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Changes of Estuarine Sedimentation Patterns by Urban Expansion: The Case of Middle Capibaribe Estuary, Northeastern Brazil

机译:城市扩张河口河口沉积模式的变化:巴西东北北京河口河口中西番

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The aim of this study is to describe the sedimentary evolution occurred during the last 200-years in the middle Capibaribe Estuary by mean of the sedimentary analysis (magnetic susceptibility, grain size, calcium carbonate, total organic matter—TOM) and geochemical parameters (sedimentation rates, heavy metal concentrations, enrichment and contamination factor) along a core. The core recorded four units and the measured sedimentation rate was 0.52 cm cm·y﹣1. The first unit, dating before 1812, showed environmental characteristics of mangrove with predominance of fine sediments, high total organic matter percentages and heavy metal concentrations probably from natural sources. The second unit, from 1812 to 1937, showed a slight increase in sand percentages and decrease in fine fraction, TOM contents and heavy metals concentrations. These characteristics may be associated with the urban expansion processes and the presence of monoculture of sugar cane occurred in the middle Capibaribe Estuary. The third unit, from 1937 to 2004, showed the highest sand percentages of the core, characterizing a unit exclusively of sand with low fine fractions percentages, total organic matter contents and heavy metals concentrations. This unit represented the intensification of the urban processes expansion of Recife City. The fourth unit showed increases in fine fraction sedimentation, TOM contents and heavy metals concentrations. This new change in sedimentation probably is consequence of rebirth of marginal estuarine banks by mangrove vegetation, due to environmental projects carried out by Recife Prefecture in the early 2000’s. It was not possible to register the anthropic contamination to middle estuary area probably due to the Barreiras Formation influences in the metal concentration records, masking the anthropic contamination inputs in estuarine region. Although, lead and arsenic showing an enrichment level indicating anthropic contamination.
机译:本研究的目的是通过沉积分析(磁性敏感,粒度,碳酸钙,总有机物-TOM)和地球化学参数(磁化率,粒径,碳酸钙,地球化学参数)来描述在中载河口的沉积演变中发生沉积演化。(沉淀沿核心的速率,重金属浓度,富集和污染因子)。核心记录了四个单位,测得的沉降率为0.52cm cm·y-1。第一个单位,约会于1812年,显示了红树林的环境特征,主要是细沉积物,高总机质百分比和大金属浓度可能来自天然来源。第二单元从1812年到1937年,砂百分比略有增加,细分零件,汤姆内容和重金属浓度降低。这些特征可能与城市扩张过程有关,并且在中间Capibarbe河口中发生了单一栽培的单一栽培。第三单位从1937年到2004年显示出核心的最高含量百分比,其特征在于具有低细分级分,总有机物质含量和重金属浓度的砂的单位。本机构代表了累积城市的城市流程的加剧。第四个单元显示出细馏分沉积,汤姆内容和重金属浓度的增加。这种新的沉降变化可能是红树林植被的边缘河口银行重生的后果,因2000年初累累累累物县开展的环境项目。可能由于金属浓度记录中的Barreiras形成影响,掩盖了雌曲调区域中的人类污染输入,是不可能对中河内污染的影响。虽然,铅和砷显示出富集水平,表明人类污染。

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