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1.
自然水体生物膜、悬浮颗粒物和沉积物吸附铅、镉的热力学参数比较 总被引:7,自引:5,他引:7
采用实验室模拟的方法研究了松花江自然水体生物膜、悬浮颗粒物和沉积物吸附铅、镉的热力学规律。根据吸附热力学参数(Γmax、k和Kd)综合比较3种固相物质的吸附能力,并讨论吸附能力存在差异的原因。结果表明:Langmuir型及Freundlich等温式可以很好地描述3种固相物质吸附热力学规律,三者吸附铅、镉的能力为生物膜>悬浮颗粒物>沉积物,生物膜、悬浮颗粒物和沉积物对铅的吸附能力均明显高于对镉的吸附能力。 相似文献
2.
湿地水环境中表层沉积物吸附铅、镉能力的研究 总被引:6,自引:2,他引:6
在选定的实验条件下,对向海自然保护区5个不同类型湿地水体的表层沉积物样品进行了铅、镉的热力学吸附实验.结果表明,沉积物样品吸附铅、镉的过程符合Langmuir和Freundlich(n=8,p= 0.01) 等温吸附曲线.在所讨论的范围内,沉积物样品吸附铅、镉的能力与样品中铁、锰氧化物及有机质含量存在着显著的相关性.表层沉积物吸附铅、镉的能力小于生物膜吸附铅、镉的能力,即在湿地水环境中,生物膜对重金属迁移转化的作用相对于表层沉积物而言更重要. 相似文献
3.
多壁碳纳米管固相萃取快速检测水样中铅镉铜铁 总被引:1,自引:1,他引:0
传统的固相萃取填料应用于环境样品的重金属处理过程中,存在pH不稳定和不同极性萃取物共同萃取较为困难等方面的不足,因此寻找新型固相萃取填料显得尤为重要。本文采用多壁碳纳米管填充固相萃取柱,萃取水中金属元素铅、镉、铜和铁,采用石墨炉原子吸收光谱法测定铅和镉,电感耦合等离子体发射光谱法测定铜和铁。实验考察了多壁碳纳米管的性质、溶液pH值、洗脱溶液、样品流速以及基体效应对测定结果的影响。结果显示:溶液pH=9,1 mol/L硝酸为洗脱溶液,样品流速为2 mL/min时,外径8 nm未修饰的多壁碳纳米管有较好的萃取效率,对溶液中铅、镉、铜和铁的最大吸附容量分别为44.91、42.31、54.68和49.07 mg/g,四种元素的吸附容量均衡;钾、钠、钙、镁离子以及苯和甲苯等基质对四种金属元素的萃取影响不大。方法回收率为95.3%~99.5%,精密度(RSD,n=7)为1.2%~3.2%。本方法采用外径8 nm的多壁碳纳米管固相萃取,与传统萃取方法相比,富集效果好、回收率较高,而且操作简便、准确度高;与前人采用外径20~30 nm的多壁碳纳米管的性能相比,镉和铜的吸附容量更高,还可实现对铁的吸附,且铅、镉、铜和铁四种元素的吸附容量均衡,更适合用于检测水样中的金属元素。 相似文献
4.
土壤中铅铜锌镉的吸附特性 总被引:5,自引:0,他引:5
以徐州王庄矿(WZK)、奎河(KH)、背景-1(BG-1)和背景-2(BG-2)等4个土壤样品为供试对象,加入不同浓度梯度的铅、铜、锌、镉离子,通过静态实验研究了铅、铜、锌、镉的吸附特性。结果表明,土壤对4个重金属的吸附量与加入到土壤中的重金属离子浓度呈正相关性,它们之间大部分满足线性相关关系。在4个土壤样品中加入铅、铜、锌、镉离子的初始浓度比为10:10:10:1时,平衡浓度为Czn〉Ccu〉CPh〉Ccd,吸附量为Scd〉SPh〉Scu〉Szn,4个土壤样品对铅、铜、锌、镉离子的吸附能力依次为WZK〉KH〉BG-2〉BG-1。在所选实验条件下,土壤对铅、铜、锌、镉的吸附能力受土壤中铅、铜、锌、镉的含量、土壤有机质含量、阳离子交换量、土壤饱和含水量和土壤的pH值影响较大。 相似文献
5.
