Gibbs free binding energy and adsorption energy between cations and charged soil particles were used to evaluate the interactions between ions and soil particles.The distribution of Gibbs free adsorption energies coul...Gibbs free binding energy and adsorption energy between cations and charged soil particles were used to evaluate the interactions between ions and soil particles.The distribution of Gibbs free adsorption energies could not be determined experimentally before the development of Wien effect measurements in dilute soil suspensions.In the current study,energy relationships between heavy metal ions and particles of Hapli-Udic Argosol(Alfisol)and Ferri-Udic Argosol were inferred from Wien effect measurements in dilute suspensions of homoionic soil particles(<2μm)of the two soils,which were saturated with ions of five heavy metals,in deionized water.The mean Gibbs free binding energies of the heavy metal ions with Hapli-Udic Argosol and Ferri-Udic Argosol particles diminished in the order of Pb^(2+)>Cd^(2+)>Cu^(2+)>Zn^(2+)>Cr^(3+),where the range of binding energies for Hapli-Udic Argosol(7.25-9.32 kJ mol^(-1))was similar to that for Ferri-Udic Argosol(7.43-9.35 kJ mol^(-1)).The electrical field-dependent mean Gibbs free adsorption energies of these heavy metal ions for Hapli-Udic Argosol and for Ferri-Udic Argosol descended in the order:Cu^(2+)≥Cd^(2+)≥Pb^(2+)>Zn^(2+)>Cr^(3+), and Cd^(2+)>Cu^(2+)>Pb^(2+)>Zn^(2+)>Cr^(3+),respectively.The mean Gibbs free adsorption energies of Cu^(2+),Zn^(2+),Cd^(2+), Pb^(2+),and Cr^(3+)at a field strength of 200 kV cm^(-1),for example,were in the range of 0.8-3.2 kJ mol^(-1)for the two soils.展开更多
目前,工业上广泛采用“分解-浮选”工艺生产KCl,但是在光卤石分解过程中NaCl对KCl晶体的影响尚不明确。在光卤石的分解结晶阶段,由于KCl和NaCl的明显聚集,使得两种颗粒在浮选阶段的分离效率较差。以NaCl掺杂光卤石为原料,开展了分解-浮...目前,工业上广泛采用“分解-浮选”工艺生产KCl,但是在光卤石分解过程中NaCl对KCl晶体的影响尚不明确。在光卤石的分解结晶阶段,由于KCl和NaCl的明显聚集,使得两种颗粒在浮选阶段的分离效率较差。以NaCl掺杂光卤石为原料,开展了分解-浮选制备KCl实验。以NaCl的粒径和含量为变量,结合扫描电子显微镜-能谱仪(scanning electron microscope-energy dispersive spectrometer,SEM-EDS)图像,研究了NaCl的粒度和含量对精矿中KCl品位的影响。研究结果显示,掺杂的NaCl粒径对精矿中KCl的影响较大。当NaCl粒径在40~60目时,随着光卤石中NaCl含量的升高,浮选后精矿品位基本不变,K^(+)平均含量为44.39%;当NaCl粒径在60~80目和100目下时,随着光卤石中NaCl含量的升高,浮选后精矿中K^(+)含量明显降低,K^(+)含量分别降低至36.08%和35.48%,而Na+含量分别升高至6.27%和8.36%。此外,SEM和EDS结果表明精矿中的杂质NaCl是以黏附或者嵌入的方式生长在KCl晶体上,从而导致浮选KCl的同时NaCl一起选出,使得精矿中K^(+)含量降低。该研究结果成功揭示了盐田低钾光卤石矿生产钾肥过程中NaCl和KCl难分离的主要原因,为盐湖钾资源的高效利用提供了研究基础。展开更多
Interactions of three heavy metal ions, Cu2+, Cd2+, and Pb2+, and, for comparison, Na+ with electrodialytic clay fractions (less than 2μm in diameter) of four paddy soils as well as a yellow-brown soil as a control s...Interactions of three heavy metal ions, Cu2+, Cd2+, and Pb2+, and, for comparison, Na+ with electrodialytic clay fractions (less than 2μm in diameter) of four paddy soils as well as a yellow-brown soil as a control soil were evaluated based on measurements of the Wien effect in dilute suspensions with a clay concentration of 10 g kg-1 in four nitrate solutions of 2×10-4/z mol L-1, where z is the cation valence, and a nitric acid solution of 3×10-5 mol L-1.Field strengths ranging from 15 to 230 kV cm-1 were applied for measuring the electrical conductivities (ECs) of the suspensions. The mean free binding energies between the various cations and all of the soils determined from exchange equilibrium increased in the order: Na+ < Cd2+ < Cu2+ < Pb2+. In general, the ECs of the suspensions in the sodium nitrate solution were smaller than those of the suspensions in the heavy metal solutions because of the lower electrophoretic mobility of sodium compared to the divalent cations. In terms of relative electrical conductivity-field strength relationships, relative electrical conductivity (REC) of suspensions containing various cations at field strengths larger than about 50 kV cm-1 were in the descending order: Na+ > Cu2+ > Cd2+ > Pb2+ for all tested soils. A characteristic parameter of the REC-field strength curves,△REG200, REG at a field strength of 200 kV cm-1 minus that at the local minimum of the concave segment of the REC-field strength curves, characterized the strength of adsorption of the cations stripped off by the applied strong electrical field, and for all soils the values of△REC200 were generally in the order: Na+ < Cu2+≤Cd2+≤Pb2+.展开更多
