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1.
Equilibrium adsorption of isoproturon on soil and pure clays   总被引：1，自引：0，他引：1  
The adsorption of isoproturon on soil and pure clay minerals has been investigated as a means of understanding its mobility in soils. Measured adsorption coefficients are correlated with soil and clay mineral properties. Soil organic matter controlled the adsorption of isoproturon at organic carbon contents exceeding 27 g kg?1, whereas at less than this threshold, clay mineral surfaces appeared to control adsorption. The effect of varying temperature suggests that adsorption of isoproturon is a physical process. From the comparison of the fits of linear, Freundlich, and Langmuir adsorption isotherms to the data, the adsorption is best described as a partition process.  相似文献   

2.
Effluents containing phosphorous as phosphate ions are frequently discharged in freshwater resources contributing to the eutrophication and directly interfering in the biological equilibrium. Clam shell residues and sewage sludge were combined for preparing efficient adsorbents for phosphate removal from aqueous medium. The adsorbents were characterized before and after adsorption testing, and the adsorption equilibrium and kinetics were investigated. Phosphate removal of 89?±?1% was attained for samples prepared with 0.1?< X <?1.0, where X corresponds to sewage sludge/clam shell mass ratio. The analyses of the experimental errors indicated that the phosphorous removal followed the Elovich kinetic model, which describes adsorption in very heterogeneous surfaces. On the other hand, the best modelling was achieved using the Koble–Corrigan isotherm model, which incorporate different aspects of both Langmuir and Freundlich isotherms to represent the equilibrium data. The observed adsorption capacity (21.4 mgP g?1) are comparable or greater to that observed for other adsorbents described in the literature.  相似文献   

3.
Abstract

The extractant Mehlich‐1 is routinely used in Brazil for determination of soil nutrients, whereas Mehlich‐3 has been suggested as a promising extractor for soil fertility evaluation. Both were used for extraction of molybdenum (Mo) in Brazilian soils with Mo dosage by the KI+H2O2 method. The Langmuir and Freundlich isotherms were used to study soil Mo adsorption. Mehlich‐1 extracted more Mo than Mehlich‐3 in soils with high contents of organic matter, clay, and iron (Fe) oxides. Mehlich‐3 and Mehlich‐1 extractions correlated positively and significantly with amorphous Fe oxides, crystalline Fe oxides, and organic matter. Molybdenum recovering rates correlated to crystalline Fe oxides and clay contents but not to organic matter, pH, and Mo adsorption capacity. Amorphous and crystalline Fe oxides, clay, and organic matter were responsible for most of the Mo adsorption. The Langmuir isotherm described better the Mo adsorption to soil amorphous Fe oxides and organic matter than the Freundlich isotherm.  相似文献   

4.
The effects of different fertilization techniques—mineral [21% nitrogen (N)], organomineral (10% N), mycorrhiza inoculumns, wine-producing residues (three different formulas: distiller's residue, 2.2% N; anaerobic digestate, 2.8% N; and the same plus mycorrhizas inoculum), and compost by farm residues (2.0% N)—on adsorption of boron (B) were investigated. The soils, collected after a triennial lettuce (Lactuca sativa L. cv. ‘Bacio’) cultivation, were equilibrated using six B concentrations [0, 1, 5, 20, 50, and 100 mg B L?1, as boric acid (H3BO3)]. The B adsorption was studied at two soil mass (ms) to solution volume (vs) ratios, ms/vs = 0.5 and 1, and the Langmuir, Eadie–Hofstee, Freundlich, and Temkin adsorption equations were fitted to the B adsorption data. The proportion of adsorbed B was gradually less in the more concentrated solutions, with differences in ms/vs ratio and in treatments: the percentage of B adsorbed was greater for ms/vs = 0.5 and for distiller's residue and mineral fertilizer. The Freundlich isotherm represented the measured B adsorption data well; at ms/vs = 0.5, the values of Freundlich adsorption maxima Xm varied from 93.14 to 111.88 mg kg?1 (organomineral fertilizer and distiller's residue, respectively; at ms/vs = 0.5) and from 32.14 to 40.32 mg kg?1 (mineral fertilizer and control, respectively; at ms/vs = 1). In our study, generally the B adsorption was greater with mineral fertilizers and distiller's residue, whereas the organomineral fertilizer led to a decrease in B adsorption. The parameters of adsorption isotherms were significantly correlated, at various degrees, with the exchangeable cation sodium. The adsorption isotherms were well explained by the lower soil mass to volume solution ratio in the order Freundlich > Temkin ≌ Langmuir > Headie–Hofstee.  相似文献   