共存镉/铜对沉积物(生物膜)中主要组分吸附阿特拉津的影响 总被引:1,自引:0,他引:1
采用选择性萃取分离技术对沉积物(生物膜)中非残渣态组分(铁、锰氧化物和有机质)进行分离,研究阿特拉津(atrazine,AT)-Cd-Cu系中共存重金属对选择性萃取前后沉积物(生物膜)吸附AT的影响.研究结果表明:共存体系中,沉积物(生物膜)中铁氧化物对AT的吸附贡献最大,其次是有机质,而锰氧化物则抑制AT的吸附;共存镉促进了AT在沉积物(生物膜)原样及各非残渣态组分上的吸附,镉质量浓度为0.2 mg/L时,促进作用最显著,各组分对阿特拉津的吸附贡献增加了3.20%~32.31%(沉积物)和1.61%~17.10%(生物膜),但随镉质量浓度的增加,其促进作用减弱;共存铜抑制沉积物(生物膜)原样及铁氧化物、有机质对AT的吸附,铜质量浓度为75.0 mg/L时,其抑制作用最强,铁氧化物和有机质对阿特拉津的吸附贡献分别降低了29.21%、22.36%(沉积物)和9.46%、77.27%(生物膜),但同时减弱了锰氧化物对AT吸附的抑制作用,其吸附贡献分别提高了28.98%(沉积物)和17.46%(生物膜). 相似文献
6.
盐岩矿的水溶法开采是获得人类生活必需品和重要工业原料——盐的重要途径之一。在水溶法开采中,岩盐矿中的水溶性重金属会随着母液到达地表环境和后续的岩盐产品中,可能对地表环境造成污染和危害人体健康,故对岩盐矿中水溶性重金属的检测非常重要。岩盐矿中的水溶性铜铅锌镉含量较低,而盐分含量过高,过高的盐分含量会影响ICP-OES的雾化效率,故很难用ICP-OES直接测量重金属含量。本文以巯基棉为吸附材料,从溶液pH、洗脱液浓度、洗脱液体积等方面研究了分离富集岩盐矿中水溶性铜铅锌镉的实验条件。结果表明,在pH=7的介质中,巯基棉对铜铅锌镉有良好的吸附性能,被吸附的铜铅锌镉可用7 m L盐酸(15%)定量洗脱,溶液中的钠对吸附无明显影响。对解吸后的溶液,铜铅锌镉的回收率均≥92.2%,钠回收率仅0.04%,基本实现了铜铅锌镉与钠的分离,达到了ICP-OES检测要求。 相似文献
7.
空气滤膜吸附采集甘肃某农场大气粉尘样品,采用盐酸—硝酸—氢氟酸—高氯酸溶解,电感耦合等离子体质谱法(ICP-MS)同时测定溶液中铬、铜、砷、镉、铅等重金属元素含量,分析农田环境大气颗粒中的重金属元素对农作物的影响,同时验证不同仪器工作参数对测定结果的影响。实验表明:在选定的实验条件下,分析元素的检出限低,准确性和精密度... 相似文献
8.
