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The Functions of China Marginal Sea Sediments in the Cycle of Biogenic Elements

机译:中国边缘海沉积物在生物成因循环中的作用

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摘要

The contents of biogenic elements in China marginal sea sediments are related to their grain sizes, river transport, et al. In general, the finer the grain size is, the higher the contents of organic matter and OC, N, P are, the lower the contents of S and Si are. The biogeochemical environments of sediments are related to Eh, pH, temperature content of OC, Fe~(3+)/Fe~(2+) radio, water dynamics condition, grain size of sediment, S system in sediment interstitial waters, et al., and they influence the early diageneses and cycle of biogenic elements in sediments. In most regions of China marginal sea, the flux directions of S~(2-), HS~-, H_4SiO_4, PO_4~(3-), NH~(4+) across the sediment-water interface are from sediment to the overlying seawater, the flux directions of SO_4~(2-), HCO_3~-, NO_3~-, NO_2~- across the sediment-water interface are from the overlying seawater to sediment. The irrigation of living things is important in the cycle of the biogenic elements across sediment-water interfaces.
机译:中国边缘海沉积物中生物成因的含量与其粒径,河流运输等相关。通常,晶粒尺寸越细,有机物和OC,N,P的含量越高,S和Si的含量越低。沉积物的生物地球化学环境与Eh,pH,OC的温度含量,Fe〜(3 +)/ Fe〜(2+)辐射,水动力学条件,沉积物的粒径,沉积物间隙水的S系统等有关。 ,并且它们影响沉积物中早期成岩作用和生物成因元素的循环。在中国边缘海的大部分地区,沉积物-水界面的S〜(2-),HS〜-,H_4SiO_4,PO_4〜(3-),NH〜(4+)的通量方向是从沉积物到上覆海水中,SO_4〜(2-),HCO_3〜-,NO_3〜-,NO_2〜-穿过沉积物-水界面的通量方向是从上覆海水到沉积物。生命的灌溉对于沉积物-水界面中生物元素的循环至关重要。

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