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Studies on the regional feature of organic carbon in sediments off the Huanghe River Estuary waters

机译:黄河口水域沉积物中有机碳的区域特征研究

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Organic carbon (OC) in definitely small area sediments(according to marine dimension) off the Huanghe River Estuary is investigated in order to evaluate the feature of regional difference of physical and chemical properties in marginal sea sediments. The distributions of OC in sediments with natural grain size and the relationship with the pH, Eh, Es and Fe~(3+)/Fe~(2+) are discussed. In addition,OC decomposition rates in surfacial/subsurfacial sediments are estimat-ed.OC concentrations range from 0.26% to 1.8%(wt)in the study area. Significant differences in OC content and in horizontal distribution as well as various trends in surfacial /subsurfacial sediments exhibit the feature of regional difference remarkably in marginal sea sediments. The complicated distribution of OC in surface sediments is due to the influence of bacterial activity and abundance, bioturbation of benthos and physical disturbance. The OC decomposition rate constant in surfacial/subsurfacial sediments ranges from 0.009 7 to 0.076 a~(-1) and the relatively high values may be mainly related to bacteria that are mainly responsible for OC mineralization;meio-and macrofauna affect OC degradation both directly, through feeding on it, and indirectly through bioturbation and at the same time coarse sediments are also disadvantageous to OC preservation. In almost all the middle and bottom sediments the contents of OC decrease with the increase of deposition depth, which indicates that mineralization of OC in the middle and bottom sediments has occurred via processes like SO_4~(2-) reduction and Fe-oxide reduction.
机译:为了评估边缘海沉积物理化性质的区域差异特征,研究了黄河口外一定面积(根据海洋尺度)的沉积物中的有机碳(OC)。讨论了自然粒径沉积物中OC的分布及其与pH,Eh,Es和Fe〜(3 +)/ Fe〜(2+)的关系。此外,还估算了表面/表面下沉积物中的OC分解率。研究区域的OC浓度范围为0.26%至1.8%(wt)。边缘海沉积物中OC含量和水平分布的显着差异以及表面/亚表面沉积物的各种趋势表现出区域差异的特征。 OC在表层沉积物中的复杂分布是由于细菌活性和丰度,底栖生物的生物扰动和物理干扰的影响。表层/表层下沉积物中的OC分解速率常数范围为0.009 7至0.076 a〜(-1),相对较高的值可能主要与造成OC矿化的细菌有关;中,大型动物直接影响OC的降解,通过摄食,间接地通过生物扰动以及同时粗颗粒沉积物也不利于OC的保存。几乎所有中下部沉积物中OC的含量随沉积深度的增加而降低,这表明中下部沉积物中OC的矿化是通过SO_4〜(2-)还原和Fe-氧化物还原等过程发生的。

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