为揭示农药(晶体乐果、甲霜灵、阿特拉津、马拉硫磷、扑草净)与重金属(铜、锌、铅、镉、镍)10种污染物共存时的复合污染规律,以阿特拉津为目标污染物,采用分辨度为Ⅲ的210-6分式析因实验设计,并用完全折叠实验和区组设计进行辅助,通过多元线性回归的建模方法筛选并建立了以阿特拉津为因变量、10种污染物因子主效应和二阶交互效应为自变量的多元线性回归吸附模型。研究表明:共存体系中因子主效应项铅、铜、锌、镉、镍和农药晶体乐果显著抑制(显著性水平α=0.05)阿特拉津在沉积物上的吸附,与阿特拉津产生竞争吸附效应,因重金属主效应产生的拮抗作用占总拮抗作用的63.5%,其拮抗作用从大到小为镍、镉、晶体乐果、锌、铅、铜;在以镍为关键自变量的二阶交互效应项中,因二阶交互效应项产生的协同或拮抗作用占阿特拉津吸附能力的35.3%,其中,铅、镉和晶体乐果抑制镍与阿特拉津的竞争吸附,与阿特拉津在沉积物上的吸附发生协同作用,协同作用从大到小为镉×镍、铅×镍、镍×晶体乐果;而镍作为调节自变量的二阶交互效应项镍阿特拉津会促进阿特拉津的吸附,说明多种污染物共存体系中重金属镍对阿特拉津在沉积物上吸附影响作用的复杂性和重要性。 相似文献
9.
铜(Ⅱ)在高岭石表面的吸附 总被引:7,自引:1,他引:6
在天然水体系中,铜、铅、镉等重金属元素的形态分布、迁移、归宿和生物有效性强烈取决于重金属元素在水体颗粒物表面的分配趋势.本文对铜(Ⅱ)在常见的重要粘土矿物--高岭石表面的吸附进行了实验和模式研究,结果表明,在同时考虑自由水合离子CU2+和羟基金属离子CuOH+与高岭石表面络合的情况下,单一表面基团、无静电表面络合模式能很好地描述铜(Ⅱ)的吸附行为.拟合得到的CuoH+的络合常数比Cu2+的大得多. 铜(Ⅱ)在高岭石表面的吸附量随pH值的升高而增加.吸附铜的两种表面化合态,>SOCu+和>SOCuOH的浓度在实验的pH范围内,也随pH值升高而增加,并且以>SOCu+为主. 相似文献
10.
阿拉尔河下游沉积物对铀的吸附及其影响因素 总被引:2,自引:0,他引:2
采用静态吸附实验,研究了阿拉尔河下游沉积物对水溶液中铀的吸附机制,分析了反应时间、pH值、粒径、固液比、铀初始浓度等因素对沉积物吸附铀的影响,并对其吸附动力学过程和热力学性质进行了探究。结果表明:阿拉尔河河流沉积物对铀的吸附在16 h左右趋于平衡;溶液pH值对沉积物吸附铀具有显著影响,当pH=6~7时,吸附率最大;在一定条件下,吸附率与固液比呈正相关,与粒径及铀初始浓度呈负相关;吸附量与固液比呈负相关,与铀初始浓度呈正相关;吸附动力学过程遵循准二级动力学模型,由两个以上步骤共同控制;吸附热力学符合Freundlich吸附等温模型,沉积物对铀的吸附以多分子层吸附为主,是自发、吸热的熵增过程。 相似文献
11.
Competitive adsorption,release and speciation of heavy metals in the Yellow River sediments,China 总被引:2,自引:0,他引:2
Qingyun Fan Jiang He Hongxi Xue Changwei LÜ Ying Liang Saruli Ying Sun Lili Shen 《Environmental Geology》2007,53(2):239-251
The competitive adsorption and the release of selected heavy metals and their speciation distribution before and after adsorption
in the Yellow River sediments are discussed. The adsorption of metals onto sediments increases with increasing pH value and
decreases with increasing ionic strength. The competitive coefficient K
c and the distribution coefficient K
d are obtained to analyze the competitive abilities of selected heavy metals, which are ranked as Pb > Cu >> Zn > Cd. The competition
among selected heavy metals becomes more impetuous with increasing ion concentration in water. Speciation analysis was done
by an improved analytical procedure involving five steps of sequential extraction. Cu, Pb and Zn were mainly transformed into
the carbonate-bound form (50.8–87.7%) in adsorption. Most of (60.7–77.3%) Cd was transformed into the exchangeable form, and
the percentage of carbonate-bound Cd was 19.7–30.4%. The release reaction was so quick that the release capacity of selected
heavy metals from sediments to aqueous solution reached half of the maximum value only in 30 s. As opposed to adsorption,
the release capacities of selected heavy metals were ranked as Cd > Zn >> Cu > Pb. In this study, Cd produces the most severe
environmental hazards, because its concentration in the release solution is 85.8 times more than the human health criteria
of US EPA. 相似文献
12.