To investigate the interactions of oppositely charged sites on the surfaces of variable-charge soil particles with cations and anions,and to evaluate the mean Gibbs free binding and adsorption energies of various cati...To investigate the interactions of oppositely charged sites on the surfaces of variable-charge soil particles with cations and anions,and to evaluate the mean Gibbs free binding and adsorption energies of various cations on particles of red soil and latosol,clay fractions smaller than 2 μm were separated from samples of the two variable-charge soils.Ferric oxides were removed from part of the clay fractions,which were then saturated with various chlorides(NaCl,KCl,CaCl2,CdCl2 or LaCl3).Electrical conductivities(EC) of dilute suspensions of the original and of the iron oxides-free clay fractions in deionized water were measured with the SHP-2 short high-voltage pulse apparatus,which enables measurement of the Wien effect at field strengths(E) from 14 to 250 kV cm-1.The Wien effect(EC-E) curves revealed EC increases of red soil suspensions between 14 and 200 kV cm-1,of 8.3,8.4,12.1,5.9,and 1.2 μS cm-1 for NaCl,KCl,CaCl2,CdCl2,and LaCl3,respectively,reflecting the differing interactions with the various cations and chloride.The EC increments with the iron-free red soil suspensions were higher,being 29.7,17.2,and 15.3 μS cm-1 for NaCl,CaCl2,and CdCl2,respectively.In the natural latosol suspensions the EC increments were practically zero,whereas in the iron-free fractions there were significant EC increments of 10.3,5.7,5.0,and 1.6 μS cm-1 for NaCl,CaCl2,CdCl2,and LaCl3,respectively.展开更多
基金Project supported by the National Natural Science Foundation of China(Nos.40401030 and 20577054).
文摘Gibbs free binding energy and adsorption energy between cations and charged soil particles were used to evaluate the interactions between ions and soil particles.The distribution of Gibbs free adsorption energies could not be determined experimentally before the development of Wien effect measurements in dilute soil suspensions.In the current study,energy relationships between heavy metal ions and particles of Hapli-Udic Argosol(Alfisol)and Ferri-Udic Argosol were inferred from Wien effect measurements in dilute suspensions of homoionic soil particles(<2μm)of the two soils,which were saturated with ions of five heavy metals,in deionized water.The mean Gibbs free binding energies of the heavy metal ions with Hapli-Udic Argosol and Ferri-Udic Argosol particles diminished in the order of Pb^(2+)>Cd^(2+)>Cu^(2+)>Zn^(2+)>Cr^(3+),where the range of binding energies for Hapli-Udic Argosol(7.25-9.32 kJ mol^(-1))was similar to that for Ferri-Udic Argosol(7.43-9.35 kJ mol^(-1)).The electrical field-dependent mean Gibbs free adsorption energies of these heavy metal ions for Hapli-Udic Argosol and for Ferri-Udic Argosol descended in the order:Cu^(2+)≥Cd^(2+)≥Pb^(2+)>Zn^(2+)>Cr^(3+), and Cd^(2+)>Cu^(2+)>Pb^(2+)>Zn^(2+)>Cr^(3+),respectively.The mean Gibbs free adsorption energies of Cu^(2+),Zn^(2+),Cd^(2+), Pb^(2+),and Cr^(3+)at a field strength of 200 kV cm^(-1),for example,were in the range of 0.8-3.2 kJ mol^(-1)for the two soils.
基金STS Regional key projects of CAS(KFJ-STS-QYZD-2-21-06-002)Qinghai province science and technology department Key R&D and transformation plan(2021-GX-C04).
