Exciting news! We're transitioning to the Statewide California Earthquake Center. Our new website is under construction, but we'll continue using this website for SCEC business in the meantime. We're also archiving the Southern Center site to preserve its rich history. A new and improved platform is coming soon!

Comprehensive Study on Reservoir-induced Seismicity in the Xiaowan Reservoir, Yunnan Province, China

Wei Hua, Naichen Ke, & YAQIONG DAI

Published August 5, 2018, SCEC Contribution #8277, 2018 SCEC Annual Meeting Poster #071 (PDF)

Poster Image: 
The Xiaowan reservoir is located in the middle section of the Lancang River in the west of Yunnan province, China, and the Xiaowan Reservoir Digital Seismic Station Network (XRDSSN) had been in operation since 21 May 2005. Its filling operations took place in five phases, starting on December 16, 2008. The seismicity in the Xiaowan reservoir area after the impoundment has changed obviously with respect to the pre-impoundment. A notable increase in seismicity was only observed during the third filling phase, starting on July 15, 2010. Seismicity increase was mostly localized within two clusters, located to the northwest and west of the dam. Seismicity rates in these clusters showed a significant correlation with the water level increase, with the seismicity starting to increase when the water level reached the area covered by the two clusters, which additionally support they were induced by the reservoir impoundment. 3-D shear wave velocity images, measured by the local earthquake tomography method SIMUL2000, show that low-Vs anomalies after the impoundment can be found beneath and around the Lancang River and the Heihui River in the reservoir area, where the two clusters are located. It may be related to the water loading and unloading and water permeation. We further investigate source parameters for 44 pre-impoundment earthquakes and 164 post-impoundment earthquakes with ML≥2.0. Corner frequencies, seismic moments, and stress drops are obtained based on the spectral analysis of regional data, upon corrections for geometrical spreading, frequency-dependent Q, and site effects. Our results show that during the post-impoundment phase reservoir-induced seismicity (RIS) inside the two clusters have systematically lower stress drops with respect to those occurring at further distance, and surrounding natural tectonic earthquakes, by a factor of about two to three times, suggesting a possible source characteristic that differentiate reservoir-induced seismicity from natural tectonic earthquakes.

Hua, W., Ke, N., & DAI, Y. (2018, 08). Comprehensive Study on Reservoir-induced Seismicity in the Xiaowan Reservoir, Yunnan Province, China. Poster Presentation at 2018 SCEC Annual Meeting.

Related Projects & Working Groups