The uptake and release of trace metals (Cu, Ni, Zn, Cd, and Co) in estuaries are studied using river and sea end-member waters
and suspended particulate matter (SPM) collected from the Changjiang Estuary, China. The kinetics of adsorption and desorption
were studied in terms of environmental factors (pH, SPM loading, and salinity) and metal concentrations. The uptake of the
metals studied onto SPM occurred mostly within 10 h and reached an asymptotic value within 40 h in the Changjiang Estuary.
As low pH river water flows into the high pH seawater and the water become more alkaline as it approaches to the seaside of
estuary, metals adsorb more on SPM in higher pH water, thus, particulate phase transport of metal become increasingly important
in the seaward side of the estuary. The percentage of adsorption recovery and the distribution coefficients for trace metals
remained to be relatively invariable and a significant reduction only occurred in very high concentrations of metals (>0.1 mg L−1). The general effect of salinity on metal behavior was to decrease the degree of adsorption of Cu, Zn, Cd, Co, and Ni onto
SPM but to increase their adsorption equilibrium pH. The adsorption–desorption kinetics of trace metals were further investigated
using Kurbatov adsorption model. The model appears to be most useful for the metals showing the conservative behavior during
mixing of river and seawater in the estuary. Our work demonstrates that dissolved concentration of trace metals in estuary
can be modeled based on the metal concentration in SPM, pH and salinity using a Kurbatov adsorption model assuming the natural
SPM as a simple surfaced molecule. 相似文献
13.
Simultaneous competitive adsorption behavior of Cd, Cu, Pb and Zn onto nine soils with a wide physical–chemical characteristics
from Eastern China was measured in batch experiments to assess the mobility and retention of these metals in soils. In the
competitive adsorption system, adsorption isotherms for these metals on the soils exhibited significant differences in shape
and in the amount adsorbed. As the applied concentration increased, Cu and Pb adsorption increased, while Cd and Zn adsorption
decreased. Competition among heavy metals is very strong in acid soils with lower capacity to adsorb metal cations. Distribution
coefficients (K
dmedium) for each metal and soil were calculated. The highest K
dmedium value was found for Pb and followed by Cu. However, low K
dmedium values were shown for Zn and Cd. On the basis of the K
dmedium values, the selectivity sequence of the metal adsorption is Pb > Cu > Zn > Cd and Pb > Cu > Cd > Zn. The adsorption sequence
of nine soils was deduced from the joint distribution coefficients (K
dΣmedium). This indicated that acid soils with low pH value had lower adsorption capacity for heavy metals, resulting in much higher
risk of heavy metal pollution. The sum of adsorbed heavy metals on the soils could well described using the Langmuir equation.
The maximum adsorption capacity (Q
m) of soils ranged from 32.57 to 90.09 mmol kg−1. Highly significant positive correlations were found between the K
dΣmedium and Q
m of the metals and pH value and cation exchange capacity (CEC) of soil, suggesting that soil pH and CEC were key factors controlling
the solubility and mobility of the metals in soils. 相似文献
14.
