Analysis of Trend in Groundwater-Quality Parameters: A Case Study

Subhankar Ghosh, M. Jha
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Abstract

In the 21st century, groundwater has a pivotal role in ensuring water, food, and environmental securities worldwide. Systematic observation, protection and restoration are essential for sustainable management of water resources. Regular monitoring is key to investigate temporal changes in groundwater quality, and statistical trend tests define whether these changes are significant or not. This study focuses on investigating trend in seasonal groundwater quality in an alluvial coastal basin of West Bengal, India. The seasonal groundwater-quality data (pH, TH, TDS, Fe2+ and HCO3ˉ) of pre-monsoon and post-monsoon seasons were collected for 2011–2018 period and analyzed using three non-parametric statistical trend detection tests, namely: (i) Original Mann-Kendall (M-K) test, (ii) Modified Mann-Kendall (mM-K) test, and (iii) Spearman Rank Order Correlation (SROC) test. The trend magnitudes were estimated by using the Sen’s slope estimation test. Statistical analyses revealed that seasonal concentrations of all five groundwater-quality parameters have large spatial (block-wise) variation within the study area. The results of trend analyses indicated that seasonal TH and TDS concentrations mainly have significant decreasing trends (α = 5% or 1%), whereas seasonal HCO3ˉ and Fe2+ concentrations mostly show significant increasing trends (α = 5% or 1%) in different blocks. However, seasonal pH concentrations exhibited no trend. The mM-K test was found to be over-sensitive in finding trends than M-K and SROC tests. The SROC test was found to be less sensitive in detecting trends than M-K and mM-K tests. Trend magnitudes of seasonal pH, TH, TDS, HCO3ˉ and Fe2+ concentrations varied from –0.03/year to 0.23/year, –57.44 mg/L/year to 25.88 mg/L/year, –172.98 mg/L/year to 92.58 mg/L/year, –15.81 mg/L/year to 27.88 mg/L/year, and –0.05 mg/L/year to 0.61 mg/L/year, respectively. Continuous and proper groundwater-quality monitoring is critically required in all aquifer systems. The outcomes of this study will aid policy-makers in appropriately monitoring and managing groundwater quality.
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地下水水质参数变化趋势分析——以实例为例
在21世纪,地下水在确保全球水、粮食和环境安全方面发挥着关键作用。系统的观测、保护和恢复是水资源可持续管理的必要条件。定期监测是调查地下水水质时间变化的关键,统计趋势检验可以确定这些变化是否显著。本文研究了印度西孟加拉邦海岸冲积盆地的季节性地下水水质变化趋势。收集了2011-2018年季风前和季风后季节地下水水质数据(pH、TH、TDS、Fe2+和HCO3 - h),采用原始Mann-Kendall (M-K)检验、修正Mann-Kendall (mM-K)检验和Spearman秩序相关(SROC)检验3种非参数统计趋势检测方法进行分析。采用Sen 's斜率估计检验估计趋势震级。统计分析表明,5个地下水水质参数的季节浓度在研究区内具有较大的空间(块方向)变化。趋势分析结果表明,不同区域TH和TDS浓度以季节性显著降低为主(α = 5%或1%),HCO3 - h和Fe2+浓度以季节性显著升高为主(α = 5%或1%)。然而,季节pH浓度没有变化趋势。mM-K检验在发现趋势方面比M-K和SROC检验过于敏感。SROC检验对趋势的检测灵敏度低于M-K和mM-K检验。季节pH、TH、TDS、HCO3 +和Fe2+浓度变化趋势分别为-0.03 ~ 0.23、-57.44 ~ 25.88 mg/L、-172.98 ~ 92.58 mg/L、-15.81 ~ 27.88 mg/L和-0.05 ~ 0.61 mg/L/年。在所有含水层系统中,持续和适当的地下水质量监测是至关重要的。这项研究的结果将有助于决策者适当地监测和管理地下水质量。
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