease of 18.12% in the contribution of MAOC to the SOC pool. Straw return improved the P status of the saline soil by increasing soil available P (14.80%), organic P (35.91%) and Ca2-P contents (4.68%). The structural equation model showed that straw and P applications could promote maize growth (indicated by dry matter weight, P accumulation, antioxidant enzyme activity and MDA content) through improving soil C and P availabilities.
Conclusion:
This study provides evidence that straw return together with adequate P supply in saline soil can promote crop nutrient accumulation, attenuate the oxidation damage on crop growth, and be beneficial for SOC turnover and soil P activation.
1 Introduction
Saline soils are widely distributed in the world, with a total area of approximately 833 million hectares, accounting for 8.7% of the world’s land area (). The fertility and productivity of saline soil are usually low, which affects regional economic and social development. It is estimated that on average, 3.47 t of soil organic carbon (SOC) is lost per hectare of soil due to salinization (). On one hand, salt may reduce the productivity of crops, thereby reducing plant residue contributions to soil organic matter (SOM) (); on the other hand, the saline soil usually has a high sodium ion content, which leads to dispersion of soil particles and is not conducive to the formation of soil aggregates, thus weakening the physical protection of SOC and aggravating its loss. The application of organic materials, such as crop straw, manure, or compost, are widely applied as management measures to increase soil carbon (C) and reduce salinization (; ; ).
Straw return is considered a reliable measure to improve the quality of saline soil (), which can significantly ameliorate the physical, chemical and biological characteristics of the soil and promote crop growth in a relatively short term (; ). After entering the soil, the straw will be fragmented, decomposed and participate in the formation of different C fractions under the combined effects of biological and abiotic factors. Among the SOC fractions, particulate organic carbon (POC), which is susceptive to environmental change and represents unstable C components, can accumulate rapidly in the soil and can be used as an early indicator of the change in SOC (; ), and mineral-associated organic carbon (MAOC), which can exist in soil for a long time, is considered to be an important component maintaining the stability of the C pool and contributing to global climate change mitigation (). Previous studies generally found that straw return could increase the content of unstable C components such as POC and easily oxidizable organic carbon (EOC) () and that of MAOC () in saline soils. However, for the proportions of SOC fraction, the straw return might increase (; ), be unaffected, or decrease () the contribution of POC to SOC.
Nutrient availability may be an important factor affecting soil C fractions allocation. An abundant supply of phosphorus (P) and nitrogen (N) has been shown to be necessary for the growth of soil microorganisms and to increase SOC sequestration (). Some studies found that POC and MAOC contents increased with increasing N addition (). The meta-analysis also showed that the C and N contents of the substrate could strongly affect the POC and MAOC contents (). However, it has not been reported whether the composition of SOC fractions is affected by P availability under the condition of straw return in saline soil.
Nutrient availability is also an important factor affecting crop productivity. Saline soil has a low organic matter content and weak capacity for nutrient retention and supply and generally cannot provide enough nutrients for crops (). The saline soil of the Yellow River Delta is developed from the alluvial parent material of the Yellow River. Due to the high content of calcium carbonate in the soil, the fixation of soil water-soluble P (i.e., soil available P is transformed into insoluble P components such as Ca-P) is quite strong in this region (), thus causing P deficiency in crops and making them more vulnerable to salt stress. A recent study by suggests that straw return combined with P fertilizer application can increase the phosphorus activation coefficient (i.e., the proportion of soil available P to total P) and improve the soil available P content in coastal saline soil. However, some studies do not support a clear effect of straw return on soil P availability (). Furthermore, found that straw return (20 years) showed a significant increase in subtropical paddy soil P accumulation (13% ~ 20%) but had no significant influence on inorganic P fractions. At present, it is still unclear how straw return affects P fraction distribution in saline soil and whether it can alleviate salt stress on crop growth.
