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通过中子衍射研究东欧Unionidae科淡水双壳贝类的全球晶体学织构。

Global Crystallographic Texture of Freshwater Bivalve Mollusks of the Unionidae Family from Eastern Europe Studied by Neutron Diffraction.

作者信息

Pakhnevich Alexey, Nikolayev Dmitry, Lychagina Tatiana, Balasoiu Maria, Ibram Orhan

机构信息

Borissiak Paleontological Institute, Russian Academy of Sciences, 117647 Moscow, Russia.

Frank Laboratory of Neutron Physics, Joint Institute for Nuclear Research, 141980 Dubna, Russia.

出版信息

Life (Basel). 2022 May 13;12(5):730. doi: 10.3390/life12050730.

DOI:10.3390/life12050730
PMID:35629397
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9147449/
Abstract

The crystallographic texture of the whole valves of bivalve mollusks from the family Unionidae Linnaeus, 1758 and Linnaeus, 1758 is studied using pole figures measured using neutron diffraction. The use of neutron diffraction, in contrast to X-rays, makes it possible to study the valves without destroying them. Thus, we can discuss the study of the global texture of the entire valve. It was revealed that the pole figures of aragonite in the valves repeat their shape. The pole density maxima for from the Danube Delta and the Gulf of Finland in the Baltic Sea, living at different salinities and temperatures, differs by 0.41 mrd. The maximum value of the crystallographic texture for from the Danube Delta was also measured (5.07 mrd). In terms of texture sharpness, it surpasses the shell of marine bivalve mollusks, which are partially or completely composed of aragonite. Although and Linnaeus, 1758 have different microstructures, their pole figures are very similar in isolines pattern, but differ in pole density maxima. No relationship was found between the crystallographic texture and the microstructure in . In addition, we report good qualitative agreement between aragonite X-ray pole figures of Lea, 1834 from the Czech river Luznice, and neutron pole figures of from the Danube Delta.

摘要

利用中子衍射测量的极图,对1758年林奈所定的蚌科双壳贝类整个瓣膜的晶体学织构进行了研究。与X射线不同,使用中子衍射可以在不破坏瓣膜的情况下对其进行研究。因此,我们可以讨论整个瓣膜的整体织构研究。结果表明,瓣膜中霰石的极图重复了它们的形状。来自多瑙河三角洲和波罗的海芬兰湾、生活在不同盐度和温度下的[具体物种未明确]的极密度最大值相差0.41毫弧度。还测量了来自多瑙河三角洲的[具体物种未明确]的晶体学织构的最大值(5.07毫弧度)。在织构清晰度方面,它超过了部分或完全由霰石组成的海洋双壳贝类的贝壳。虽然[具体物种未明确]和1758年林奈所定的[具体物种未明确]具有不同的微观结构,但它们的极图在等值线模式上非常相似,但极密度最大值不同。在[具体物种未明确]中未发现晶体学织构与微观结构之间的关系。此外,我们报告了来自捷克卢日尼采河的1834年利所定的[具体物种未明确]的霰石X射线极图与来自多瑙河三角洲的[具体物种未明确]的中子极图之间有良好的定性一致性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/ecce12dc8980/life-12-00730-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/2b7809b9af81/life-12-00730-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/f8667e2f77d7/life-12-00730-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/132bc5035480/life-12-00730-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/178598fa9783/life-12-00730-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/1504bb95c9bf/life-12-00730-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/0550e70e42ce/life-12-00730-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/ecce12dc8980/life-12-00730-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/2b7809b9af81/life-12-00730-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/f8667e2f77d7/life-12-00730-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/132bc5035480/life-12-00730-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/178598fa9783/life-12-00730-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/1504bb95c9bf/life-12-00730-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/0550e70e42ce/life-12-00730-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f4bf/9147449/ecce12dc8980/life-12-00730-g007.jpg

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本文引用的文献

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Ocean acidification impacts mussel control on biomineralisation.
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