首页> 外文期刊>Environmental earth sciences >Periodic variations of rainfall, groundwater level and dissolved radon from the perspective of wavelet analysis: a case study in Tengchong, southwest China
【24h】

Periodic variations of rainfall, groundwater level and dissolved radon from the perspective of wavelet analysis: a case study in Tengchong, southwest China

机译:小波分析视角下的降雨,地下水位和溶解氡的周期性变化 - 以中国西南部腾冲的一个案例研究

获取原文
获取原文并翻译 | 示例
       

摘要

The dynamic variations of groundwater have been extensively studied, but there are few studies on the long-term time-frequency features of groundwater dynamic variations. Here we report the dynamic characteristics of the groundwater level and dissolved radon concentration based on the long-term (January 1988-March 2018) daily observation records and regional precipitation data in the Tengchong area, China. The results show that the precipitation (2-3 years and 13 years), groundwater level (13 years), and dissolved radon (9 years) all have multi-year periodic variations, which might be controlled by climate and solar radiation. The groundwater levels were highly correlated with rainfall amount, while the radon concentration variations were not only affected by rainfall but also by other complex factors. Furthermore, the changes of groundwater level and radon concentration lagged behind that of precipitation by about 3 months, and as the cycle range increased, the lag time tended to stabilize. During the observation period, the dissolved radon concentrations increased and decreased sharply. Radon concentration remained correlated with precipitation during the anomalous period. After the anomaly disappeared in 2002, however, its annual periodic characteristics weakened. The increase of radon concentrations may cause a potential risk for water utilization that requires more attention.
机译:地下水的动态变化已经过广泛研究,但是对地下水动态变化的长期时频特征几乎没有研究。在这里,我们报告了基于长期(2018年1月 - 2018年3月至3月)日常观察记录和中国腾冲区的区域降水数据的地下水位和溶解氡浓度的动态特征。结果表明,降水量(2-3岁和13岁),地下水位(13岁)和溶解氡(9年)都有多年的定期变体,可能由气候和太阳辐射控制。地下水位与降雨量高度相关,而氡浓度变化不仅受降雨量的影响,而且由其他复杂因素的影响。此外,地下水位和氡浓度的变化落后于约3个月的降水量,随着循环范围的增加,延迟时间趋于稳定。在观察期间,溶解的氡浓度急剧增加并急剧下降。氡浓度与异常时期的沉淀保持相关。然而,在2002年消失后,其年度周期性特征削弱了。氡浓度的增加可能导致需要更多关注的水利用风险。

著录项

  • 来源
    《Environmental earth sciences》 |2021年第15期|492.1-492.13|共13页
  • 作者

    Yang Tao; Wang Guangcai;

  • 作者单位

    China Univ Geosci State Key Lab Biogeol & Environm Geol Beijing 100083 Peoples R China|China Univ Geosci MOE Key Lab Groundwater Circulat & Environm Evolu Beijing 100083 Peoples R China|China Univ Geosci Sch Water Resources & Environm Beijing 100083 Peoples R China;

    China Univ Geosci State Key Lab Biogeol & Environm Geol Beijing 100083 Peoples R China|China Univ Geosci MOE Key Lab Groundwater Circulat & Environm Evolu Beijing 100083 Peoples R China|China Univ Geosci Sch Water Resources & Environm Beijing 100083 Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Groundwater; Radon; Precipitation; Time-series analysis; Wavelet transform;

    机译:地下水;氡;降水;时间序列分析;小波变换;
  • 入库时间 2022-08-19 02:45:27

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号