干湿循环条件下砾石风化特征及其养分资源化潜力
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宁夏大学土木与水利工程学院

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Effect of Dry-Wet Cycles on Gravel Weathering and Topsoil Nutrient Supplement in Gravel-Mulched Farmland
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1.Ningxia University College of Civil and Water Conservancy Engineering;2.宁夏大学土木与水利工程学院

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    摘要:

    针对西北砂田覆盖层砾石在水-岩作用下风化特征及其对耕层土壤营养元素补充效应不明的问题,以连续种植30年以上且处于休耕期的退化砂田为研究对象,选取砂田中主要粒径范围的砾石,分析其物理与化学风化特征对干湿循环的响应,并揭示元素淋溶对耕层土壤营养元素的调控机制。结果表明:(1)压砂砾石以硅酸盐矿物为主,具备一定的风化潜力和养分释放能力。干湿循环条件下弱碱性水体对砾石化学风化作用有限,物理风化占主导地位。水-岩作用显著促进砾石质量损失并提高吸水效率(P<0.05),其中细粒砾石(5~10 mm)响应最为敏感,质量损失率和吸水率最高,分别为2.09%和1.70%,相较于对照组分别提高了242.11%和23.10%;(2)次生矿物之间未发生明显转化,但绿泥石因温差效应和淋溶作用在细粒级中流失最显著(下降10%)。伴随孔隙填充型富镁绿泥石的流失,耕层土壤中元素呈现不同程度富集,元素释放序列表现为:Mg>Ca>Fe>>Mn>K>Zn。(3)相关性与主成分分析进一步表明,砾石物理风化特征与土壤造岩元素含量显著相关(P<0.05),水-岩作用对砾石裂化及土壤元素组成具有显著影响。总之,干湿循环作用促进了压砂砾石的风化进程,砾石裂化过程中元素淋溶对耕层土壤营养元素具有重要调控作用,能够为改良砂田土壤环境、遏制砂田退化及实现复垦提供新视角。

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    【Objective】To address the unclear weathering characteristics of gravel of northwestern gravel-mulched farmlands under water-rock interaction and its subsequent effect on topsoil nutrient supplementation. 【Method】A semi-field experiment was conducted using degraded gravel-mulched farmland that had been fallowed after over 30 years of continuous cropping. Gravels within the predominant particle size range were selected to analyze their physical and chemical weathering responses to dry-wet cycles. Furthermore, the regulatory mechanism of element leaching on topsoil nutrients was elucidated. 【Result】The results indicated that: (1)the gravel was primarily composed of silicate minerals. Under dry-wet cycling, weakly alkaline water caused limited chemical weathering, making physical weathering the dominant process. Water-rock interaction significantly promoted gravel mass loss and increased water absorption efficiency (P < 0.05). Fine-grained gravel (5-10 mm) was the most responsive, exhibiting peak mass loss and water absorption rates of 2.09% and 1.70%, representing increases of 242.11% and 23.10% compared to the control group without dry-wet cycles. (2)Although no significant transformation was detected among secondary minerals, chlorite experienced the most substantial loss (10%) in fine-grained gravel due to temperature fluctuations and leaching. The dissolution of magnesium-rich chlorite, which primarily exists as pore fillings, led to varying enrichment of elements in the topsoil, showing a release sequence of Mg > Ca > Fe > Mn > K > Zn. (3)Correlation and principal component analyses confirmed that the physical weathering characteristics of the gravel were significantly correlated with the content of lithophilic elements in the soil (P < 0.05). 【Conclusion】In conclusion, dry-wet cycling promotes the weathering process of mulch gravel, and element leaching during breakdown plays a crucial role in regulating topsoil nutrients. This study provides new insights for improving the soil environment, mitigating degradation, and facilitating reclamation in gravel-mulched farmlands.

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黄亚浩,李 旭,安文举,李王成,张一帆,何雷.干湿循环条件下砾石风化特征及其养分资源化潜力[J].土壤学报,,[待发表]
HUANG Yahao, LI Xu, AN Wenju, LI Wangcheng, ZHANG Yifan, HE Lei. Effect of Dry-Wet Cycles on Gravel Weathering and Topsoil Nutrient Supplement in Gravel-Mulched Farmland[J]. Acta Pedologica Sinica,,[In Press]

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  • 收稿日期:2026-01-09
  • 最后修改日期:2026-07-17
  • 录用日期:2026-07-31
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