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运用H、O同位素资料分析地下热水的补给来源——以鲁西北阳谷-齐河凸起为例
引用本文:张保建,徐军祥,马振民,沈照理,亓 麟.运用H、O同位素资料分析地下热水的补给来源——以鲁西北阳谷-齐河凸起为例[J].地质通报,2010,29(4):603-609.
作者姓名:张保建  徐军祥  马振民  沈照理  亓 麟
作者单位:1. 中国地质大学,北京,100083
2. 山东省地矿局,山东,济南,250013
3. 济南大学城市发展学院,山东,济南,250002
4. 中国水利水电科学研究院,北京,100044
基金项目:山东省国土资源厅矿产资源补偿费项目 
摘    要:通过对阳谷-齐河凸起地下热水的化学成分、同位素及其地热地质条件的分析,对这一地区的地下热水的补给来源进行了研究。本区地下热水的δD为-65‰~-80.67‰,δ18O为-9.2‰~-10.2‰,均分布在全球雨水线的附近,说明该区地下热水主要为大气降水成因。济南北地热田地下热水的补给高程为256m,此范围大致相当于济南南部山区及其以南的泰山北麓;聊城东地热田地下热水的补给高程为411m,此范围大致相当于泰山山脉及其周边的中山区。聊城东地热田地下热水的2H过量参数d明显低于济南北地热田,说明聊城东地热田地下热水的补给区比后者更远。

关 键 词:H、O同位素  2H过量参数  地下热水  补给来源  阳谷-齐河凸起  鲁西北

Analysis on groundwater supply sources using hydrogen and oxygen isotope data-a case study of Yanggu-Qihe salient,northwestern Shandong,China
ZHANG Bao-jian,XU Jun-xiang,MA Zhen-min,SHEN Zhao-li,QI Lin.Analysis on groundwater supply sources using hydrogen and oxygen isotope data-a case study of Yanggu-Qihe salient,northwestern Shandong,China[J].Geologcal Bulletin OF China,2010,29(4):603-609.
Authors:ZHANG Bao-jian  XU Jun-xiang  MA Zhen-min  SHEN Zhao-li  QI Lin
Institution:ZHANG Bao-jian1,XU Jun-xiang2,MA Zhen-min3,SHEN Zhao-li1,QI Lin41. China University of Geosciences,Beijing 100083,China,2. Sh,ong Bureau of Geology , Mineral Resource,Ji\'nan 250013,Sh,ong,3. School of City Development,University of Ji\'nan,Ji\'nan 250002,4. China Institute of Water Resources , Hydropower Research,Beijing 100044
Abstract:Based on analyzing the chemical composition,isotope,terrestrial heat and geological condition,this paper studied supply sources of ground hot water in this area. The δD is -65‰ to -80.67‰ and the δ~(18)O is -9.2‰ to -10.2‰,both are located in the vicinity of the global rainfall line indicating the main cause of ground wacer in the area is atmospheric precipitation.Northern ji'nan geothermal field ground hot water supply elevation is 256m,which is roughly equivalent to the mountains south of Ji'nan and the northern foot of Taishan mountain;while geothermal field ground hot water supply elevation in the east of Liaocheng is 41 lm,which is roughly equivalent to Taishan mountain and its surrounding mountains.Excess parameter of deuterium (d) of geothermal fidd ground hot water in the east of Liaocheng was significantly lower than that of geothermal field in the north of Ji'nan.It indicates that geother-mal field ground hot water supply area in the east of Liaocheng is farther than the latter one.
Keywords:hydrogen and oxygen isotope  excess parameter of deuterium(d)  groundwater  supply sources  Yanggu - Qihe salient  northwestern Shandong
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