地球学报
地毬學報
지구학보
ACTA GEOSCIENTIA SINICA
2014年
6期
741-750
,共10页
高存荣%冯翠娥%刘文波%赤井纯治%久保田喜裕%小林巌雄
高存榮%馮翠娥%劉文波%赤井純治%久保田喜裕%小林巌雄
고존영%풍취아%류문파%적정순치%구보전희유%소림암웅
地壳表层%砷污染%砷循环%污染模式%污染类型%还原解吸
地殼錶層%砷汙染%砷循環%汙染模式%汙染類型%還原解吸
지각표층%신오염%신순배%오염모식%오염류형%환원해흡
the earth’s surface%arsenic contamination%arsenic cycle%contamination pattern%contamination type%reduction absorption
为了更好地监测和预测地下水砷污染,揭示由自然原因引起的地下水砷污染规律和机制,通过多年来对内蒙古河套平原地下水砷污染的调查研究,在充分了解和掌握砷的化学与地球化学性质以及世界各国地下水砷污染状况与分布特征的基础上,总结了砷在自然环境中的分布和污染地下水的机理。文章阐述了4种地下水砷污染类型的形成机理,并提出了地壳表层砷的循环与污染地下水模式,通过该模式在基本掌握某一地区地质环境背景的情况下,可以初步预测其可能发生地下水砷污染的地段。地下水砷污染是砷在地壳表层循环过程中发生的一种环境水文地球化学现象,污染区的分布与特定的地质、地理背景和环境条件有关。在还原解吸污染类型中,封闭的环境、硫元素和有机碳的存在是地层中砷溶出的主要控制因素。今后应加强对封闭的冲积或湖积平原、河流入湖或入海三角洲等地区地下水砷污染的调查与监测。
為瞭更好地鑑測和預測地下水砷汙染,揭示由自然原因引起的地下水砷汙染規律和機製,通過多年來對內矇古河套平原地下水砷汙染的調查研究,在充分瞭解和掌握砷的化學與地毬化學性質以及世界各國地下水砷汙染狀況與分佈特徵的基礎上,總結瞭砷在自然環境中的分佈和汙染地下水的機理。文章闡述瞭4種地下水砷汙染類型的形成機理,併提齣瞭地殼錶層砷的循環與汙染地下水模式,通過該模式在基本掌握某一地區地質環境揹景的情況下,可以初步預測其可能髮生地下水砷汙染的地段。地下水砷汙染是砷在地殼錶層循環過程中髮生的一種環境水文地毬化學現象,汙染區的分佈與特定的地質、地理揹景和環境條件有關。在還原解吸汙染類型中,封閉的環境、硫元素和有機碳的存在是地層中砷溶齣的主要控製因素。今後應加彊對封閉的遲積或湖積平原、河流入湖或入海三角洲等地區地下水砷汙染的調查與鑑測。
위료경호지감측화예측지하수신오염,게시유자연원인인기적지하수신오염규률화궤제,통과다년래대내몽고하투평원지하수신오염적조사연구,재충분료해화장악신적화학여지구화학성질이급세계각국지하수신오염상황여분포특정적기출상,총결료신재자연배경중적분포화오염지하수적궤리。문장천술료4충지하수신오염류형적형성궤리,병제출료지각표층신적순배여오염지하수모식,통과해모식재기본장악모일지구지질배경배경적정황하,가이초보예측기가능발생지하수신오염적지단。지하수신오염시신재지각표층순배과정중발생적일충배경수문지구화학현상,오염구적분포여특정적지질、지리배경화배경조건유관。재환원해흡오염류형중,봉폐적배경、류원소화유궤탄적존재시지층중신용출적주요공제인소。금후응가강대봉폐적충적혹호적평원、하류입호혹입해삼각주등지구지하수신오염적조사여감측。
In order to better monitor and predict groundwater arsenic contamination and reveal the law and mechanism of groundwater arsenic contamination caused by natural factors, the authors carried out investigation and research on groundwater arsenic contamination in Hetao Plain of Inner Mongolia for years. Based on fully understanding and grasping of arsenic chemical and geochemical properties as well as the situation and distribution characteristics of groundwater arsenic contamination all over the world, the authors summarized the distribution of arsenic in natural environment and the mechanism of groundwater arsenic contamination. This study expounded the formation mechanism of four types of groundwater arsenic contamination and presented the patterns of arsenic cycle and groundwater arsenic contamination on the earth’s surface. With the basic mastering of the geological environment background of a certain region, these patterns could offer a preliminary prediction of the possible locations of arsenic contamination. This study indicates that arsenic contamination in groundwater is an environmental hydrogeochemical phenomenon, which happens in the arsenic cycle on the earth’s surface. The distribution of contaminated areas is related to specific geological and geographical backgrounds and environmental conditions. This study suggests that, in the reductive desorption contamination type, such factors as the closed environment, sulfur and organic carbon constitute the main control factors for the dissolution of arsenic in strata. In the future, it is necessary to reinforce the investigation and monitoring of arsenic contamination in groundwater in closed alluvium-acustrine plains, river-lake deltas, and river-sea deltas.