The occurrence of thallium in sea water and marine sediments
The occurrence of thallium in sea water and marine sediments
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DOI：
10.1016/0009-2541(70)90013-6
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发表时间：
1970
期刊：
影响因子：
3.9
通讯作者：
A. D. Matthews;J. P. Riley
中科院分区：
文献类型：
--
作者：
A. D. Matthews;J. P. Riley
用中子活化法研究了北大西洋某站水体中铊的浓度。在11个深海沉积物中测定了铊的含量。实验表明，该元素在海洋中的地球化学平衡可以通过吸附在铁锰矿物的含水二氧化锰相上以及通过掺入伊利石和类似粘土矿物的晶格中来维持。
The concentration of thallium in the water column at a station in the North Atlantic has been investigated using a neutron activation procedure. Values ranging from 9.4–16.6 ng/l were found. Thallium has been determined in 11 deep sea sediments. Experiments suggest that the geochemical balance of the element in the oceans may be maintained by adsorption on the hydrous manganese dioxide phase of ferro-manganese minerals and by incorporation into the lattice of illite and similar clay minerals.