海州湾海洋牧场表层沉积物中磷形态及释放通量

Forms and releasing flux of phosphorus in the surface sediments in Haizhou Bay marine ranching

  • 摘要: 为了解海州湾海洋牧场建设对沉积物-水界面磷酸盐交换的影响,于2017年5月采集了海州湾海洋牧场区表层沉积物及对应站点上覆水、间隙水等样品。采用SMT法(standard measurement test)分级提取磷的不同形态,包括可交换态磷(Ex-P)、铁铝态结合磷(Fe/Al-P)、钙结合态磷(Ca-P)并测定其浓度,结合室内磷通量模拟实验,尝试探索沉积物-水界面磷交换通量。结果显示,海州湾海洋牧场区表层沉积物中总磷(TP)浓度为392.44~463.46 μg/g,IP浓度为219.21~282 μg/g,Ca-P浓度为117.73~130.07 μg/g。无机磷(IP)是磷的主要赋存形态;分级提取的磷形态浓度顺序为Ca-P > Ex-P > Fe/Al-P,对照区各种磷形态浓度大于鱼礁区,上覆水中的各种形态磷浓度均高于间隙水。室内模拟实验显示,沉积物中各种形态磷的浓度增加,IP仍为磷的主要赋存形态;沉积物-水界面TP、TDP(可溶性总磷酸盐)、\rmPO_4^3 - (可溶性正磷酸盐)的交换通量分别为−0.53~−0.05、−0.15~−0.01、−0.03~−0.29 mmol/(m2·d)。实验初期交换速率较快,然后趋于平缓,与对照区相比,海洋牧场区磷的交换通量稍大,但都表现为从上覆水体向沉积物中迁移,即沉积物中的磷表现为上覆水的汇。

     

    Abstract: In order to understand the impact of Haizhou Bay marine ranching construction on the phosphate exchange at sediment-water interface, multiple surface sediments, overlying water and interstitial water samples were collected from the Haizhou Bay ocean ranch area in May 2017. The different forms of phosphorus were extracted by SMT (Standard Measurement Test), including exchangeable phosphorous (Ex-P), iron-aluminum bound phosphorous (Fe/Al-P), calcium-bound phosphate (Ca-P), then their amounts were determined. The phosphorus exchange flux at the sediment-water interface was estimated under the phosphorus flux simulation incubation experiment. The results showed that the contents of the total phosphorus (TP), inorganic phosphorus (IP) and Ca-P in the surface sediments of Haizhou Bay marine ranching ranged from 392.44 to 463.46 μg/g, 219.21 to 282 μg/g and 117.73 to 130.07 μg/g, respectively. The IP was found as the major form of phosphorus. The order of the contents of different forms of phosphorus was Ca-P> Ex-P> Fe/Al-P. The contents of phosphorus in the control area were greater than that in the reef area. The concentrations of various forms of phosphorus in the overlying water were higher than the sediment pore water. Laboratory phosphorus flux simulation experiments showed that the content of various forms of phosphorus in sediments were higher after the incubation process, and IP still the main form of phosphorus. The exchange fluxes of TP, TDP, and \rmPO_4^3 - at the sediment-water interface were estimated at −0.53—−0.05 mmol/(m2·d), −0.15—−0.01 mmol/(m2·d) and −0.03—−0.29 mmol/(m2·d), respectively. The exchange rate was faster at the initial stage of the incubation experiment, and then tended to stabilize. Compared with the control area, the exchange flux of phosphate in the marine ranching was slightly greater, but both showed the tendency that phosphorus migrate from the overlying water to sediment. It suggests that phosphorus in surface sediments acts as a sink of overlying water. These results are expected to provide scientific basis for the reef construction and restoration projects of Haizhou Bay Marine Ranch.

     

/

返回文章
返回