Saline soils in the Yellow River Delta account for more than 70% of its terrestrial area () and pose a great threat to soil fertility and crop production. In recent years, the comprehensive development and utilization of saline soils in the Yellow River Delta has become a national strategy in China. In this study, regarding the typical saline soil in the Yellow River Delta as the research object, the effects of straw return combined with P fertilizer on maize growth, soil C fractions and soil P fractions were investigated. The objectives of this study were (1) to clarify how straw return and P application affect maize growth and resistance to salt stress, (2) to analyze the effects of straw return and P application on SOC fractions, and (3) to explore whether P fraction allocation in saline soil varies with straw return level. We hypothesized that (1) the combination of straw return and P fertilizer application could promote maize growth and enhance the activity of plant antioxidants; (2) straw return would increase the proportion of soil readily available organic C (POC and EOC) and decrease that of MAOC, while P application would weaken this effect because the increase in P availability promotes microbial proliferation and increases the uptake of readily available organic C by microorganisms (; ); and (3) straw returning could improve the P availability in saline soil, as indicated in most other soils ().
2 Materials and methods
2.1 Soil and straw used
The saline soil used in this study was collected from the 0~20 cm soil layers of medium-salinity soil at the Wudi experimental station of Shandong Agricultural University (demonstration center of the “Bohai Granary” project), Binzhou, Shandong Province, China (37°54′40″-37°57′38″ N, 117°54′21″-117°56′40″ W) in September 2019. The soil has a silt texture comprising 7.1% sand (> 0.05 mm), 80.9% silt (0.002~0.05 mm) and 12.0% clay (< 0.002 mm) and was classified as Fluvic Cambisols (FAO soil classification). The basic physical and chemical properties of the study soil were as follows: pH 8.55, SOM 9.16 g kg-1, total N 0.63 g kg-1, available P 26.56 mg kg-1, available potassium (K) 232.67 mg kg-1 and electrical conductivity at a soil:water ratio of 1:5 (EC1:5) 1033.58 μs/cm. After collection, the soil was air-dried and finely ground to remove vegetation and stones and then passed through a sieve (2 mm). The wheat straw used in the pot experiment was oven-dried and ground through a 2 mm sieve. The straw contained 0.88% N, 0.14% P and 1.16% K.
2.2 Experimental design
The maize pot experiment was conducted at the experimental station of Shandong Agriculture University (36°17′ N, 117°15′ E). Six treatments with four replicates were set up: control (CK, without straw or P application), conventional P application (CP), high P application (HP), straw return (S), straw return with conventional P application (SCP), straw return with high P application (SHP). Briefly, one maize (Zea mays L., Ziyu 2) seedling was planted in a plastic basin (upper inner diameter 32 cm, lower inner diameter 26 cm, height 29 cm) filled with 15 kg of air-dried soil. The specific amounts of chemical fertilizer and straw are shown in Table 1. N fertilizer had a basal to the topdressing ratio of 1:1, and P and K fertilizers were all used as basal fertilizers. Topdressing was carried out at the big flare stage of maize. Fertilizers are urea (N 46%), diammonium phosphate (N 15%, P2O5 42%) and potassium sulfate (K2O 50%). Seeds were sown on July 11th, 2020 and emerged on July 18th, 2020.
Table 1
| Treatments | Wheat straw | N | P2O5 | K2O | |
|---|---|---|---|---|---|
| Basal | Top dressing | ||||
| CK | 0 | 112.5 | 112.5 | 0 | 75 |
| CP | 0 | 112.5 | 112.5 | 150 | 75 |
| HP | 0 | 112.5 | 112.5 | 300 | 75 |
| S | 6200 | 112.5 | 112.5 | 0 | 75 |
| SCP | 6200 | 112.5 | 112.5 | 150 | 75 |
| SHP | 6200 | 112.5 | 112.5 | 300 | 75 |
Fertilizer and straw application rates in the pot experiment (kg hm-2).
