Janaki-Raman D, Jonathan M P, Srinivasalu S, Armstrong-Altrin J S, Mohan S P, Ram-Mohan V
Department of Geology, School of Earth and Atmospheric Sciences, University of Madras, Guindy Campus, Chennai - 600 025, India.
Environ Pollut. 2007 Jan;145(1):245-57. doi: 10.1016/j.envpol.2006.03.012. Epub 2006 May 15.
Core sediments from Mullipallam Creek of Muthupet mangroves on the southeast coast of India were analyzed for texture, CaCO(3), organic carbon, sulfur and acid leachable trace metals (Fe, Mn, Cr, Cu, Ni, Co, Pb, Zn and Cd). Textural analysis reveals a predominance of mud while CaCO(3) indicates dissolution in the upper half of the core, and reprecipitation of carbonates in reduction zones. Trace metals are diagenetically modified and anthropogenic processes control Pb and, to some extent, Ni, Zn and Fe. A distinct event is identified at 90 cm suggesting a change in deposition. Strong relationship of trace metals with Fe indicates that they are associated with Fe-oxyhydroxides. The role of carbonates in absorbing trace metals is evident from their positive relationship with trace metals. Comparison of acid leachable trace metals indicates increase in concentrations in the study area and the sediments act as a sink for trace metals contributed from multiple sources.
对印度东南海岸穆图佩特红树林的穆利帕勒姆溪的岩心沉积物进行了质地、碳酸钙、有机碳、硫和酸可浸出痕量金属(铁、锰、铬、铜、镍、钴、铅、锌和镉)分析。质地分析显示以泥质为主,而碳酸钙表明在岩心的上半部分溶解,在还原区碳酸盐再沉淀。痕量金属发生了成岩作用改变,人为过程控制着铅,并在一定程度上控制着镍、锌和铁。在90厘米处识别出一个明显事件,表明沉积发生了变化。痕量金属与铁的强相关性表明它们与铁的羟基氧化物有关。碳酸盐与痕量金属的正相关关系表明了其在吸收痕量金属方面的作用。酸可浸出痕量金属的比较表明研究区域内浓度增加,沉积物充当了多种来源贡献的痕量金属的汇。