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Spatial decline distribution of groundwater levels of confined aquifer in the whole Red River Delta, Vietnam

机译:越南红河三角洲整个承压含水层地下水位的空间下降分布

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Monitoring and interpreting changes in groundwater levels are essential for groundwater management. However, a fairly wide groundwater monitoring network over the Red River Delta, Vietnam was not set up until 1995. This paper investigated trends and their slopes in groundwater level series (1995- 2009) in 63 observation wells for confined aquifer by the non-parametric Mann-Kendall trend test and Sen's slope estimator. The analyses revealed that groundwater levels experienced significant downward trends almost all wells and time series. Spatial distribution of different trend slope was clarified over the delta in which central and coastal areas showed more serious downward trend slopes than other areas. Trend results for 18 different time series (e.g. monthly, seasonal, annual means and so on) were quite similar regardless to time series to be studied. While annual cycle in groundwater levels were strongly associated with those in rainfall and river water levels, long-term downward trends could result from increasing groundwater withdrawal.
机译:监测和解释地下水位的变化对于地下水管理至关重要。但是,直到1995年,越南红河三角洲才建立了相当广泛的地下水监测网络。本文采用非参数方法研究了63座受限含水层观测井中地下水位系列的趋势及其坡度(1995-2009年)。 Mann-Kendall趋势检验和Sen的斜率估计器。分析表明,地下水位几乎在所有井和时间序列中都经历了显着的下降趋势。明确了三角洲不同趋势坡度的空间分布,其中中部和沿海地区的下降趋势斜率比其他地区更为严重。无论要研究的时间序列如何,18个不同时间序列(例如,每月,季节性,年度平均值等)的趋势结果都非常相似。尽管地下水位的年循环与降雨和河水位的年循环密切相关,但长期的下降趋势可能是由于地下水抽取量增加所致。

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