A study on the adsorption characteristics of cadmium and zinc onto acidic and alkaline soils 总被引:1,自引:1,他引:0
Myoung-Jin Kim 《Environmental Earth Sciences》2014,72(10):3981-3990
The adsorption of cadmium (Cd) and zinc (Zn) with similar chemical properties is examined onto three soil samples: one is alkaline and the others are acidic. The distribution coefficient (K d) and the Freundlich constant (K F) for Zn are slightly higher than those for Cd, implying that the adsorption affinity of Zn is a little greater and less mobile. However, Cd and Zn usually show comparable results in the kinetic, isotherm, and envelope experiments. The adsorption of the heavy metals is relatively rapid and the reaction is almost completed within 15 min. The kinetics for both Cd and Zn are very well explained by the parabolic diffusion model. The maximum adsorption of the heavy metals is obtained at high pH, high temperature, and low ionic strength. The adsorption capacity on the alkaline soil is more significantly affected by the temperature as compared to the acidic soil. It is found that the adsorption affinity of the two heavy metals is mainly affected by the soil properties, such as pH, pHPZC, organic matter, and total carbon. It is also confirmed that the chemical properties of the heavy metals are important factors in their adsorption onto soil. The adsorption isotherms of Cd and Zn are well described in both Freundlich and Langmuir models at the usual pH (soil pH). Under acidic and alkaline pHs, however, only the Freundlich model describes the adsorption of both heavy metals satisfactorily. 相似文献
15.
对中国南方的3个水稻土样品进行了Cd、Pb单一离子和混合离子吸附特点的研究。结果表明,3个水稻土样品中Cd、Pb的吸附特点都相似,Langmuir等温方程可很好地描述Cd、Pb的吸附等温线。3个土壤样品中,有较高pH值和较低有机物、CEC浓度、粘土含量、高岭石含量的2个土壤样品对Cd、Pb有较大的吸附量,且其等温吸附拟合的最大吸附量(B)也较大。在两组分混合溶液中,尽管共存离子的存在影响了土壤对单一离子的吸附,同时土壤对Cd的吸附在一定程度上受影响的程度大,但3个土壤样品都表现出对Pb有强的吸附能力。在3个土壤样品中,Langmuir等温方程中Pb的健合能常数(K)都大于Cd的健合能常数(K),混合溶液中的K值高于单一溶液的K值,表明2种金属离子对吸附位点的竞争提高了特定吸附位点的保持力,使金属离子在土壤中特定位点的吸附更加坚固。 相似文献
16.
水稻土中重金属元素Cd、Pb的竞争吸附
——以长株潭地区水稻土为例 总被引:3,自引:0,他引:3
对中国南方的3个水稻土样品进行了Cd、Pb单一离子和混合离子吸附特点的研究。结果表明,3个水稻土样品中Cd、Pb的吸附特点都相似,Langmuir等温方程可很好地描述Cd、Pb的吸附等温线。3个土壤样品中,有较高pH值和较低有机物、CEC浓度、粘土含量、高岭石含量的2个土壤样品对Cd、Pb有较大的吸附量,且其等温吸附拟合的最大吸附量(B)也较大。在两组分混合溶液中,尽管共存离子的存在影响了土壤对单一离子的吸附,同时土壤对Cd的吸附在一定程度上受影响的程度大,但3个土壤样品都表现出对Pb有强的吸附能力。在3个土壤样品中,Langmuir等温方程中Pb的健合能常数(K)都大于Cd的健合能常数(K),混合溶液中的K值高于单一溶液的K值,表明2种金属离子对吸附位点的竞争提高了特定吸附位点的保持力,使金属离子在土壤中特定位点的吸附更加坚固。 相似文献
17.