5.
Abstract

The use of the Langmuir isotherm equation to calculate phosphate (P) adsorption maximum was investigated by studying P adsorption by boehmite (a soil mineral) at pH 3.25, 4.00, and 5.50. This well‐defined simple system was designed to eliminate other influencing reactions and factors in an attempt to study only the adsorption process. The Langmuir adsorption maximum was compared to three other methods (Kd, “concentration null”, and graphical) for determining the value of this constant. There was generally good agreement between methods at the different pH's, except the “concentration null” at pH 3.25 and the Langmuir at pH 4.00. It appears that at least three of the methods (Langmuir included) can be used independently to develop the adsorption envelope, which peaked at pH 4.00. At maximum adsorption, approximately 20% of the surface was covered by P, suggesting monolayer adsorption at specific sites on the surface. Apparently the simple Langmuir isotherm equation, if used correctly, may give valid adsorption maximum values.  相似文献   

6.
Chang  T. W.  Wang  M. K.  Lin  C. 《Water, air, and soil pollution》2002,138(1-4):199-209
While sorbate/sorbent, sorbate/water, and sorbent/water (S/W)ratios in a batch system are known to affect the adsorption ofsorbate, the effect of different S/W ratios on the adsorptionof inorganic sorbates has seldom been addressed. This studyinvestigates the adsorption phenomena of Cu2+ in differentsorbate/sorbent/water ratios in a batch system. Batch experimentsare performed to examine the adsorption, and the linear (K D), Langmuir (K L), and Freundlich (K F) adsorption coefficients of Cu2+ in lateritic soil. These experiments are conducted using solutions with initial concentrations of 0.5 to 50 mg Cu2+ L-1 equilibratedwith an appropriate amount of soil to give S/W ratios of 0.1 to 2 g mL-1. Although the variations in the sorbed amountand adsorption coefficients apparently originate from a changein the sorbate/sorbent/water ratio, only the equilibrium concentration significantly affects adsorption. On the otherhand, the linear and Langmuir isotherm cannot adequately describethe adsorption data. In this study, the Freundlich equation gavean excellent fit to the adsorption data with a goodness-of-fit(R2) > 0.984. However, adsorption isotherms should be regarded as only a curve-fitting model or a mathematical tool and cannot be employed to interpret any particular adsorptionmechanism. Meanwhile, the solids effect reveals that K F andmaximum adsorption (b) of the Langmuir equation increase when S/W ratio decreases. The sorbate in the stagnant phase must beconsidered as part of the equilibrium concentration in the solidphase to avoid underestimating the sorbed amount at a lower S/Wratio and/or a higher sorbate concentration level.  相似文献   

7.
Abstract

Zinc adsorption by 10 (pH 4.0–6.5) cultivated mineral soils from Finland was studied in batch experiments. Additions of Zn ranged up to 600 mg kg?1 of soil and the corresponding equilibrium concentrations were 0.1–13 mg 1?1. In each soil, Zn adsorption conformed to the Freundlich isotherm. Despite a relatively low initial Zn adsorption by the acidic soils, each of the soils proved to have a high potential to adsorb Zn, but the capacity was highly pH dependent. In addition to the conventional Freundlich adsorption isotherms, calculated separately for each soil, extended Freundlich-type isotherms that also incorporate soil pH and other soil characteristics were used to describe Zn adsorption of several soils simultaneously in one equation. The pH-dependent Freundlich adsorption isotherm proved to serve as a practical tool to assess Zn adsorption by soils varying in pH and other characteristics.  相似文献   

8.
Knowledge of phosphorus(P) sorption dynamics across different soil types could direct agronomic and environmental management of P. The objective of this study was to predict P isotherm parameters for a national soil population using data of routine laboratory tests. Langmuir and Freundlich sorption parameters were calculated from two different ranges(0–25 and 0–50 mg P L~(-1)) using an archive of representative agricultural soil types from Ireland.Multiple linear regression(MLR) identified labile forms of aluminium(Al) and iron(Fe), organic matter(OM), cation exchange capacity(CEC), and clay as significant drivers. Langmuir and Freundlich sorption capacities, Freundlich affinity constant, and Langmuir buffer capacity were predicted reliably, with R~2 of independent validation 0.9. Sorption isotherm parameters were predicted from P sorbed at a single concentration of 50 mg P L~(-1)(S_(50)). An MLR prediction of P sorption maximum in the 0–50 mg P L~(-1) range was achieved, to an accurate standard, using S_(50), OM, and Mehlich-3 Fe(R~2 of independent calibration and validation being 0.91 and 0.95, respectively). Using Giles' four shapes of isotherms(C, L, H, and S), L non-strict-and C-shaped isotherm curves accounted for 64% and 27% of the soils, respectively. Hierarchical clustering identified a separation of isotherm curves influenced by two ranges of Mehlich-3 Al. Soils with a low range of Mehlich-3 Al(2.5–698 mg kg~(-1)) had no incidence of rapid sorption(C shape). Single point indices, Al, or available soil data make the regression approach a feasible way of predicting Langmuir parameters that could be included with standard agronomic soil P testing.  相似文献   

