华南西部火山岛地区滨海浅层地下水的水质现状研究

doi:10.19388/j.zgdzdc.2017.04.11

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Abstract Separated by Qiongzhou Strait, Leizhou Peninsula and Hainan Island have similar climate and geological environment. Recently,with the quick development of economy and society, the extract and usage of underground water is becoming frequent and the problems of development against environment protection have become prominent. In order to understand the distribution, variation of underground water and the link between distribution, variation and environment, the authors drilled shallow underground monitoring wells, and then sampled and analyzed the samples in laboratory along Leizhou Peninsula and Hainan Island shorelines. The analysis results show that beside few wells, the concentration of total amount of dissolved solids (TDS) and the main ions (Cl^-, SO42- and Na⁺) in underground water are at high level. TDS and Cl^- have maximum concentration nearly to 39.00 g/L and 20.00 g/L respectively, and also are featured with relatively frequent vibration, revealing that the type of underground water changed from weak acidic and bicarbonate to Cl^- types and are related with tidal cycles. Constrained by geological environment, the resilience of shallow underground in most wells falls into average or weak grade and the water quality is IV-V types, which will not change at least in shortterm. Therefore, the underground water quality has close relationship with geological environment and human activities, and it is probably affected by the release of deep ancient seawater. The influence factors of the underground water quality are complicated, so more attention should be paid to the further monitoring and research.

Key words： shoreline zone underground water seawater intrusion water quality

Received: 14 November 2016

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	Articles by authors
	GAN Huayang
	LIN Jinqing
	XIA Zhen
	HE Haijun
	LU Jianfei
	HUANG Xiangqing
	ZHANG Shunzhi

Cite this article:

GAN Huayang,LIN Jinqing,XIA Zhen, et al. Study on current state of shallow underground water quality along shoreline of volcanic islands in western South China[J]. , 2017, 4(4): 80-87.

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http://www.zgdzdcbjb.com/EN/10.19388/j.zgdzdc.2017.04.11 OR http://www.zgdzdcbjb.com/EN/Y2017/V4/I4/80

[1] 杨丽芝,杨雪柯,刘春华.山东平原地区浅层地下水有机污染特征分析[J].中国地质调查,2015,2(8):25-30.
[2] 景佳俊,陶文杰,管祯.对江苏沛县新庄铁矿区富水性规律的初步认识[J].中国地质调查,2016,3(6):68-74.
[3] 苏春田,潘晓东,李兆林,等.云南广南岩溶区水文地质环境地质调查进展[J].中国地质调查,2015,2(8):9-16.
[4] 梁永平,赵春红,唐春雷,等.北方岩溶区水文地质环境地质调查进展——以北京西山岩溶区为例[J].中国地质调查,2015,2(8):1-8.
[5] 揭江.引发雷州半岛地区干旱的典型生态环境[J].地下水,2014,36(5):114-116.
[6] 车秀芬,张京红,黄海静,等.海南岛气候区划研究[J].热带农业科学,2014,34(6):60-65,70.
[7] 张文杰,谭红兵,陈喜,等.广东硇洲岛地下水化学演化及成因机理[J].水文,2012,32(3):51-59.
[8] 周祖光.海南岛地下水资源特征与开发利用[J].水资源保护,2005,21(3):48-51.
[9] 夏真,林进清,郑志昌,等.北部湾广西海岸带地质环境综合监测进展及成果[J].中国地质调查,2016,3(1):52-57.
[10] 广州海洋地质调查局.北部湾广西近岸海洋地质环境与地质灾害调查报告[R].广州:广州海洋地质调查局,2013.
[11] 广州海洋地质调查局.雷州半岛东部滨海湿地地质调查与生态环境评价报告[R].广州:广州海洋地质调查局,2013.
[12] 广州海洋地质调查局.海南岛东北部滨海湿地地质调查与生态环境评价报告[R].广州:广州海洋地质调查局,2014.
[13] 广州海洋地质调查局.海南岛南部滨海湿地地质调查与生态环境评价报告[R].广州:广州海洋地质调查局,2015.
[14] 广州海洋地质调查局.海南岛西北部滨海湿地地质调查与生态环境评价报告[R].广州:广州海洋地质调查局,2016.
[15] 黄向青,林进清,甘华阳,等.雷州半岛东岸地下水化学要素变化以及海水入侵特征[J].地下水,2013,35(3):38-42,48.
[16] 何海军,石要红,甘华阳,等.海南岛东北部地下水化学及海水入侵特征分析[J].广东化工,2014,41(19):50-51,53.
[17] 路剑飞,甘华阳,张顺枝,等.琼东北滨海浅层地下水水质变化特征分析[J].中山大学学报:自然科学版,2016,55(1):137-148.
[18] 李家熙,吴功建.中国生态环境地球化学图集[M].北京:地质出版社,1999.
[19] 姚锦梅,周训,李娟,等.广东雷州半岛玄武岩地下水水文地球化学特征及演化模拟[J].地质通报,2007,26(3):327-334.
[20] 张胜华,朗喜白,任雅娴,等.2014年雷州半岛地下水水位年内动态变化分析[J].人民珠江,2016,37(4):32-35.