2.3 Nutrient accumulation
At the mature stage of maize growth, the maize plant was destructively sampled, washed with distilled water, and separated into three parts: root, straw (including stem, leaf and corn cob) and grain. The root, straw and grain were oven-dried at 75°C, weighed, and then milled. The total N, P and K contents in each part were determined by the Kjeldahl method, vanadium-molybdenum yellow colorimetric method and flame atomic absorption spectrophotometry method, respectively ().
2.4 Antioxidant enzyme activities and MDA content
Fresh leaves (the ear leaf) of maize were taken at the tasseling stage for the determination of leaf antioxidant enzyme activities and malondialdehyde (MDA) content. Specifically, 0.2 g of fresh leaves were placed in a precooled mortar, and 1.8 mL phosphate buffer (pH = 7.8) was added to the ice bath to grind the leaves into a homogenate. The grinding solution was transferred into a 2 mL centrifuge tube and centrifuged at 12000 r·min-1 for 10 min at 4°C. The supernatant, which was the crude enzyme extract, was stored at -20°C for further use for the determination of peroxidase (POD) and superoxide dismutase (SOD) activities. Alternatively, the phosphate buffer used above was replaced with saline extract to obtain the enzyme extract for the determination of catalase (CAT) activity. The extract was replaced with the extract from the MDA kit, and the obtained enzyme extract was used for the determination of MDA content.
Then, the enzyme extracts were further processed for POD, SOD, CAT and MDA measurements using A084-3-1, T001-1, A007-1-1 and A003-3-1 kits (Nanjing Jiancheng Bioengineering Institute), respectively. Finally, the absorbance values were measured at 420 nm, 550 nm, 405 nm and 532 nm using a plate reader (Synergy HTX, BioTek, USA).
2.5 Determination of soil C and P fractions
After the maize plant was harvested, soil samples were collected, air-dried, and ground through 10 mesh, 20 mesh and 100 mesh sieves as needed to determine the contents of C fractions (including POC, MAOC and EOC) and P fractions (including soil organic P, inorganic P and available P). The soil EOC content was determined by the 0.02 mol·L-1 KMnO4 oxidation method (). Briefly, 5 g air-dried soil was mixed with 20 mL 0.02 mol·L-1 KMnO4 solution and shook at 200 pm for 2 min, then centrifuged at 3000 rpm for 5 min. The supernatant was transferred and diluted, and the absorbance value was determined at 550 nm. Soil POC and MAOC content was measured by wet sieving-K2Cr2O7 oxidation method: 20 g air-dried soil which passed through 2 mm sieve was dispersed in 100 mL sodium hexametaphosphate (5%) for 18 h, and then sieved through a 53 μm sieve, the particles remaining on the sieve is POC fraction, and the particles passed through the 53 μm sieve is MAOC fraction. The POC fraction was oven-dried at 65°C for 48 h and then determined by the K2Cr2O7 oxidation method. MAOC was calculated by subtracting the POC content from the SOC content ().
Soil available P (AP) was extracted with 0.5 mol L-1 NaHCO3 and determined by the molybdenum antimony colorimetric method (). Inorganic P fractions were classified by the grading method for calcareous soils (). Briefly, 1 g of soil was extracted sequentially by 0.25 mol·L-1 NaHCO3 solution, 0.5 mol·L-1 NH4OAc solution, 0.1 mol·L-1NaOH - 0.1 mol·L-1 NaCO3 solution, a mixed solution of 40 mL 0.3mol·L-1 C6H5Na3O7 and 10 mL 0.5 mol·L-1 NaOH, 0.5 mol·L-1 1/2 H2SO4 solution and then measured by molybdenum blue colorimetric method to obtain Ca2-P content, Ca8-P content, Al-P content, Fe-P content, O-P and Ca10-P in turn. Organic P was determined by the Scorching method (). Briefly, both the soil subsample scorched at 550°C (to convert organic P into inorganic P) and the soil subsample without scorching were leached with 0.2 mol·L-1 1/2 H2SO4 solution, and the inorganic P content was determined. The difference in inorganic P content between the scorched and unscorched subsamples was the organic P content.
