Scholarlink

The genetic mechanism of groundwater in Zhanhua County has not reached a unified conclusion so far, which has limited the effective utilization of groundwater in this area. The analysis of hydrogeochemical characteristics and groundwater types is of great significance for the study of genetic mechanism of the groundwater. By collecting the groundwater samples in Zhanhua County, the water chemical component analysis was carried out, and the main water chemical indexes such as pH value, TDS, ion composition and hardness were studied accordingly. The results show that the pH value of the groundwater in Zhanhua County is between 7.0 and 10.2, which was alkaline or neutral. Most of the TDS values are greater than 50 g/L, indicating that the groundwater is brine. The hardness value is greater than 450 mg/L, indicating that it is extremely hard water. The main anion in groundwater is Cl−, the main cation is Na+, and in addition to 7 major ions, it also contains NO3− and Br−. According to the Shukarev classification, the groundwater type is 49-D water, according to the Sulin classification, the groundwater type is MgCl2 water.

错误：搜索内容不能为空，请输入英文关键词
错误：关键词超出字数限制，请精简
高级检索

The Groundwater Type and Relevant Hydrogeochemical Characteristics in Zhanhua County, Shandong Province, China

  • 会议论文

  • 发表日期：

    2026年

查看全文
  • Guangzeng Song,
  • Meng Xu,
  • Junru Zhao,
  • Xile Li

摘要

The genetic mechanism of groundwater in Zhanhua County has not reached a unified conclusion so far, which has limited the effective utilization of groundwater in this area. The analysis of hydrogeochemical characteristics and groundwater types is of great significance for the study of genetic mechanism of the groundwater. By collecting the groundwater samples in Zhanhua County, the water chemical component analysis was carried out, and the main water chemical indexes such as pH value, TDS, ion composition and hardness were studied accordingly. The results show that the pH value of the groundwater in Zhanhua County is between 7.0 and 10.2, which was alkaline or neutral. Most of the TDS values are greater than 50 g/L, indicating that the groundwater is brine. The hardness value is greater than 450 mg/L, indicating that it is extremely hard water. The main anion in groundwater is Cl−, the main cation is Na+, and in addition to 7 major ions, it also contains NO3− and Br−. According to the Shukarev classification, the groundwater type is 49-D water, according to the Sulin classification, the groundwater type is MgCl2 water.