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生物炭-壳聚糖磁性复合吸附剂的制备及去除地下水中铅和铜

杨梦楠, 孙晗, 曹海龙, 贾增华, 冯政远, 郑丽君, 陈男

杨梦楠,孙晗,曹海龙,等. 生物炭-壳聚糖磁性复合吸附剂的制备及去除地下水中铅和铜[J]. 岩矿测试,2023,42(3):563−575. DOI: 10.15898/j.ykcs.202208230155
引用本文: 杨梦楠,孙晗,曹海龙,等. 生物炭-壳聚糖磁性复合吸附剂的制备及去除地下水中铅和铜[J]. 岩矿测试,2023,42(3):563−575. DOI: 10.15898/j.ykcs.202208230155
YANG Mengnan,SUN Han,CAO Hailong,et al. Preparation and Application of Biochar-Chitosan Magnetic Composite Adsorbent for Removal of Lead and Copper from Groundwater[J]. Rock and Mineral Analysis,2023,42(3):563−575. DOI: 10.15898/j.ykcs.202208230155
Citation: YANG Mengnan,SUN Han,CAO Hailong,et al. Preparation and Application of Biochar-Chitosan Magnetic Composite Adsorbent for Removal of Lead and Copper from Groundwater[J]. Rock and Mineral Analysis,2023,42(3):563−575. DOI: 10.15898/j.ykcs.202208230155

生物炭-壳聚糖磁性复合吸附剂的制备及去除地下水中铅和铜

基金项目: 企事业单位委托项目“长江流域典型金属矿山酸性土壤及地下水污染协同修复技术研发”(342021399)
详细信息
    作者简介:

    杨梦楠,硕士研究生,主要从事生态环境系统修复研究工作。E-mail:yangyangwd@hotmail.com

    通讯作者:

    陈男,教授,博士生导师,地下水科学与工程专业,主要从事地下水污染控制与修复技术研究。E-mail:chennan@cugb.edu.cn

  • 中图分类号: X523;G264.3

Preparation and Application of Biochar-Chitosan Magnetic Composite Adsorbent for Removal of Lead and Copper from Groundwater

  • 摘要:

    壳聚糖作为天然多糖有机物,具有对环境友好的特性,其含有的大量含氮官能团可吸附水中的金属离子。但壳聚糖类吸附剂在酸性条件下适应性差,实际使用过程中需要调节pH值,因此增加了运行成本。本文选用农林废弃物花生壳(CC)和玉米芯(PS)制备生物炭,与壳聚糖进行结合,并引入磁性因子Fe3O4,制备了花生壳生物炭-壳聚糖磁性复合吸附剂(PSC)和玉米芯生物炭-壳聚糖磁性复合吸附剂(CCC),并研究这两种吸附剂对水中Pb2+和Cu2+的吸附性能,同时利用实际含多种金属离子的地下水对所制备的材料进行实验,以评估其实际应用潜能。比表面积仪(BET)分析表征显示,CCC相比PSC的比表面积和平均孔径更大,两种吸附剂在pH 4~7范围内均表现出稳定的吸附性能。循环5个周期后,两种吸附剂仍对Pb2+和Cu2+的去除率保持在85%以上,表现出良好的循环利用性能。CCC对Pb2+和Cu2+的最大吸附容量分别为169.10mg/g和18.69mg/g,均大于PSC的最大吸附容量。同时,CCC可有效去除含重金属地下水中的多种金属离子。在处理实际含Pb2+和Cu2+的废水时可优先选择CCC材料作为吸附剂。吸附动力学实验结果表明,两种材料对Pb2+的吸附以物理吸附为主,对Cu2+的吸附以化学吸附为主。pH值影响实验和X射线光电子能谱(XPS)表征结果说明两种材料主要通过静电吸引和含氮官能团与金属离子的螯合作用去除Pb2+和Cu2+。本文使用农林废弃物制备生物炭降低了成本,引入的磁性因子方便了脱附过程,生物炭-壳聚糖磁性复合材料的制备方法有效地改善了壳聚糖类材料在酸性条件下的适应性,所制备的材料是一种去除地下水中Pb2+和Cu2+污染的有效潜在吸附剂。