2.6 Statistical analysis
Statistical analyses were conducted using SPSS 18.0 (SPSS Inc., Chicago, IL, USA) and R v.4.3.1 software (http://cran.r-project.org). All figures were drawn with Origin 2017 software (Origin Lab Inc., Northampton, MA, USA). Normal distribution and chi-square tests were performed on the data before analysis and logarithmic conversion was performed if necessary. Significant differences in dry matter weight (Dw), N accumulation (Na), P accumulation (Pa), K accumulation (Ka), CAT, POD, SOD, MDA, soil C fractions and soil P fractions among treatments were tested by one-way and two-way analysis of variance (ANOVA) followed by Duncan’s multiple range test. The effects of straw return, P addition, soil C and P fractions on plant growth factors (antioxidant enzyme activity, MDA content, nutrient accumulation and Dw) were fitted using structural equation model. The structural equation model was analyzed at Amos 28.0 (SPSS Inc., Chicago, IL, USA). The response ratio (RR) of each variable to straw returning (or P addition) was calculated as the ln-ratio of the value in the straw returning (or P addition) treatment to that in the corresponding control. One-sample T test was used to test the significant differences between the RR value and value “0”. Statistical significance was set at p < 0.05. All data are presented as the mean ± standard error (SE).
3 Results
3.1 Dry matter weight and nutrient accumulation of maize
The addition of straw had no significant effect on maize dry matter weight but increased N, P and K accumulations by 11.21%, 38.62% and 14.13%, respectively (p < 0.05) (Figure 1; Supplementary Figure 1). The RRs of nutrient accumulations to straw addition were highest in no P fertilizer (Non-P) level (Supplementary Figure 1). Dry matter weight and nutrient accumulations increased with increasing P application rate, but the trends were not consistent across the different straw conditions: the accumulation of N, P and K all showed high application rate of P fertilizer (HP) = conventional application rate of P fertilizer (CP) > Non-P under the condition without straw addition and showed HP > CP = Non-P under the condition with straw addition (p < 0.05) (Figure 1). Generally, HP soils had higher RRs of dry matter weight and nutrient accumulations than CP soils (Supplementary Figure 2).
Figure 1
3.2 Antioxidant enzyme activity and MDA content of maize plants
Straw application reduced the activities of POD, SOD, CAT and the content of MDA in maize plants by 31.69%, 38.99%, 45.96% and 27.04%, respectively (p < 0.05) (Figure 2). The RRs of POD, SOD, CAT and MDA to straw return was negative (Supplementary Figure 1). SOD activity, POD activity and MDA content decreased with increasing P application rate in the absence of straw. In treatments with straw addition, the MDA content of the S treatment was 48.65% and 77.89% higher than that of the SCP and SHP treatments, respectively (p < 0.05) (Figure 2). In straw-absent soils, the RRs of POD, SOD and MDA to P addition were much greater under HP level than under CP level (Supplementary Figure 2A).
Figure 2
3.3 SOC content and fractions
The SOC, EOC, POC contents and POC/SOC ratio in straw-added soils were on average 9.07%, 10.23%, 17.00% and 7.27% higher than those in non-straw soils, while the corresponding MAOC content and MAOC/SOC ratio were much lower (p < 0.05) (Figures 3, 4). EOC/SOC ratio had no difference among all treatments (Figure 4). The effects of P application rate on soil C fraction were different with C fractions and straw return levels: under the condition without straw addition, there was no significant difference in soil EOC content among the three P application rates, but the POC content of the CP and HP treatments was 10.31% and 15.18% higher than that of the CK treatment, respectively; under the condition of straw addition, the soil EOC and POC contents increased with increasing P application rate, but no significant change in EOC/SOC or POC/SOC was found. Regardless of the straw addition levels, P application tended to decrease soil MAOC content and MAOC/SOC ratio (p < 0.05) (Figure 4).
