Severity: Warning
Message: file_get_contents(https://...@pubfacts.com&api_key=b8daa3ad693db53b1410957c26c9a51b4908&a=1): Failed to open stream: HTTP request failed! HTTP/1.1 429 Too Many Requests
Filename: helpers/my_audit_helper.php
Line Number: 176
Backtrace:
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 176
Function: file_get_contents
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 250
Function: simplexml_load_file_from_url
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 1034
Function: getPubMedXML
File: /var/www/html/application/helpers/my_audit_helper.php
Line: 3152
Function: GetPubMedArticleOutput_2016
File: /var/www/html/application/controllers/Detail.php
Line: 575
Function: pubMedSearch_Global
File: /var/www/html/application/controllers/Detail.php
Line: 489
Function: pubMedGetRelatedKeyword
File: /var/www/html/index.php
Line: 316
Function: require_once
In this study, we focused on the effect of pressure on the crystal structures of dioxides of group 14 elements, SiO, GeO, and CO. Systematic searches for their crystal structures using the artificial force induced reaction method generated 219 and 147, 102 and 63, and 148 and 76 structures for SiO, GeO, and CO, respectively, at 1 and 10 atm. At 1 atm, cristobalite-like, quartz, anatase-like, and stishovite were stable structures for SiO and GeO. At 10 atm, structures of stishovite and CaCl type were relatively stable for SiO and GeO. At 1 atm of CO, molecular crystals were the most stable, whereas, quartz-like and cristobalite-like structures were obtained as stable structures at 10 atm. We discuss these pressure dependent structural variations systematically using the obtained structural dataset.
Download full-text PDF |
Source |
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9054535 | PMC |
http://dx.doi.org/10.1039/d0ra03359f | DOI Listing |
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