Miller Jerry R, Anderson Jamie B, Lechler Paul J, Kondrad Shannon L, Galbreath Peter F, Salter Emory B
Department of Geosciences and Natural Resources Management, Western Carolina University, Cullowhee, NC 28723, USA.
Sci Total Environ. 2005 Nov 1;350(1-3):204-24. doi: 10.1016/j.scitotenv.2005.01.030.
Field and laboratory investigations were undertaken to determine (1) the relations between discharge, Pb concentration, and the Pb isotopic composition of the dissolved load in Richland Creek, western North Carolina, and (2) the potential influence of varying Pb water chemistry on the Pb isotopic abundances in liver and bone tissues of rainbow trout (Oncorhynchus mykiss). Stream waters were characterized by relatively low Pb concentrations during periods of base flow exceeding 10 days in length. Moreover, greater than 65% of the Pb was derived from orchard soils located upstream of the monitoring site which are contaminated by lead arsenate. During small to moderate floods, the dissolved load exhibited Pb concentrations more than twice as high as those measured during base flow, but the contribution of Pb from lead arsenate was relatively low and varied directly with discharge. In contrast to smaller events, Pb from lead arsenate in an 8- to 10-year (overbank) event in May 2003 was minimal during peak flow conditions, suggesting that discharge-source relations are dependent on flood magnitude. The hydrologic and geochemical data demonstrate that aquatic biota in Richland Creek are subjected to short-term variations in Pb concentrations and Pb isotopic abundances within the dissolved load ranging from a few hours to few a weeks. Laboratory studies demonstrated that when rainbow trout were exposed to elevated Pb concentrations with a distinct isotopic fingerprint, the bone and liver rapidly acquire isotopic ratios similar to that of the water. Following exposure, bone retains Pb from the contaminant source for a period of months, while the liver excreted approximately 50% of the accumulated Pb within a few days and nearly all of the Pb within a few weeks. Differences in the rates of excretion resulted in contrasting isotopic ratios between the tissues. It seems plausible, then, that previously observed differences between the isotopic composition of bone and liver in rainbow trout from Richland Creek are related to their short-term exposure to Pb from soils contaminated with Pb arsenate that result from fluctuating hydrologic conditions. If these trends prove to be common in other contaminated aquatic environments, it may be possible to use the Pb isotopic composition of bone as an indicator of the long-term exposure to Pb and the liver as a biomarker for short-term Pb exposures.
开展了野外和实验室调查,以确定:(1)北卡罗来纳州西部里奇兰溪的流量、铅浓度与溶解负荷中铅同位素组成之间的关系;(2)变化的铅水化学对虹鳟(Oncorhynchus mykiss)肝脏和骨骼组织中铅同位素丰度的潜在影响。在基流持续超过10天的时期,溪流水体的特点是铅浓度相对较低。此外,超过65%的铅来自监测点上游受砷酸铅污染的果园土壤。在小到中等洪水期间,溶解负荷中的铅浓度比基流期间测得的浓度高出两倍多,但砷酸铅中铅的贡献相对较低,且与流量直接相关。与较小的事件不同,2003年5月一次8至10年一遇(漫滩)事件中,在洪峰流量条件下,砷酸铅中的铅含量极少,这表明流量与来源的关系取决于洪水规模。水文和地球化学数据表明,里奇兰溪中的水生生物受到溶解负荷中铅浓度和铅同位素丰度在数小时到数周内的短期变化影响。实验室研究表明,当虹鳟暴露于具有独特同位素指纹的升高的铅浓度时,骨骼和肝脏会迅速获得与水相似的同位素比率。暴露后,骨骼在数月内保留来自污染物源的铅,而肝脏在几天内排出约50%积累的铅,几周内几乎排出所有铅。排泄速率的差异导致组织间同位素比率形成对比。那么,之前在里奇兰溪虹鳟中观察到的骨骼和肝脏同位素组成差异似乎与它们短期暴露于因水文条件波动而受砷酸铅污染的土壤中的铅有关。如果这些趋势在其他受污染的水生环境中也很常见,那么有可能将骨骼的铅同位素组成用作长期铅暴露的指标,将肝脏用作短期铅暴露的生物标志物。