中国地质
中國地質
중국지질
CHINESE GEOLOGY
2009年
6期
1382-1394
,共13页
汪振立%邓通德%王瑞敏%邵文军%徐明%廖万琪
汪振立%鄧通德%王瑞敏%邵文軍%徐明%廖萬琪
왕진립%산통덕%왕서민%소문군%서명%료만기
稀土元素%岩石%土壤%脐橙%迁聚特征
稀土元素%巖石%土壤%臍橙%遷聚特徵
희토원소%암석%토양%제등%천취특정
Rare Earth Element (REE)%rock%soil%navel orange%characteristics of migration and accumulation
在赣南稀土高背景区和稀土低背景区不同地质环境脐橙果同,系统采集岩、土、脐橙植物样,用ICP-MS法测定样品中15种稀土元素的含量,并对稀土元素在岩石、土壤和脐橙植物体内的分布、迁移、累积特征进行了研究.结果表明:a.基岩的稀土元素含量影响(决定)土壤各层位的稀土元素含量;b.土壤环境中稀土元素含量高低直接影响脐橙植物体稀土元素含量,但不完全成正比;c.基岩的稀土元素配分模式基本上贯穿土壤各层位、脐橙植物体各器官;d.岩、土、脐橙三大环节稀土无素的百分含量,总的趋势是轻稀土比重逐渐增高,重稀土比重逐渐降低,但重稀土在脐橙植物体末稍器官比例有所增加;e.岩土脐橙生态系统立体刮面中,稀土元素的垂直方向运动呈向量关系;f.由于土壤-植物壁垒作用和脐橙植物体自身的选择性吸收、控制性积累功能,高、低稀土背景区脐橙果肉的稀土含量均低于国家食品卫生限量标准.
在贛南稀土高揹景區和稀土低揹景區不同地質環境臍橙果同,繫統採集巖、土、臍橙植物樣,用ICP-MS法測定樣品中15種稀土元素的含量,併對稀土元素在巖石、土壤和臍橙植物體內的分佈、遷移、纍積特徵進行瞭研究.結果錶明:a.基巖的稀土元素含量影響(決定)土壤各層位的稀土元素含量;b.土壤環境中稀土元素含量高低直接影響臍橙植物體稀土元素含量,但不完全成正比;c.基巖的稀土元素配分模式基本上貫穿土壤各層位、臍橙植物體各器官;d.巖、土、臍橙三大環節稀土無素的百分含量,總的趨勢是輕稀土比重逐漸增高,重稀土比重逐漸降低,但重稀土在臍橙植物體末稍器官比例有所增加;e.巖土臍橙生態繫統立體颳麵中,稀土元素的垂直方嚮運動呈嚮量關繫;f.由于土壤-植物壁壘作用和臍橙植物體自身的選擇性吸收、控製性積纍功能,高、低稀土揹景區臍橙果肉的稀土含量均低于國傢食品衛生限量標準.
재공남희토고배경구화희토저배경구불동지질배경제등과동,계통채집암、토、제등식물양,용ICP-MS법측정양품중15충희토원소적함량,병대희토원소재암석、토양화제등식물체내적분포、천이、루적특정진행료연구.결과표명:a.기암적희토원소함량영향(결정)토양각층위적희토원소함량;b.토양배경중희토원소함량고저직접영향제등식물체희토원소함량,단불완전성정비;c.기암적희토원소배분모식기본상관천토양각층위、제등식물체각기관;d.암、토、제등삼대배절희토무소적백분함량,총적추세시경희토비중축점증고,중희토비중축점강저,단중희토재제등식물체말초기관비례유소증가;e.암토제등생태계통입체괄면중,희토원소적수직방향운동정향량관계;f.유우토양-식물벽루작용화제등식물체자신적선택성흡수、공제성적루공능,고、저희토배경구제등과육적희토함량균저우국가식품위생한량표준.
Samples of rocks, soils and navel orange trees were taken systematically in several orchards located in different geological conditions characterized by rich or poor REE in southern Jiangxi Province. The contents of 15 rare earth elements in these samples were measured by using the method of ICP-MS, and the distribution, migration and accumulation of REE in rocks, soils and navel orange plants were studied. Some conclusions have been reached: a. The content of REE in the bedrock affects or decides the content of REE in all layers; b. The content of REE in soil directly affects the content of REE in navel orange plants; nevertheless, they are sometimes not in a direct proportion with each other; c. The distribution pattern of REE in bedrock seems to be the same in every layer of the soil and in all organs of the navel orange plants; d. General trend of the percentage content of REE in rock, soil and navel orange plants is that the proportion of the light REE increases gradually and that of the heavy REE decreases gradually. However, the percentage content of the heavy REE somewhat increases in the peripheral organs of navel orange plants; e. In the three-dimensional profile of the rock-soil-navel orange system, the vertical direction of movement of the REE assumes the relationship between vectors, f. The content of REE in navel orange flesh is lower than the limitation standard stipulated by national food and health regulations.