钙离子和pH对长江河口青草沙水库水体磷含量的影响

Impact of Calcium and pH on Content of Phosphorus in Water of Qingcaosha Reservoir of Yangtze Estuary

  • 摘要: 选取长江河口水库,通过对水体钙离子(Ca2+)和pH影响沉积物中的磷吸附-释放作用以及沉积物不同形态磷变化的分析,并运用X射线衍射(XRD)技术进行沉积物成分分析,研究水体Ca2+和pH对水体磷浓度的影响。结果表明:Ca2+的存在能促进沉积物吸附水体磷,而抑制沉积物中的磷释放至水体,导致水体磷浓度降低;在Ca2+的作用下,当pH<3,沉积物对水体磷呈现负吸附状态,表现为沉积物释放磷的过程,水体磷浓度升高;当pH>3时,沉积物表现为吸附磷状态,使得水体磷浓度降低。沉积物上的钙结合态磷(Ca-P)浓度增加后,沉积物中羟基磷酸钙〔Ca5(OH)(PO4)3〕晶体化合物浓度也增加,并且沉积物出现新的钙结合态晶体化合物。在碱性条件下,Ca2+的存在能促进水体磷浓度降低。 

     

    Abstract: To study the effect of calcium ion and pH on phosphorus content in the water in the Yangtze Estuary Reservoir, the rule of phosphorus adsorption and release in the sediment and the change of various forms of phosphorus affected by calcium ion and pH was analyzed, and the components of the sediment was further analyzed by XRD technology. The result suggested that Ca2+ significantly increased the adsorption of sediment on phosphorus while inhibiting the release of phosphorus from sediment, and thus the content of phosphorus in the water decreased. With the action of Ca2+, under pH<3, the sediment significantly decreased the release of phosphorus, it increased the content phosphorus in the water. Under pH>3, the sediment significantly increased the adsorption of phosphorus, and decreased the content phosphorus in the water. When the content of Ca binding P (Ca-P) fraction increased in the sediment, the content of Ca5(OH)(PO4)3increased, and new material of Ca -binding crystalline compound appeared on the sediment. In alkaline condition, the content of phosphorus in the water decreased because of Ca2+.

     

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