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Influential factors on the exchange rate of dissolved inorganic nutrients at the sediment-water interface in Jiaozhou Bay, China

机译:胶州湾沉积物-水界面溶解性无机养分交换速率的影响因素

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摘要

Incubation experiments are carried out to study the exchange rates of dissolved inorganic nutrients including silicate, phosphate, ammonium, nitrite, and nitrate (v_(SiO_3-Si), v_(PO_4-P), v_(NH_4-N), v_(NO_2-N) and v_(NO_3-N)) at the sediment-water interface in the Jiaozhou Bay. Major factors influencing the exchange rates are discussed in detail, which include the dissolved inorganic nutrient concentrations in porewater (C_(pw)), water and clay contents, and grain size of the sediments (C_(H_2O), C_(clay) and GS_(sed)). The results may provide insight into the dynamics of nutrient transport and the environmental capacity of nutrients in Jiaozhou Bay, and should be beneficial to solving the problems caused by excessive nutrient input this area.
机译:进行孵化实验以研究溶解的无机养分的交换速率,包括硅酸盐,磷酸盐,铵,亚硝酸盐和硝酸盐(v_(SiO_3-Si),v_(PO_4-P),v_(NH_4-N),v_(NO_2 -N)和v_(NO_3-N))在胶州湾的沉积物-水界面。详细讨论了影响汇率的主要因素,包括孔隙水中溶解的无机养分浓度(C_(pw)),水和粘土含量以及沉积物的粒径(C_(H_2O),C_(粘土)和GS_ (sed))。研究结果可以为胶州湾的养分运移动态和养分的环境容量提供洞察力,对解决该地区因养分过多而引起的营养不良问题具有一定的借鉴意义。

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