  • 碲和硒是稀散元素,在高新科技领域具有重要应用,已被中国和欧美国家列为战略性关键矿产资源1-2。一直以来全球碲、硒矿产资源主要采自斑岩-矽卡岩铜金矿床,如中国广东大宝山铜矿和江西城门山铜矿3-4,研究斑岩矿床中碲、硒的产出情况对国家资源战略保障具有重要意义。云南普朗斑岩型铜金矿床位于三江特提斯成矿域义敦岛弧南部,属于超大型斑岩矿床,已探明铜资源储量4.31Mt,金资源量113t5。矿区内出露的地层为中三叠统尼汝组和上三叠统图姆沟组,侵入岩为普朗复式岩体,由石英闪长玢岩(~216Ma)、石英二长斑岩(~215Ma)和花岗闪长斑岩(~206Ma)组成,岩体出露总面积约为11km2图1)。前人对普朗矿床的地质特征、成岩成矿时代、成矿物质来源、成矿流体性质等作了大量工作,但对矿床中碲硒的含量和赋存状态等研究还较为薄弱。本文报道了普朗矿床中产出的碲化物和硒化物,以期为斑岩矿床中碲硒的勘查和综合利用提供资料。

    图  1  普朗斑岩铜金矿床地质简图(据Leng等5修改)
    Figure  1.  Geological map of the Pulang porphyry Cu-Au deposit (Modified from Leng, et al 5 ).

    本次研究对象主要为普朗矿床中的铜精矿和钼精矿样品,测试分析均在东华理工大学核资源与环境国家重点实验室完成。样品的矿相学观察利用ZEISS Axio Scope A1光学显微镜及ZEISS Sigma 300场发射扫描电镜完成,扫描电镜的加速电压为20kV,发射电流为10μA6。矿物成分利用JXA-8530F Plus型电子探针分析完成,实验设定加速电压为15kV,电流为20nA,探针直径为1μm,使用ZAF方法对X射线强度进行校正。分析标样选择砷化镓(As),黄铜矿(Cu),黄铁矿(Fe、S),自然银(Ag),碲铋矿(Te、Bi),辉钼矿(Mo),自然铅(Pb),自然锑(Sb),硒化镉(Se),自然金(Au),自然铂(Pt),自然钯(Pd)。测试主量元素的精确度和准确度均小于2%。

    普朗铜金矿床中的碲和硒含量高,并形成大量碲化物、硒化物和富硒矿物。矿床精矿中的碲和硒含量分别达74.3×10−6和270×10−6。碲在钾化带中的含量为0.3×10−6~0.43×10−6,较绢英岩化带中的高(0.02×10−6~0.12×10−6),由矿体中心向外,碲品位逐渐降低7。硒在钾化带和绢英岩化带的含量无明显差别,分别为1.49×10−6~2.44×10−6和1.04×10−6~3.00×10−6。矿石中的碲与金呈正相关关系,硒与银呈正相关关系。普朗铜矿床中,碲和硒主要以碲化物、硒化物和富硒矿物形式存在,形成辉碲铋矿、碲钯矿、硒银矿和富硒方铅矿等(图2)。辉碲铋矿是普朗含量最多的碲化物,反射光下为白色略带淡蓝色,矿物成分较均一,Bi含量为58.36%~61.24%,Te含量为31.03%~34.50%,S含量为3.76%~4.54%(图2e)。普朗辉碲铋矿中含有较高的Se(0.77%~3.63%)。辉碲铋矿的化学式为Bi2.02~2.08(Te1.74~1.93S0.85~1.01Se0.08~0.332.90~2.98。碲钯矿属于独立铂族元素矿物,在自然界很少见,中国斑岩矿床中仅江西德兴有报道8,在全球其他斑岩矿床中非常少见。普朗碲钯矿粒径为1~5μm,反射光下呈亮白色(图2a)。碲钯矿中Pd和Pt可以类质同象取代,因此含量变化较大,Pd含量为16.26%~25.69%,Pt含量为4.82%~17.66%,Te含量为61.25%~66.76%(图2f)。碲钯矿化学式为(Pd0.64~0.98Pt0.09~0.370.98~1.03Te1.97~1.02。硒银矿是普朗含量最多的硒化物,反射光下为白色带微蓝绿色(图2c)。硒银矿中普遍含S,含量为0.55%~2.65%,Ag含量普遍偏低,为70.22%~72.77%,Se含量为24.09%~27.31%(图2g)。硒银矿化学式为Ag1.89~1.98(Se0.87~1.01S0.05~0.241.02~1.11。富硒方铅矿属于PbS1-xSex矿物,其中x值可在0~1之间连续变化。普朗富硒方铅矿S和Se的含量变化大,分别为4.01%~12.52%和1.85%~19.13%,Pb含量为73.91%~82.52%,大多数样品中含有Ag,最高含量达1.61%。普朗富硒方铅矿形成了较完整的PbS-PbSe固溶体系列(图2h),化学式为Pb0.98~1.01(S0.35~0.97Se0.07~0.670.99~1.02

