Effect of multiple factors on the adsorption of Cd in an alluvial soil from Xiba, China

https://doi.org/10.1016/j.jconhyd.2020.103605Get rights and content

Highlights

  • The effects of organic matter, Fe/Mn oxides on Cd adsorption.

  • The effects of pH, ionic strength, background electrolyte on Cd adsorption.

  • Adsorption thermodynamics and kinetics of Cd.

Abstract

The effects of organic matter, free Fe oxides and Mn oxides in an alluvial soil on adsorption of Cd were studied through selective chemical extraction and adsorption experiments. Compared to untreated soil, after H2O2 treatment for removal of organic matter and NH2OH·HCl treatment for removal Mn oxides, the distribution coefficient (Kd) decreased by a maximum of 25.2% and 64.1%, respectively. After dithionite-citrate-bicarbonate treatment for removal of free Fe oxides, Kd increased by 1670.2%. After increasing the solution pH from 2 to 3, Kd increased by 2842.1%, whereas after increasing the solution pH from 3 to 7, the adsorption tended stabilize. As the ionic strength increased from 0.001 M to 0.1 M NaNO3, Kd gradually decreased, whereas at the same ionic strength, Kd decreased as the initial concentration of Cd increased. The effects of different background electrolytes on Cd adsorption was as follows: Ca2+ > Mg2+ > K+ > Na+ for cations and Cl ≈ SO42− > NO3 for anions. The adsorption capacity of Cd increased as the increased of temperature, and it's a spontaneous endothermic process. The pseudo second-order rate model described the process of Cd adsorption well.

Introduction

Cd is the seventh most toxic heavy metal as per ranking among environmental pollutants by the Agency for Toxic Substance and Disease Registry (ATDSR, 2017). The world health organization (WHO, 2000) reported that the average background concentration of Cd was 0.1–0.4 mg kg−1 in soil. in recent years, with the development of industry and intensive agriculture, a large amount of Cd has entered into the soil environment, causing the content of Cd in the soil in some areas to exceed the recommended level. Cd is more bioavailable and mobile than other metals (Li et al., 2015). It can easily enter the human food chain, causing a range of acute and chronic disease symptoms, as well as cause serious damage to the kidneys, lungs, and liver (Bedoui et al., 2008).

Soil is a complex heterogeneous system. As soil components, iron oxides, manganese oxides, and organic matter are important adsorption carriers, which play an important role in the transfer, transformation, and other environmental geochemical behaviors of Cd in soil (Dong et al., 2000; Li et al., 2015). A variety of methods are used to study the effects of soil components on Cd adsorption. For example, firstly, we can study the adsorption capacity of synthetic or semi-synthetic pure substances to Cd and then perform an extrapolation (Covelo et al., 2007; Tan et al., 2018). Secondly, we can analyze the correlation between mineral composition and content/distribution of Cd in soil (Lee, 2006; Holm et al., 2003). Thirdly, we can compare the adsorption capacity of Cd after separation of specific component by selective chemical extraction (Li et al., 2015; Zhao et al., 2014). However, overall analysis by selective chemical extraction technology is an effective method for accurately evaluating the adsorption effect of specific components on heavy metals in soil and their adsorption mechanism (Sarkar et al., 2014).

It is well known that the conditions of solution chemistry (e.g., pH, ionic strength, background electrolyte type etc) can also significantly affect the Cd adsorption in soil (Chen et al., 2011; Loganathan et al., 2012). The pH mainly affects Cd adsorption by changing the speciation of Cd, such as Cd(OH)3, Cd(OH)20, CdOH+, and Cd2+ (Hu et al., 2014), and the surface charge of the adsorbent (Hu et al., 2011). The ionic strength and background electrolyte mainly affect the adsorption of Cd by affecting the structure of the double electrode layer of the adsorbent (Wang et al., 2013; Malamis and Katsou, 2013), competing with Cd for adsorption sites or forming soluble complexes with Cd (Wang et al., 2013; Dai et al., 2013). However, the effects of the three types of solution chemistry conditions on Cd adsorption show different characteristics due to the differences in the physicochemical features of the studied soil.

The adsorption equilibrium is influenced not only by soil components and solution chemistry conditions but also by the kinetic and the thermodynamics processes. The adsorption of Cd, as with other heavy metals, is recognized as a two-step process (Axe et al., 2006). That is, adsorption is divided into the initial rapid adsorption stage, followed by the slow adsorption stage. The temperature affects the adsorption process mainly through the following mechanism. As the temperature increases, the viscosity of the solution decreases (Nouri et al., 2007) and the kinetic energy of the ions in the solution increases, increasing the diffusion rate of the metal ions (Malamis and Katsou, 2013; Wang et al., 2019). The increase in the temperature promotes the hydrolysis of metal ions, reducing the electrostatic repulsion between the sorbate and the surface of the adsorbent (Fan et al., 2009). Moreover, an elevated temperature results in an increase in the number of the active adsorption sites on the solid (Goyal et al., 2003; Puranik and Paknikar, 1999). However, it has also been reported that an increase in the temperature enhances the tendency of Cd to escape from the solid surface, thus reducing the ability of the adsorbent to remove Cd (Öztürk et al., 2014; Sharma et al., 2007).The thermodynamic parameters (i.e.,△G0,△H0 and△S0) will also change with temperature (Chen and Wang, 2006).

