Thermal conductivity of sedimentary rocks in the Sichuan basin, Southwest China

Boning Tang,Chuanqing Zhu,Shengbiao Hu,Ming Xu,Tiange Chen

doi:10.1177/0144598718804902

Abstract

The optical scanning method was adopted to measure the thermal conductivities of 418 drill-core samples from 30 boreholes in Sichuan basin. All the measured thermal conductivities mainly range from 2.00 to 4.00 W/m K with a mean of 2.85 W/m K. For clastic rocks, the mean thermal conductivities of sandstone, mudstone, and shale are 3.06 ± 0.73, 2.57 ± 0.42, and 2.48 ± 0.33 W/m K, respectively; for carbonate rocks, the mean thermal conductivities of limestone and dolomite are 2.53 ± 0.44 and 3.55 ± 0.71 W/m K, respectively; for gypsum rocks, the mean thermal conductivity is 3.60 ± 0.64 W/m K. The thermal conductivities of sandstone and mudstone increase with burial depth and stratigraphic age, but this trend is not obvious for limestone and dolomite. Compared with other basins, the thermal conductivities of sandstone and mudstone in Sichuan basin are distinctly higher, while the thermal conductivities of limestone are close to Tarim basin. The content of mineral composition such as quartz is the principal factor that results in thermal conductivity of rocks differing from normal value. In situ thermal conductivity of sandstones was corrected with the consideration of water saturation. Finally, a thermal conductivity column of sedimentary formation of the Sichuan basin was given out, which can provide thermal conductivity references for the research of deep geothermal field and lithospheric thermal structure in the basin.

Highlights

Thermophysical property of rock is a fundamental parameter in the research of geothermics of sedimentary basin
The capacity of heat transmission shown by thermal conductivity which directly affects distribution of geothermal field and deep thermal structure is the key issue in the research of thermal regime in the sedimentary basin (Miao et al, 2013; Ray et al, 2007)
In contrast with the conclusion proposed by Liu et al (2011) that limestone samples of the Tarim basin are basically bioclastic calcarenite with abundant biogenic materials, we found that there are a mass of biogenic materials and argillaceous materials in limestone of the Sichuan basin (Deng et al, 1982; Xu et al, 2013; Zhou et al, 2009), and it seems that the mineral composition of limestone in the Sichuan basin is similar to that in the Tarim basin

Summary

Introduction

Thermophysical property of rock is a fundamental parameter in the research of geothermics of sedimentary basin. Keywords Thermal conductivity, correction for water saturation, mineral composition, sedimentary rocks, Sichuan basin

Results

Conclusion