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重金属与磷质黏土的相互作用:吸附与解吸行为

Heavy metal interactions with phosphatic clay: sorption and desorption behavior.

作者信息

Singh S P, Ma L Q, Harris W G

机构信息

Soil Science Division, Univ. of Idaho, Moscow 83844-2339, USA.

出版信息

J Environ Qual. 2001 Nov-Dec;30(6):1961-8. doi: 10.2134/jeq2001.1961.

Abstract

Heavy metals produced and released during agricultural and industrial activities may pose a serious threat to the environment. This study investigated the effectiveness of phosphatic clay, a by-product of the phosphate mining industry, for immobilizing heavy metals (Pb(+2), Cd(+2), and Zn(+2)) from aqueous solutions. A batch equilibrium technique was adopted to evaluate metal sorption in the presence of 0.05 M KNO3 background electrolyte solution. The amounts of metals sorbed onto phosphatic clay decreased in the order Pb(+2) > Cd(+2) > Zn(+2). Desorption data suggest that a large fraction of metals sorbed onto phosphatic clay stayed intact under a wide variation in extracting solution pH (ranging from 3 to 10). Desorption rates were slowest for Pb followed by Cd and Zn. Only 8.1 to 23.1% of Pb, 8.4 to 45% of Cd, and 21.9 to 73.9% of Zn sorbed on phosphatic clay was mobilized by USEPA toxicity characteristic leaching procedure (TCLP) solutions at pH 2.93+/-0.05 and 4.93+/-0.05, respectively. Formation of fluoropyromorphite [Pb10(PO4)6(F2)], confirmed by scanning electron microscopy (SEM) and X-ray diffraction (XRD), after reaction of aqueous Pb with phosphatic clay suggested that precipitation remained the dominant mechanism for Pb removal from aqueous solution. In the case of aqueous Cd and Zn interaction with phosphatic clay, we are not able to confirm the formation of a new amorphous and/or crystalline phase on the basis of available information. Other possible sorption mechanisms for Cd and Zn may include sorption and coprecipitation. Thus, phosphatic clay may be an effective amendment for in situ immobilization of heavy metals in contaminated soils and sediments.

摘要

农业和工业活动中产生并释放的重金属可能对环境构成严重威胁。本研究调查了磷矿开采行业的副产品——磷质黏土对从水溶液中固定重金属(Pb(+2)、Cd(+2)和Zn(+2))的有效性。采用批次平衡技术评估在0.05 M KNO3背景电解质溶液存在下的金属吸附情况。吸附在磷质黏土上的金属量按Pb(+2) > Cd(+2) > Zn(+2)的顺序递减。解吸数据表明,在提取溶液pH值广泛变化(范围为3至10)的情况下,吸附在磷质黏土上的大部分金属保持完整。Pb的解吸速率最慢,其次是Cd和Zn。在pH值为2.93±0.05和4.93±0.05的美国环境保护局毒性特征浸出程序(TCLP)溶液中,分别只有8.1%至23.1%吸附在磷质黏土上的Pb、8.4%至45%的Cd和21.9%至73.9%的Zn被活化。通过扫描电子显微镜(SEM)和X射线衍射(XRD)证实,水溶液中的Pb与磷质黏土反应后形成了氟磷灰石[Pb10(PO4)6(F2)],这表明沉淀仍然是从水溶液中去除Pb的主要机制。对于水溶液中的Cd和Zn与磷质黏土的相互作用,根据现有信息我们无法确认形成了新的无定形和/或结晶相。Cd和Zn的其他可能吸附机制可能包括吸附和共沉淀。因此,磷质黏土可能是原位固定污染土壤和沉积物中重金属的有效改良剂。

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