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常见重金属在翅碱蓬(Suaeda heteroptera)根际沉积物系统季节迁移变化
朱鸣鹤1, 方飚雄1, 丁永生2, 蒋艳敏1, 陈 捷3, 黄绍堂4, 严小军1, 丁德文5
1.宁波大学;2.上海海事大学海洋环境与工程学院;3.中国科学院大连化学物理研究所;4.宁波市出入境检验检疫局;5.国家海洋局第一海洋研究所 海洋生态环境科学与工程国家海洋局重点实验室
摘要:
应用原子吸收光谱法(AAS)和电感耦合等离子体原子发射光谱法(ICP-AES)对翅碱蓬-根际沉积物系统常见重金属(Cu、Pb、Zn 和 Cd)总量和不同化学形态含量进行了季节跟踪测定。结果表明, 系统中 Cu、Zn、Pb 和 Cd 环境化学行为呈现显著季节变化。从化学形态上看, 根际沉积物中 Cu和 Pb 在生理周期内均以残渣态为主, 有机结合态在夏季和秋季达较高值。Zn 在生理周期内均以交换态为主且随季节变化明显, 碳酸结合态和铁锰结合态随季节变化不明显。Cd 以残渣态为主, 交换态在春季达最高。从总量上看, 根际沉积物中的 Cu、Zn、Pb 的总量在夏季和秋季具有较高值。从系统迁移情况看, 植物对Cu和Pb吸收量均为冬季>春季>秋季>夏季, 且大部分限制于地下; 其体内分布除秋季 Pb 为根>叶>茎外, 其它时期均为根>茎>叶。 Zn 吸收量为秋季>夏季>冬季>春季, 且绝大部分被吸收至地上。Zn 吸收和分布取决于根际沉积物生物有效含量; 总之, 春季植物体重金属向根际沉积物迁移。夏季和秋季, Cu 、Pb 和 Cd 由根际沉积物向植物体迁移变化并不明显, 而 Zn 正好相反。4 种元素在冬季均为根际沉积物向植物体内迁移。
关键词:  常见重金属, 翅碱蓬, 根际沉积物, 季节迁移, 累积吸收
DOI:10.11693/hyhz201005018018
分类号:
基金项目:宁波市自然科学基金项目, 2006A610080 号、2007A610056 号; 宁波市海洋渔业局项目, 9-19 号, 2006.9—2009.9; 宁波大学科研基金项目, XK200562 号、XY0600062 号; 宁波大学人才引进项目, 2005.10—2007.10; 宁波市 4321 人才工程项目, 2007.3—2011.3; 王宽诚基金资助, 2005—2008。
SEASONAL TRANSFORMATION VARIATION OF COMMON HEAVY METALS IN SUAEDA HETEROPTERA-RHIZOSPHERE SEDIMENT
ZHU Ming-He1, FANG Biao-Xiong1, DING Yong-Sheng2, JIANG Yan-Min1, CHEN Jie3, HUANG Shao-Tang4, YAN Xiao-Jun1, DING De-Wen5
1.Ningbo University;2.College of Ocean Environment and Engineering, Shanghai Maritime University;3.Dalian Institute of Chemical Physics, Chinese Academy of Sciences;4.Ningbo Entry-Exit Inspection and Quarantine Bureau;5.Key Laboratory of Science and Engineering for Marine Ecological Environment, First Institute of Oceanography, State Oceanic Administration,
Abstract:
Environmental chemical behaviors of Cu, Pb, Zn, and Cd in Suaeda heteroptera-rhizosphere sediment were studied using samples from a wetland near Liaohe Oil Field, North China. These metals show distinct seasonal variations. In the rhizosphere sediment, Cu and Pb are the major component in the whole physiological cycle in residuals state, and the content of their organic bound species reached high level in blossom period, seasonal variation of the exchangeable was clear. Carbonates and Fe-Mn oxides reached peak value in different periods. Zn exists dominates the whole physiological cycle in exchangeable state and varies seasonally, while its residuals took the second place, and its organic bound is the least; seasonal variations of carbonates and Fe-Mn oxides are weak. Cd is in residual state mainly, and its exchangeable reaches the highest level in seeding period. The total content of Cu, Pb and Zn in rhizosphere sediment is in the orders of fruit period>seedling period>flower period>growth period, and root>stem>leaf except Pb in root>leaf>stem. The metal accumulation and distribution depends on plant physiological mechanism.
Key words:  Familiar heavy metals, Suaeda heteroptera, Rhizosphere sediment, Seasonal variation, Accumulation and absorption
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