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现代地质 ›› 2014, Vol. 28 ›› Issue (6): 1329-1336.

• 水文地质 • 上一篇    

江苏泗阳城区浅层地下水化学特征及其影响因素

汪名鹏1,2   

  1. (1.中国矿业大学 资源与地球科学学院,江苏 徐州221116;
    2.江苏省水文地质工程地质勘察院,江苏 淮安223005)
  • 出版日期:2014-12-27 发布日期:2015-01-30
  • 作者简介:汪名鹏,男,高级工程师,硕士研究生,1973年出生,水文地质与工程地质专业,主要从事水文地质、工程地质、环境地质勘查与研究工作。Email:ahwmp@163.com。
  • 基金资助:

    江苏省省级地勘基金项目“洪泽湖北部黄泛区平原地质环境调查评价”(苏财建〔2011〕425号)。

Hydrochemical Characteristics and Influencing Factors of Shallow Groundwater in Siyang Area,Jiangsu Province

WANG Ming-peng1,2   

  1. (1.School of Resources and Earth Science, China University of Mining and Technology,Xuzhou,Jiangsu221116,China;
    2.Jiangsu Province Institute of Hydrogeological and Engineering Geological Investigation,Huai’an,Jiangsu223005,China)
  • Online:2014-12-27 Published:2015-01-30

摘要:

根据现场取样分析,对江苏泗阳城区浅层地下水水文地质特征、水化学组分在空间上的分布特征进行了研究,并对其形成特点和影响因素进行探讨。结果表明:研究区浅层地下水水化学类型呈现明显的平面分带性,京杭运河西南侧浅层地下水阴离子中HCO-3占主导地位,溶解性总固体(TDS)多小于1 g/L,总硬度小于450 mg/L,水质一般较好;京杭运河东北侧浅层地下水阴离子以HCO-3、Cl-、SO2-4为主,TDS多介于1~3 g/L,总硬度大于450 mg/L,为微咸水,水质变差。研究区NH+4-N、NO-3-N污染较明显,空间分布具有明显的地域性差异;高浓度分布在京杭运河两岸以及泗阳农场一带,纵向上NH+4-N高浓度主要集中在小于18 m的浅层地下水,NO-3-N多在8~20 m的浅层地下水富集。研究区浅层地下水水化学组分现状特征及其差异性的形成与演化,受海陆交互相沉积环境、含水介质、地下水补径条件以及人类活动等因素的影响。

关键词: 浅层地下水, 空间分布特征, 水化学类型, 三氮, 影响因素, 泗阳城区, 江苏

Abstract:

Based on experimental data of the shallow groundwater samples, the hydrogeological characteristics in Siyang area and spatial distributions of the chemical components were studied,meanwhile, the formation characteristics and influencing factors were discussed. The results showed that the hydrochemical type of shallow groundwater in Siyang area presented some horizontal zoning regularity. In the southwest of the Grand Canal, HCO-3 is the predominant anion of the shallow groundwater; total dissolved solids (TDS) is less than 1  g/L; total hardness is less than 450 mg/L, and the water quality is generally good. While in the northeast of the Grand Canal, the predominant anions of shallow groundwater areHCO-3,Cl-and SO2-4; TDS usually is within 1-3 g/L; total hardness is more than 450 mg/L; the water is brackish and the quality is bad. In addition, the ammonium nitrogen and nitrate nitrogen contaminations of the shallow groundwater are obvious in Siyang area, and the spatial distributions there have significantly uneven regional differences, ammonium nitrogen and nitrate nitrogen concentrations are high at both sides of the Grand Canal and near the Siyang farm.NH+4-N high-concentration in shallow groundwater is less than that in 18 meters in the vertical, while NO-3-N  highconcentration in shallow groundwater is within 8-20 meters. The spatial variations of hydrochemical characteristics of shallow ground-water in Siyang area are affected by the interactive marine and terrestrial deposit, the chemical constituents of the supply source, supply and runoff flow conditions of aquifer medium and human activities.

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