不同粒级黑土胶体对铅的等温吸附特征

采集了黑土样品并从中提取了3种粒级(5~10、2~5和1~2μm)的胶体,测试了胶体的比表面积、颗粒粒径分布和颗粒矿物质组成等特征参数。在不同温度(25、35、45和55℃)、不同pH(2、4和6)条件下,使用黑土胶体对铅离子作等温吸附实验,并用Langmuir、Freundlich和Dubinin-Redushkevich(D-R)吸附等温方程对实验数据进行了拟合。结果显示,黑土胶体对铅具有较强的吸附能力;不同温度下黑土胶体对铅的吸附等温式能很好地符合Freundlich模式(R2=0.94~0.98)和D-R模式(R2=0.91~0.98),随温度的升高,黑土胶体对铅离子的吸附能力增加;不同pH条件下,不同粒径黑土胶体对铅的吸附等温式较好地符合Freundlich模式,而当粒径小于5μm时,胶体对铅的吸附等温式能很好地符合Langmuir、Freundlich和D-R模式;随pH的升高,黑土胶体对铅离子的吸附能力增加;小粒径的胶体对铅具有更强的吸附能力;黑土胶体对铅的吸附属于化学吸附。     

硫酸活化市政污泥吸附Pb2+

以城市污水厂脱水剩余污泥为原材料,采用硫酸活化法制备活化剩余污泥,讨论了溶液初始pH、铅离子的浓度、接触时间和吸附剂投加量等因素对处理含铅废水效能影响,探讨了其吸附动力学特征.结果表明,活化剩余污泥对铅离子有较好吸附效果,10 min内吸附率达到75％,45 min内吸附基本达到平衡,在偏酸性或中性条件下,吸附容量随着初始pH增大而增大.采用4种动力学方程(准一级吸附动力学方程、准二级吸附动力学方程、颗粒扩散吸附动力学方程、Elov-ich动力学方程)对其吸附数据进行吸附动力学拟合,通过分析得出,准二级吸附动力学方程能较好地反映该吸附过程,其相关系数R2均达到0.999以上.     

改性松针对水体中铅(II)的吸附

探讨了改性松针(GXLsp)作为吸附剂对水体中铅离子的吸附性能,考察了吸附时间、溶液pH值、吸附剂用量、盐离子浓度、Pb(II)初始浓度及温度对改性松针吸附Pb(II)的影响。利用Langmuir和Freundlich等温线模型对实验数据进行非线性拟合分析,结果表明,Freundlich等温线模型能很好地描述松针对Pb(II)的吸附过程。热力学参数表明吸附是一个自发的吸热过程。改性松针对铅的吸附行为符合拟二级动力学方程,表明吸附过程是以化学吸附为主。在293K时松针对Pb(II)的饱和吸附量为318.3 mg/g,因此,GXLsp可作为一种高效低值生物质吸附剂以去除水体中重金属Pb(II)的污染。     

粉质粘土和粉质砂土对铬渣渗滤液中Cr(Ⅵ)吸附特性

针对铬渣堆场及其渗滤液生态环境污染严重这一热点问题，在对锦州铬渣堆场附近不同土壤取样测定基础上，采用振荡平衡法，测定吸附时间、污染物浓度、pH值、温度等条件改变对粉质粘土和粉质砂土吸附Cr（Ⅵ）的影响，研究2种土壤对Cr（Ⅵ）的吸附特性，获得土壤吸附的等温吸附曲线，建立吸附动力学方程。结果显示，吸附时间、污染物浓度、pH值、温度等都对土壤吸附Cr（Ⅵ）有不同程度的影响。粉质粘土和粉质砂土对Cr（Ⅵ）的吸附可用Langmuir方程、Freundlich方程和Temkin方程很好地描述，以Freundlich方程为最佳。粉质粘土和粉质砂土的Elovich型公式、双常数速率公式、抛物线扩散公式3种动力学方程的拟合程度顺序均为：Elovich型公式>双常数速率公式>抛物线扩散公式，粉质粘土相较粉质砂土动力学拟合程度更高且吸附性更好。     

