McBride Murray B, Frenchmeyer Meredith, Kelch Sabrina E, Aristilde Ludmilla
Soil and Crop Sciences Section, School of Integrative Plant Science, College of Agriculture and Life Sciences, Cornell University, Ithaca, NY, USA.
Soil and Crop Sciences Section, School of Integrative Plant Science, College of Agriculture and Life Sciences, Cornell University, Ithaca, NY, USA.
J Colloid Interface Sci. 2017 Jan 15;486:309-315. doi: 10.1016/j.jcis.2016.09.079. Epub 2016 Sep 30.
Calcium-oxalates (Ca-Ox), which are widely produced by microorganisms and plants, are ubiquitous and persistent biominerals in the biosphere. We investigated the potential trapping of two phytotoxic metals, cadmium (Cd) and zinc (Zn) by isomorphous substitution into the crystalline structure of Ca-Ox precipitated over a wide range of Cd/Ca or Zn/Ca ratio in solution. We employed atomic absorption spectroscopy, X-ray diffraction (XRD), and optical microscopy to evaluate our hypotheses that favorable solid-solution conditions and structural framework of crystal habits promote selective metal trapping within Ca-Ox precipitates. Chemical analysis demonstrated more effective Cd-Ox/Ca-Ox than Zn-Ox/Ca-Ox co-precipitate formation at the same trace metal mole fraction in solution. The XRD results revealed sequestration of Cd, but not Zn, within Ca-Ox monohydrate (whewellite). Comparative chemical analysis with Cd-Ox formation in the absence of Ca-Ox showed that the whewellite solid-solution formation lowered the solubility of Cd below that of pure Cd-Ox. The XRD patterns indicated that Zn precipitated as a separate pure Zn-Ox crystal that is largely excluded from the Ca-Ox structure. Furthermore, the presence of Zn in solution favored the formation of the less stable Ca-Ox dihydrate (weddellite) over whewellite. In agreement with the XRD data, visualization of the co-precipitates by optical microscopy illustrated combined mineral phases of Cd-Ox with Ca-Ox whereas Zn-Ox and Ca-Ox exhibited two distinct mineral morphologies. Our findings shed light into the structural factors that are most critical in facilitating the trapping of toxic trace metals within Ca-Ox crystals.
草酸钙(Ca - Ox)广泛由微生物和植物产生,是生物圈中普遍存在且持久的生物矿物。我们研究了在溶液中一系列Cd/Ca或Zn/Ca比例下沉淀的Ca - Ox晶体结构通过同晶替代对两种植物毒性金属镉(Cd)和锌(Zn)的潜在捕获作用。我们采用原子吸收光谱法、X射线衍射(XRD)和光学显微镜来评估我们的假设,即有利的固溶条件和晶体习性的结构框架促进了Ca - Ox沉淀物中金属的选择性捕获。化学分析表明,在溶液中相同痕量金属摩尔分数下,Cd - Ox/Ca - Ox共沉淀的形成比Zn - Ox/Ca - Ox更有效。XRD结果显示,一水合Ca - Ox(水草酸钙石)中捕获了Cd,但未捕获Zn。与在没有Ca - Ox的情况下形成Cd - Ox的对比化学分析表明,水草酸钙石固溶体的形成使Cd的溶解度低于纯Cd - Ox。XRD图谱表明,Zn以单独的纯Zn - Ox晶体形式沉淀,该晶体在很大程度上被排除在Ca - Ox结构之外。此外,溶液中Zn的存在有利于形成比水草酸钙石稳定性更低的二水合Ca - Ox(水钙草酸石)。与XRD数据一致,通过光学显微镜对共沉淀物的观察显示Cd - Ox与Ca - Ox的混合矿物相,而Zn - Ox和Ca - Ox呈现出两种不同的矿物形态。我们的研究结果揭示了在促进Ca - Ox晶体中捕获有毒痕量金属方面最关键的结构因素。