稻虾共作土壤溶解性有机质光谱特征及其与土壤交换态镉的关系

Spectral characteristics of dissolved organic matter in rice-shrimp co-cropping soils and their relationships with soil exchangeable cadmium

  • 摘要: 镉(Cd)是我国农田土壤污染最严重的重金属元素, 土壤溶解性有机质(DOM)对Cd在土壤环境中的迁移和转化具有重要影响, 但稻田土壤中Cd的迁移性和生物有效性与DOM光谱特征参数的关系是否受稻虾共作模式的影响尚不明确。因此, 本研究以传统稻作模式(CK)为对照, 以稻虾共作模式(RS)为研究对象, 通过紫外-可见光谱和三维荧光光谱, 解析RS模式在水稻生育期稻前期(T1)、分蘖期(T2)、孕穗期(T3)和黄熟期(T4)土壤DOM光谱特征及组成变化; 利用相关性与逐步回归模型, 建立RS和CK模式土壤DOM与可交换态镉(Cdex)含量的关系。研究结果如下: 1)与其他生育期相比, 两种模式在T4时芳香性和疏水性DOM最多; RS模式土壤DOM分子量随水稻生长呈下降趋势, 且T4时期DOM更倾向生物源。2) RS与CK模式下土壤DOM均主要由类色氨酸(C1)、腐殖质(C2和C3)和类富里酸(C4)组成, 但各组分占比在生育期无显著变化规律; CK和RS模式荧光指数(FI)均>1.9, 腐殖化指数(HIX)均<4; RS的自生源指数(BIX)为0.68~0.80, 高于CK模式(0.60~0.68), 表明两种模式DOM均具有一定程度的内源性本土特征。3)两种模式下, 土壤交换态Cd (Cdex)含量均随水稻生育期推进呈上升趋势, 但RS模式在T2—T4时期, 其Cdex含量和变化幅度均低于CK模式。两种模式Cdex含量均与光谱斜率比(SR)和类富里酸组分(C4)呈显著或极显著相关(P<0.05或P<0.01或P<0.001)表明Cdex含量与DOM腐殖化程度、分子量大小、来源及组分密切相关。逐步回归分析表明, 与DOM分子量大小相关的因子(E2/E3SR)对Cdex含量的预测具有重要影响。本研究结果可为理解稻虾共作模式对土壤Cd污染的潜在影响提供理论参考。

     

    Abstract: Cadmium (Cd) is the most severe heavy metal pollutant in China’s farmland soils. Soil dissolved organic matter (DOM) significantly influences Cd migration and transformation in soil environments, but whether the relationship between Cd mobility, bioavailability, and DOM spectral characteristics in paddy soils is affected by the rice-crayfish co-culture mode (RS) remains unclear. Therefore, this study used traditional rice cultivation (CK) as the control and RS as the research object. Through UV-Vis spectroscopy and three-dimensional fluorescence spectroscopy, we analyzed changes in DOM spectral characteristics and composition in RS-mode soils during rice growth stages pre-rice stage (T1), tillering stage (T2), booting stage (T3), and yellow maturity stage (T4). Correlation analysis and stepwise regression models were employed to establish relationships between soil DOM and exchangeable Cd (Cdex) content in RS and CK modes. The results are as follows: Compared with other growth stages, both modes exhibited the highest aromaticity and hydrophobic DOM at T4. The molecular weight of DOM in RS-mode soils showed a decreasing trend during rice growth, with DOM at T4 being more biogenic in origin. Soil DOM in both RS and CK modes primarily consisted of tryptophan-like components (C1), humic components (C2 and C3), and fulvic-like components (C4). However, the proportional distribution of these components showed no significant variation pattern across growth stages. The fluorescence index (FI) values of both CK and RS modes exceeded 1.9, while humification index (HIX) values were below 4. The biological index (BIX) of RS (0.68–0.80) was higher than that of CK (0.60–0.68), indicating that DOM in both modes possessed endogenous characteristics to some extent. Under both modes, soil exchangeable Cd (Cdex) content increased progressively during rice growth stages. However, RS mode exhibited lower Cdex content and smaller fluctuation ranges from T2 to T4 compared with CK. Cdex content in both modes showed significant or highly significant correlations (P < 0.05 or P < 0.01) with spectral slope ratio (SR) and fulvic-like components (C4), demonstrating close associations between Cdex content and DOM humification degree, molecular weight, source, and composition. Stepwise regression analysis revealed that factors related to DOM molecular weight (E2/E3 and SR) critically influenced Cdex content prediction.These findings provide theoretical references for understanding the potential impacts of rice-crayfish co-culture systems on soil Cd pollution.

     

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