钛(Ⅳ)和铝(Ⅲ)改性沸石去除水溶液中过量氟离子

制备了负载铝沸石(Al-Z)和负载钛沸石(Ti-Z)复合材料并测试了2种吸附材料对氟离子的吸附性能。未改性的人造沸石对氟离子几乎没有吸附作用,室温下2 g·L~(-1)的Al-Z和4 g·L~(-1)的Ti-Z的最大吸附量分别为32.94 mg·g~(-1)和15.03 mg·g~(-1)。在偏酸性和中性条件下有利于Al-Z对氟离子的吸附;Ti-Z对氟离子的吸附效果在酸性条件下较好;Zeta电位结果表明Al-Z对氟离子的吸附较Ti-Z有更广泛的pH适应能力;Al-Z和Ti-Z受CO2-3和PO3-4共存离子的影响对氟离子的去除率下降,且Ti-Z受影响程度更大,这是因为CO2-3和PO3-4的存在会改变溶液的pH值,使溶液呈碱性,从而影响吸附剂对氟离子的吸附效果;准二级动力学模型和Freundlich等温线方程符合描述这两种改性沸石对氟离子的吸附行为。与Ti-Z相比,Al-Z在吸附剂用量、氟离子吸附量、对pH与共存阴离子的适应性方面表现更好,是一种非常具有应用前景的氟离子吸附剂。     

热改性蛇纹石对Pb~(2+)的吸附平衡及动力学研究

采用等温吸附法比较了天然的蛇纹石和700℃热改性处理的热改性蛇纹石对含铅废水的吸附效果,并采用Langmuir、Freundlich方程及Lagrange假二级动力学方程、粒内扩散方程对实验数据进行了拟合,研究了pH对吸附效果的影响,并对2种蛇纹石做了X衍射。结果表明:Pb2+质量浓度大于50mg/L时,热改性蛇纹石吸附效果更好,吸附率在92%以上;天然蛇纹石对Pb2+的吸附符合Freundlich方程和Lagrange假二级动力学方程,以化学吸附为主,有多个控速步骤,热改性蛇纹石对Pb2+的最大吸附量为78.13mg/g;在pH6的条件下,天然蛇纹石对Pb2+的吸附效果更好。     

磷酸活化植物基活性炭对水溶液中铅的吸附

以棉秆与互花米草为原料,采用磷酸活化法制备了低成本的植物基活性炭,通过静态实验研究了其对重金属铅的吸附性能。结果表明,在活化温度为500℃、活化时间为2 h条件下,制备的棉秆和互花米草活性炭比表面积为1 570m2/g和856 m2/g,含氧酸官能团含量分别为1.43 mmol/g和1.27 mmol/g。在25℃下,两种活性炭对重金属铅的Langmuir最大吸附量分别为119 mg/g和111 mg/g,吸附最佳pH为4.3,吸附平衡符合Freundlich方程,离子交换在吸附过程中发挥了重要作用。     

聚甲亚胺酰胺树脂对水中Cu~(2+)的吸附

制备了聚甲亚胺酰胺树脂,对其进行傅里叶变换红外光谱分析。采用批处理方法实验了pH、铜离子初始浓度、吸附时间、吸附剂用量对吸附量的影响,研究了等温吸附模型和吸附动力学模型。优化后的吸附条件为:在铜离子溶液体积50 mL、初始浓度为300 mg/L、pH为6.0时,吸附剂投放量50 mg、吸附时间60 min,此时吸附量达到269.1 mg/g,去除率达89.7%。25℃时在研究浓度范围内,铜离子吸附过程用Langmuir等温线模型和Freundlich等温线模型描述均可;与准一级动力学方程、Elovich方程及内扩散方程相比,准二级动力学方程能更好地描述其吸附动力学过程。     

