潜水地下水动态成因类型的综合判别方法——以三江平原松花江流域为例

A comprehensive discrimination method for the genetic type of groundwater regime of phreatic water: a case study in the Songhua River basin of the Sanjiang Plain

  • 摘要: 传统地下水动态类型的判别方法存在受人为主观因素影响大、易产生多解性等问题。为提高地下水动态成因类型判断的可靠性,本文提出了基于水文地质条件定性分析与实测数据定量分析相结合的综合判别方法。根据研究区的气象、水文及水文地质条件等,将地下水各补给项及排泄项对地下水动态的影响进行定量化,对动态数据进行相关分析及逻辑判断,辨识出对地下水位动态贡献最大的补给项和排泄项,并依此确定地下水动态的成因类型。基于该方法,以三江平原松花江流域2011年及2015年相同的57个地下水观测点为例,结合地下水位埋深、地下水位、河水位、降水量、观测井距河流的距离、包气带岩性等资料,将研究区地下水动态成因类型共划分为水文型、降水入渗型、降水入渗-蒸发型、降水入渗-径流型、降水入渗-开采型和人工开采型6种类型;对比2011年及2015年研究区地下水动态类型的变化,降水入渗型、降水入渗-径流型等天然地下水动态成因类型占比减少,而受人类活动影响的地下水动态成因类型占比增加,表明人工开采活动对地下水动态的影响日益增强。相比根据地下水动态曲线特征确定动态成因类型的传统定性分析方法,本研究提出的综合判别方法能够在充分考虑水文地质条件的基础上,结合定量化方法识别地下水位动态的驱动因素,提高地下水动态成因类型判别的科学性、可靠性以及工作效率。

     

    Abstract: Traditional methods for discriminating the genetic type of groundwater regime have some problems, such as being substantially affected by human subjective factors and the ease of producing multiple solutions. To improve the discrimination reliability of the genetic type of groundwater regime, this study proposes a comprehensive discrimination method combining a qualitative analysis of hydrogeological conditions and quantitative analysis of measured data. Firstly, according to the meteorological, hydrological, and hydrogeological conditions of the study area, the effects of various groundwater recharge and discharge items on groundwater regime are quantified. Then, a correlation analysis and logical judgment are carried out based on the dynamic data. The recharge and discharge items that contribute the most to the groundwater regime are identified, and the genetic types of the groundwater regime are named and determined accordingly. Based on this method, this study uses the same 57 groundwater observation points in the Songhua River basin of the Sanjiang Plain as in 2011 and 2015. These data were combined with the groundwater level depth, groundwater level, river water level, precipitation, distance from the observation well to the river, and lithology of the unsaturated zone. The genetic types of the groundwater regime in the study area were divided into six types: hydrological type, precipitation infiltration type, precipitation infiltration-evaporation type, precipitation infiltration-runoff type, precipitation infiltration-exploitation type and exploitation type. Comparing the changes in the genetic type of groundwater regime of the study area from 2011 to 2015 revealed thatthe proportion of natural genetic types, such as precipitation infiltration type and precipitation infiltration-runoff type, decreased, whereas the proportion of the genetic type affected by human activities increased. This indicated that the impact of human exploitation activities on the groundwater regime is increasing. Compared with the traditional qualitative analysis method based on the characteristics of the groundwater regime curve, the comprehensive discrimination method proposed in this study can identify the driving factors of groundwater regime, while fully considering the hydrogeological conditions and combined with quantitative methods, which improves the scientific reliability and work efficiency of the discrimination of the genetic type.

     

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