对中国南方的3个水稻土样品进行了Cd、Pb单一离子和混合离子吸附特点的研究。结果表明,3个水稻土样品中Cd、Pb的吸附特点都相似,Langmuir等温方程可很好地描述Cd、Pb的吸附等温线。3个土壤样品中,有较高pH值和较低有机物、CEC浓度、粘土含量、高岭石含量的2个土壤样品对Cd、Pb有较大的吸附量,且其等温吸附拟合的最大吸附量(B)也较大。在两组分混合溶液中,尽管共存离子的存在影响了土壤对单一离子的吸附,同时土壤对Cd的吸附在一定程度上受影响的程度大,但3个土壤样品都表现出对Pb有强的吸附能力。在3个土壤样品中,Langmuir等温方程中Pb的健合能常数(K)都大于Cd的健合能常数(K),混合溶液中的K值高于单一溶液的K值,表明2种金属离子对吸附位点的竞争提高了特定吸附位点的保持力,使金属离子在土壤中特定位点的吸附更加坚固。 相似文献
18.
Comparison of trace metal adsorption onto different solid materials and their chemical components in a natural aquatic environment 总被引:1,自引:0,他引:1
Solid materials such as suspended particulate matter (SPM), deposited sediment (DS) and natural surface coatings (NSC, composed of biofilms and associated minerals) are important sinks and potential sources of pollutants in natural aquatic environments. Although these materials can exist in the same water body, few studies have been conducted to compare their ability to adsorb trace metals. In this study, the adsorption of Pb, Cu and Cd by these solids, collected from an urban lake, was investigated. In addition, the metal adsorption properties of the main components of these solids, namely Mn and Fe oxides and organics, were also investigated using the method of selective extraction followed by metal adsorption. The solids that co-existed in water showed similarities and differences in their compositions. For each metal, adsorption to the solids occurred in the same order: NSC > SPM > DS. For Pb and Cd, Fe and Mn oxides and organics contributed to the adsorption by NSC and SPM, and the adsorption by DS was dominated by Fe oxides. For Cu, the organics were the main adsorptive phase. The specific adsorption capability of these components decreases in the following order: Mn oxides > Fe oxides > organics. Overall, the results presented herein indicate that different solids and their components played important roles in the adsorption of trace metals. 相似文献
19.
Experimental studies on the retention of metals (Cu, Co, Ni, and Zn) in bentonite samples from the Grau Region (Northern Peru)
have been accomplished using monometallic, bimetallic, trimetallic, and tetrametallic solutions. Parameters such as pH and
concentration of dissolved metals and organic compounds have been evaluated by means of batch adsorption experiments. Adsorption
rates indicate the suitability of these bentonites in the environmental industry for heavy metals retention purposes. In addition
to its quality as physical barrier to avoid the dispersion through the environment of polluted leachates, bentonite, due to
its high cation exchange capacity, can act also as a chemical barrier, protecting the quality of surface and groundwater systems,
while limiting the migration of heavy metals in solid residues or sludge stocked in security landfills. Adsorption rates of
tested bentonites were proved to decrease when concentrations of both metal and organic compounds, as well as the number of
ionic species, increase in solution; additionally, lower metal removal rates from solution were obtained when extremely acidic
conditions were achieved. 相似文献
20.
铬是一种重金属痕量元素,人体通过食物链摄入过量的铬会在人体内富集,随之产生中毒反应。研究Cr(III)的浓度、反应时间、反应温度、pH值等因素对Cr(III)在黄土上吸附特性的影响,结果表明黄土对Cr(III)的吸附非常迅速,并且吸附量非常大,等温吸附模型Freundlich和Dubinin-Radushkevich(D-R)模型都能很好地解释Cr(III)在黄土上的吸附过程。热动力学分析表明,吸附是一个自发的过程,升温可促进吸附作用的进行。随着温度的不断升高,Cr(III)的吸附量逐渐增大。溶液的pH值是影响Cr(III)吸附效果的一个重要因素,当pH>6时,Cr(III)几乎完全被去除。利用X光衍射图谱和红外光谱分析,探讨黄土与Cr(III)的结合机制,黄土中的高岭土、石英等黏土矿物以及有机质成分对吸附过程起重要作用。 相似文献