Trace metal distributions in two saltmarsh substrates, Illawarra region, New South Wales

G. S. Ohmsen, B. E. Chenhall, B. Jones
{"title":"Trace metal distributions in two saltmarsh substrates, Illawarra region, New South Wales","authors":"G. S. Ohmsen, B. E. Chenhall, B. Jones","doi":"10.31646/WA.156","DOIUrl":null,"url":null,"abstract":"The vertical and lateral distributions of Pb, Cu, Zn and Fe in the substrates of two saltmarshes, 3 and 14km respectively, from the heavy industrial centre of Port Kembla have been determined. Particulate matter within the sediment reflects the differing contribution to each site from this point source, which is highlighted by the presence of up to 70% of anthropogenic components in the finer sediment in the saltmarsh at Purry Burry Point. The particulate material derived from industrial and pyrometallurgical processes has previously been assumed to be inert in the surrounding environment. However, in the intertidal zone occupied by the saltmarshes, the redox conditions of the substrate exert a major control over the distribution of both trace metals and diagenetic iron mineralogy. The distribution of Fe in the substrates at both sites is strongly controlled by redox conditions, with the secondary Fe oxides akageneite (β-FeOOH) and goethite (α-FeOOH) developing in response to oxidising conditions, whereas pyrite and marcasite are stable under reducing conditions. Redox values also probably influence the distribution of trace mentals, with zinc profiles from Purry Burry Point showing peaks in concentration in response to redox boundaries within the substrate. Lead and copper are less responsive, indicating these trace metals may be contained in relatively inert phases such as slag.","PeriodicalId":197128,"journal":{"name":"Wetlands Australia Journal","volume":"58 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2010-01-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"6","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Wetlands Australia Journal","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31646/WA.156","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 6

Abstract

The vertical and lateral distributions of Pb, Cu, Zn and Fe in the substrates of two saltmarshes, 3 and 14km respectively, from the heavy industrial centre of Port Kembla have been determined. Particulate matter within the sediment reflects the differing contribution to each site from this point source, which is highlighted by the presence of up to 70% of anthropogenic components in the finer sediment in the saltmarsh at Purry Burry Point. The particulate material derived from industrial and pyrometallurgical processes has previously been assumed to be inert in the surrounding environment. However, in the intertidal zone occupied by the saltmarshes, the redox conditions of the substrate exert a major control over the distribution of both trace metals and diagenetic iron mineralogy. The distribution of Fe in the substrates at both sites is strongly controlled by redox conditions, with the secondary Fe oxides akageneite (β-FeOOH) and goethite (α-FeOOH) developing in response to oxidising conditions, whereas pyrite and marcasite are stable under reducing conditions. Redox values also probably influence the distribution of trace mentals, with zinc profiles from Purry Burry Point showing peaks in concentration in response to redox boundaries within the substrate. Lead and copper are less responsive, indicating these trace metals may be contained in relatively inert phases such as slag.
新南威尔士州伊拉瓦拉地区两个盐沼基质中痕量金属的分布
测定了距肯布拉港重工业中心3 km和14km两个盐沼底物中Pb、Cu、Zn和Fe的垂直和横向分布。沉积物中的颗粒物质反映了这个点源对每个地点的不同贡献,这一点在Purry Burry point盐沼中细小沉积物中高达70%的人为成分的存在中得到了突出体现。来自工业和火法冶金过程的颗粒物质以前被认为在周围环境中是惰性的。然而,在盐沼占据的潮间带,底物的氧化还原条件对微量金属和成岩铁矿物学的分布起主要控制作用。两个地点的底物中铁的分布受氧化还原条件的强烈控制,次生铁氧化物akageneite (β-FeOOH)和针铁矿(α-FeOOH)在氧化条件下发育,而黄铁矿和马氏铁矿在还原条件下稳定。氧化还原值也可能影响微量金属的分布,来自Purry Burry Point的锌剖面显示出浓度峰值,以响应底物内的氧化还原边界。铅和铜的反应性较差,表明这些微量金属可能包含在相对惰性的相中,如炉渣。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信