• ISSN 1008-505X
  • CN 11-3996/S

连续施用外源硅对红壤性水稻土硅组分和土壤性质的影响

Effects of continuous application of exogenous silicon on silicon fractions and soil properties in red paddy soil

  • 摘要:
    目的 我国南方红壤性水稻土普遍存在酸化、有效硅不足等问题,制约水稻高产稳产。本研究通过连续施用有机与无机外源硅,探究其对红壤性水稻土硅组分和土壤性质的影响及相互作用关系,为协同提升红壤稻田地力提供理论依据。
    方法 在江西省红壤及种质资源研究所采集红壤性水稻土,于2023及2024年连续开展两年4茬水稻盆栽试验。硅处理包括:硅酸钠(NaSi)、稻草(S)、稻壳生物炭(RBC)和竹叶生物炭(BBL)。于每茬早、晚稻收获前1天,用土钻在盆栽桶内垂直、均匀取3钻,测定土壤有效硅及各硅组分含量、团聚体组成,以及有机碳、碱解氮、有效磷、速效钾、阳离子交换量(CEC)、交换性钾钠和非晶态铁铝含量。
    结果 施用外源硅不同程度地提高了土壤有效硅、可移动态硅、吸附态硅、有机结合态硅和(氢)氧化物结合态硅含量,增加了土壤中硅的有效性,提高了团聚体的稳定性。硅酸钠对有效硅含量和有效性的提升效果显著优于3个富硅有机物料处理,且有效硅含量增幅从第1茬的62.42%提升到第4茬的267.6%。与CK相比,连续施用硅酸钠提高了土壤团聚体平均重量直径(MWD)和>0.25 mm粒级团聚体的占比(R0.25),土壤pH值增加了1.35~2.40个单位,速效钾、交换性钾含量分别提高了1.27~4.59、1.31~2.29倍,提高了非晶态铁12.14%~19.96%、非晶态铝6.43%~8.82%。3个有机硅源(S、RBC、BBL)均不同程度地提高了土壤有机碳、碱解氮和有效磷含量,2024年晚稻季S和RBC处理土壤MWD值显著高于BBL和NaSi处理。各有机硅源提升有机碳含量的效果表现为BBL>S>RBC,提升碱解氮的效果表现为S>RBC>BBL;S和RBC处理提升有效磷含量的效果相近,BBL对有效磷无显著影响;3个有机硅源对速效钾和交换性钾、钠均无显著影响。相关分析表明,土壤可移动态硅和吸附态硅含量与土壤pH、交换性钾钠、非晶态铝、有效硅含量呈极显著正相关(P<0.01),与非晶态铁含量呈显著正相关(P<0.05)。(氢)氧化物结合态硅含量与土壤有效磷、碱解氮、阳离子交换量呈极显著正相关(P<0.01)。
    结论 连续施用外源硅可提高红壤性水稻土pH、有效硅含量及其有效性,提升土壤结构稳定性。施用硅酸钠可快速、累积性提升有效硅含量和其有效性,提高速效钾含量,但对有机碳无提升作用,且会降低有效磷含量。施用富含硅的有机物料对土壤有效硅供应能力的提升效果弱于硅酸钠,但可提高土壤有机碳含量,增加速效氮、磷含量,更有效提高土壤结构的稳定性。因此,应协同施用有机无机硅源,以提升红壤硅素营养和肥力水平。

     

    Abstract:
    Objectives Acidification and inadequate available silicon were widespread constraints limiting high and stable rice yields in the red paddy soils of southern China. This study investigated the effects of continuous application of organic and inorganic silicon sources on soil silicon fractions, soil properties, and their interactions in red paddy soil, aiming to provide a theoretical basis for the coordinated improvement of soil fertility in red paddy fields.
    Methods Red paddy soil was collected from the Jiangxi Academy of Red Soil and Germplasm Resources. A two-year pot experiment with four consecutive rice crops was conducted in 2023 and 2024. The silicon treatments included sodium silicate (NaSi), rice straw (S), rice husk biochar (RBC), and bamboo leaf biochar (BBL). Soil samples were collected one day before the harvest of each early and late rice crop. Three vertical and evenly distributed soil cores were taken from each pot using a soil auger. The contents of soil available Si and different Si fractions, soil aggregate composition, soil organic carbon, alkali-hydrolyzable nitrogen, available phosphorus, available potassium, cation exchange capacity (CEC), exchangeable K and Na, and amorphous Fe and Al were analyzed.
    Results The application of exogenous silicon increased the contents of soil available silicon, mobile Si, adsorbed Si, organically bound Si, and oxide/hydroxide-bound Si to varying degrees, thereby enhancing soil silicon availability and improving aggregate stability. Sodium silicate showed a significantly stronger effect on increasing available silicon content and silicon availability than the three silicon-rich organic materials, with the increase in available silicon rising from 62.42% in the first rice crop season to 267.6% in the fourth rice crop season. Compared with CK, continuous application of sodium silicate increased the mean weight diameter (MWD) of soil aggregates and the proportion of aggregates >0.25 mm (R0.25). Soil pH increased by 1.35–2.40 units, while available potassium and exchangeable K increased by 1.27–4.59 times and 1.31–2.29 times, respectively. Amorphous Fe and amorphous Al increased by 12.14%–19.96% and 6.43%–8.82%, respectively.The three organic silicon sources, namely S, RBC, and BBL, increased soil organic carbon, alkali-hydrolyzable nitrogen, and available phosphorus to varying degrees. In the late rice season of 2024, the MWD values under S and RBC were significantly higher than those under BBL and NaSi. The effects of the three organic silicon sources on increasing soil organic carbon followed the order BBL > S > RBC, whereas their effects on alkali-hydrolyzable nitrogen followed the order S > RBC > BBL. The effects of S and RBC on available phosphorus were similar, while BBL had no significant effect on available phosphorus. The three organic silicon sources had no significant effects on available potassium, exchangeable K, or exchangeable Na. Correlation analysis showed that mobile Si and adsorbed Si were extremely significantly positively correlated with soil pH, exchangeable K and Na, amorphous Al, and available silicon (P<0.01), and significantly positively correlated with amorphous Fe (P<0.05). Oxide/hydroxide-bound Si was extremely significantly positively correlated with available phosphorus, alkali-hydrolyzable nitrogen, and CEC (P<0.01).
    Conclusions Continuous application of exogenous silicon increased soil pH, available Si content, and Si availability in red paddy soil, while also enhancing soil structural stability. Sodium silicate rapidly and cumulatively increased available Si content and Si availability, and improved available potassium content; however, it did not increase soil organic carbon and even reduced available phosphorus content. Although Si-rich organic materials were less effective than sodium silicate in improving soil available Si supply capacity, they showed greater advantages in increasing soil organic carbon, alkali-hydrolyzable nitrogen, and available phosphorus contents, as well as improving soil structural stability. Therefore, the combined application of organic and inorganic silicon sources is recommended to improve silicon nutrition and overall soil fertility in red paddy soils.

     

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