水文
水文
수문
HYDROLOGY
2015年
4期
7-13,26
,共8页
袁瑞强%龙西亭%王鹏%宋献方
袁瑞彊%龍西亭%王鵬%宋獻方
원서강%룡서정%왕붕%송헌방
氯离子质量平衡%干旱区和半干旱区%地下水补给%示踪剂%非饱和带
氯離子質量平衡%榦旱區和半榦旱區%地下水補給%示蹤劑%非飽和帶
록리자질량평형%간한구화반간한구%지하수보급%시종제%비포화대
chloride mass balance%arid and semi-arid areas%groundwater recharge%tracers%unsaturated zone
氯离子质量平衡法(CMB)利用惰性示踪剂Cl-可以揭示区域地下水平均补给速率,补给事件和环境、气候变化事件等信息,可为相关研究提供可靠的信息。虽然该方法简单、有效,已经得到大量应用,但是也具有明显的局限性。综述了基于CMB法的相关研究,回溯了该方法的提出和演化,讨论了其主要假设条件和应用的局限性,阐明为了准确地应用该方法需要加强的方面。首先要重视氯离子干沉降的观测和研究。其次要加强氯离子沉降空间变化的观测和研究。在方法上要注意综合采用多种示踪剂、土壤理化性质和平行钻孔等手段来研究。最后要加强对氯离子平衡过程,及其相关的自然过程和人类活动的研究。对促进氯离子质量平衡法在地下水研究方面的应用和发展,具有一定的参考价值。
氯離子質量平衡法(CMB)利用惰性示蹤劑Cl-可以揭示區域地下水平均補給速率,補給事件和環境、氣候變化事件等信息,可為相關研究提供可靠的信息。雖然該方法簡單、有效,已經得到大量應用,但是也具有明顯的跼限性。綜述瞭基于CMB法的相關研究,迴溯瞭該方法的提齣和縯化,討論瞭其主要假設條件和應用的跼限性,闡明為瞭準確地應用該方法需要加彊的方麵。首先要重視氯離子榦沉降的觀測和研究。其次要加彊氯離子沉降空間變化的觀測和研究。在方法上要註意綜閤採用多種示蹤劑、土壤理化性質和平行鑽孔等手段來研究。最後要加彊對氯離子平衡過程,及其相關的自然過程和人類活動的研究。對促進氯離子質量平衡法在地下水研究方麵的應用和髮展,具有一定的參攷價值。
록리자질량평형법(CMB)이용타성시종제Cl-가이게시구역지하수평균보급속솔,보급사건화배경、기후변화사건등신식,가위상관연구제공가고적신식。수연해방법간단、유효,이경득도대량응용,단시야구유명현적국한성。종술료기우CMB법적상관연구,회소료해방법적제출화연화,토론료기주요가설조건화응용적국한성,천명위료준학지응용해방법수요가강적방면。수선요중시록리자간침강적관측화연구。기차요가강록리자침강공간변화적관측화연구。재방법상요주의종합채용다충시종제、토양이화성질화평행찬공등수단래연구。최후요가강대록리자평형과정,급기상관적자연과정화인류활동적연구。대촉진록리자질량평형법재지하수연구방면적응용화발전,구유일정적삼고개치。
Chloride is used as the inert tracer in the chloride mass balance method (CMB) to discover the variances of groundwater recharge rates and to offer reliable information about environment and climate changes. The method is simple and valid gaining a wide range of applications, although the limits are also obvious. In this paper, research based on CMB and evolutions of the method were widely reviewed. Hypotheses and limits were discussed. Future works were emphasized. Dry depositions of chloride need to be observed, and spa-tial variance of the depositions should be studied well. Multi-tracers, soil properties and duplicated borehole should be em ployed to en-hance cross validations. The need of studies on the budget of chloride and the related natural processes and anthropogenic activities was highlighted. Our work contributes to promote the applications and developments of the method in groundwater hydrology.