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生态学杂志 ›› 2026, Vol. 45 ›› Issue (7): 2156-2165.doi: 10.13292/j.1000-4890.202607.011

• ·矿区生态过程与生态修复专栏· (专栏组织专家: 伍松林、王少锋、王美娥、刘允佳) • 上一篇    下一篇

碎石含量和入渗水量对废石场优先流的影响

熊姝臻1,梁佳星2,罗根华3,吕刚1*


  

  1. 1辽宁工程技术大学环境科学与工程学院, 辽宁阜新 123000; 2沈阳农业大学林学院, 沈阳 110866; 3毕节职业技术学院, 贵州毕节 551700)
  • 出版日期:2026-07-10 发布日期:2026-07-08

Influence of gravel content and infiltration volumes on the preferential flow of waste rock.

XIONG Shuzhen1, LIANG Jiaxing2, LUO Genhua3, Lv Gang1*   

  1. (1School of Environmental Science and Engineering, Liaoning Technical University, Fuxin 123000, Liaoning, China; 2College of Forestry, Shenyang Agricultural University, Shenyang 110866, China; 3Bijie Vocational and Technical College, Bijie 551700, Guizhou, China).

  • Online:2026-07-10 Published:2026-07-08

摘要: 阐明废石场边坡内部优先流发育特征,对优化废石场复垦方案,提升其长期稳定性具有关键作用。本研究以辽宁省阜新市恒泰铁矿为对象,采用室内染色示踪试验和统计分析相结合的方法,分析2~7 cm碎石粒径条件下,不同碎石含量(65%、75%、85%)及入渗水量(90、120、150 mm)对优先流发育的影响,借助图像处理技术,基于多个指标对碎石土优先流发育情况进行评价。结果表明:(1)碎石含量对优先流发育具有双重调控作用,碎石含量65%条件下,优先流发育受到抑制,表现为染色形态变异系数最大而优先流比、长度指数及总染色面积比均为最小;随碎石含量增加,优先流发育显著增强,当碎石含量达85%时,呈现最优优先流发育特征。(2)入渗水量是驱动优先流发育的关键动力,不同碎石含量条件下,入渗水量从90 mm增加至150 mm时,优先流比和长度指数均显著增加,染色形态变异系数显著降低(P<0.01)。(3)碎石含量75%是优先流发育的临界阈值,≤75%时主要为水力驱动控制,>75%时基质作用为主导。(4)优先流比、长度指数、总染色面积比均与染色形态变异系数呈负向线性关系(P<0.01),四者共同构成了优先流发育的整体特征。(5)四阶多项式函数能较为准确描述优先流的非线性衰减特征。综上,优先流发育过程中会形成碎石含量入渗水量“双阈值”调控机制,碎石含量85%与入渗水量150 mm共同作用下,可实现最优水分运移,而75%碎石含量为调控水力驱动与基质作用的平衡点。


关键词: 工程堆积体, 碎石土, 优先流, 土壤入渗, 染色示踪

Abstract: Elucidating the development characteristics of the preferential flow within waste rock slopes is crucial for optimizing the reclamation plans and enhancing long-term stability. This study was conducted on the Hengtai Iron Mine in Fuxin City, Liaoning Province. By combining laboratory staining and tracer tests, the effects of gravel contents (65%, 75%, 85%) and infiltration volumes (90, 120, 150 mm) on preferential flow development were analyzed under the conditions of gravel particle size ranging from 2 to 7 cm. Using image processing technology, the preferential flow in gravel soil was evaluated through multiple indicators. The results showed that: (1) The gravel content had a dual regulatory effect on preferential flow development. Under the gravel content of 65%, preferential flow development was inhibited, characterized by the highest coefficient of variation in staining morphology but the lowest preferential flow ratio, length index, and total staining area ratio. As the gravel content increased, preferential flow development significantly intensified. The optimal preferential flow development characteristics were observed when gravel content reached 85%. (2) Infiltration volume was the key driving force for the development of preferential flow. Under different gravel contents, when the infiltration volume increased from 90 mm to 150 mm, both the preferential flow ratio and length index significantly increased, but the coefficient of variation of staining morphology significantly decreased (P<0.01). (3) The gravel content of 75% was a critical threshold for preferential flow development. When it was ≤75%, preferential flow development was mainly controlled by hydraulic drive, and when it was >75%, matrix action was dominant. (4) The preferential flow ratio, length index, and total dye coverage all exhibited a negative relationship with the coefficient of variation of staining morphology (P<0.01), collectively forming the comprehensive characteristics of preferential flow development. (5) Fourth-order polynomial function could accurately describe the nonlinear attenuation characteristics of preferential flows. In conclusion, a dual threshold regulation mechanism of gravel content and infiltration volume is formed during the development of preferential flow. Under the combined action of gravel content of 85% and infiltration volume of 150 mm, optimal water transport can be achieved, while 75% gravel content is the balance point for regulating hydraulic drive and matrix action.


Key words: engineering deposit, gravel soil, preferential flow, soil infiltration, staining tracer