MnO_2@矿渣去除废水中的铊

以工业磁性矿渣构建具有二氧化锰包覆层(MnO_2@矿渣)的吸附剂,用于去除废水中的重金属铊元素。并探究吸附剂投加量、反应时间、反应pH、离子强度、有机物等影响因素及除铊机理。结果表明:在碱性条件下(pH=10),MnO_2@矿渣对水中的铊的吸附率达99.5%以上,10 min内达到吸附平衡;MnO_2@矿渣对铊的吸附容量随投加量的增大而增大,随离子强度的增大而减小,有机物对吸附铊的影响表现出差异性。吸附过程符合拟二级动力学模型,等温吸附适用Langmuuir和Freundlich方程描述;通过X-射线粉末衍射(XRD)、扫描电子显微镜(SEM)-X射线能谱(EDS)表征手段分析,证实成功制备了MnO_2@矿渣;傅里叶变换红外(FT-IR)和X射线光电子能谱(XPS)的结果表明MnO_2@矿渣对Tl(I)的去除是一个表面羟基络合、氧化和沉淀的过程。重复利用实验表明MnO_2@矿渣有很好的脱附与再生能力。     

硝酸改性对不同介孔结构生物质炭铅吸附的影响

在通过成功制备2种不同介孔结构的生物质炭AC-1与AC-2的基础上,研究了硝酸氧化改性对不同介孔结构生物质炭铅吸附特性的影响与等温吸附特性。低温氮吸附测试表明,生物质炭AC-1与AC-2的微孔孔容相近,而介孔孔容相差较大,分别为0.319和0.535 cm3·g-1。改性后AC-2-HNO3的介孔孔容与表面含氧酸官能团含量均高于AC-1-HNO3。吸附数据表明,硝酸改性可增强介孔生物质炭对水中铅的吸附去除能力,特别是改性前吸附量较低的AC-2,由于具有较大的介孔孔容和介孔尺寸,经硝酸改性后对铅的吸附性能与去除率均高于微孔孔容相近的生物质炭AC-1,这表明增大介孔孔容与介孔尺寸不仅有利于在介孔炭上接枝活性吸附位,并可缩短被吸附重金属铅离子到吸附活性点的路径,增大硝酸改性生物质炭活性位点对水中铅离子的捕捉机率,从而增大改性生物质炭对铅的吸附性能。Freundlich模型能很好地描述改性前后4种炭对铅的吸附行为,说明上述生物质炭的吸附位主要是非均匀孔隙或表面。     

Lead sorption in calcareous soils

The sorption of lead by three soils that differed in texture and calcium carbonate content was studied at three different temperatures. Lead sorption was found to conform to both Freundlich and Langmuir isotherms. Soil adsorption maxima were derived from the reciprocal of the slope obtained by a least-squares fit of Langmuir plots for each soil. The highest adsorption capacity was exhibited by CaCO(3)-rich soil (773.55 mmol Pb kg(-1)). Raising the temperature from 298 K to 308 and 318 K increased the sorption capacity of all of the soils.     

Adsorption of methabenzthiazuron on six allophanic and nonallophanic soils: effect of organic matter amendment

This article reports on methabenzthiazuron [1-(1,3-benzothiazol-2-yl)-1,3-dimethylurea] (MBT) adsorption process on six agricultural allophanic and nonallophanic soils. The effect of amendment with exogenous organic matter was also studied. Adsorption kinetic fits an hyperbolic model. MBT adsorption reached an apparent equilibrium within 2 h and followed a second-order reaction. The maximum adsorbed amounts for natural soils ranged from 32 to 145 microg g(-1). Rate constants were considered relatively low (0.27-1.5 x 10(-4) [microg g(-1)](1-n) s-1); the slow process was attributed to a combined effect of difussion and adsorption. MBT adsorption fits the Freundlich model with r values > or =0.998 at P < or = 0.001 significance levels. Kf and Freundlich exponents (l/n) ranged from 5.3 to 82.1 cm3 g(-1) and from 0.66 to 0.73, respectively. Kf values for soils with a low organic matter content were lower than that obtained from the only typical allophanic soil derived from volcanic ash under study. Lineal regression analysis between Kf and organic matter content of nonallophanic soils gave a correlation coefficient of 0.980 (P = 0.02). Dispersion of Kd values together with close values of K(OM) indicate that organic matter (OM) was the principal component responsible for MBT adsorption in unamended soils. Addition of peat decreased soil pH and increased adsorption capacity for allophanic and nonallophanic soils. Kinetic experiments showed enhancements of Xmax values and lower rate constants.     