Figure 3
Figure 4
3.4 Soil phosphorus fractions
The effects of straw return on soil P fractions varied with P application rates and P fraction types. For soils without P addition, the contents of AP, organic P and total inorganic P (TIP) were not affected by straw return, whereas positive effects were found in P-added soils. The soil AP content of the SCP and SHP treatments was 19.52% and 15.52% higher than that of the CP and HP treatments, respectively, and the corresponding increases in the soil organic P content were 34.44% and 65.59%, respectively. Straw return raised the soil TIP content by 3.63% and 3.60% at the CP and HP application rates, respectively (p < 0.05) (Figure 5; Supplementary Table 1). Except for Ca2-P, the proportions of inorganic P fractions to TIP were not affected by straw return (p > 0.05) (Supplementary Table 1). With the increase in the P application rate, the proportions of Ca2-P and O-P to TIP increased, while the proportion of Ca10-P decreased.
Figure 5
3.5 Factors affecting maize dry matter weight
A structural equation model (SEM) was conducted to fit the relationships among plant growth factors, soil C and P fractions (Figure 6). The results showed that straw return, P addition, AP, and soil C fractions showed negative effects on MDA, with AP showing the greatest negative effect on that. These variables, together with antioxidant enzyme, explain 86% of the total variance in MDA. Straw return, P addition, AP, soil C fractions, MDA and P accumulation showed positive effects, while antioxidant enzymes showed negative effects on Dw. Particularly, P accumulation had the largest positive effect on Dw. Generally, straw return and P addition altered antioxidant enzyme levels, MDA content, nutrient accumulation and dry matter weight of maize plants through changing soil C fractions (EOC and POC) and P availability.
Figure 6
4 Discussion
4.1 Effect of straw and P applications on dry matter weight and nutrient accumulation of maize
Our results showed that straw addition had no significant effect on the dry matter weight of maize but significantly increased N, P and K accumulations (p < 0.05) (Figure 1; Supplementary Figure 1), indicating that straw return can effectively improve nutrient use efficiencies. This may be because straw return provides more substrates for microbes and stimulates microbial activity, which accelerates the process of nutrient mineralization by microorganisms and increases the nutrient availability of the soil, which in turn increases the nutrient accumulation of maize. It was confirmed by the finding of that straw addition increased the contents of available N (AN), available P (AP) and available K (AK) in saline soils. Our results showed that straw return is an important measure to improve crop growth and nutrient uptake in saline soil.
In this study, a high application rate of P (HP) increased the N, P and K accumulations and dry matter weight of maize regardless of straw return, while the conventional application rate of P (CP) only increased the N, P and K accumulations of maize when straw was not applied (Figure 1; Supplementary Figure 2). Considering the high content of CaCO3 in saline soils of the Yellow River Delta, which strongly fixes water-soluble P and reduces soil P availability (), it is reasonable to obtain the result that P addition (regardless of the conventional or high application rate) promotes maize growth and nutrient accumulation. However, the promoting effects of conventional P application on plant nutrient accumulation might be covered by the straw return management, because straw return not only bring plant-derived P into soil but also active soil original P.
