Rock heat production and its contribution to terrestrial heat flow in the Northern Songliao Basin, Northeast China.

Saved in:
Bibliographic Details
Title: Rock heat production and its contribution to terrestrial heat flow in the Northern Songliao Basin, Northeast China.
Authors: Fu, Xiuli1,2,3 (AUTHOR), Li, Xiao4,5 (AUTHOR), Zhu, Chuanqing4,5 (AUTHOR) zhucq@cup.edu.cn, Su, Yangxin2,3 (AUTHOR), Cui, Kunning2,3 (AUTHOR), Meng, Qi-an1,2 (AUTHOR)
Source: Journal of Radioanalytical & Nuclear Chemistry. Aug2024, Vol. 333 Issue 8, p3751-3765. 15p.
Subjects: Terrestrial heat flow, Radioactive elements, Columns
Abstract: The heat production rates of different rocks in the northern Songliao Basin were analyzed by measuring the contents of radioactive heat-producing elements (i.e., U, Th, and K) in the rock samples. U. Th and K have different heat generation contributions, with the contribution of U being greater than those of Th and K. The average heat production rate of sedimentary layers in the northern Songliao Basin was observed to be 1.54–1.91 μW/m3. Finally, this study developed a heat production column for the sedimentary layers in the northern Songliao Basin, which provided essential parameters for investigating the lithospheric thermal structure of this area. [ABSTRACT FROM AUTHOR]
Copyright of Journal of Radioanalytical & Nuclear Chemistry is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
Database: Engineering Source
Full text is not displayed to guests.
Description
Abstract:The heat production rates of different rocks in the northern Songliao Basin were analyzed by measuring the contents of radioactive heat-producing elements (i.e., U, Th, and K) in the rock samples. U. Th and K have different heat generation contributions, with the contribution of U being greater than those of Th and K. The average heat production rate of sedimentary layers in the northern Songliao Basin was observed to be 1.54–1.91 μW/m3. Finally, this study developed a heat production column for the sedimentary layers in the northern Songliao Basin, which provided essential parameters for investigating the lithospheric thermal structure of this area. [ABSTRACT FROM AUTHOR]
ISSN:02365731
DOI:10.1007/s10967-024-09515-5