    图  2  碲硒矿物显微照片及矿物元素含量三元图
    a—碲钯矿反射光镜下照片; b—碲钯矿BSE照片; c—硒银矿反射光镜下照片; d—硒银矿BSE照片; e— Bi-Te-S体系三元图; f— Te-Pd-Pt体系三元图; g—Ag-Se-S体系三元图; h—Pb-Se-S体系三元图。Mol—辉钼矿; Mrk—碲钯矿; Nau—硒银矿; Py—黄铁矿。
    Figure  2.  Photomicrographs of tellurium and selenium minerals and ternary plots of element contents. a—Reflected light photomicrograph of merenskyite; b—BSE image of merenskyite; c—Reflected light photomicrograph of naumannite; d—BSE image of naumannite; e—Ternary plot of Bi-Te-S system; f—Ternary plot of Te-Pd-Pt system; g—Ternary plot of Ag-Se-S system; h—Ternary plot of Pb-Se-S system. Mol=Molybdenite, Mrk=Merenskyite, Nau=Naumannite, Py=Pyrite.

    矿床中的碲和硒可以指示物质来源和成矿过程。碲和硒具有亲硫特点,碲会部分进入硫化物晶格,但更易形成碲的独立矿物;硒属于强亲硫元素,在较高温的条件下易于进入硫化物晶格,在中低温条件下,硫含量较低时,可形成硒的独立矿物。洋壳中的铁锰结壳、页岩及浮游沉积物等是自然界中碲和硒的重要储库9,因此在洋陆俯冲过程中,大陆岩石圈地幔和洋壳的部分熔融会形成富碲、硒的岩浆10-11。碲和硒在硫化物熔体中的相容性很高(D硫化物/硅酸盐>600),碲倾向于存在液相硫化物(SL)中,而硒则更易进入单硫化物固熔体(MSS)(DTe SL/硅酸盐/DSe SL/硅酸盐为5~9,DTe MSS/硅酸盐/DSe MSS/硅酸盐为0.5~0.8)12。当富碲、硒的岩浆到达下地壳,会结晶分异形成富Co、Ni的硅酸盐矿物,碲、硒存在硫化物熔体中继续向上运移;当岩浆到达中地壳,温度低于900℃时,硫化物熔体与Te-Se熔体发生相分离;当岩浆到达上地壳,侵位形成班岩体及Cu矿床,Ag-Pt-Pd则高度集中在富Te-Se熔体中,并最终形成贵金属矿物13。普朗铜金矿床中的碲和硒可能与区内晚三叠世的俯冲造山密切相关,富碲和硒的岩浆也促进了铂族元素的富集成矿。

    普朗斑岩铜金矿床中碲化物和硒化物的发现,对资源的综合利用及矿床成因研究具有重要意义。矿床中碲和硒的资源量规模大,大部分以独立矿物形式存在,且常与Au-Ag-PGE共生,具有较好的经济回收利用价值。碲化物和硒化物的产出也为成矿物质来源及岩浆演化过程提供了新的研究方向。

  • 图  1   生物炭-壳聚糖磁性复合材料合成示意图

    Figure  1.   Schematic diagram of biochar-chitosan magnetic composite.

