河北联合大学学报(自然科学版)
河北聯閤大學學報(自然科學版)
하북연합대학학보(자연과학판)
Journal of Hebei United university natural sclence edition
2015年
1期
5-11
,共7页
地下水动态%水化学特征%聚类分析
地下水動態%水化學特徵%聚類分析
지하수동태%수화학특정%취류분석
groundwater dynamic%water chemistry characteristics%cluster analysis
研究开采影响下地下水动态特征是进行矿井水文地质条件实时研究、科学防治矿井水害及合理开采的重要基础。选取煤5顶板含水层为代表,分析1998~2009年以来24个水样的Na+、Ca2+、Mg2+、Cl-、SO42-、HCO3-、NO3-、矿化度及 pH 值大小变化,结果表明含水层水化学特征稳定,动态不明显。因此,选取1950-2009年各时段内不同含水层水样113个,进行水化学特征聚类分析,得出4组典型分类:第四系冲积层孔隙承压水及煤5顶板(A 段、B 段)水;煤5-煤7、煤12-1顶底板水;煤12-2、煤14、K3及G层水;奥陶系石灰岩岩溶水;分类与含水层水文地质循环特征相符。研究结果对整个东欢坨矿区的防治水工作具有一定意义。
研究開採影響下地下水動態特徵是進行礦井水文地質條件實時研究、科學防治礦井水害及閤理開採的重要基礎。選取煤5頂闆含水層為代錶,分析1998~2009年以來24箇水樣的Na+、Ca2+、Mg2+、Cl-、SO42-、HCO3-、NO3-、礦化度及 pH 值大小變化,結果錶明含水層水化學特徵穩定,動態不明顯。因此,選取1950-2009年各時段內不同含水層水樣113箇,進行水化學特徵聚類分析,得齣4組典型分類:第四繫遲積層孔隙承壓水及煤5頂闆(A 段、B 段)水;煤5-煤7、煤12-1頂底闆水;煤12-2、煤14、K3及G層水;奧陶繫石灰巖巖溶水;分類與含水層水文地質循環特徵相符。研究結果對整箇東歡坨礦區的防治水工作具有一定意義。
연구개채영향하지하수동태특정시진행광정수문지질조건실시연구、과학방치광정수해급합리개채적중요기출。선취매5정판함수층위대표,분석1998~2009년이래24개수양적Na+、Ca2+、Mg2+、Cl-、SO42-、HCO3-、NO3-、광화도급 pH 치대소변화,결과표명함수층수화학특정은정,동태불명현。인차,선취1950-2009년각시단내불동함수층수양113개,진행수화학특정취류분석,득출4조전형분류:제사계충적층공극승압수급매5정판(A 단、B 단)수;매5-매7、매12-1정저판수;매12-2、매14、K3급G층수;오도계석회암암용수;분류여함수층수문지질순배특정상부。연구결과대정개동환타광구적방치수공작구유일정의의。
During the long-term production of mine,a large number of water gushing and drainage lead to conspicuous change to groundwater dynamic.It's an important basis to study the characteristics of groundw-ater under the influence of rational exploitation and hydrogeological geology.Selecting the roof of the 5 th coal seam as the representative aquifer,analyzed the content of Na+,Ca2+,Mg2+,Cl-,SO4 2-,HCO3-,NO3-, salinity and pH value on 24 water samples since 1998 to 2009,the results show that the chemical character-istics of the aquifer water is stable,and the dynamic is not obvious.Therefore,1 1 3 chemical samples in dif-ferent aquifer water are used for water chemical cluster analysis.Obtained 4 typical classification groups:Water from quaternary alluvium pore confined aquifer and roof of coal 5 aquifer;Water from coal 5-7,coal 12-1 aquifer;Water from coal 12-2,coal 14,K3 and G aquifer;Water from ordovician limestone aquifer.The classification and characteristic of hydrological geology match well.