Riverine alluvial plains are usually densely populated, with relatively well developed agriculture, due to the flatness of the terrain and good quality of the soil; however, this also leads to heavy metal pollution of the latter. To date, the reports in the literature regarding the effect of multiple factors on Cd adsorption in alluvial acidic soils have been inadequate. In this study, selective chemical extraction technology and adsorption experiments were applied to investigate: (1) the quantitative analysis of the effects of organic matter, free Fe oxides, and Mn oxides in an alluvial soil on Cd adsorption; (2) the effects of solution chemistry conditions (pH, ionic strength, background electrolyte) on Cd adsorption; and (3) the thermodynamics and kinetic characteristics of Cd adsorption. The research results should provide a theoretical basis and data support for soil Cd pollution prevention, treatment, and remediation.

Section snippets

Soil characterization

Topsoils (0–20 cm) used in this study were sampled from an alluvial soil from the Muxi River, near Hongyue coal mine, located in Xiba town, southwest China. Soil samples were naturally dried, crushed, and passed through a 2 mm nylon sieve after removing plant residues, stones and other large particles. Soil pH was determined by pH meter in a 1:2.5 (soil/solution). Soil organic matter was analyzed by the K2Cr2O7 oxidation method (Nelson and Sommers, 1982). The free Fe oxides and amorphous Fe

XRD and FTIR analyses

Fig. 1 is the XRD pattern of the alluvial Soil. The main mineral are quartz, muscovite and feldspar. The characteristic peaks of clay minerals aren't obvious, probably because the clay minerals are poorly crystallized, resulting in low and broad diffraction peaks. It is also that clay minerals possible be coated by other soil components, causing the diffraction peaks of clay minerals disappear (Xiong, 1985). FT-IR spectra of the studied soil samples before the adsorption experiments is

Conclusions

In this study, selective chemical extraction and adsorption experiments results revealed that organic matter and Mn oxides (specially the latter) can enhance the adsorption of Cd, but free Fe oxides may hinder the adsorption of Cd in soil. The adsorption capacity rapidly increases in the pH range of 2–3 and does not change significantly in the pH range of 3–7. The adsorption capacity of Cd decreases gradually as ionic strength increases. The effect of the background electrolyte divalent cations

Acknowledgment

Thanks to Hongtao Li, for his help in the lab experiment, Financial supports from key research and development project of Sichuan Province (No. 18ZDYF3447).

References (60)

  • J.O. Agbenin et al.

    Competitive adsorption of copper and zinc by a Bt horizon of a savanna Alfisol as affected by pH and selective removal of hydrous oxides and organic matter

    Geoderma

    (2004)
  • Agency for Toxic Substance and Disease Registry USA

    Toxicological Profle for Cadmium

    (2017)
  • B. Anna et al.

    Adsorption of Cd(II), Cu(II), Ni(II) and Pb(II) onto natural bentonite: study in mono- and multi-metal systems

    Environ. Earth Sci.

    (2015)
  • L. Axe et al.

    Long-term fate of metal contaminants in soils and sediments

  • K. Bedoui et al.

    Removal of cadmium(II) from aqueous solution using pure smectite and Lewatite S 100, the effect of time and metal concentration

    Desalination

    (2008)
  • H.B. Bradl

    Adsorption of heavy metal ions on soils and soils constituents

    J. Colloid Interface Sci.

    (2004)
  • C.L. Chen et al.

    Adsorption of Ni(II) from aqueous solution using oxidized multiwall carbon nanotubes

    Ind. Eng.Chem. Res.

    (2006)
  • Y.G. Chen et al.

    Effect of contact time, pH, and ionic strength on Cd(II) adsorption from aqueous solution onto bentonite from Gaomiaozi, China

    Environ. Earth Sci.

    (2011)
  • E.F. Covelo et al.

    Competitive sorption and desorption of heavy metals by individual soil components

    J. Hazard. Mater.

    (2007)
  • L. Dai et al.

    Fabrication of titanate nanotubes/iron oxide magnetic composite for the high efficient capture of radionuclides: a case investigation of 109Cd(II)

    J. Radioanal. Nucl. Chem.

    (2013)
  • D.M. Dong et al.

    Adsorption of Pb and Cd onto metal oxides and organic material in natural surface coatings as determined by selective extractions: new evidence for the importance of Mn and Fe oxides

    Water Res.

    (2000)
  • Y.H. Dong et al.