9.
土壤和氧化铁对氟化物的吸附和解吸   总被引：5，自引：0，他引：5  
邵宗臣  陈家坊 《土壤学报》1986,23(3):236-242
本文研究了两种土壤(砖红壤和黄棕壤)和两种合成氧化铁(无定形氧化铁和针铁矿)对氟化钠溶液的吸附和解吸现象,讨论了氟离子吸附的吸附等温线特征.根据实验资料和吸附等温线的拟合情况,我们认为,砖红壤和无定形氧化铁用Langmuir公式来描述,黄棕壤和针铁矿用Freundlich公式来描述更为适宜.氟离子的解吸量均低于吸附量.研究结果表明,由于水洗和醇洗,一部分以静电引力所吸附的氟离子被洗去,造成氟离子解吸量偏低.  相似文献   

10.
Abstract

Clinoptilolite, a zeolite mineral with a high cation exchange capacity and surface area, has ion‐exchange properties that can be utilized to adsorb NH4 +, protecting it from losses during composting of N‐rich animal manures. Ammonium adsorption by the natural zeolite clinoptilolite was studied to ascertain the effectiveness of the zeolite as an NH4 + adsorbent at pH 4, 5, 6, and 7. The NH4 + adsorption data were fitted to the one‐ and two‐surface Langmuir, Freundlich, and Temkin isotherms. All models described the NH4 +adsorption data successfully (r2≥0.939). The one‐surface Langmuir, Freundlich, and Temkin were converted to pH‐dependent forms. The amount of NH4 + adsorbed increased as pH and initial NH4 +concentration increased. From the one‐surface Langmuir isotherm, the NH4 +adsorption capacity (Xm) of the zeolite increased linearly with pH (r2=0.994), and was estimated to be 9,660 mg N kg‐1 at pH4, 11,220 mg N kg‐1 at pH 5, 12,720 mg N kg‐1 at pH 6, and 13,830 mg N kg‐1 at pH 7. The adsorption of higher amounts of NH4 +with increasing pH and initial NH4 +concentration is an important characteristic of the zeolite that can be beneficial to minimizing N‐losses via NH3volatilization during composting of N‐rich animal manures.  相似文献   

11.
Langmuir adsorption isotherms are unlikely to be appropriate when applied to the adsorption of charged phosphate ions on charged oxide surfaces. It is more likely that the adsorption model proposed by Bowden et al. (1973, 1974 and 1977) for adsorption on variable charge variable potential surfaces will be applicable. Theoretical isotherms were calculated from this model for a series of pH values and ionic strengths. It is shown that these isotherms can be split into two or more Langmuir isotherms in much the same way as has been done by various authors for experimental isotherms. The parameters of the Langmuir isotherms behave in the same way as those derived from the experimental isotherms. The charging characteristics of the theoretical isotherms are also similar to that observed experimentally. Because the model which is based on a single type of adsorption site is closely similar to the experimental isotherms, it is erroneous to split the isotherms into a series of Langmuir isotherms unless there are good a priori reasons.  相似文献   

12.
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13.
The kinetics and mechanism of methylene blue adsorption onto raw pine cone biomass (Pinus radiata) was investigated under various physicochemical parameters. The extent of the methylene blue dye adsorption increased with increases in initial dye concentration, contact time and solution pH but decreases with the amount of adsorbent, salt concentration and temperature of the system. Overall the kinetic studies showed that the methylene blue adsorption process followed pseudo-second-order kinetics among various kinetic models tested. The different kinetic parameters including rate constant, half-adsorption time and diffusion coefficient are determined at different physicochemical conditions. Equilibrium data were best represented by Langmuir isotherm among Langmuir and Freundlich adsorption isotherm. The maximum monolayer adsorption capacity of pine cone biomass was 109.89 mg/g at 30°C. The value of separation factor, R L, from Langmuir equation and Freundlich constant, n, both give an indication of favourable adsorption. Thermodynamic parameters such as standard Gibbs free energy (?G 0), standard enthalpy (?H 0), standard entropy (?S 0) and the activation energy (A) were calculated. A single-stage batch absorber design for the methylene blue adsorption onto pine cone biomass has been presented based on the Langmuir isotherm model equation.  相似文献   

