耕作模式对苏打盐碱土结构稳定性与玉米产量的影响

    Effect of tillage mode on structural stability and maize yield in soda saline alkali soils

    • 摘要: 为探究不同耕作模式对苏打盐碱土结构稳定性、碱化程度及玉米产量的影响,在西辽河平原开展为期2年不同耕作方式配合秸秆还田的田间试验。设置常规耕作(CK)、深翻耕作(DT)、粉垄耕作(ST)、深翻+秸秆还田耕作(DST)、粉垄+秸秆还田耕作(SST)5种处理。结果表明,相比常规耕作CK处理,其他耕作处理显著提高各土层土壤大团聚体含量(R0.25)75.9% ~ 334.7%,显著降低微团聚体(< 0.25 mm)含量6.1% ~ 24.8%(P < 0.05),有效改善苏打盐碱地土壤结构稳定性;耕作层(0 ~ 20 cm)土壤水稳性团聚体平均质量直径(mean weight diameter,MWD)高于玉米根层(>20 ~ 40 cm)和心土层(>40 ~ 60 cm),耕作层以DST处理最大,提高了85.1%,玉米根层以SST处理最大,提高了104.7%,心土层以SST处理最大,显著高于其他处理10.4%~48.9%(P < 0.05);土壤钠吸附比(sodium adsorption ratio,SAR)随土壤深度增加呈增加趋势,玉米收获后CK处理土壤SAR与背景值无显著差异(P > 0.05),土壤碱化风险大,其他处理SAR降幅为0.4% ~ 10.3%,可缓解土壤钠质化,以DST处理效果较好。4种处理2年玉米平均增产37.8% ~ 65.7%,水分利效率(water use efficiency,WUE)平均提高46.7% ~ 91.7%(P < 0.05),以DST处理效果最好。玉米产量与耕作层R0.25、根层MWD呈正显著相关(P < 0.05),与10 ~ 20 cm土层的SAR呈负显著相关(P < 0.05);WUE与耕作层R0.25MWD呈正显著相关(P < 0.05),与根层SAR呈负显著相关(P < 0.05)。综上,建议深翻+秸秆还田为苏打盐碱地适宜的耕作模式,可实现改善西辽河平原苏打盐碱地土壤结构稳定性、玉米高产高效的目标。

       

      Abstract: To investigate the effects of different tillage modes on the structural stability, the degree of alkalization and maize yield, a 2-year field experiment of different tillage methods combined with straw returning was carried out in West Liaohe Plain. Five treatments were set up in the experiment, namely conventional tillage (CK treatment), deep turning tillage (DT treatment), powder ridge tillage (ST treatment), deep turning-straw returning tillage (DST treatment), and powder ridge-straw returning tillage (SST treatment). The experimental results showed that compared with CK treatment, other tillage treatments significantly increased the soil macro-aggregate content (R0.25) by 75.9%-334.7%, and significantly decreased the soil micro-aggregate content (< 0.25 mm) by 6.1%-24.8% (P < 0.05). The change in aggregate composition effectively improved the stability of the soil structure in soda saline soils, making the soil more conducive to root growth and water-air circulation. Regarding the average mass diameter (MWD) of soil water-stable aggregates, it was determined that the value in the tillage layer (0-20 cm) was higher than that in the maize root layer (20-40 cm) and the subsoil layer (40-60 cm). Compared with CK treatment, MWD of soil water-stable aggregates with DST treatment was the largest in the tillage layer, which increased by 85.1%. The MWD with SST treatment was the highest in maize root layer, which increased by 104.7%. The MWD with SST treatment was the largest in the subsoil layer, which was significantly higher than that treated with other treatments by 10.4%-48.9% (P < 0.05). The soil sodium adsorption ratio (SAR), a crucial indicator of soil alkalization, increased with increasing soil depth. Following maize harvest, the soil SAR of CK treatment was not significantly different from the background value (P > 0.05), suggesting a high risk of soil alkalization under conventional tillage. However, the SAR of the other treatments decreased by 0.4%-10.3%, which could alleviate soil sodicity to some extent. Among these, the SST and DST treatments were more effective, suggesting that the combination of tillage and straw return could play a role in reducing soil alkalinity. Compared with CK treatment, the average maize yield of these four treatments (DT, ST, DST, and SST treatment) for 2 years increased by 37.8%-65.7% and water use efficiency (WUE) increased by 46.7%-91.7% (P < 0.05) , and DST treatment had the best effect. This showed the possibility for water-saving agriculture in soda-saline-alkaline regions in addition to demonstrating the beneficial effects of various tillage patterns on maize yield. The correlations between different components were further illustrated using correlation analysis. MWD in the rhizosphere and R0.25 in the tillage layer had a substantial and positive correlation with maize yield (P < 0.05), suggesting that high-yield maize production benefits from well-structured soil in these regions. In the 10-20 cm soil layer, it was also strongly and negatively linked with SAR (P < 0.05), indicating that high soil alkalinity in this layer may prevent maize from growing. In the tillage layer, WUE had a substantial and positive correlation with R0.25 and MWD (P < 0.05), while in the rhizosphere, it had a significant and negative correlation with SAR (P < 0.05). In conclusion, a thorough examination of the experimental data suggested that the deep turning-straw returning tillage was the suitable cultivation mode for soda saline-alkali land. In the soda-saline-alkaline soils of West Liaohe Plain, the deep turning-straw returning tillage could help stabilize the soil structure and guarantee high yield and high-efficiency maize production. It offered a scientific foundation for the long-term growth of agriculture in comparable regions.

       

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