    Effect of pH, ionic strength, foreign ions, fulvic acidand temperature on 109Cd(II) sorption to γ-Al2O3

    J. Radioanal. Nucl. Chem.

    (2012)
  • Q.H. Fan et al.

    Comparison of Ni2+ sorption to bare and ACT-graft attapulgites: effect of pH, temperature and foreign ions

    Surf. Sci.

    (2008)
  • Q.H. Fan et al.

    Sorption of Eu(III) on attapulgite studied by batch, XPS, and EXAFS techniques

    Environ. Sci. Technol.

    (2009)
  • N. Fiol et al.

    Determination of sorbent point zero charge: usefulness in sorption studies

    Environ. Chem. Lett.

    (2009)
  • GBT 50123-1999

    Standard for Soil Test Method. National Standard Promulgated by the Ministry of Housing and Urban-Rural Development, PRC

    (1999)
  • N. Goyal et al.

    Comparative studies on the microbial adsorption of heavy metals

    Adv. Environ. Res.

    (2003)
  • G.L. Guo et al.

    Partition and characterization of cadmium on different particle-size aggregates in Chinese Phaeozem

    Geoderma

    (2013)
  • S.S. Gupta et al.

    Immobilization of Pb(II), Cd(II) and Ni(II) ions on kaolinite and montmorillonite surfaces from aqueous medium

    J. Environ. Manag.

    (2008)
  • Y.S. Ho et al.

    The kinetics of sorption of divalent metal ions onto sphagnum moss peat

    Water Res.

    (2000)
  • P.E. Holm et al.

    Correlation of cadmium distribution coefficients to soil characteristics

    J. Environ. Qual.

    (2003)
  • X.J. Hu et al.

    Adsorption of chromium (VI) by ethylenediamine-modified cross-linked magnetic chitosan resin: isotherms, kinetics and thermodynamics

    J. Hazard. Mater.

    (2011)
  • X.J. Hu et al.

    Effects of background electrolytes and ionic strength on enrichment of Cd(II) ions with magnetic graphene oxide–supported sulfanilic acid

    J. Colloid Interface Sci.

    (2014)
  • M.Q. Jiang et al.

    Adsorption of Pb(II), Cd(II), Ni(II) and Cu(II) onto natural kaolinite clay

    Desalination

    (2010)
  • H. Jiang et al.

    Effects of pH and low molecular weight organic acids on competitive adsorption and desorption of cadmium and lead in paddy soils

    Environ. Monit. Assess.

    (2012)
  • W.T. Jiao et al.

    Effects of organic matter on cadmium adsorption–desorption in three soils

    Environ. Chem.

    (2005)
  • M.J. Kim

    A study on the adsorption characteristics of cadmium and zinc onto acidic and alkaline soils

    Environ. Earth Sci.

    (2014)
  • S. Lee

    Geochemistry and partitioning of trace metals in paddy soils affected by metal mine tailings in Korea

    Geoderma

    (2006)
  • Z.w. Li et al.

    Influence of removal of organic matter and iron and manganese oxides on cadmium adsorption by red paddy soil aggregates

    RSC Adv.

    (2015)
  • P. Loganathan et al.

    Cadmium sorption and desorption in soils: a review

    Crit. Rev. Environ. Sci. Technol.

    (2012)
  • Cited by (13)

    • The co-transport of Cd(Ⅱ) with nanoscale As<inf>2</inf>S<inf>3</inf> in soil-packed column: Effects of ionic strength

      2022, Chemosphere
      Citation Excerpt :

      The reaction of Cd(Ⅱ) with sites on the soil surface is shown below in terms of organic matter (8–11) and clay minerals(12-14) (Fang et al., 2009; Ren et al., 2020). ( 2)the IS had an impact on the structure of the double electrode layer of soil (Ren et al., 2020). H2A + Cd2+ = CdHA+ + H+H2A + Cd2+ = CdA + 2H+H2B + Cd2+ = CdHB+ + H+H2B + Cd2+ = CdB + 2H+SiOH + Cd2+ = SiO− − Cd2++H+SiOH + Cd2+ + H2O = SiO− − CdOH++2H+AlOH + Cd2+ = AlOCd+ + H+

    • A review on adsorptive separation of toxic metals from aquatic system using biochar produced from agro-waste

      2021, Chemosphere
      Citation Excerpt :

      Ion exchange process is a chemical method to remove the dissolved ions from polluted water. The heavy metals are available in dissolved form in water and it gets effectively separated by the ion exchange process (Smara et al., 2005; Hsien Lee et al. 2006; Kiefer et al., 2007; Badawy et al., 2009; Pal and Banat, 2014; Kołodyńska et al., 2017; Nekouei et al., 2019; Gossuin et al., 2020; Ren et al., 2020a,b). The dissolved ions in the water gets exchanged with ions in the reversible ion-exchange material and there is no any change in the structure of the material during the ion exchange process.

    View all citing articles on Scopus
    View full text