14.
Solutions containing different P concentrations were equilibrated with samples of an allophanic soil from Navarra (Spain) to determine whether P sorption conformed qualitatively and quantitatively to the Langmuir, Freundlich and Sokolowska isotherms.Phosphorus sorption conformed to the Langmuir isotherm. When the sorption d data were plotted according to the conventional and Hofstee forms, two linear relationships were obtained. At the lower equilibrium P concentrations the K1 parameter determined by regression analysis was higher than those corresponding to higher equilibrium P concentrations. The values obtained for K1 and K2 by the conventional and Hofstee equations were different. A procedure for evaluating the coefficients for higher equilibrium P concentrations was proposed. The K1 and K2 values so obtained allowed us to generate an experimental curve by addition of calculated adsorption data. This suggests that the curve-splitting technique is satisfactory.The sorption data also conformed to the Freundlich and Sokolowska equations, but in the latter it was necessary to evaluate two different sets of parameters.The same experimental data can be adjusted to the three different equations, in one case with only one set of constants and in the other two cases with two different sets of parameters, one for the lower P concentrations and the other for the higher ones. Besides, to fit the experimental data to the Langmuir and Sokolowska equations, it was necessary to split the isotherm into two regions and these two regions were different for the Langmuir and the Sokolowska equations. This suggests that the parameters do not have any chemical signification and that they are only “curve fitting”.A study of the effect of pH on the P sorption indicated that low pH notably increased the P sorption.The soil samples had very high phosphate sorption capacity probably due to the very large specific surface and reactivity of the allophane.  相似文献   

15.
评价5种最常用的数学模型对中国不同类型的稻谷(籼稻、粳稻、糯稻)吸附与解吸等温线数据的拟合效果，以确定最佳拟合模型及其参数。测定中国不同类型稻谷的吸附与解吸等温线数据，用非线性回归进行统计分析并评价数学模型的拟合效果。结果表明，美国农业工程学会(ASAE)推荐的修正Chung-Pfost模型及其参数并不能与中国稻谷的吸附与解吸等温线数据很好地拟合。Strohman-Yoerger模型最适于拟合籼稻、粳稻的吸附与解吸等温线及糯稻的吸附等温线。而修正Oswin模型最适合拟合糯稻的解吸等温线。Strohman-Yoerger模型拟合籼稻、粳稻吸附等温线的参数C1、C2、C3、C4分别为1.44871、0.20898、7.32345、0.18647；拟合解吸等温线的参数C1、C2、C3、C4分别为2.25071、0.24167、8.32543、0.19035；拟合珍糯吸附等温线的参数为1.55680，0.19179，6.19676，0.17155。修正Oswin模型拟合珍糯的解吸等温线的参数为13.63642，-0.05638，3.60042。本研究为中国的稻谷贮藏与加工提供了基础性数据。  相似文献   

16.
Extensive use of chemical fertilizers in agriculture can induce high concentration of ammonium nitrogen(NH4+-N) in soil. Desorption and leaching of NH4+-N has led to pollution of natural waters. The adsorption of NH4+-N in soil plays an important role in the fate of the NH4+-N. Understanding the adsorption characteristics of NH4+-N is necessary to ascertain and predict its fate in the soil-water environment, and pedotransfer functions(PTFs) could be a convenient method for quantification of the adsorption parameters. Ammonium nitrogen adsorption capacity, isotherms, and their influencing factors were investigated for various soils in an irrigation district of the North China Plain. Fourteen agricultural soils with three types of texture(silt, silty loam, and sandy loam) were collected from topsoil to perform batch experiments. Silt and silty loam soils had higher NH4+-N adsorption capacity than sandy loam soils.Clay and silt contents significantly affected the adsorption capacity of NH4+-N in the different soils. The adsorption isotherms of NH4+-N in the 14 soils fit well using the Freundlich, Langmuir, and Temkin models. The models’ adsorption parameters were significantly related to soil properties including clay,silt, and organic carbon contents and Fe2+ and Fe3+ ion concentrations in the groundwater. The PTFs that relate soil and groundwater properties to soil NH4+-N adsorption isotherms were derived using multiple regressions where the coefficients were predicted using the Bayesian method. The PTFs of the three adsorption isotherm models were successfully verified and could be useful tools to help predict NH4+-N adsorption at a regional scale in irrigation districts.  相似文献   

