不同改良材料对黄壤阳离子交换量的协同调控及贡献
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1.西南大学资源环境学院;2.重庆文理学院化学与环境工程学院

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国家重点研发计划项目(2023YFD1900300)和重庆市自然科学基金项目(CSTB2025NSCQ-LZX0021, 2024NSCQ-LZX0152)共同资助


Synergistic Regulation and Contribution of Different Amendment Materials to Cation Exchange Capacity of Yellow Soil
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1.Chongqing Key Laboratory of Interface Processes and Soil Health, College of Resources and Environment, Southwest University;2.College of Chemistry and Environmental Engineering, Chongqing University of Arts and Sciences

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Supported by the National Key R&D Program of China (No. 2023YFD1900300), the Natural Science Foundation Project of Chongqing, China (Nos. CSTB2025NSCQ-LZX0021 and 2024NSCQ-LZX0152)

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    摘要:

    土壤阳离子交换量(CEC)是评价土壤肥力与缓冲性能的核心指标,准确评估土壤CEC对土壤改良具有重要意义。以黄壤为研究对象,主要采用矿物质和电解质材料,并结合有机材料进行室内培养实验,利用离子选择电极法测定了不同pH条件下的黄壤CEC,探究改良材料对黄壤CEC的影响及贡献机制。结果表明:(1)改良材料通过提升黄壤pH影响CEC,且CEC随pH升高而增大,例如培养75 d时,pH增加了0.38~1.27个单位,增幅达6.35%~21.24%,在培养实际pH下CEC提高了4.59~13.55 cmol·kg-1,增幅达35.56%~105.00%;(2)不同类型材料对黄壤pH、CEC具有显著的协同提升效果,在pH7条件下,培养75 d的矿物质+有机质(DB3CH)材料处理的CEC较单一矿物质(D和B1)材料处理分别提高了49.57%和35.01%,电解质+有机质(KCa3H)材料处理的CEC较单一电解质材料处理(K和Ca1)分别提高了19.27%和10.37%;(3)低pH范围内,土壤颗粒对pH变化的响应更敏感,多数处理组在pH4~7区间的CEC提升较高,在高pH段CEC提升减缓;(4)改良材料对黄壤CEC的直接贡献占据主导(72.98%~90.60%),而通过提升pH的间接贡献相对较低(9.40%~27.02%)。有机质材料、电解质材料和矿物质材料分别通过官能团解离、优化吸附环境、增加永久电荷/比表面积提升黄壤CEC。本研究结果可为酸性土壤改良和肥力提升提供理论依据与实践经验,未来可进一步结合田间长期定位试验,验证实际环境条件下不同改良材料的可持续性与生态效应的协同贡献,推动黄壤耕地质量定向培育与农业绿色发展。

    Abstract:

    【Objective】Yellow soils are an important agricultural resource in China. However, the productivity of the yellow soil has been significantly altered by both climate change and anthropogenic activities. Thus, to improve the understanding of the response mechanisms of yellow soil to these changes, this study systematically evaluates the effects of mineral and electrolyte materials combined with organic matter on soil cation exchange capacity (CEC) under different pH conditions.【Methods】A soil incubation experiment was conducted using yellow soil with 14 treatment groups: (1) CK (no amendment); (2) D (dolomite, 6 gkg-1); (3) B1 (sodium-based bentonite, 2 gkg-1); (4) DB1 (dolomite 6 gkg-1 + sodium-based bentonite 2 gkg-1); (5) DB2 (dolomite 6 gkg-1 + sodium-based bentonite 4 gkg-1); (6) DB3 (dolomite 6 gkg-1 + sodium-based bentonite 6 gkg-1); (7) DB3C (dolomite 6 gkg-1 + sodium-based bentonite 6 gkg-1 + carboxymethyl cellulose 1 gkg-1); (8) DB3CH (dolomite 6 gkg-1 + sodium-based bentonite 6 gkg-1 + carboxymethyl cellulose 1 gkg-1 + potassium humate 2 gkg-1); (9) K (potassium nitrate, 0.5 gkg-1); (10) Ca1 (calcium phosphate,0.33 gkg-1); (11) KCa1 (potassium nitrate 0.5 gkg-1 + calcium phosphate 0.33 gkg-1); (12) KCa2 (potassium nitrate 0.5 gkg-1 + calcium phosphate 0.66 gkg-1); (13) KCa3 (potassium nitrate 0.5 gkg-1 + calcium phosphate 1 gkg-1); (14) KCa3H (potassium nitrate 0.5 gkg-1 + calcium phosphate 1 gkg-1 + potassium humate 2 gkg-1). The CEC under actual soil pH and varying pH conditions was determined using the ion-selective electrode method. 【Result】The results indicated that (1) the amendment materials affected CEC by increasing soil pH. For instance, at the 75th day of incubation, the soil pH increased by 0.38-1.27 pH units, with an enhancement range of 6.35%-21.24%; the CEC increased by 4.59-13.55 cmolkg-1, with an enhancement range of 35.56%-105.00%. (2) Different types of ameliorants exerted a significant synergistic effect on increasing the pH and CEC of yellow soils. For example, at pH 7.0, the CEC of the soil treated with mineral + organic matter (DB3CH) was 49.57% and 35.01% higher than that of the soil treated with single minerals (D and B1), respectively, after 75 days of incubation; while the CEC of the soil treated with electrolyte + organic matter (KCa3H) was 19.27% and 10.37% higher than that of the soil treated with single electrolytes (K and Ca1), respectively. (3) Soil particles were more sensitive to pH changes in the low pH range. The CEC of most treatments showed a substantial increase in the pH intervals of 4.0-7.0, whereas the CEC increment slowed down in the high pH range. (4) The direct contribution of amended materials to the CEC of yellow soil is dominant (72.98%-90.60%), while the indirect contribution through increasing pH is relatively low (9.40%-27.02%). 【Conclusion】Organic materials directly provide negative charges through the dissociation of functional groups; inorganic electrolyte materials optimize the adsorption environment by supplying base cations; while mineral materials increase the CEC via their high permanent charge, large specific surface area, and pH-elevating effect. The findings of this study can provide a theoretical basis and practical experience for the amelioration of acidic soils and the improvement of soil fertility. Future research could further combine long-term field in-situ experiments to verify the synergistic contributions of different ameliorative measures to sustainability and ecological effects under actual environmental conditions. This can promote the directional improvement of cultivated yellow soil quality and the green development of agriculture.

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殷萁潞,单文龙,李睿,牛佳慧,丁武泉,刘新敏.不同改良材料对黄壤阳离子交换量的协同调控及贡献[J].土壤学报,DOI:10.11766/trxb202512310626,[待发表]
YIN Qilu, SHAN Wenlong, LI Rui, NIU Jiahui, DING Wuquan, LIU Xinmin. Synergistic Regulation and Contribution of Different Amendment Materials to Cation Exchange Capacity of Yellow Soil[J]. Acta Pedologica Sinica, DOI:10.11766/trxb202512310626,[In Press]

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  • 收稿日期:2025-12-31
  • 最后修改日期:2026-06-02
  • 录用日期:2026-08-25
  • 在线发布日期: 2026-08-28
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