相关实验视频
Updated: Jun 15, 2025

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Continuous Hydrologic and Water Quality Monitoring of Vernal Ponds
Published on: November 13, 2017
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[对济南宝图泉区水化特征和控制因素的空间变异性进行分析]
Qing-Yu Xu1,2, Chun-Wei Liu1,2, Chang-Suo Li1,2
1801 Institute of Hydrogeology and Engineering Geology, Shandong Provincial Bureau of Geology & Mineral Resources, Jinan 250014, China.
Huan jing ke xue= Huanjing kexue
|August 21, 2024
概括
济南宝图泉的地下水是性的,化学成分因充电区而异. 碳酸盐和石膏矿物质的溶解,受人类活动的影响,塑造了水的形状.
科学领域:
- 水文地质学 水文地质学
- 环境化学环境化学
- 地质化学 地质化学
背景情况:
- 济南宝图泉区是一个重要的地地下水系统.
- 了解水化学特性对于水资源管理至关重要.
研究的目的:
- 研究地地下水的水化学特性和离子来源.
- 分析不同功能区 (间接充电,直接充电,放电) 的空间变化.
主要方法:
- 水样采集和测试.
- 水化学参数统计,多变量统计,自我组织地图,图形分析和离子比.
- 地下水流系统理论与区域物理地理和水文地质条件的整合.
主要成果:
- 地下水是性的,典型的碳酸盐矿物溶解.
- 由于不同的排水路径,水化学具有显著的空间变化.
- 水化学从HCO3-Ca演变为HCO3·SO4-Ca类型,从间接充电到放电区域,有石溶解的证据.
- 离子源主要包括岩石矿物溶解,阴离子交换和矿物溶解平衡,受人类活动的影响.
结论:
- 地下水化学主要由矿物溶解和水文地质条件控制.
- 石膏溶解有助于 Ca2+ 和 SO42- 在地下水中.
- 人类活动对宝图泉地区的地下水水化学有重大影响.
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