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鸟粪石压电性质的首个实验证据。

First experimental evidence of the piezoelectric nature of struvite.

作者信息

Prywer Jolanta, Kruszyński Rafał, Świątkowski Marcin, Soszyński Andrzej, Kajewski Dariusz, Roleder Krystian

机构信息

Institute of Physics, Lodz University of Technology, ul. Wólczańska 219, 90-924, Łódź, Poland.

Institute of General and Ecological Chemistry, Lodz University of Technology, Żeromskiego 116, 90-924, Łódź, Poland.

出版信息

Sci Rep. 2021 Jul 21;11(1):14860. doi: 10.1038/s41598-021-94410-2.

DOI:10.1038/s41598-021-94410-2
PMID:34290345
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8295349/
Abstract

In this paper, we present the first experimental evidence of the piezoelectric nature of struvite (MgNHPO·6HO). Using a single diffusion gel growth technique, we have grown struvite crystals in the form of plane parallel plates. For struvite crystals of this shape, we measured the piezoelectric coefficients d and d. We have found that at room temperature the value of piezoelectric coefficient d is 3.5 pm/V, while that of d is 4.7 pm/V. These values are comparable with the values for other minerals. Struvite shows stable piezoelectric properties up to the temperature slightly above 350 K, for the heating rate of 0.4 K/min. For this heating rate, and above this temperature, the thermal decomposition of struvite begins, which, consequently, leads to its transformation into dittmarite with the same non-centrosymmetric symmetry as in case of struvite. The struvite-dittmarite transformation temperature is dependent on the heating rate. The higher the heating rate, the higher the temperature of this transformation. We have also shown that dittmarite, like struvite exhibits piezoelectric properties.

摘要

在本文中,我们展示了鸟粪石(MgNH₄PO₄·6H₂O)压电性质的首个实验证据。使用单扩散凝胶生长技术,我们生长出了平行平板状的鸟粪石晶体。对于这种形状的鸟粪石晶体,我们测量了压电系数d₃₁和d₃₃。我们发现,在室温下,压电系数d₃₁的值为3.5皮米/伏,而d₃₃的值为4.7皮米/伏。这些值与其他矿物的值相当。对于0.4开尔文/分钟的升温速率,鸟粪石在略高于350 K的温度下仍表现出稳定的压电性能。在此升温速率及高于此温度时,鸟粪石开始热分解,进而导致其转变为迪特马石,其具有与鸟粪石相同的非中心对称对称性。鸟粪石 - 迪特马石的转变温度取决于升温速率。升温速率越高,该转变的温度越高。我们还表明,迪特马石与鸟粪石一样具有压电性能。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/835ddad98681/41598_2021_94410_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/b8be13f7330e/41598_2021_94410_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/6f0ca32f8f29/41598_2021_94410_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/c96d1271b94d/41598_2021_94410_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/8162ef1288fd/41598_2021_94410_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/b662f24ab697/41598_2021_94410_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/f9e7369fd76f/41598_2021_94410_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/cec990ec9408/41598_2021_94410_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/b88dc08798a8/41598_2021_94410_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/ab1981fa3ee8/41598_2021_94410_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/e326528ff566/41598_2021_94410_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/599bcc69802f/41598_2021_94410_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/835ddad98681/41598_2021_94410_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/b8be13f7330e/41598_2021_94410_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/6f0ca32f8f29/41598_2021_94410_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/c96d1271b94d/41598_2021_94410_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/8162ef1288fd/41598_2021_94410_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/b662f24ab697/41598_2021_94410_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/f9e7369fd76f/41598_2021_94410_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/cec990ec9408/41598_2021_94410_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/b88dc08798a8/41598_2021_94410_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/ab1981fa3ee8/41598_2021_94410_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/e326528ff566/41598_2021_94410_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/599bcc69802f/41598_2021_94410_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a13/8295349/835ddad98681/41598_2021_94410_Fig12_HTML.jpg

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本文引用的文献

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Struvite formation and decomposition characteristics for ammonia and phosphorus recovery: A review of magnesium-ammonia-phosphate interactions.用于氨和磷回收的鸟粪石形成与分解特性:镁-氨-磷酸盐相互作用综述
Chemosphere. 2018 Mar;194:504-514. doi: 10.1016/j.chemosphere.2017.12.004. Epub 2017 Dec 5.
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Nitrogen and Phosphorus Harvesting from Human Urine Using a Stripping, Absorption, and Precipitation Process.利用汽提、吸收和沉淀工艺从人尿中回收氮和磷。
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Phosphate enhance recovery from wastewater by mechanism analysis and optimization of struvite settleability in fluidized bed reactor.
通过机理分析和优化流化床反应器中鸟粪石的沉降性能,磷酸盐可提高废水的回收率。
Sci Rep. 2016 Aug 30;6:32215. doi: 10.1038/srep32215.
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Sci Rep. 2015 May 11;5:10183. doi: 10.1038/srep10183.
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Phosphorus recovery from wastewater by struvite crystallization: property of aggregates.通过鸟粪石结晶从废水中回收磷:聚集体的性质。
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Kinetics of struvite to newberyite transformation in the precipitation system MgCl2-NH4H2PO4NaOH-H2O.MgCl₂-NH₄H₂PO₄-NaOH-H₂O沉淀体系中鸟粪石向磷酸二氢镁转化的动力学
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