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Impact of rainfall on spatio-temporal distribution of sediment organic matter along the Chittagong Coast, Bangladesh

机译:降雨对孟加拉国吉大港沿岸沉积物有机质时空分布的影响

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Sediment organic matter regulates the coastal biogeochemical cycle which is influenced by rainfall pattern and has potential relationship with organic carbon as well as mud characteristics. The objective of present research was to identify the impact of precipitation on the spatiotemporal variation inorganic features of intertidal mudflats. Three locations were selected in freshwater zone; two were in brackish water region and last three locations situated in marine waters from Halda to Salimpur coast. Two sites from each location were designated as the highest high tide level (onshore) and lowest low tide level (offshore) of the intertidal zone during winter (December to February) and monsoon (June to August) spanning between 2013 and 2014. Sediment organic matter and carbon were measured by combustion and Walkey-Black wet oxidation in turn. Average organic matter content in monsoon were found 4.5±0.03, 2.3±0.01 and 2.4 in freshwater, brackish and marine locations whereas 5.2±0.6, 3.9±0.14 and 5.4±0.04% investigated during winter. Precipitation pattern varies from different seasons and locations that have impact on land runoff, freshwater inflow, mixing and circulation. Mud dominated coastal intertidal zones represented high organic matter content than sand dominated coast. Furthermore, depositional pattern, transport, erosion-accretion processes, tidal action, wave characteristics and seasonal inconstancy control the organic matter characteristics in the coastal sediment. This research suggests the necessity of periodic observation of rainfall pattern and organic matter distribution to assess the intertidal deposits which support the stabilization of local geomorphology and biogeochemistry in Chittagong coastal region. Res. Agric., Livest. Fish.3(1): 175-186, April 2016.
机译:沉积物有机质调节着沿海生物地球化学循环,该循环受降雨模式的影响,并且与有机碳以及泥质特征有潜在的关系。本研究的目的是确定降水对潮间带滩涂无机物时空变化的影响。在淡水区选择了三个地点;其中两个位于咸淡水区域,最后三个位于从Halda到Salimpur海岸的海水中。在2013年至2014年之间的冬季(12月至2月)和季风(6月至8月),每个位置的两个高潮位被指定为潮间带的最高高潮位(陆上)和最低低潮位(离岸)。通过燃烧和Walkey-Black湿式氧化依次测量物质和碳。在淡水,咸淡和海洋地区季风中平均有机物含量为4.5±0.03、2.3±0.01和2.4,而冬季调查的平均有机物含量为5.2±0.6、3.9±0.14和5.4±0.04%。降雨方式因季节和地点的不同而不同,这些都会影响土地径流,淡水流入,混合和循环。泥质为主的沿海潮间带比沙质为主的沿海代表了更高的有机质含量。此外,沉积模式,运移,侵蚀积累过程,潮汐作用,波浪特征和季节不稳定性控制着沿海沉积物中的有机物特征。这项研究表明有必要定期观察降雨模式和有机质分布以评估潮间带沉积物,以支持吉大港沿海地区局部地貌和生物地球化学的稳定。 Res。 Agric。,Livest。 Fish.3(1):175-186,2016年4月。

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