Studies on the sorption and desorption characteristics of Zn(II) on the surface soils of nuclear power plant sites in India using a radiotracer technique

Zinc adsorption was studied in the soils of three nuclear power plant sites of India. 65Zn was used as a radiotracer to study the sorption characteristics of Zn(II). The sorption of zinc was determined at 25 and 45 degrees C at pH 7.8+/-0.2 in the solution of 0.01 M Ca(NO3)2 as supporting electrolyte. The sorption data was tested both in Freundlich and Langmuir isotherms and could be described satisfactorily. The effect of organic matter and other physico-chemical properties on the uptake of zinc was also studied in all the soil samples. The results showed that the cation exchange capacity, organic matter, pH and clay content were the main contributors to zinc sorption in these soils. The adsorption maximum was found to be higher in the soil on Kakarpara Atomic Power Plant sites soils having high organic matter and clay content. The zinc supply parameters of the soils are also discussed. In the desorption studies, the sequential extraction of the adsorbed zinc from soils showed that the diethylene triamine penta acetic acid extracted maximum amount of adsorbed zinc than CaCl2 and Mg(NO3)2. The zinc sorption on the soil and amount of zinc retention after extractants desorption shows a positively correlation with vermiculite and smectite mineral content present in the clay fraction of the soil. The amount desorbed by strong base (NaOH) and demineralised water was almost negligible from soils of all the sites, whereas the desorption by strong acid (HNO3) was 75-96% of the adsorbed zinc.     

Effect of organic acids on adsorption and desorption of rare earth elements

Effect of citric, malic, tartaric and acetic acids on adsorption of La, Ce, Pr and Nd by and desorption from four typical Chinese soils was studied. Generally, adsorption capacities of rare earth elements (REEs) were significantly correlated with the cation exchange capacity (CEC) of soils. In the presence of acetic acids adsorption of REEs was similar to that in the presence of Ca(NO3)2. However, in the presence of citric, malic and tartaric acids adsorption of REEs by Heilongjiang, Zhejiang and Guangdong soils decreased to varying extents if compared with that in the presence of nitrate and acetic acid. The significance of suppression followed the order of citric acid > malic acid > tartaric acid > acetic acid, which was consistent with the order of stability of complexes of REEs with these organic acids. However, the adsorption increased with increasing equilibrium solution pH. For Jiangxi soil with low soil pH, CEC and organic matter these organic acids exerted an even more serious suppression effect on the adsorption of REEs. Another feature of the relationship between the adsorption of REEs and equilibrium solution pH was that the adsorption of REEs decreased with increase of pH from 2 to 4.5 and then slightly increased with further increase of pH. Desorption of REEs varied with soils and with organic acids as well. REEs were released easily from Heilongjiang, Zhejiang and Guangdong soils in the presence of organic acid. Generally, desorption of REEs decreased with increasing equilibrium solution pH. Effect of organic acids on desorption of REEs from Jiangxi soil was more complicated. In the presence of citric and malic acids no decrement and/or slight increase in desorption of REEs were observed over the equilibrium solution pH from 3 to 6.5. The reasons for this were ascribed to the strong complexing capacity of citric and malic acids and low soil pH, CEC and organic matter of Jiangxi soil.     

