雅加达湾沉积物的晚全新世重金属记录

R. Zuraida, R. Rahardiawan, Y. Permanawati, I. Adhirana, Andrian Ibrahim, Nazar Nurdin, H. Permana
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引用次数: 0

摘要

本文报道了公元600年以来雅加达湾沉积物中铜、锌、铅、镉和铬的记录,并重建了自那时以来的环境变化。本研究使用了2010年由海洋地质研究所搭载RV Geomarin I在雅加达湾东部采集的150 cm长的重力岩心(TJ-17, 106.902488°E, 5.99381°S)的样本。雅加达湾沉积物中的重金属含量被用来从这个地点追踪陆地上的环境变化。采用原子吸收光谱法对每隔5cm采集的大量样品进行重金属浓度分析。结果得出背景水平Cu为16 ppm, Zn为75 ppm, Pb为20 ppm, Cd为0.01 - 0.15 ppm, Cr为80 ppm。重金属的垂直记录显示了该地区环境变化的两个阶段:从公元600年到公元1600年和公元1800年以后。这些变化被解释为与西爪哇地区人类活动引起的土地利用变化有关。
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LATE HOLOCENE HEAVY METALS RECORD OF JAKARTA BAY SEDIMENTS
This paper reports copper, zinc, lead, cadmium, and chromium records of Jakarta Bay sediment since 600 AD and reonstruct environmental changes since that time. Jakarta Bay This study uses samples from a 150 cm long gravity core (TJ-17, 106.902488°E, 5.99381°S) that was acquired from the eastern part of Jakarta Bay in 2010 onboard RV Geomarin I by the Marine Geological Institute. Heavy metal content in Jakarta Bay sediments is used to track environmental changes onland from this site. Heavy metal concentration was analyzed using atomic absorption spectrometry on bulk samples that were taken in 5 cm interval. The results yield background level of Cu at 16 ppm, Zn at 75 ppm, Pb at 20 ppm, Cd at 0.01 – 0.15 ppm, and at Cr 80 ppm. Vertical record of heavy metals show two stages of environmental changes in the region: from 600 AD to 1600 AD and 1800 AD onward. These changes are interpeted as related to land use changes caused by human activity in the West Java region.
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来源期刊
自引率
0.00%
发文量
6
审稿时长
16 weeks
期刊最新文献
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