文摘目前,工业上广泛采用“分解-浮选”工艺生产KCl,但是在光卤石分解过程中NaCl对KCl晶体的影响尚不明确。在光卤石的分解结晶阶段,由于KCl和NaCl的明显聚集,使得两种颗粒在浮选阶段的分离效率较差。以NaCl掺杂光卤石为原料,开展了分解-浮选制备KCl实验。以NaCl的粒径和含量为变量,结合扫描电子显微镜-能谱仪(scanning electron microscope-energy dispersive spectrometer,SEM-EDS)图像,研究了NaCl的粒度和含量对精矿中KCl品位的影响。研究结果显示,掺杂的NaCl粒径对精矿中KCl的影响较大。当NaCl粒径在40~60目时,随着光卤石中NaCl含量的升高,浮选后精矿品位基本不变,K^(+)平均含量为44.39%;当NaCl粒径在60~80目和100目下时,随着光卤石中NaCl含量的升高,浮选后精矿中K^(+)含量明显降低,K^(+)含量分别降低至36.08%和35.48%,而Na+含量分别升高至6.27%和8.36%。此外,SEM和EDS结果表明精矿中的杂质NaCl是以黏附或者嵌入的方式生长在KCl晶体上,从而导致浮选KCl的同时NaCl一起选出,使得精矿中K^(+)含量降低。该研究结果成功揭示了盐田低钾光卤石矿生产钾肥过程中NaCl和KCl难分离的主要原因,为盐湖钾资源的高效利用提供了研究基础。
基金Project supported by the National Key Basic Research Support Foundation of China (No. 2002CB410808)the National Natural Science Foundation of China (No. 40401030)
文摘Interactions of three heavy metal ions, Cu2+, Cd2+, and Pb2+, and, for comparison, Na+ with electrodialytic clay fractions (less than 2μm in diameter) of four paddy soils as well as a yellow-brown soil as a control soil were evaluated based on measurements of the Wien effect in dilute suspensions with a clay concentration of 10 g kg-1 in four nitrate solutions of 2×10-4/z mol L-1, where z is the cation valence, and a nitric acid solution of 3×10-5 mol L-1.Field strengths ranging from 15 to 230 kV cm-1 were applied for measuring the electrical conductivities (ECs) of the suspensions. The mean free binding energies between the various cations and all of the soils determined from exchange equilibrium increased in the order: Na+ < Cd2+ < Cu2+ < Pb2+. In general, the ECs of the suspensions in the sodium nitrate solution were smaller than those of the suspensions in the heavy metal solutions because of the lower electrophoretic mobility of sodium compared to the divalent cations. In terms of relative electrical conductivity-field strength relationships, relative electrical conductivity (REC) of suspensions containing various cations at field strengths larger than about 50 kV cm-1 were in the descending order: Na+ > Cu2+ > Cd2+ > Pb2+ for all tested soils. A characteristic parameter of the REC-field strength curves,△REG200, REG at a field strength of 200 kV cm-1 minus that at the local minimum of the concave segment of the REC-field strength curves, characterized the strength of adsorption of the cations stripped off by the applied strong electrical field, and for all soils the values of△REC200 were generally in the order: Na+ < Cu2+≤Cd2+≤Pb2+.
基金supported by the Knowledge Innovation Program of the Chinese Academy of Sciences (No.ISSASIP 0718)the National Natural Science Foundation of China (Nos.40401030 and 40871114)
文摘To investigate the interactions of oppositely charged sites on the surfaces of variable-charge soil particles with cations and anions,and to evaluate the mean Gibbs free binding and adsorption energies of various cations on particles of red soil and latosol,clay fractions smaller than 2 μm were separated from samples of the two variable-charge soils.Ferric oxides were removed from part of the clay fractions,which were then saturated with various chlorides(NaCl,KCl,CaCl2,CdCl2 or LaCl3).Electrical conductivities(EC) of dilute suspensions of the original and of the iron oxides-free clay fractions in deionized water were measured with the SHP-2 short high-voltage pulse apparatus,which enables measurement of the Wien effect at field strengths(E) from 14 to 250 kV cm-1.The Wien effect(EC-E) curves revealed EC increases of red soil suspensions between 14 and 200 kV cm-1,of 8.3,8.4,12.1,5.9,and 1.2 μS cm-1 for NaCl,KCl,CaCl2,CdCl2,and LaCl3,respectively,reflecting the differing interactions with the various cations and chloride.The EC increments with the iron-free red soil suspensions were higher,being 29.7,17.2,and 15.3 μS cm-1 for NaCl,CaCl2,and CdCl2,respectively.In the natural latosol suspensions the EC increments were practically zero,whereas in the iron-free fractions there were significant EC increments of 10.3,5.7,5.0,and 1.6 μS cm-1 for NaCl,CaCl2,CdCl2,and LaCl3,respectively.