RETRACTION: Hydrate Dissociation Model with Time Fractional Derivative

IF 1.2 4区地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS

Geofluids Pub Date : 2026-04-10 DOI:10.1155/gfl/9815168

Geofluids

引用次数: 0

Abstract

RETRACTION: X. Fang, H. Lian, W. Luo, M. Liu, C. Chen, and Q. Wang, “Hydrate Dissociation Model with Time Fractional Derivative,” Geofluids 2022, no. 1 (2022): 5598287, https://doi.org/10.1155/2022/5598287.

The above article, published online on 12 April 2022 in Wiley Online Library (wileyonlinelibrary.com), has been retracted by agreement between the Journal Editor-in-Chief, Umberta Tinivella and John Wiley & Sons Ltd. The retraction has been agreed due to unattributed overlap between this article and [1].

Several attempts by the journal to contact the authors have not resulted in a reply.

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缩回：水合物解离模型与时间分数导数

引用本文：方晓明，刘明明，李辉，罗伟，“基于时间分数导数的水合物解离模型”，《地球物理学报》，2012，第1期。1 (2022): 5598287, https://doi.org/10.1155/2022/5598287.The上述文章于2022年4月12日在线发表在Wiley在线图书馆（wileyonlinelibrary.com）上，经杂志主编Umberta Tinivella和John Wiley & & Sons Ltd.协议撤回。由于这篇文章与b[1]之间存在未署名的重叠，因此已同意撤回。该杂志几次试图联系作者，但都没有得到回复。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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来源期刊

Geofluids 地学-地球化学与地球物理

CiteScore

2.80

自引率

17.60%

发文量

835

期刊介绍： Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.