17.
Poly(acrylamide-acrylic acid-dimethylaminoethyl methacrylate) P(AAm-AA-DMAEMA) resin was prepared by the template copolymerization. PAAm was used as a template for the copolymerization of DMAEMA and AA in aqueous solution using gamma rays. The adsorption of indigo carmine and eriochrome black-T anionic dyes from aqueous media on P(AAm-AA-DMAEMA) has been investigated. The adsorption behavior of this resin has been studied under different adsorption conditions: dye concentrations (50?C500 mg l?1), contact times, temperature (30?C55°C), and pH values (2?C7). The amount of dye adsorbed increased with increasing resin content, but it had a little change with temperature and decreased slightly with increasing pH. Adsorption data of the samples were modeled by the pseudo-first-order and pseudo-second-order kinetic equations in order to investigate dye adsorption mechanism. It was found that the adsorption kinetics of the resin followed a pseudo-second-order model with rate constant (k 2) of 2.5?×?10?3 and 1.8?×?10?2 g (mg?1 min?1) for indigo carmine and eriochrome black-T, respectively. Equilibrium isotherms were analyzed using the Langmuir and Freundlich isotherms. It was seen that the Freundlich model fits the adsorption data better than the Langmuir model.  相似文献   

18.
Laboratory and greenhouse experiments were conducted to determine the influence of soil properties on adsorption and desorption of boron (B) as well as to estimate the degree of reversibility of adsorption reactions. The utility of Freundlich and Langmuir equations for characterizing the plant availability of applied B in soils was established using soybean [Glycine max (L.) Merr.] as a test crop. The adsorption-desorption study revealed that Fe2O3 and clay were primarily responsible for retaining added B in all the 25 different soils under investigation. Organic carbon, pH and cation exchange capacity (CEC) positively influenced the adsorption of B while free Fe2O3, organic carbon and clay retarded release of B from these soils. The degree of irreversibility (hysteresis) of B adsorption/desorption increased with increase in organic carbon and CEC of these soils. Freundlich isotherm proved more effective in describing B adsorption in soils as compared to Langmuir equation. The split Langmuir isotherm demonstrated that any of the adsorption maxima, calculated from lower, upper or entire isotherm, could be of practical use. Contrary, bonding energy coefficient, calculated either at lower or higher equilibrium concentration failed to show any practical benefit. Regression models as a function of B application rate and adsorption equation parameters to predict B uptake from applied B, demonstrated the utility of Langmuir and Freundlich equation parameters.  相似文献   

19.
At low solution concentrations of copper in the presence of 0.05 M CaCl2, adsorption isotherms for copper on soil samples were essentially linear. Although no direct correlations were found between isotherm gradients and individual soil properties, the gradients were of the same order of magnitude as predictions based on gradients obtained for some specific soil components. The soil components which appear to be most important in copper adsorption and which were used to obtain the predictions were organic matter and iron and manganese oxides. The amounts of adsorbed copper remaining isotopically exchangeable or extractable with EDTA in the short term increased with the amount of copper adsorbed but the proportions of adsorbed copper estimated by each of these techniques remained constant. Concentrations of copper in solution increased (adsorption decreased) at pH values below 4.5 and above 6.5.  相似文献   

20.
On the relation of herbicide adsorption and soil organic fraction Freundlich adsorption isotherms were measured for four herbicides (atrazine, terbuthylazine, chlorotoluron, isoproturon) and 24 soil horizons, which are typical of Schleswig-Holstein, northern Germany. The relationship between the adsorption constant (KFr) of a chemical and the fraction of organic carbon (fOC) of the soil horizons was evaluated. Chemical specific K'OC-values, that are independent of soil organic carbon fraction varied considerably for each herbicide (CV about 50%); therefore these values as well as KOC-values, that are determined by linear regression of KFr and fOC should be evaluated critically before application. K'OC- and KOC-values derived from experiments showed decreasing affinity of the herbicides to soil horizons in the order terbuthylazine > chlorotoluron > atrazine ? isoproturon. Calculation of KOC from KOW or water solubility of each herbicide, however, led to changes in the above mentioned ranking. Hence, especially KOW or water solubility based KOC-values may lead to false conclusions concerning chemical mobility. For atrazine, terbuthylazine and isoproturon Freundlich adsorption constants increased overproportionally with increasing organic carbon content of soils. The relationships between KFr and fOC therefore were described better by a non-linear equation (second order polynom) than by a linear approach. Contrary, for chlorotoluron a linear relation between KFr and fOC holds at least for the range of fOC investigated in this study.  相似文献   

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