Next Article in Journal
Duration of Hydrothermal Alteration and Mineralization of the Don Manuel Porphyry Copper System, Central Chile
Next Article in Special Issue
Raman and Photoluminescence Mapping of Gem Materials
Previous Article in Journal
An Application of Simultaneous Stochastic Optimization at a Large Open-Pit Gold Mining Complex under Supply Uncertainty
Previous Article in Special Issue
New Insights for Gem-Quality Mn-Bearing Diopside-Omphacite, Violane Variety, from Saint Marcel (Val D’Aosta, Italy): Its Trace Elements and Spectroscopic Characterization
 
 
Article
Peer-Review Record

Silicon-Oxygen Region Infrared and Raman Analysis of Opals: The Effect of Sample Preparation and Measurement Type

Minerals 2021, 11(2), 173; https://doi.org/10.3390/min11020173
by Neville J. Curtis 1,2, Jason R. Gascooke 2,* and Allan Pring 2,*
Reviewer 1: Anonymous
Reviewer 2: Anonymous
Reviewer 3: Anonymous
Minerals 2021, 11(2), 173; https://doi.org/10.3390/min11020173
Submission received: 27 November 2020 / Revised: 29 January 2021 / Accepted: 2 February 2021 / Published: 7 February 2021
(This article belongs to the Special Issue Gemstone Analysis by Spectroscopy and Microscopy)

Round 1

Reviewer 1 Report

Reviewer comments

Minerals-1035164 by Neville J. Curtis and co-authors: Silicon-oxygen region infra-red and Raman analysis of opals: the effect of sample preparation and measurement type  

 

Dear authors and editor, thank you for the opportunity to review this manuscript about advanced spectroscopic methods used to characterize a variety of opals. With this manuscript the authors provide a well-illustrated extensive dataset for opaline materials, extending their previous study on, for example, opal XRD and Raman spectroscopy characteristics. The text is well-written and refer to the relevant literature. The order and structure of the paragraphs is reasonable and the figures are well-chosen and relevant. In conclusion, this is an excellent piece of work. I am pleased to recommend it for acceptance after minor amendments.

 

Abstract: L22-23: X-ray powder diffraction.

 

General remark: Use the terms peak or band consistently. They are not synonymous. For XRD it should be peak. For IR and Raman spectra it should be band. This must be corrected throughout the entire manuscript.

 

L36 (and, e.g., 58, 236): “POC arises if the lepispheres in opal-AG..”

            The “particles” in opal-AG are spheres. Lepispheres are observed in opal-CT.

 

L34 (and, for example, L47 and 548): low/α-cristobalite

 

L39-41: “Etching of opal-AG… is  not  required  to  show  the arrangement,  uniformity  and  size  of  the  spheres.”. 

 

Figure 1c actually appears to be the only unetched sample showing individual spheres. The others show ordered/disordered pores in a more or less homogeneous mass. Maybe the sentence in L39-41 could be a little adjusted accordingly.

 

L112: Spectra instead of samples.

 

L113: Band instead of peak.

 

L158-159: “XRD patterns were collected as before [7].” There is enough space in the manuscript to include at least one or two sentences about the measurement conditions. This should include the cathode material, step size, etc.

 

L236-239: What is the detection limit for Na and K, and what do you mean with cementing medium? The silica cementing the spheres?

 

L260: “..while the those..”. Delete “the”.

 

L347: “than” instead of “that”.

 

L628-629: “Mineral impurities such as clays or other minerals are again unlikely to be a factor as they are not seen in the XRD patterns.”

Keep in mind that the XRD detection limit is about 1 vol.%.

 

L1086: Do you mean 42°2θ? What is the wavelength used here?

Author Response

Please see attachment

Author Response File: Author Response.docx

Reviewer 2 Report

Please see attachment below

Comments for author File: Comments.pdf

Author Response

Please see attachment below.

Author Response File: Author Response.pdf

Reviewer 3 Report

Curtis et al. provide a detailed set of diffuse reflectance and ATR IR spectra, Raman spectra, and XRD patterns of a variety of natural opals (opal-A, opal-CT, and opal-C) to better describe the spectral characteristics of opals and their structures. This manuscript will be a useful reference to those in the scientific community who study any variety of amorphous or paracrystalline silica using spectral techniques. The methodology and data presented are sound. I have a few minor comments and edits in the attached document. I recommend this manuscript be published after these minor comments and edits are addressed.

Comments for author File: Comments.pdf

Author Response

Please see the attachment

Author Response File: Author Response.docx

Back to TopTop