raybet体育在线 院报 ›› 2025, Vol. 42 ›› Issue (7): 150-156.DOI: 10.11988/ckyyb.20240421

• 岩土工程 • 上一篇    下一篇

裂隙岩层地下水位动态变化对降雨的响应

曹小为1,2(), 徐小涛2, 李晨3, 姜成海3, 宋林辉1()   

  1. 1 南京工业大学 数理科学学院, 南京 211800
    2 徐州地铁集团有限公司,江苏 徐州 221000
    3 中铁隧道集团二处有限公司,河北 廊坊 065201
  • 收稿日期:2024-04-24 修回日期:2024-08-22 出版日期:2025-07-01 发布日期:2025-07-01
  • 通信作者:
    宋林辉(1980-),江西高安人,教授,博士,主要从事岩土力学方面的研究工作。E-mail:
  • 作者简介:

    曹小为(1986-),安徽望江人,高级工程师,硕士,研究方向为岩土工程地下水渗流。E-mail:

  • 基金资助:
    国家自然科学基金项目(52106246); 国家自然科学基金项目(51578164)

Response of Dynamic Changes in Groundwater Level in Fractured Rock Layers to Rainfall

CAO Xiao-wei1,2(), XU Xiao-tao2, LI Chen3, JIANG Cheng-hai3, SONG Lin-hui1()   

  1. 1 School of Physical and Mathematical Sciences, Nanjing Tech University, Nanjing 211800,China
    2 Xuzhou Metro Group Co., Ltd., Xuzhou 221000, China
    3 China Railway Tunnel Group Second Division Co., Ltd., Langfang 065201, China
  • Received:2024-04-24 Revised:2024-08-22 Published:2025-07-01 Online:2025-07-01

摘要:

地下水位是地下结构工程抗浮设计的关键参数,为明确裂隙岩层中地下水位动态变化对降雨的响应规律,运用实测手段,测试得到裂隙岩层中的水位变化数据和场地的降雨量数据,并对两者进行线性拟合分析。结果表明:地下水位变化与降雨密切相关,丰水期升高、枯水期降低,水位峰谷变化幅度范围为3.34~17.55 m;另外,地下水位增量随降雨量的增长斜率在0.006~0.025之间变化,反映出地下水位变化对降雨的响应快慢不一,主要受降雨强度、场地地势、地表水系和开挖施工等因素的影响。结合岩层的透水性可给出抗浮设计建议措施,裂隙岩渗透系数>20 m/d时,地下结构需增强被动抗浮措施或增加主动排水减压措施,渗透系数在10~20 m/d时需适当增加抗浮安全系数,渗透系数<10 m/d时则按正常工况设计。研究成果可以为地铁车站抗浮设计提供参考。

关键词: 裂隙岩层, 地下水位, 降雨量, 线性拟合, 渗透系数

Abstract:

[Objectives] Large-scale urban underground space development has led to numerous anti-floating problems. Groundwater level is a key parameter in the anti-floating design of underground structures, but it is inherently dynamic and influenced by various factors. This study aims to investigate how groundwater level in fractured rock layers dynamically responds to rainfall. [Methods] Field monitoring was conducted along a subway line, with seven groundwater level monitoring points and two meteorological monitoring points installed. Real-time data of groundwater level in fractured rock layers and rainfall at the site were collected. Based on these data, the annual variation patterns of groundwater level and rainfall were analyzed. Groundwater level increments under moderate to heavy rainfall conditions (daily rainfall ≥10.0 mm) were extracted, and a linear fit was performed between rainfall and groundwater level increments. [Results] Groundwater level variations were closely related to rainfall, rising during wet periods and falling during dry periods, with peak-to-valley amplitudes ranging from 3.34 to 17.55 meters. Additionally, the slope of the linear fitting between groundwater level increment and rainfall ranged from 0.006 to 0.025, indicating varying response speeds of groundwater level changes to rainfall. These differences were mainly influenced by rainfall intensity, site topography, surface water systems, and excavation activities. Based on the permeability of the rock layers, recommendations for anti-floating design were proposed: when the permeability coefficient of fractured rock exceeds 20 m/d, underground structures should strengthen passive anti-floating measures or increase active drainage and pressure relief measures; when the permeability coefficient ranges from 10 to 20 m/d, the anti-floating safety factor should be appropriately increased; when the coefficient is below 10 m/d, standard design practices are sufficient. [Conclusions] The study identifies the main factors influencing groundwater level fluctuations, quantifies the response of groundwater level to rainfall, and proposes an anti-floating design method that accounts for the permeability coefficient of rock layers. This approach addresses the limitations of traditional anti-floating designs that assume a uniform design water level and provides practical guidance for the anti-floating design of subway stations.

Key words: fractured rock layers, groundwater level, rainfall, linear fitting, permeability coefficient

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