4.2 Effect of straw and P applications on antioxidant enzyme activity and MDA content of maize
It is well known that SOD, CAT, POD and MDA are all major indicators of crop stress tolerance, in which SOD, CAT and POD can breakdown the peroxides and superoxide anions produced in plants and mitigate the physiological damage caused by environmental stresses, and MDA (one of the products of lipid peroxidation) can reflect the extent of oxidative damage to the cell membrane (). Our data showed that straw return significantly reduced SOD, CAT, POD activities and MDA content in maize leaves (p < 0.05) (Figure 2; Supplementary Figure 1). This may be because straw addition increases soil cation exchange capacity (CEC) and ion adsorption capacity, thereby reducing the soluble salt content of the soil and decreasing the salt stress to maize (). Previous study by found that straw application in an Orthic Anthorsols reduced the MDA content of the crop but induced an increase in both SOD and POD activities. We speculate that this inconsistency is related to the fact that the plants experienced environmental stress in our study but not in their study (). Furthermore, the organic acids produced during straw decomposition could promote the production of soil exchangeable Ca2+, which is beneficial for increasing cell membrane stability. Therefore, the plant is less physiologically damaged, and the antioxidant enzyme activity is reduced after straw return.
The POD and SOD activities of maize decreased with increasing P application rates in the absence of straw; however, no significant difference in antioxidant enzyme activities (i.e., SOD, POD, CAT) was found among the different P fertilizer levels after straw addition (p > 0.05) (Figure 2; Supplementary Figure 2). This may be because straw return reduces the salt stress to the crop and downregulates the activity of antioxidant enzymes, as mentioned above; thus, the antioxidant levels of the crop were not sensitive to P application. The MDA content decreased with increasing P application rate in our study (Figure 2D), confirming the stabilizing effect of P fertilizer on cell membrane structure ().
4.3 Effect of straw and P applications on SOC fractions
Our results showed that straw addition increased the contents of SOC, EOC and POC, and decreased the content of MAOC (Figures 3, 4). also found that straw return can enhance the unstable C fraction (i.e., POC, EOC) of soil. This may be attributed to the fact that the labile C fraction is more sensitive to field management practices and the high level of polysaccharides (cellulose and hemicellulose) in straw (). The effect of straw return on MAOC content has great variability. For instance, found that straw return could increase MAOC content in low-salinity soil and medium-salinity soil, whereas found that straw return may have either increased, decreased, or no significant effect on MAOC content under three different climates. It was found that straw addition increased the proportion of POC in SOC, while decreased that of MAOC in SOC (Figure 4). The decrease in MAOC content and MAOC/SOC may be due to the positive priming effect of SOC mineralization caused by straw addition, as indicated by the finding of that the positive priming effect was accompanied by a decrease in MAOC content. Straw return might lead to more MAOC decomposition rather than synthesis in saline soils, partly because excess Na+ can dislodge organic matter from clay particles.
We found that P application (particularly at a high rate) led to an increase in EOC and POC content (Figure 4). This may be attributed to the following reasons: i) P addition stimulates soil microbial activity () and increases the synthesis of extracellular enzymes (), and ii) P application promotes desorption of organic C adsorbed on soil colloids and alleviates microbial C limitation (), thus accelerating the turnover of soil C pools and resulting in more active and less stable C fractions (). Our results showed that P application decreased the contribution of MAOC to the SOC pool (Figure 4). Similar to our findings, found that P addition decreases the contribution of microbial residuals, which are considered to be the predominant source of MAOC (), to the SOC pool, indicating that P application may reduce SOC stability.
4.4 Effect of straw application on soil P availability
Straw addition generally increased soil P availability in our study, as indicated by the increases in soil available P, organic P and Ca2-P contents (p < 0.05) (Figure 5; Supplementary Figure 1; Supplementary Table 1), showing a strong ability to activate soil P. Soil P availability depends mainly on the dissolution of stationary P (i.e. insoluble P compounds in the soil and P held in clay particles) and the mineralization of organic P (). Straw return can significantly improve soil hydrothermal conditions (i.e., soil moisture and soil temperature) (), increase organic acid exudation (), and effectively enhance microbial proliferation and promote phosphatase production (), thus directly or indirectly affecting the soil P activation process. Our results are consistent with the findings of ; in saline soil and andosol, respectively.