Sorption of lead in soil as a function of pH: a study case in México

Reactions of lead sorption onto soil are largely affected by properties and composition of soil and its solution. In this study, the lead sorption onto regosol eutric soil from Francisco I. Madero, Zacatecas, Mexico is evaluated at different pH values. Soil samples were suspended in lead solutions of 10, 25, 50, 100, 150, 200, 300, and 400 mg/l (as Pb(NO3)2). The pH was adjusted at 2, 3, 4, and 5.5 with nitric acid for each of the lead solution concentrations. In all the cases the ionic strength was I=0.09 M with calcium nitrate. The solid-liquid-ratios were fixed in 1:100 and 1:200 g/ml. The results show that lead sorption increases when pH increases. Experimental isotherms were adjusted by both Langmuir and Freundlich models. The Langmuir affinity parameter, K, indicates that the lead sorption capacity of Francisco I. Madero soils is largely perceptible to pH changes.     

Adsorption characteristics of pesticides methamidophos and glyphosate by two soils

Contributions of organic matter and minerals in soil were evaluated by comparing changes in adsorption of methamidophos (MDP) and glyphosate (GPS) before and after removal of organic matter from argaltoll (mollisol) and typustalf (alfisol) soils. Adsorption isotherms of MDP and GPS by the two soils comforted to Freundlich equation, and the adsorption capacity of GPS by argaltoll soil was higher than that of MDP. Due to the removal of organic matter from soils, K(f) values of MDP and GPS adsorbed by argaltoll soil, which were calculated from Freundlich equations and the measure of adsorption capacity, decreased by 46.1% and 75.0%, and these by typustalf soil decreased by 34.9% and 52.5%, respectively. Results from this study suggested that soil organic matter made greater contributions to adsorption of GPS, but soil minerals could provide more available adsorption sites for MDP.     

Sorptive behavior of the phenylamide fungicides,mefenoxam and metalaxyl,and their acid metabolite in typical Cameroonian and German soils

Laboratory soil sorption experiments were conducted on mefenoxam, formulated metalaxyl (F-metalaxyl), pure metalaxyl (P-metalaxyl) and metalaxyl acid metabolite to elucidate differences in their sorptive behaviour on typical Cameroonian forest soil (sand clay loam, pH 4.8 and 3.01% OC) and German soil (sandy loam, pH 7.2, 1.69% OC) using a batch equilibrium method. The data obtained on all test chemicals conformed to linear and Freundlich adsorption isotherms. The Langmuir equation failed to describe the sorption of the substances tested. All substances were adsorbed to a greater extent by the Cameroonian soil. The average percentage adsorptions for mefenoxam, F-metalaxyl, P-metalaxyl and the acid metabolite on the Cameroonian soil were 27.8%, 28.3%, 31.8% and 46.8% respectively while for the German soil they were 21.7%, 21.5%, 24.7% and 9.8% respectively. The KD and KF parameters and the Freundlich exponential term (1/n) were low, indicating that the interactions between soil particles and the fungicides were weak. The sorption parameters were lower in the German soil. P-metalaxyl exhibited a higher adsorption capacity than F-metalaxyl in both soils. Mefenoxam and F-metalaxyl exhibited similar sorption parameters in soils, whereas those of P-metalaxyl and acid metabolite differed. Differences observed in the adsorption between the two soils could be attributed to their properties. Desorption studies revealed that the adsorbed fungicides were not firmly retained by soil particles and their adsorption was reversible. Desorption of adsorbed mefenoxam, P-metalaxyl and of the acid metabolite from German soil was almost completely reversible with percentage desorption rates of more than 91.0%, whereas the rate for F-metalaxyl was 74.1%. All compounds exhibited some resistance to desorption from the Cameroonian soil, with percentage desorption rates less than 77.0%. Therefore if degradation in the soil is slow the fungicides described have a potential to leach to lower soil horizons.     

