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首页> 外文期刊>Chilean Journal of Agricultural Research >Changes in sediment properties and bacterial community in marine sediments after entering the coastal land in Bohai Bay, northern China
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Changes in sediment properties and bacterial community in marine sediments after entering the coastal land in Bohai Bay, northern China

机译:中国北部渤海湾沿海地陆地沉积物沉积物及细菌群落的变化

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In coastal areas of Bohai Bay, China, marine sediments were used for land reclamation. However, vegetation cannot grow well on the reclaimed land because marine sediments have different ecological functions than soil. Changing marine sediment into soil rapidly and accelerating the soil-forming process is key to solving this ecological problem on reclaimed land. Therefore, in this study, we not only measured the chemical properties of marine sediments during an 8 yr soil formation period to explore fertility changes, but we also used MiSeq sequencing to analyze and compare the bacterial community structure and diversity before and after the 8 yr land reclamation. Our results showed: (1) Marine sediment changed from severe to mild salinization during the 8 yr of soil formation, and the sediment salinity decreased significantly to 7.3 g kg-1 (p 0.05). However, pH of the sediment was always 8.5 and did not change significantly. In addition, the total fertility of the sediment decreased significantly after 8 yr. Especially, the content of nitrate-N in marine sediment decreased significantly by 86.23% (p 0.05) after 8 yr of soil formation. Also, the content of available P and soil organic matter decreased significantly by 45.92% and 26.22%, respectively. (2) The total abundance of bacteria increased while the community diversity decreased after the sediments were removed from the ocean environment for 8 yr. The bacterial community composition changed, and results of our redundancy analysis (RDA) indicated that the change was mainly affected by pH, soil contents including, available P, nitrate-N, ammonia-N, Na+, and Cl-, as well as salinity.
机译:在中国渤海湾沿海地区,海洋沉积物用于陆地填海。然而,由于海洋沉积物与土壤不同的生态功能,植被不能很好地发展。将海洋沉积物迅速改变为土壤,加速土壤成矿过程是解决重新土地上这种生态问题的关键。因此,在这项研究中,我们不仅在8年的土壤形成时间内测量了海洋沉积物的化学性质,以促进生育率变化,但我们也使用MISEQ测序在8年前和之后分析和比较了在8年前和之后的细菌群落结构和多样性土地复垦。我们的结果表明:(1)海洋沉积物在土壤形成的8年期间从严重转变为温和的盐渍化,沉积物盐度明显减少至7.3g kg-1(p <0.05)。然而,沉积物的pH值始终> 8.5,并且不会显着变化。此外,在8年后,沉积物的总肥力显着下降。特别是,在土壤形成8年后,海洋沉积物中硝酸盐-N的含量显着降低了86.23%(P <0.05)。而且,可用P和土壤有机物的含量分别下降了45.92%和26.22%。 (2)细菌的总丰富在从海洋环境中除去沉积物后,群体多样性降低了8年。细菌群落组成改变,我们的冗余分析结果(RDA)表明,该变化主要受PH,土壤含量,包括可用的P,硝酸盐-N,氨-N,Na +和Cl-的影响,以及盐度。

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