Analysis of variation characteristics of karst groundwater quality in Guiyang City
-
摘要: 为了解长时间尺度岩溶地下水的水质变化特征,本文以贵阳市中心城区为例,选取1984年和2014年48组原位取样点的丰季水质数据,并结合地下水赋存环境和城市发展特征进行对比分析。结果显示:研究区地下水水质较好,整体有恶化的趋势;1984年仅有9处地下水水质超标,多数超标点为原生背景成因,2014年有14处水质超标,多数超标点为人类活动引起;地下水化学类型在30年间变化较大,近一半取样点地下水由HCO3型变成HCO3·SO4型水,研究区地下水硫酸盐化明显;新老城区地下水水质逐步好转,城乡结合部地带则是地下水污染的高发区,农业区因人类活动强度较低,地下水水质变化相对平缓。建议在岩溶城市的地下水资源开发和地下水环境保护工作中,应综合考虑不同区域的岩溶水文地质条件和人类活动特征,有的放矢的开展评价监测管理。针对工作区地下水硫酸盐化现象开展研究,并对城乡结合部开展综合整治,加强对农业区地下水环境的综合保护,以遏制区内地下水污染趋势,预防地下水污染事件的发生。Abstract: The aim of this study is to understand the longtime underground water quality variation characteristics in karst regions. Choosing karst underground water of central Guiyang city as the object, the variation characteristics of karst underground water quality of Guiyang in 30 years were analyzed using 48 samples collected in 1984 and 2014, respectively. The results show that the ground water quality is good as a whole, while having a tendency to deteriorate. Only 9 sampling sites of 1984 were not suitable for drink directly, which was mainly caused by primary background environment. In 2014, 14 sampling sites were not suitable for drink, most of which was caused by human activities. The hydrochemical types of underground water have changed greatly over the 30 years, about half of the controlling points were changing into the HCO3·SO4 type from the type of HCO3 Underground water was getting sulfation obviously. Underground water quality in old and new city zones were getting better, and that in rural-urban conjunctions was easily polluted. Due to the low degree of human activities , the water quality in agricultural areas were changing gently. In the work of groundwater resources development and environmental protection, karst hydrogeology conditions and human activities characters in different areas should be considered synthetically and the objective-oriented evaluation of monitoring and management should be carried out. Aiming at the phenomenon of groundwater salinization in the work area, the comprehensive improvement of the urban-rural conjunctions should be strengthened to facilitate comprehensive protection of the groundwater environment in agricultural areas, so as to curb the trend of groundwater pollution and prevent the occurrence of groundwater pollution incidents.
-
[1] 陈泮勤,孙成权.国际全球变化研究核心计划[M].北京:气象出版社,1994:1-2. [2] 安芷生,符淙斌.全球变化科学的进展[J]. 地球科学进展,2001,16(5):678. [3] 邹胜章,于晓英,卢海平. 基于自动监测的柳州鸡喇地下河水质变化特征[J]. 中国岩溶,2011,30(1):22-26. [4] 张贵,周翠琼,康晓波. 云南开远南洞地下河水质演变特征[J]. 中国岩溶,2008,27(4):366-370. [5] 唐伟,裴建国,殷建军,等. 桂林毛村岩溶地下河二十多年来的水质演化趋势研究[J].中国岩溶,2010,29(3):331-336. [6] 刘松霖. 淄博市大武水源地地下水水质演化规律分析及污染趋势预测[D].北京:中国地质大学(北京),2013. [7] 裴建国. 寨底地下河系统水质演化趋势及碳汇通量分析[D].北京:中国地质大学(北京),2012. [8] 杨秀丽,曾群,苏泽志. 贵阳市地下水污染现状评价及防治对策[J]. 贵州地质,2010,27(4):291-295. [9] 杨秀丽,罗维,邹胜章. 贵阳观山湖区至白云区地下水有机污染现状与防治对策[J]. 中国岩溶,2015,34(4):375-381. [10] 王中美,廖义玲,李明琴,等. 贵阳市水文地质条件及环境效应研究[J]. 水土保持研究,2012,19(1):226-229. [11] 王中美,谭正莲. 贵阳市岩溶地下水动态特征分析[J]. 贵州大学学报(自然科学版),2013,30(1):27-32. [12] 王中美. 贵阳市岩溶地下水4种污染离子的空间分布特征[J]. 贵州农业科学,2013,41(5):158-164. [13] 刘奇.贵阳岩溶地下水水质评价及污染风险性研究[D].贵阳:贵州大学,2006. [14] 戴传固.贵州省区域地质志[M].北京:地质出版社,2002. [15] GB/T 5750.1-5750.13-2006, 生活饮用水标准检验方法 [S].北京:中国标准出版社. [16] DZ/T02902015,地下水水质标准[S].北京:地质出版社. [17] 费宇红,张兆吉,郭春艳,等. 区域地下水质量评价及影响因素识别方法研究:以华北平原为例[J]. 地球学报,2014,35(2):131-138. [18] 王明章. 黔北寒武系白云岩盆地型水源地水化学特征及水资源开发利用对策[J]. 贵州地质,1995(4):326-332. [19] 王明章.贵州省岩溶区地下水及地质环境[M].北京:地质出版社,2015.
点击查看大图
计量
- 文章访问数: 1784
- HTML浏览量: 317
- PDF下载量: 963
- 被引次数: 0