    图  2   (a)PS、(b)CC、(c)PSC和(d)CCC的SEM图像

    Figure  2.   SEM images of (a) PS, (b) CC, (c) PSC and (d) CCC

    图  3   (A)Fe3O4(a线)、壳聚糖(b线)、CCC(c线)、PSC(d线)的XRD谱图;(B)材料在不同pH条件下(4、7、10)的溶胀性

    Figure  3.   (A) XRD patterns of Fe3O4 (line a), chitosan (line b), CCC (c line) and PSC (d line); (B) Swelling properties of materials under different pH conditions (pH=4, 7, 10).

    图  4   pH对PSC和CCC吸附Cu2+和Pb2+效果的影响

    Figure  4.   Effect of pH on adsorption of Cu2+ and Pb2+ by PSC and CCC (Dosage=4g/L, initial concentration of Cu2+ and Pb2+ are both 50mg/L).

    图  5   PSC和CCC对(a)Pb2+和(b)Cu2+的循环利用性

    Figure  5.   The recycling of (a)Pb2+ and (b)Cu2+ by PSC and CCC.

    图  6   PSC(a)、吸附Pb2+后PSC(b)、吸附Cu2+后PSC(c)、CCC(d)、吸附Pb2+后CCC(e)、吸附Cu2+后CCC(f)的XPS谱图

    Figure  6.   XPS spectra of PSC (a), PSC after Pb2+ adsorption (b), PSC after Cu2+ adsorption (c), CCC (d), CCC after Pb2+ adsorption (e), CCC after Cu2+ adsorption (f).

    表  1   PSC和CCC吸附Pb2+、Cu2+动力学模型拟合参数以及PSC和CCC吸附Pb2+、Cu2+等温线模型拟合参数

    Table  1   Fitting parameters of kinetic models for Pb2+ and Cu2+ adsorption by PSC and CCC, and the fitting parameters of PSC and CCC adsorption of Pb2+ and Cu2+ isotherm models.

    金属离子制备
    材料
    伪一级动力学模型伪二级动力学模型
    K1R2χ2k2R2χ2
    Pb2+PSC0.03750.9980.0420.00620.9360.114
    CCC0.00450.9990.0440.00040.9860.121
    Cu2+PSC0.00720.9960.0490.00090.9970.135
    CCC0.00370.9880.0820.00210.9970.056
    金属离子制备
    材料
    Langmuir模型Freundlich模型
    qmKLR2χ2KF1/nR2χ2
    Pb2+PSC189.090.00170.9990.7020.7660.7490.9928.460
    CCC86.720.00360.9981.4201.2200.6220.9849.706
    Cu2+PSC18.690.01230.9810.9731.2770.4190.9522.372
    CCC14.340.01970.9790.6672.720.3680.9280.375
    下载: 导出CSV

    表  2   PSC和CCC吸附Pb和Cu的性能与其他材料对比

    Table  2   Comparison of the adsorption capacities of PSC and CCC with other materials.

    吸附剂最大吸附容量(mg/g)参考文献
    PbCu
    二甘酸功能化磁性壳聚糖70.57-[36]
    EDTA-改性壳聚糖/SiO2/Fe3O4123.544.4[37]
    磁性花生壳28.3-[38]
    磁性壳聚糖/纤维素微球45.888.2[39]
    介孔CoFe2O4纳米颗粒32.1-[40]
    CCC169.1018.69本研究
    PSC86.7214.34本研究
    注:“-”表示文献中未提供数据。
    下载: 导出CSV
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出版历程
  • 收稿日期:  2022-08-22
  • 修回日期:  2022-11-19
  • 录用日期:  2023-01-17
  • 网络出版日期:  2023-05-29
  • 刊出日期:  2023-06-29

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