stands for Digital Object Identifier
and is the unique identifier for objects on the internet. It can be used to create persistent link and to cite articles.
Using DOI as a persistent link
To create a persistent link, add「http://dx.doi.org/」
before a DOI.
For instance, if the DOI of an article is 10.5297/ser.1201.002 , you can link persistently to the article by entering the following link in your browser: http://dx.doi.org/ 10.5297/ser.1201.002 。
The DOI link will always direct you to the most updated article page no matter how the publisher changes the document's position, avoiding errors when engaging in important research.
Cite a document with DOI
When citing references, you should also cite the DOI if the article has one. If your citation guideline does not include DOIs, you may cite the DOI link.
DOIs allow accurate citations, improve academic contents connections, and allow users to gain better experience across different platforms. Currently, there are more than 70 million DOIs registered for academic contents. If you want to understand more about DOI, please visit airiti DOI Registration （ doi.airiti.com ） 。
- Abbott, G. D., G. Y. Wang, T. I. Eglinton, A. K. Home, and G. S. Petch, 1990: The kinetics of sterane biological marker release and degradation processes during the hydrous pyrolysis of vitrinite kerogen. Geochim. Cosmochim. Acta., 54, 2451-2461.
- Barker, C. E., 1991: Implications for organic maturation studies of evidence for a geologically rapid increase and stabilization of vitrinte reflectance at peak temperature: Cerro Prieto geothermal system, Mexico. AAPG Bull., 75, 1852-1863.
- Behar, F., and P. G. Hatcher, 1995: Artificial coalification of a fossil wood from brown coal by confined system pyrolysis. Energy & Fuels., 9, 984–994.
- Behar, F., M. D. Lewan, F. Lorant, and M. Vandenbroucke, 2003: Comparison of artificial maturation of lignite in hydrous and nonhydrous conditions Org. Geochem., 34, 575–600.
- Behar, F., S. Kressmann, J. L. Rudkiewicz, and M. Vandenbroucke, 1991: Experimental simulation in a confined system and kinetic modelling of kerogen and oil cracking. Org. Geochem., 19, 173–189.
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