摘要
研究了黄河中下游12个沉积物的临界磷平衡浓度(EPC0),以此判断沉积物是磷'源'还是磷'汇'.用修改后的Langmuir等温吸附模型对吸附实验数据进行了拟合,结果得到最大吸附容量(PAC),Langmuir吸附平衡常数(k).利用所得拟合参数通过公式计算方法得到EPC0、原有交换态磷(NAP)以及固-液分配系数Kp值并考察了环境因子(pH、离子强度)对吸附作用的影响.沉积物的EPC0均大于上覆水体中的磷浓度,沉积物有向上覆水体释放磷的能力.吸附容量与总有机碳(TOC)含量有较好的正相关关系.pH<6.0,沉积物释放磷并且随着pH增大吸附量增加很快;6<pH<9.7,P的吸附量维持在一个较恒定的水平;pH>9.7,吸附量略有增高.随着Ca2+离子强度的增加,沉积物对磷的吸附量减小.
The equilibrium phosphate concentration（EPC0） of the Yellow River bed sediments has been measured,which was used to predict whether bed sediments are acting as a source or sink of soluble reactive phosphate（SRP）.The modified Langmuir isotherm equation was used to describe phosphate（P） sorption on the Yellow River sediments.The maximum P sorption capacity（PAC） and P-binding energy constant（k） were obtained by the modified Langmuir isotherm model.Native adsorbed exchangeable phosphorus（NAP）,the EPC0,and partitioning coefficients（Kp） were subsequently calculated by the corresponding formulae.The influence of pH values and ion strength were evaluated.All the EPC0s are higher than the P concentration in the overlying water,indicating a potential source of phosphate from the sediments.PAC is linearly related to the contents of TOC of the sediment. The sorption capacity of P increased rapidly with pH below 6.0,and then reached a plateau between pH 6.0 to 9.7,and finally maintained at a slightly higher level from pH 9.7 to 12.0.The adsorption of P by the sediment decreased with the increase in Ca^2＋ ionic strength.
出处
《环境科学》
EI
CAS
CSCD
北大核心
2008年第8期2137-2142,共6页
Environmental Science
基金
国家自然科学基金项目(20467002)
关键词
黄河沉积物
磷
吸附
Yellow River bed sediment
phosphate
adsorption
