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钚和镅在地中海西部及直布罗陀海峡的垂直和水平通量。

Vertical and horizontal fluxes of plutonium and americium in the western Mediterranean and the Strait of Gibraltar.

作者信息

León Vintró L, Mitchell P I, Condren O M, Downes A B, Papucci C, Delfanti R

机构信息

Department of Experimental Physics, University College Dublin, Belfield, Ireland.

出版信息

Sci Total Environ. 1999 Sep 30;237-238:77-91. doi: 10.1016/s0048-9697(99)00126-6.

Abstract

New data on the vertical distributions of plutonium and americium in the waters of the western Mediterranean and the Strait of Gibraltar are examined in terms of the processes governing their delivery to, transport in and removal from the water column within the basin. Residence times for plutonium and americium in surface waters of approximately 15 and approximately 3 years, respectively, are deduced, and it is shown that by the mid 1990s only approximately 35% of the 239,240Pu and approximately 5% of the 241Am deposited as weapons fallout still resided in the water column. Present 239,240Pu inventories in the water column and the underlying sediments are estimated to be approximately 25 TBq and approximately 40 TBq, respectively, which reconcile well with the time-integrated fallout deposition in this zone, taken to be approximately 69 TBq. The data show that there are significant net outward fluxes of plutonium and americium from the basin through the Strait of Gibraltar at the present time. These appear to be compensated by net inward fluxes of similar magnitude through the Strait of Sicily. Thus, the time-integrated fallout deposition in the western basin can be accounted for satisfactorily in terms of present water column and sediment inventories. Enhanced scavenging on the continental shelves, as evidenced by the appreciably higher transuranic concentrations in shelf sediments, supports this contention.

摘要

本文根据钚和镅进入、在西地中海和直布罗陀海峡水体中迁移以及从水柱中去除的过程,研究了该区域水体中钚和镅垂直分布的新数据。推断出钚和镅在表层水中的停留时间分别约为15年和约3年,结果表明,到20世纪90年代中期,作为武器沉降物沉积的239,240Pu中只有约35%、241Am中只有约5%仍存在于水柱中。据估计,目前水柱和下层沉积物中239,240Pu的存量分别约为25太贝克勒尔和40太贝克勒尔,这与该区域时间积分沉降物沉积量(约69太贝克勒尔)吻合良好。数据表明,目前钚和镅通过直布罗陀海峡从该盆地有显著的净向外通量。这些通量似乎由通过西西里海峡的类似大小的净向内通量所补偿。因此,就目前水柱和沉积物存量而言,西部盆地的时间积分沉降物沉积量可以得到令人满意的解释。陆架上的清除作用增强,这从陆架沉积物中明显较高的超铀元素浓度可以得到证明,这支持了这一观点。

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