首页> 外文期刊>Journal of Asian earth sciences >Assesment of the response of the meteorological/hydrological parameters on the soil gas radon emission at Hsinchu, northern Taiwan: A prerequisite to identify earthquake precursors
【24h】

Assesment of the response of the meteorological/hydrological parameters on the soil gas radon emission at Hsinchu, northern Taiwan: A prerequisite to identify earthquake precursors

机译:评估台湾北部新竹市气象/水文参数对土壤gas气排放的响应:确定地震前兆的先决条件

获取原文
获取原文并翻译 | 示例
       

摘要

The present study is an attempt to assess and quantify the influence of the meteorological (atmospheric temperature and pressure) and hydrological (rainfall and ground water head-GWH) parameters on the soil gas radon emission at Hsinchu, northern Taiwan. The quasi-periodic variations corresponding to diurnal and semi diurnal periods were estimated and eliminated by decomposing the time series for the period of September 16, 2009 to March 5, 2010 to singular spectrum analysis. The reconstructed non-periodic variations, which reproduce the salient feature of recorded time series, were searched for meteorological/hydrological influences in radon emission. The combined response of barometric pressure and atmosphere temperature are found to be small when compared to the total variability in radon. The influence of rainfall on radon is found to be strongest. At the onset of rainfall, radon shows a step-jump that attains peak with a time lag of 12-15 h. This enhancement is attributed to entrapment of soil gas in the top soil cover as increased soil moisture prevents escape of radon into the atmosphere (capping effect). The decay of radon after the recession of rainfall is approximated by double exponential decay terms, one corresponding to the natural decay of radon with half life of 3.84 days and second representing slow weakening of capping effect. The third effect related to internal loading due to rise and fall of groundwater modulates the propagation of radon in overlying strata, accounting for the long term variations in radon. The rainfall inflicted changes in radon look strikingly similar to earthquake related precursory or co-seismic perturbations, inferred by long term synotopic observations. It is surmised that unless radon variations are corrected for meteorological/hydrological contamination, some precursory signals are masked on one hand while on the other hand some anomalies are falsely viewed as earthquake precursors.
机译:本研究旨在评估和量化气象(大气温度和压力)和水文(降雨和地下水水头-GWH)参数对台湾北部新竹市土壤gas气排放的影响。通过将2009年9月16日至2010年3月5日期间的时间序列分解为奇异频谱分析,可以估算和消除与昼夜和半昼期相对应的准周期变化。搜索重建的非周期性变化,其再现记录的时间序列的显着特征,以寻找for排放中的气象/水文影响。与ra的总变化相比,大气压力和大气温度的组合响应很小。发现降雨对ra的影响最大。在降雨开始时,ra呈现出阶跃跃迁,并达到12-15小时的峰值。这种增强归因于土壤气体截留在顶部土壤覆盖层中,因为增加的土壤水分可防止ra逃逸到大气中(封盖效应)。降雨衰退后ra的衰减可通过双指数衰减项来近似,其中一个对应于half的自然衰减,半衰期为3.84天,第二个代表加盖效应的减弱。与地下水上升和下降引起的内部负荷有关的第三个影响是don在上覆地层中的传播,这是ra长期变化的原因。降雨引起的changes变化看起来与地震相关的前兆或同震微扰非常相似,这是通过长期的综合观测得出的。据推测,除非针对气象/水文污染校正ra的变化,否则一方面掩盖了一些先兆信号,而另一方面却错误地将某些异常视为地震的先兆。

著录项

相似文献

  • 外文文献
  • 专利
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