4.5 Factors affecting the growth of maize plants
The SEM results showed that SOC fractions (including EOC and POC) had a high negative standardized total effect on antioxidant enzyme (including SOD and POD) activities of plants, and soil AP was negatively correlated with plant MDA content (Figure 6), suggesting an important role of SOC fractions and P availability in plant resistance to salt stress. In addition, AP had the highest and positively standardized total effect on plant P accumulation (Figure 6). These results reflected the improvement effect of P on plant growth. Saline soil in the Yellow River Delta is characterized by severe P deficiency and low biological productivity. The addition of straw and P fertilizer increased soil AP content, thereby improving the absorption of P by maize and promoting plant growth (). Our results echoed the findings of that the combined application of P and organic amendments could reduce the negative impact of salt on wheat and increase the accumulation of P, thus improving the yield and quality of wheat.
5 Conclusion
In this study, straw return with P application (particularly at a high rate) improved the nutrient accumulations of maize and alleviated the oxidative damage of maize plants from salt stress. Both straw return and P supply increased the POC content of saline soils while decreased the contribution of MAOC to SOC, indicating the acceleration of SOC turnover. Meanwhile, straw return improved soil P availability, as suggested by the increases in the contents of soil available P and organic P. The reduction effects of P application on plant antioxidant enzyme activities were buffered, while the increasing effect of that on soil P availability was enhanced by straw return. These results suggest that straw return together with adequate P supply could play important roles in alleviating oxidation damage on plants and activating the C and P pools of saline soils (Figure 7). Future studies should pay more attention to the microbial participation mechanisms in these processes for a better understanding of soil C-P interactions, and on the other hand, long-term open field experiment should be conducted to test the generality of these findings.
Figure 7
Statements
Data availability statement
The original contributions presented in the study are included in the article/Supplementary Material. Further inquiries can be directed to the corresponding authors.
Author contributions
ZG: Data curation, Formal analysis, Investigation, Writing – original draft. WY: Data curation, Formal analysis, Investigation, Writing – original draft. HW: Conceptualization, Funding acquisition, Project administration, Writing – review & editing. WH: Formal analysis, Writing – original draft. YT: Visualization, Writing – original draft. GH: Resources, Writing – review & editing. YL: Methodology, Writing – review & editing. HP: Software, Writing – review & editing. QY: Software, Writing – review & editing. YZ: Conceptualization, Funding acquisition, Project administration, Writing – review & editing.
Funding
The author(s) declare financial support was received for the research, authorship, and/or publication of this article. National Key R&D Program of China (2021YFD190090207, 2021YFD190090101), Natural Science Foundation of Shandong Province (ZR2021MD020), and Major Science and Technology Innovation Projects in Shandong Province (2021CXGC010804).
Conflict of interest
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
Publisher’s note
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.
Supplementary material
The Supplementary Material for this article can be found online at: https://www.frontiersin.org/articles/10.3389/fpls.2024.1336300/full#supplementary-material
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Summary
Keywords
straw return, P addition, antioxidant enzyme, particulate organic carbon, soil P availability, saline soil
Citation
Guo Z, Ye W, Wang H, He W, Tian Y, Hu G, Lou Y, Pan H, Yang Q and Zhuge Y (2024) Straw and phosphorus applications promote maize (Zea mays L.) growth in saline soil through changing soil carbon and phosphorus fractions. Front. Plant Sci. 15:1336300. doi: 10.3389/fpls.2024.1336300
Received
10 November 2023
Accepted
03 January 2024
Published
19 January 2024
Volume
15 - 2024
Edited by
Junjie Lin, Zhejiang University of Science and Technology, China
Reviewed by
Kailou Liu, Jiangxi Institute of Red Soil, China
Xiao Liu, Ludong University, China
Updates
Copyright
© 2024 Guo, Ye, Wang, He, Tian, Hu, Lou, Pan, Yang and Zhuge.
This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Hui Wang, huiwang@sdau.edu.cn; Yuping Zhuge, zhugeyp@sdau.edu.cn
†These authors have contributed equally to this work and share first authorship
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