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Study on seawater intrusion in Laizhou bay coastal zone based on groundwater model

机译:基于地下水模型的莱州湾沿岸带海水入侵研究

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Seawater intrusion in coastal zone is a common gradually changed geological hazard. After seawater intrusion, the coastal groundwater is polluted into seawater, which directly causes great damage to local industrial and agricultural production and residents' health. In order to better understand the geological hazard, the chlorinity of groundwater in six monitoring sites which had different distance with the coast was detected by silver nitrate titration method based on the groundwater model of Laizhou Bay coast to collect the chlorinity of groundwater in the six monitoring sites from April 2013 to April 2017. The local seawater intrusion was analyzed taking the monthly average precipitation data in February and March of the same year into account. The results showed that in terms of time distribution, groundwater chlorinity in the monitoring site far from the coast had no significant fluctuation as time went on, but had an upward trend. Groundwater chlorinity in the monitoring site near the coast fluctuated significantly with time and had an upward trend. Especially in 2015, drought caused more seawater intrusion and greater chlorine fluctuation; in spatial distribution, with the increase of distance with the coast, the chlorinity of groundwater decreased gradually except fluctuation in 2015 caused by drought, the seawater intrusion area was approaching inland as time went on, and the transverse distribution of seawater intrusion area was irregular.
机译:沿海地区的海水入侵是一种常见的逐渐改变的地质灾害。海水入侵后,沿海地下水被污染成海水,直接损害当地的工农业生产和居民的健康。为了更好地了解地质灾害,根据莱州湾沿岸地下水模型,采用硝酸银滴定法对硝酸盐滴定法检测了六个与沿海不同距离的监测点的地下水中氯含量,以收集六个监测点中的地下水氯含量。在2013年4月至2017年4月期间,对当地海水入侵情况进行了分析,并考虑了同年2月和3月的月平均降水量数据。结果表明,在时间分布上,远离海岸的监测点的地下水含氯量随时间的推移没有明显的波动,但呈上升趋势。海岸附近监测点的地下水含氯量随时间波动很大,并呈上升趋势。特别是在2015年,干旱导致更多的海水入侵和更大的氯气波动;在空间分布上,随着距海岸的距离增加,除由于干旱引起的2015年波动外,地下水的氯含量逐渐降低,随着时间的推移,海水入侵面积逐渐接近内陆,海水入侵面积的横向分布不规则。

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