吉林大学学报(地球科学版)
吉林大學學報(地毬科學版)
길림대학학보(지구과학판)
JOURNAL OF JILIN UNIVERSITY(EARTH SCIENCE EDITION)
2009年
6期
1087-1094
,共8页
苏小四%万玉玉%董维红%侯光才
囌小四%萬玉玉%董維紅%侯光纔
소소사%만옥옥%동유홍%후광재
马莲河%河水与地下水转化%水化学%同位素%地下水
馬蓮河%河水與地下水轉化%水化學%同位素%地下水
마련하%하수여지하수전화%수화학%동위소%지하수
Malianhe River%hydraulic relationship between river and groundwater%hydrogeochemical%isotope%groundwater
查明地表水与地下水的转化关系是建立区域水循环模式、揭示水资源形成机制、评价水资源总量以及可持续开发利用水资源的必要环节.马莲河位于我国西北干旱半干旱气候区,流域内水资源时空分布不均,生态环境脆弱,水资源问题严重.受到区域气候、地质构造和自然地理环境的影响,河水与地下水的转化频繁、关系复杂.在分析了流域内地下水动力场特征的基础上,应用水化学方法和同位素技术相结合的方法分析了马莲河河水与地下水的相互转化关系.马莲河河水主要以接受地下水补给为主,仅在中游个别河段与地下水的水力联系较弱.
查明地錶水與地下水的轉化關繫是建立區域水循環模式、揭示水資源形成機製、評價水資源總量以及可持續開髮利用水資源的必要環節.馬蓮河位于我國西北榦旱半榦旱氣候區,流域內水資源時空分佈不均,生態環境脆弱,水資源問題嚴重.受到區域氣候、地質構造和自然地理環境的影響,河水與地下水的轉化頻繁、關繫複雜.在分析瞭流域內地下水動力場特徵的基礎上,應用水化學方法和同位素技術相結閤的方法分析瞭馬蓮河河水與地下水的相互轉化關繫.馬蓮河河水主要以接受地下水補給為主,僅在中遊箇彆河段與地下水的水力聯繫較弱.
사명지표수여지하수적전화관계시건립구역수순배모식、게시수자원형성궤제、평개수자원총량이급가지속개발이용수자원적필요배절.마련하위우아국서북간한반간한기후구,류역내수자원시공분포불균,생태배경취약,수자원문제엄중.수도구역기후、지질구조화자연지리배경적영향,하수여지하수적전화빈번、관계복잡.재분석료류역내지하수동력장특정적기출상,응용수화학방법화동위소기술상결합적방법분석료마련하하수여지하수적상호전화관계.마련하하수주요이접수지하수보급위주,부재중유개별하단여지하수적수력련계교약.
It is the key work to determine the hydraulic relationship between surface water and groundwater for setting up the local water hydrologic cycle, opening out water resources forming-mechanism, evaluating water resources quantity and sustainably developing water resources. In Malianhe River catchment located in arid and semi-arid climatic zones, water resources are unevenly distributed in temporal and spatial with fragile ecological environment, therefore water resources problem become serious. Affected by local climate, geological structure and geographical environment,the interaction between river water and groundwater can not be understood yet due to the frequent and complex interaction. Therefore, the interaction of surface water and groundwater has been studied by hydrogeochemical and isotopic methods based on analyzing the characteristics of groundwater hydrodynamic field. Through the analysis, it can be known that Malianhe River water is dominantly recharged by the groundwater of Lower Cretaceous Huanhe aquifer except for minority section in the midstream where hydraulic connection between the river and the groundwater is weak.