长期施肥下砂姜黑土矿物结合态有机碳(MAOC)源解析
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1.中国科学院南京土壤研究所;2.安徽省农业科学院土壤肥料研究所;3.中国农业科学院农业资源与农业区划研究所

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国家重点研发计划项目(2023YFD1900201,2023YFD1900204)和中国科学院南京土壤研究所自主部署项目(ISSASIP2214)资助


Origins of Mineral-associated Organic Carbon (MAOC) Under Long-term Fertilization in a Vertisol
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Affiliation:

1.Institute of Soil Science,Chinese Academy of Sciences;2.Soil and Fertilizer Research Institute, Anhui Academy of Agricultural Sciences;3.Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences

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Supported by the National Key Research and Development Program of China (Nos .2023YFD1900201, 2023YFD1900204), and the Self-deployed Project of Institute of Soil Science, Chinese Academy of Sciences (No.ISSASIP2214)

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    摘要:

    土壤碳库中矿物结合态有机碳(Mineral-associated Organic Carbon,MAOC)的稳定性高,其组分比例的增加对提升耕地质量具有至关重要的意义。尽管长期施肥显著提升了砂姜黑土MAOC在土壤有机碳(Soil Organic Carbon, SOC)中的占比,但MAOC中植物与微生物源碳的积累特征及其对SOC的相对贡献尚不明确。本研究依托砂姜黑土长期施肥定位试验(1982—),采用生物标志物法和化学计量学法,探究了不同施肥措施[对照(CK)、单施化肥(NPK)、秸秆半量还田与化肥配施(NPKLS)和秸秆全量还田与化肥配施(NPKHS)]下耕层(0~20 cm)土壤MAOC中植物和微生物源碳的累积特征与相对贡献。结果表明,与CK处理相比,NPKHS和NPKLS处理使MAOC含量显著提高29.6%~54.3%(P < 0.05),且MAOC与SOC(R2=0.95, P<0.05)和碳投入量(R2=0.98, P<0.01)均呈显著线性正相关。植物源组分中,NPKHS处理下香草基酚类(Vanillyl phenols,V)和丁香基酚类(Syringyl phenols,S)的含量相较于CK分别增加了14.8%和13.3%,S/V和肉桂基酚类(Cinnamyl phenols,C)与香草基酚类之比C/V降低了1.27%~9.46%,但酸醛比(Ad/Al)V和(Ad/Al)S差异不显著(P>0.05)。微生物源组分中,NPKHS处理显著提高了氨基糖含量,与CK处理相比增幅高达91.4%(P<0.05)。其中,真菌残体碳(fungal necromass carbon,FNC)和细菌残体碳(bacterial necromass carbon,BNC)含量分别增加了92.7%和48.5%,并且真菌残体碳维持绝对优势(FNC/BNC=4.39)。生物标志物法表明微生物源碳贡献率高达72.6%~73.4%,而化学计量学法显示植物源碳贡献为74.0%~82.6%。与以往的草地/森林生态系统研究结果(53%~65%)相比,化学计量学法可能高估了植物源碳的贡献。综上,长期施肥主要通过增加微生物源碳积累促进了砂姜黑土MAOC的形成和稳定,对砂姜黑土区秸秆资源高效利用和耕地质量提升具有重要意义。

    Abstract:

    【Objective】Mineral-associated organic carbon (MAOC) constitutes the largest and most stable fraction of soil organic carbon (SOC), and increasing its proportion is essential for improving soil quality. Although long-term fertilization has significantly increased the MAOC proportion in SOC in Shajiang black soil, the accumulation patterns of plant- and microbial-derived carbon within MAOC, as well as their relative contributions to SOC, remain unclear. Therefore, this study aims to explore the accumulation characteristics of plant- and microbial-derived carbon and their contribution to MAOC in the 0-20 cm soil depth of Shajiang black soil under long-term fertilization. 【Method】Based on a 34-year field experiment, four treatments were established (no fertilizer and wheat straw return as CK, mineral fertilizer as NPK, mineral fertilizer with half amount of wheat straw return as NPKLS, and mineral fertilizer with full amount of wheat straw return as NPKHS). Biomarkers and chemometric methods were used to investigate the effects of long-term fertilization on plant and microbial-derived carbon in MAOC. 【Results】The results reveal that compared to CK treatment, NPKHS and NPKLS treatments significantly increased the content of MAOC by 29.6% to 54.3% (P < 0.05), with MAOC exhibiting a significant linear positive correlation with SOC (R² = 0.95, P < 0.05) and carbon input (R² = 0.98, P < 0.01). In terms of plant-derived components, the NPKHS treatment induced an increase of 14.8% and 13.3% in the contents of Vanillyl (V) and Syringyl (S) phenols, respectively, while the S/V and C/V ratios decreased by 1.27% to 9.46%. However, the differences in the acid-to-aldehyde ratios (Ad/Al)V and (Ad/Al)S were not significant (P > 0.05). For microbial-derived components, NPKHS treatment significantly elevated the amino sugar content, with an increase of up to 91.4% compared to the control (P < 0.05). Specifically, the contents of fungal residual carbon (FNC) and bacterial residual carbon (BNC) increased by 92.7% and 48.5%, respectively, with fungal necromass dominating (FNC/BNC=4.39). Biomarker analysis indicated that the microbial-derived carbon contribution rate was as high as 72.6% to 73.4%, whereas chemometric methods suggested that the plant-derived carbon contribution ranged from 74.0% to 82.6%. Compared to previous studies on grassland/forest ecosystems (53% to 65%), this proportion appears somewhat unreasonable, suggesting that the chemometric method may have overestimated the contribution from plant sources. 【Conclusion】Our findings indicate that long-term fertilization enhances the accumulation and stability of MAOC in Shajiang black soil primarily by increasing microbial-derived carbon content. This study provides an important reference for the efficient utilization of straw resources and for improving the quality of cultivated land in the Shajiang black soil region.

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俞子洲,郭自春,丁天宇,王道中,花可可,郭志斌,高 磊,彭新华.长期施肥下砂姜黑土矿物结合态有机碳(MAOC)源解析[J].土壤学报,DOI:10.11766/trxb202503120112,[待发表]
YU ZiZhou, GUO ZiChun, DING TianYu, WANG DaoZhong, HUA KeKe, GUO ZhiBin, GAO Lei, PENG XinHua. Origins of Mineral-associated Organic Carbon (MAOC) Under Long-term Fertilization in a Vertisol[J]. Acta Pedologica Sinica, DOI:10.11766/trxb202503120112,[In Press]

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  • 收稿日期:2025-03-12
  • 最后修改日期:2025-06-24
  • 录用日期:2025-07-31
  • 在线发布日期: 2025-08-25
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