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河北曲周盐渍土区的地下水化学特征
引用本文:李韵珠,陆锦文,吴金绥. 河北曲周盐渍土区的地下水化学特征[J]. 土壤学报, 2001, 38(3): 341-352
作者姓名:李韵珠  陆锦文  吴金绥
作者单位:1. 中国农业大学资源与环境学院,
2. 中国农业大学基础科学技术学院,
基金项目:国家“九五”科技攻关项目(96-004-01-14-2)资助
摘    要:对河北曲周县盐渍土区浅层地下水的水化学类型、基本化学性质、主要化学组分及其形式和微量元素的状况及分布等化学特征进行了分析和研究。资料表明,该区地下水化学类型以Cl-SO4型为主,其次为SO4-Cl型。阳离子以Ca∧2 为主,其次为Na∧ 。各地下水化学类型可用于3种特征指标,即rHCO3/r(Cl SO4)、rSO4/rCl和rNa/r(Ca Mg),加以区分。地下水矿化度平均3.11gL∧-1,最高达17gL∧-1。以Cl-SO4和SO4-Cl型的矿化度和离子强度较高。全区纳吸附比较低,基本上无钠害问题。饱和指数表明,地下水中石膏和硬石膏呈非饱和状态,而方解石、霰石呈过饱和状态。除主要游离子外,化学组分形式中CaSO∧04、MgSO∧04、CaHCO∧ 3和MgHCO∧ 3等配合物和配离子的相对浓度较高。地下水中微量元素Cr、Cd和Fe的含量较高,应注意其水质问题,除Zn外,各微量元素浓度均与矿化度呈极显著(或显著)相关。

关 键 词:盐渍土区 地下水 水化学类型 水化学特征 化学组分形式 微量元素 河北
收稿时间:1999-12-22
修稿时间:1999-12-22

CHEMICAL CHARACTERISTICS OF GROUNDWATER IN SALT-AFFECTED SOIL AREA IN QUZHOU, HEBEI
Li Yun-zhu,Lu Jin-wen and Wu Jin-sui. CHEMICAL CHARACTERISTICS OF GROUNDWATER IN SALT-AFFECTED SOIL AREA IN QUZHOU, HEBEI[J]. Acta Pedologica Sinica, 2001, 38(3): 341-352
Authors:Li Yun-zhu  Lu Jin-wen  Wu Jin-sui
Affiliation:College of Resources and Environment, China Agricultural University, Beijing 100094;College of Resources and Environment, China Agricultural University, Beijing 100094;College of Basic Sciences and Technology, China Agricultural University, Beijing 100094
Abstract:Hy drochemical types and main chemical characteristics of the shallow groundwater in salt-affected soil area in Quzhou, Hebei were described and summarized in this paper.The data showed that the principal hydrochemical types of the groundwater were Cl-SO4 and SO4-Cl.The principalcation was Ca2+, and the next was Na+.The results also indicated that the mineralization and ionic strength of the groundwater in that area were high, especially for Cl-SO4 and SO4-Cl types.The mean mineralization of the groundwater was 3.11g L-1 with the highest reaching 17g L-1.
Keywords:Salt-affected soil area  Groundwater  Hydrochemical types  Hydrochemical characteristics  Spices of chemical components  Microelements
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