{"title":"In situ High-Temperature Experiments","authors":"D. Neuville, L. Hennet, P. Florian, D. Ligny","doi":"10.2138/RMG.2013.78.19","DOIUrl":null,"url":null,"abstract":"When Frank Hawthorne (1988) edited the Reviews in Mineralogy volume on “Spectroscopic Methods in Mineralogy and Geology,” all the experiments presented had been performed at room pressure and room temperature because, at that time, vibrational and X-ray techniques were already quite difficult at ambient conditions so more sophisticated sample environments were not a priority. However, it has now become somewhat easier to perform experiments in situ at high temperatures (HT), high pressures (HP) or under combined high temperature and pressure (HP-HT). These types of experiments are becoming routine on crystals, glasses and liquids (see Shen and Wang 2014, this volume). High-temperature experiments are important because most of the physical properties of high-temperature liquids, such as magmas and melts, are related to their atomic structure. Consequently, it is important to probe the local environment of the atoms in the sample under the conditions noted above (e.g., HT). However, at very high temperatures (~≥ 1200 °C) it is difficult to use conventional furnaces because of a number of experimental difficulties associated with their use: temperature regulation, thermal inertia and spatial obstruction of the sample. Due to the progress made in the development of lasers and X-ray, neutron and magnetic sources it is now possible to perform experiments in situ at HT, HP and HT-HP on samples of millimeter or micron size. In this chapter, we discuss some of these noncommercial methods used in performing experiments at HT, and outline the best choices for heating systems with regard to the experimental requirements. Different commercial heating systems are available such as the systems available from Linkam® ( http://www.linkam.co.uk/ ) or Leica® ( http://www.leica-microsystems.com/ ) for example. These two systems are well adapted to performing experiments at HT including Raman (Neuville et al. 2014, this volume) and IR spectroscopy (Della Ventura et al. 2014, this volume) …","PeriodicalId":49624,"journal":{"name":"Reviews in Mineralogy & Geochemistry","volume":"13 1","pages":"779-800"},"PeriodicalIF":0.0000,"publicationDate":"2014-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"23","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Reviews in Mineralogy & Geochemistry","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.2138/RMG.2013.78.19","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 23
Abstract
When Frank Hawthorne (1988) edited the Reviews in Mineralogy volume on “Spectroscopic Methods in Mineralogy and Geology,” all the experiments presented had been performed at room pressure and room temperature because, at that time, vibrational and X-ray techniques were already quite difficult at ambient conditions so more sophisticated sample environments were not a priority. However, it has now become somewhat easier to perform experiments in situ at high temperatures (HT), high pressures (HP) or under combined high temperature and pressure (HP-HT). These types of experiments are becoming routine on crystals, glasses and liquids (see Shen and Wang 2014, this volume). High-temperature experiments are important because most of the physical properties of high-temperature liquids, such as magmas and melts, are related to their atomic structure. Consequently, it is important to probe the local environment of the atoms in the sample under the conditions noted above (e.g., HT). However, at very high temperatures (~≥ 1200 °C) it is difficult to use conventional furnaces because of a number of experimental difficulties associated with their use: temperature regulation, thermal inertia and spatial obstruction of the sample. Due to the progress made in the development of lasers and X-ray, neutron and magnetic sources it is now possible to perform experiments in situ at HT, HP and HT-HP on samples of millimeter or micron size. In this chapter, we discuss some of these noncommercial methods used in performing experiments at HT, and outline the best choices for heating systems with regard to the experimental requirements. Different commercial heating systems are available such as the systems available from Linkam® ( http://www.linkam.co.uk/ ) or Leica® ( http://www.leica-microsystems.com/ ) for example. These two systems are well adapted to performing experiments at HT including Raman (Neuville et al. 2014, this volume) and IR spectroscopy (Della Ventura et al. 2014, this volume) …
当Frank Hawthorne(1988)编辑矿物学评论卷“矿物学和地质学中的光谱方法”时,所介绍的所有实验都是在室温和常压下进行的,因为当时,振动和x射线技术在环境条件下已经相当困难,因此更复杂的样品环境不是优先考虑的。然而,现在在高温(HT)、高压(HP)或高温和高压组合(HP-HT)下进行原位实验变得更加容易。这些类型的实验正在成为晶体,玻璃和液体的常规(见Shen和Wang 2014,本卷)。高温实验很重要,因为大多数高温液体的物理性质,如岩浆和熔体,都与它们的原子结构有关。因此,在上述条件下(如高温)探测样品中原子的局部环境是很重要的。然而,在非常高的温度下(~≥1200°C),很难使用传统的炉,因为与它们的使用相关的一些实验困难:温度调节,热惯性和样品的空间阻塞。由于激光和x射线、中子和磁源的发展取得了进展,现在可以在高温、高温和高温-高温下对毫米或微米尺寸的样品进行原位实验。在本章中,我们将讨论在高温下进行实验时使用的一些非商业方法,并根据实验要求概述加热系统的最佳选择。不同的商业加热系统是可用的,例如Linkam®(http://www.linkam.co.uk/)或Leica®(http://www.leica-microsystems.com/)提供的系统。这两个系统非常适合在高温下进行实验,包括拉曼(Neuville et al. 2014,本卷)和红外光谱(Della Ventura et al. 2014,本卷)……
期刊介绍:
RiMG is a series of multi-authored, soft-bound volumes containing concise reviews of the literature and advances in theoretical and/or applied mineralogy, crystallography, petrology, and geochemistry. The content of each volume consists of fully developed text which can be used for self-study, research, or as a text-book for graduate-level courses. RiMG volumes are typically produced in conjunction with a short course but can also be published without a short course. The series is jointly published by the Mineralogical Society of America (MSA) and the Geochemical Society.