中国环境科学
中國環境科學
중국배경과학
CHINA ENVIRONMENTAL SCIENCE
2014年
1期
161-169
,共9页
李佳%詹艳慧%林建伟%杨孟娟%方巧%郑雯婧
李佳%詹豔慧%林建偉%楊孟娟%方巧%鄭雯婧
리가%첨염혜%림건위%양맹연%방교%정문청
镧改性沸石%改良%磷%释放%吸附
鑭改性沸石%改良%燐%釋放%吸附
란개성비석%개량%린%석방%흡부
lanthanum-modified zeolite%amendment%phosphorus%release%sorption
考察了不同反应时间、pH值、硅酸根离子浓度、DO浓度、老化时间以及初始磷浓度等条件下一种新型底泥改良剂-镧改性沸石对太湖底泥-水系统中磷的固定作用。当水中磷浓度很低时,太湖底泥和镧改性沸石改良太湖底泥均释放出磷。镧改性沸石改良太湖底泥的释磷量少于太湖底泥。镧改性沸石改良太湖底泥中金属氧化物结合态磷(NaOH-P)和钙结合态磷(HCl-P)等较为稳定形态磷含量多于太湖底泥,而镧改性沸石改良太湖底泥中氧化还原敏感态磷(BD-P)这种不稳定形态磷含量少于太湖底泥。太湖底泥和镧改性沸石改良太湖底泥对水中较高浓度磷酸盐的吸附平衡数据均可以采用 Langmuir 等温吸附模型加以描述。镧改性沸石改良太湖底泥对水中磷酸盐的吸附能力明显高于太湖底泥,且吸附能力随老化时间的增加而降低。被镧改性沸石所吸附的磷酸盐主要以NaOH-P和HCl-P等较为稳定形态磷存在,不容易被重新释放出来。上述结果表明,采用镧改性沸石对太湖底泥进行原位改良可以增强太湖底泥对磷的固定能力,减少太湖底泥磷的释放。
攷察瞭不同反應時間、pH值、硅痠根離子濃度、DO濃度、老化時間以及初始燐濃度等條件下一種新型底泥改良劑-鑭改性沸石對太湖底泥-水繫統中燐的固定作用。噹水中燐濃度很低時,太湖底泥和鑭改性沸石改良太湖底泥均釋放齣燐。鑭改性沸石改良太湖底泥的釋燐量少于太湖底泥。鑭改性沸石改良太湖底泥中金屬氧化物結閤態燐(NaOH-P)和鈣結閤態燐(HCl-P)等較為穩定形態燐含量多于太湖底泥,而鑭改性沸石改良太湖底泥中氧化還原敏感態燐(BD-P)這種不穩定形態燐含量少于太湖底泥。太湖底泥和鑭改性沸石改良太湖底泥對水中較高濃度燐痠鹽的吸附平衡數據均可以採用 Langmuir 等溫吸附模型加以描述。鑭改性沸石改良太湖底泥對水中燐痠鹽的吸附能力明顯高于太湖底泥,且吸附能力隨老化時間的增加而降低。被鑭改性沸石所吸附的燐痠鹽主要以NaOH-P和HCl-P等較為穩定形態燐存在,不容易被重新釋放齣來。上述結果錶明,採用鑭改性沸石對太湖底泥進行原位改良可以增彊太湖底泥對燐的固定能力,減少太湖底泥燐的釋放。
고찰료불동반응시간、pH치、규산근리자농도、DO농도、노화시간이급초시린농도등조건하일충신형저니개량제-란개성비석대태호저니-수계통중린적고정작용。당수중린농도흔저시,태호저니화란개성비석개량태호저니균석방출린。란개성비석개량태호저니적석린량소우태호저니。란개성비석개량태호저니중금속양화물결합태린(NaOH-P)화개결합태린(HCl-P)등교위은정형태린함량다우태호저니,이란개성비석개량태호저니중양화환원민감태린(BD-P)저충불은정형태린함량소우태호저니。태호저니화란개성비석개량태호저니대수중교고농도린산염적흡부평형수거균가이채용 Langmuir 등온흡부모형가이묘술。란개성비석개량태호저니대수중린산염적흡부능력명현고우태호저니,차흡부능력수노화시간적증가이강저。피란개성비석소흡부적린산염주요이NaOH-P화HCl-P등교위은정형태린존재,불용역피중신석방출래。상술결과표명,채용란개성비석대태호저니진행원위개량가이증강태호저니대린적고정능력,감소태호저니린적석방。
In-situ sorbent amendment is a promising contaminated sediment remediation technology. The immobilization of phosphorus (P) in Taihu Lake sediment-water systems using lanthanum-modified zeolite (LaMZ) as a novel amendment was investigated by conducting a series of experiments. P could be released from unamended and LaMZ-amended Taihu Lake sediments at a very low initial concentration of P in water. The amount of P released from LaMZ-amended Taihu Lake sediment was less than that from Taihu Lake sediment. The content of NaOH-P (P extracted with NaOH) or HCl-P (P extracted with HCl) in LaMZ-amended Taihu Lake sediment was higher than that in Taihu Lake sediment. The content of BD-P (P extracted with bicarbonate dithionite) in LaMZ-amended Taihu Lake sediment was less than that in Taihu Lake sediment. The equilibrium sorption of phosphate from aqueous solution at a high initial concentration of P (0.5~15mg/L) could be described by the Langmuir isotherm model. The phosphate sorption capacity for LaMZ-amended Taihu Lake sediment was much higher than that for Taihu Lake sediment. The phosphate sorption capacity for LaMZ-amended Taihu Lake sediment decreased with increasing aging time. Sequential extraction of P from phosphate-sorbed Taihu Lake sediment and LaMZ-amended Taihu Lake sediment indicated that most of sorbed phosphate onto LaMZ existed in NaOH-P and HCl-P forms, and was relatively stable and unlikely to be released under anaerobic condition. Results of this work indicate that in-situ LaMZ amendment is a promising method for controlling P release from Taihu Lake sediment.