Hu Yandi, Zhang Suona, Zhou Zehao, Cao Zhiqian
School of Environmental Science and Engineering, Peking University, Beijing 100871, China.
State Environmental Protection Key Laboratory of All Material Fluxes in River Ecosystems, Beijing 100871, China.
Acc Chem Res. 2024 May 7;57(9):1254-1263. doi: 10.1021/acs.accounts.3c00807. Epub 2024 Mar 15.
ConspectusThe heterogeneous coprecipitation of nanocrystals with metals on substrates plays a significant role in both natural and engineered systems. Due to the small dimensions and thereby the large specific surface area, nanocrystal coprecipitation with metals, which is ubiquitous in natural settings, exerts drastic effects on the biogeochemical cycling of metals on the earth's crust. Meanwhile, the controlled synthesis of nanocrystals with metal doping to achieve tunable size/composition enables their broad applications as adsorbents and catalysts in many engineered settings. Despite their importance, complex interactions among aqueous ions/polymers, nanocrystals, substrates, and metals are far from being well-understood, leaving the controlling mechanisms for nanocrystal formation with metals on substrates uncovered.In this Account, we discuss our systematic investigation over the past 10 years of the heterogeneous formation of representative nanocrystals with metals on typical substrates. We chose Fe(OH) and BaSO as representative nanocrystals. Mechanisms for varied metal coprecipitation were also investigated for both types of nanocrystals (i.e., Fe, Al, Cr, Cu, and Pb)(OH) and (Ba, Sr)(SO, SeO, and SeO)). Bare SiO and AlO, as well as those coated with varied organics, were selected as geologically or synthetically representative substrates. Through the integration of state-of-the-art nanoscale interfacial characterization techniques with theoretical calculations, the complex interactions during nanocrystal formation at interfaces were probed and the controlling mechanisms were identified.For BaSO and Fe(OH) formation on substrates, the local supersaturation levels near substrates were controlled by Ba adsorption and the electrostatic attraction of Fe(OH) monomer/polymer to substrates, respectively. Meanwhile, substrate hydrophobicity controlled the interfacial energy for the nucleation of both nanocrystals on (in)organic substrates. Metal ions' (i.e., Cr/Al/Cu/Pb) hydrolysis constants and substrates' dielectric constants controlled metal ion adsorption onto substrates, which altered the surface charges of substrates, thus controlling heterogeneous Fe(OH) nanocrystal formation on substrates by electrostatic interactions. The sizes and compositions of heterogeneous (Fe, Cr)(OH) and (Ba, Sr)(SO, SeO, SeO) formed on substrates were found to be distinct from those of homogeneous precipitates formed in solution. The substrate (de)protonation could alter the local solution's pH and the substrates' surface charge; substrates could also adsorb cations, affecting local Fe/Cr/Ba/Sr ion concentrations at solid-water interfaces, thus controlling the amount/size/composition of nanocrystals by tuning their nucleation/growth/deposition on substrates. From slightly supersaturated solution, homogeneous coprecipitates of microsized (Ba, Sr)(SO, SeO, SeO) formed through growth, with little Sr/Se(VI) incorporation due to higher solubilities of SrSO and BaSeO over BaSO. While cation enrichment near substrates made the local solution highly supersaturated, nanosized coprecipitates formed on substrates through nucleation, with more Sr/Se(VI) incorporation due to lower interfacial energies of SrSO and BaSeO over BaSO. The new insights gained advanced our understanding of the biogeochemical cycling of varied elements at solid-water interfaces and of the controlled synthesis of functional nanocrystals.
概述
纳米晶体与金属在基底上的非均相共沉淀在自然和工程系统中都起着重要作用。由于纳米晶体尺寸小,比表面积大,其与金属的共沉淀在自然环境中普遍存在,对地壳中金属的生物地球化学循环产生了显著影响。同时,通过金属掺杂可控合成具有可调尺寸/组成的纳米晶体,使其在许多工程领域中作为吸附剂和催化剂具有广泛应用。尽管它们很重要,但水相离子/聚合物、纳米晶体、基底和金属之间的复杂相互作用仍远未被充分理解,导致纳米晶体与金属在基底上形成的控制机制尚未被揭示。
在本综述中,我们讨论了过去10年中我们对代表性纳米晶体与金属在典型基底上的非均相形成的系统研究。我们选择Fe(OH)和BaSO作为代表性纳米晶体。还研究了这两种类型纳米晶体(即Fe、Al、Cr、Cu和Pb的(OH)以及Ba、Sr的(SO、SeO和SeO))不同金属共沉淀的机制。选择裸露的SiO和AlO以及涂覆有不同有机物的SiO和AlO作为地质或合成方面具有代表性的基底。通过将最先进的纳米级界面表征技术与理论计算相结合,探究了界面处纳米晶体形成过程中的复杂相互作用,并确定了控制机制。
对于BaSO和Fe(OH)在基底上的形成,基底附近的局部过饱和度水平分别由Ba的吸附以及Fe(OH)单体/聚合物对基底的静电吸引来控制。同时,基底疏水性控制了两种纳米晶体在(有机)无机基底上成核的界面能。金属离子(即Cr/Al/Cu/Pb)的水解常数和基底的介电常数控制金属离子在基底上的吸附,这改变了基底的表面电荷,从而通过静电相互作用控制了基底上非均相Fe(OH)纳米晶体的形成。发现在基底上形成的非均相(Fe, Cr)(OH)和(Ba, Sr)(SO, SeO, SeO)的尺寸和组成与在溶液中形成的均相沉淀物不同。基底的(去)质子化可以改变局部溶液的pH值和基底的表面电荷;基底还可以吸附阳离子,影响固 - 水界面处局部Fe/Cr/Ba/Sr离子浓度,从而通过调节它们在基底上的成核/生长/沉积来控制纳米晶体的数量/尺寸/组成。从略微过饱和的溶液中,通过生长形成了微米级的(Ba, Sr)(SO, SeO, SeO)均相沉淀物,由于SrSO和BaSeO的溶解度高于BaSO,几乎没有Sr/Se(VI)掺入。而基底附近的阳离子富集使局部溶液高度过饱和,通过成核在基底上形成了纳米级共沉淀物,由于SrSO和BaSeO相对于BaSO的界面能较低,有更多的Sr/Se(VI)掺入。这些新见解加深了我们对固 - 水界面处各种元素生物地球化学循环以及功能性纳米晶体可控合成的理解。