院报 ›› 2023, Vol. 40 ›› Issue (7): 27-31.DOI: 10.11988/ckyyb.20220176

• 水资源 • 上一篇    下一篇

济南长清岩溶地下水位与降水量、黄河水位的相关性

齐欢1,2   

  1. 1.山东省地质矿产勘查开发局 八〇一水文地质工程地质大队,济南 250014;
    2.山东省地下水环境保护与修复工程技术研究中心,济南 250014
  • 收稿日期:2022-03-01 修回日期:2022-04-29 出版日期:2023-07-01 发布日期:2023-07-12
  • 作者简介:齐 欢(1986-),男,河北邢台人,高级工程师,硕士,主要从事水文地质与环境地质勘查工作。E-mail:943314446@qq.com

Correlation Analysis of Karst Groundwater Level, Precipitation and Yellow River Water Level in Changqing District, Jinan City

QI Huan1,2   

  1. 1. Hydrogeology and Engineering Geology Team 801, Shandong Provincial Bureau of Geology & Mineral Resources, Jinan 250014, China;
    2. Shandong Engineering Research Center for Groundwater Environmental Protection and Restoration, Jinan 250014, China
  • Received:2022-03-01 Revised:2022-04-29 Online:2023-07-01 Published:2023-07-12

摘要: 为查明济南长清岩溶地下水位与降水量、黄河水位的相关性,选取2007—2019年长清—孝里铺水文地质单元4个岩溶地下水位监测井动态长期监测数据、同期降水量和黄河水位资料,采用小波相干和多元小波相干的方法对数据进行分析。结果表明:①岩溶地下水位动态存在显著的连续或间断的1 a、0.5 a高频主振荡周期。②岩溶地下水位与降水量的平均小波相干值(AWC)平均值为0.47,显著相干性百分比面积(PASC)平均值为20.64%;地下水位与黄河水位的AWC平均值为0.42,PASC平均值为13.00%,降水量对地下水位的影响程度大于黄河水位。③孝里镇广里村、归德镇—文昌街道一带岩溶地下水位与降水量、黄河水位的多元小波相干值(MWC)均较AWC至少增加了5%,说明该地区岩溶地下水位受到降水量和黄河水位的共同影响。该研究成果对于进一步认识济南沿黄地区“大气降水-地表水-地下水”转化关系和保泉供水具有重要意义。

关键词: 地下水位, 降水量, 黄河水位, 多元小波相干

Abstract: To explore the correlation between karst groundwater level, precipitation, and Yellow River water level in Changqing District, Jinan City, we utilized long-term monitoring data of four karst groundwater levels in the Changqing-Xiaolipu hydrogeological unit from 2007 to 2019, alongside data on precipitation and Yellow River water level during the same period. By applying wavelet coherence and multiple wavelet coherence methods to analyze the data, we found the following results: 1) There are significant continuous or discontinuous one-year and half-year high-frequency main oscillation cycles in the dynamics of karst groundwater level. 2) The average wavelet coherence (AWC) and percent area of significant coherence (PASC) mean values between karst groundwater level and precipitation are 0.47 and 20.64%, respectively. The mean AWC and PASC between groundwater level and Yellow River water level are 0.42 and 13.00% respectively. Precipitation has a greater impact on groundwater level than the Yellow River water level. 3) The multiple wavelet coherence (MWC) between karst groundwater level and precipitation and Yellow River water level in Guangli Village of Xiaoli Town and Guide Town-Wenchang Street area increased by at least 5% compared to AWC, indicating that the karst groundwater level in this area is affected by both precipitation and Yellow River water level. These research findings are highly significant for further understanding the transformation relationship among precipitation, surface water, and groundwater. Furthermore, our findings could potentially benefit spring protection and water supply along the Yellow River in Jinan.

Key words: groundwater level, precipitation, Yellow River water level, multiple wavelet coherence

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