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山东大汶河流域中上游古近系含水岩组水文地质特征

周乐, 刘元晴, 李伟, 朱庆俊, 李凤哲, 吕琳, 邓启军, 马雪梅, 何锦. 2019. 山东大汶河流域中上游古近系含水岩组水文地质特征[J]. 中国地质, 46(2): 316-327. doi: 10.12029/gc20190208
引用本文: 周乐, 刘元晴, 李伟, 朱庆俊, 李凤哲, 吕琳, 邓启军, 马雪梅, 何锦. 2019. 山东大汶河流域中上游古近系含水岩组水文地质特征[J]. 中国地质, 46(2): 316-327. doi: 10.12029/gc20190208
ZHOU Le, LIU Yuanqing, LI Wei, ZHU Qingjun, LI Fengzhe, LÜ Lin, Deng Qijun, MA Xuemei, HE Jin. 2019. Characteristics of the Paleogene water-bearing Formation in the middle and upper reaches of the Dawenhe River basin, Shandong Province[J]. Geology in China, 46(2): 316-327. doi: 10.12029/gc20190208
Citation: ZHOU Le, LIU Yuanqing, LI Wei, ZHU Qingjun, LI Fengzhe, LÜ Lin, Deng Qijun, MA Xuemei, HE Jin. 2019. Characteristics of the Paleogene water-bearing Formation in the middle and upper reaches of the Dawenhe River basin, Shandong Province[J]. Geology in China, 46(2): 316-327. doi: 10.12029/gc20190208

山东大汶河流域中上游古近系含水岩组水文地质特征

  • 基金项目:
    国家自然科学基金项目(41240021)和中国地质调查局水工环地质调查项目(DD20160289,DD20190259)联合资助
详细信息
    作者简介: 周乐, 女, 1987年生, 矿产普查与勘探专业, 硕士, 工程师, 主要从事于基岩山区地下水勘查理论研究; E-mail:zhoule_wei@sina.com
    通讯作者: 刘元晴, 男, 1988年, 工程师, 矿产普查与勘探专业, 从事于基岩山区水文地质调查工作; E-mail:lyq198896@126.com
  • 中图分类号: P641

Characteristics of the Paleogene water-bearing Formation in the middle and upper reaches of the Dawenhe River basin, Shandong Province

  • Fund Project: Supported by National Natural Science Foundation of China (No.41240021) and China Geological Survey (No. DD20160289, DD20190259)
More Information
    Author Bio: ZHOU Le, female, born in 1987, master, engineer, engages in theoretical study of groundwater exploration in bedrock mountain area; E-mail: zhoule_wei@sina.com .
    Corresponding author: LIU Yuanqing, male, born in 1988, engineer, engages in Hydrogeology survey in bedrock mountain area; E-mail: lyq198896@126.com
  • 利用古近系大汶口组及朱家沟组含水岩组5眼施工钻孔及55眼井孔调查资料,通过岩心、地下水常规离子组分及氢氧同位素样品测试结果,研究大汶河流域中上游莱芜盆地、大汶口盆地古近系含水岩组分布特征、物性及富水性、地下水化学及补给循环特征。结果表明:富水较好的大汶口组上段位于盆地腹部偏北,含水层岩性为半固结砂砾岩,水化学类型HCO3-Ca·Mg型为主;朱家沟组含水岩组位于盆地边界断裂下降盘,含水层岩性为溶蚀发育的灰质砾岩,水化学类型复杂多变。现代大气降水作为地下水主要补给来源,蒸发浓缩作用,方解石、白云石和石膏溶解及人类污染活动参与了地下水化学组分的形成。归纳总结3种古近系不同类型含水岩组地下水富集规律:构造裂隙控水模式、半固结含水岩组裂隙孔隙水富集模式和灰质砾岩裂隙岩溶水富集模式。

  • 加载中
  • 图 1  研究区构造位置图

    Figure 1. 

    图 2  古近系含水岩组主要出水层段岩性特征

    Figure 2. 

    图 3  地下水样品piper图

    Figure 3. 

    图 4  地下水样品Gibbs图

    Figure 4. 

    图 5  地下水化学参数关系图

    Figure 5. 

    图 6  研究区δD和δ18O的散点关系图

    Figure 6. 

    图 7  上水河村周边水文地质图

    Figure 7. 

    图 8  上水河LW-ZK12钻孔高密度剖面图

    Figure 8. 

    图 9  古近系半固结含水岩组地下水富集模式图

    Figure 9. 

    图 10  北留村钻孔(NL-ZK02)水文地质图

    Figure 10. 

    图 11  北留村钻孔(NL-ZK02)水文地质剖面图

    Figure 11. 

    表 1  研究区古近系含水岩组调查点统计表

    Table 1.  Investigation statistics of the Paleogene water-bearing Formation

    下载: 导出CSV

    表 2  研究区地下水水化学及同位素数据表

    Table 2.  Water chemistry and isotopic data of groundwater in the study area

    下载: 导出CSV
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出版历程
收稿日期:  2018-09-05
修回日期:  2018-12-18
刊出日期:  2019-04-25

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