高级检索

基于水化学特征的矿区填土地基水害水源分析

Water source analysis of mine filling foundation based onhydrochemical characteristics

  • 摘要: 目前大部分的矿区建设是基于回填丘陵沟壑区整平场地,对于这种人造特殊地质结构,易受到水害侵蚀破坏,且水害水源往往多元且不易确定。以山西某一矿区地基水害为例,通过详细的现场调查与水文钻探,确定研究区填土地基毛细水带与稳定水位位置,初步判断水源。在此基础上取水样28件,其中沉降区目标水样14件,可能水来源水样14件,对采取的水样进行水质全分析测试,采用数理统计、Piper三线图、相关性分析、水质类型对比分析法、层次聚类法、离子比例系数等方法对矿区填土地基下地下水的化学特征、水质类型与化学成因进行综合分析,确定地基填土水害具体来源。结果表明:沉降区目标水样与可能水源水样阳离子都以K++Na+为主,其中沉降区目标水样中,阴离子都以HCO-3为优势阴离子,水质类型为HCO3·Cl-Na·Mg,HCO3-Na与HCO3·SO4·Cl-Na,可能水源水样中除砂岩裂隙水主要阴离子为HCO-3,其余样品以Cl-为优势阴离子,根据综合对比分析,沉降区地下水特征与砂岩裂隙水最接近,其主要来源为砂岩裂隙水补给,其次来自煤矿污水、雨水的入渗。研究结果可为该类型填土地基水害问题判别提供理论方法,并为后续相似填土地基前期处理起到预警作用。

     

    Abstract: At present, most of the mining area construction is based on backfilling the hilly and gully area to level the site. For this special artificial geological structure, it is easy to be eroded and destroyed by water hazards, and the possible sources of water hazards are often multiple and difficult to determine.Taking the foundation water hazard of a mining area in Shanxi as an example, through detailed field investigation and hydrological drilling, the capillary water zone and stable water level of the fill foundation in the study area were determined, and the water source was preliminarily determined. On this basis, 28 water samples were taken, including 14 target water samples in the subsidence area and 14 water samples from possible water sources.The water samples were fully analyzed and tested for water quality. By means of mathematical statistics,Piper diagram, correlation analysis,water quality type comparison analysis method, hierarchical clustering method, ion ratio coefficient, the chemical characteristics, water quality type and chemical origin of groundwater under filling ground in mining area were comprehensively analyzed, and the specific sources of water hazards were determined.The results show that the target water sample and the possible source water cations in the subsidence area are dominated by K++Na+, and the anions in the target water samples in the sedimentation area are all dominated by HCO-3,and the water quality type is HCO3·Cl-Na·Mg , HCO3-Na and HCO3·SO4·Cl-Na. It is possible that HCO-3 is the main anion in the source water samples except for sandstone fissure water, and Cl- is the dominant anion in the rest of the samples.. According to the comprehensive comparison, the groundwater characteristics of the subsidence area and the sandstone fissure water are the most closely, its main source is sandstone fissure water recharge, followed by coal mine sewage and rainwater infiltration. The research results can provide a theoretical method for judging the water hazards of this type of landfill foundation, and play an early warning role for the subsequent pretreatment of similar landfill foundations.

     

/

返回文章
返回