土壤颗粒级配对镉吸附-解吸规律的影响

利用甘肃金川某地土壤通过批实验进行等温吸附和动力学解吸实验,研究不同颗粒级配的中砂对镉的吸附、解吸特征,并采用Freundlich和一级动力学方程对其吸附解吸方程进行拟合。结果表明,(1)Freundlich和一级动力学方程对该土壤吸附、解吸镉的实验适用;(2)等温吸附实验中4组不同颗粒级配的中砂对镉的吸附性很强,最大平衡吸附量依次为260.667、286.107、299.362和292.232 mg/kg,吸附性能与颗粒级配中的细粒土相对含量大小成正比;(3)4组土壤对镉的解吸在初期2 h内解吸速率均较快,在3 h左右达到吸附-解吸平衡。平衡后4组土样Ⅰ、Ⅱ、Ⅲ和Ⅳ的最大解吸量依次为0.752、0.561、0.44和0.54 mg/kg,解吸速率和平衡时最大解吸量均与颗粒级配中细颗粒相对含量密切相关。     

Differences in herbicide adsorption on soil using several soil ph modification techniques

Abstract

Effects of soil pH on weak acid and weak base herbicide adsorption by soil are often determined by modifying soil pH in the laboratory. Modification of soil pH with acidic or basic amendments such as HCl or NaOH can cause changes in the soil‐solution system that may affect pesticide adsorption. The partition coefficients (K_d) for atrazine and dicamba by Waukegan, Piano, and Walla Walla silt loam soils stabilized in the field at different pH levels were compared to the K_d obtained when the soil pH was adjusted with acidic or basic amendments before herbicide addition. NaOH addition to raise soil pH generally increased the soluble soil organic carbon (SSOC) concentration in solution compared to field soils at the same pH and to soil treated with Ca(OH)₂. NaOH decreased the soil solution ionic strength slightly. Acidifying soils increased the soil solution ionic strength, when compared to field soils at the same pH and had no effect on SSOC concentration. Dicamba adsorption to soil was minimal (K_d < 0.22) and not influenced by soil pH in the range of 4.1 to 6.0; adsorption by laboratory amended soils in some cases underestimated adsorption compared to nonamended soils. Atrazine adsorption increased with decreased pH in all soils, and was overestimated slightly by several laboratory treatments to reduce pH compared to adsorption by field soils. Treatments to raise the pH did not affect atrazine adsorption. Overall, herbicide adsorption differences due to pH modification were small (<30%), and were not affected by soil solution ionic strength, saturating cation, or SSOC concentration in solution.     

Sorption of 3,4-dichloroaniline on four contrasting Greek agricultural soils and the effect of liming

Sorption of 3,4-dichloroaniline (3,4-DCA) on four typical Greek agricultural soils, with distinct texture, organic matter content and cation exchange capacities, was compared by using sorption isotherms and the parameters calculated from the fitted Freundlich equations. The sorption process of 3,4-DCA to the soil was completed within 48-72 h. The 3,4-DCA sorption on all soils was well described by the Freundlich equation and all sorption isotherms were of the L-type. The sandy clay loam soil with the highest organic matter content and a slightly acidic pH was the most sorptive, whereas the two other soil types, a high organic matter and neutral pH clay and a low organic matter and acidic loam, had an intermediate sorption capacity. A typical calcareous soil with low organic matter had the lowest sorption capacity which was only slightly higher than that of river sand. The 3,4-DCA sorption correlated best to soil organic matter content and not to clay content or cation exchange capacity, indicating the primary role of organic matter. The distribution coefficient (K(d)) decreased with increasing initial 3,4-DCA concentration and the reduction was most pronounced with the highly sorptive sandy clay loam soil, suggesting that the available sorption sites of the soils are not unlimited. Liming of the two acidic soils (the sandy clay loam and the loam) raised their pH (from 6.2 and 5.3, respectively) to 7.8 and reduced their sorption capacity by about 50 %, indicating that soil pH may be the second in importance factor (after organic matter) determining 3,4-DCA sorption.