Seismically induced changes in groundwater levels and temperatures following the ML5.8 (ML5.1) Gyeongju earthquake in South Korea
Hydrogeological responses to earthquakes such as changes in groundwater level, temperature, and chemistry, have been observed for several decades. This study examines behavior associated with M L 5.8 and M L 5.1 earthquakes that occurred on 12 September 2016 near Gyeongju, a city located on the sout...
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Published in | Hydrogeology journal Vol. 29; no. 4; pp. 1679 - 1689 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
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Berlin/Heidelberg
Springer Berlin Heidelberg
01.06.2021
Springer Nature B.V |
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Abstract | Hydrogeological responses to earthquakes such as changes in groundwater level, temperature, and chemistry, have been observed for several decades. This study examines behavior associated with M
L
5.8 and M
L
5.1 earthquakes that occurred on 12 September 2016 near Gyeongju, a city located on the southeast coast of the Korean peninsula. The M
L
5.8 event stands as the largest recorded earthquake in South Korea since the advent of modern recording systems. There was considerable damage associated with the earthquakes and many aftershocks. Records from monitoring wells located about 135 km west of the epicenter displayed various patterns of change in both water level and temperature. There were transient-type, step-like-type (up and down), and persistent-type (rise and fall) changes in water levels. The water temperature changes were of transient, shift-change, and tendency-change types. Transient changes in the groundwater level and temperature were particularly well developed in monitoring wells installed along a major boundary fault that bisected the study area. These changes were interpreted as representing an aquifer system deformed by seismic waves. The various patterns in groundwater level and temperature, therefore, suggested that seismic waves impacted the fractured units through the reactivation of fractures, joints, and microcracks, which resulted from a pulse in fluid pressure. This study points to the value of long-term monitoring efforts, which in this case were able to provide detailed information needed to manage the groundwater resources in areas potentially affected by further earthquakes. |
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AbstractList | Hydrogeological responses to earthquakes such as changes in groundwater level, temperature, and chemistry, have been observed for several decades. This study examines behavior associated with M
L
5.8 and M
L
5.1 earthquakes that occurred on 12 September 2016 near Gyeongju, a city located on the southeast coast of the Korean peninsula. The M
L
5.8 event stands as the largest recorded earthquake in South Korea since the advent of modern recording systems. There was considerable damage associated with the earthquakes and many aftershocks. Records from monitoring wells located about 135 km west of the epicenter displayed various patterns of change in both water level and temperature. There were transient-type, step-like-type (up and down), and persistent-type (rise and fall) changes in water levels. The water temperature changes were of transient, shift-change, and tendency-change types. Transient changes in the groundwater level and temperature were particularly well developed in monitoring wells installed along a major boundary fault that bisected the study area. These changes were interpreted as representing an aquifer system deformed by seismic waves. The various patterns in groundwater level and temperature, therefore, suggested that seismic waves impacted the fractured units through the reactivation of fractures, joints, and microcracks, which resulted from a pulse in fluid pressure. This study points to the value of long-term monitoring efforts, which in this case were able to provide detailed information needed to manage the groundwater resources in areas potentially affected by further earthquakes. Hydrogeological responses to earthquakes such as changes in groundwater level, temperature, and chemistry, have been observed for several decades. This study examines behavior associated with ML 5.8 and ML 5.1 earthquakes that occurred on 12 September 2016 near Gyeongju, a city located on the southeast coast of the Korean peninsula. The ML 5.8 event stands as the largest recorded earthquake in South Korea since the advent of modern recording systems. There was considerable damage associated with the earthquakes and many aftershocks. Records from monitoring wells located about 135 km west of the epicenter displayed various patterns of change in both water level and temperature. There were transient-type, step-like-type (up and down), and persistent-type (rise and fall) changes in water levels. The water temperature changes were of transient, shift-change, and tendency-change types. Transient changes in the groundwater level and temperature were particularly well developed in monitoring wells installed along a major boundary fault that bisected the study area. These changes were interpreted as representing an aquifer system deformed by seismic waves. The various patterns in groundwater level and temperature, therefore, suggested that seismic waves impacted the fractured units through the reactivation of fractures, joints, and microcracks, which resulted from a pulse in fluid pressure. This study points to the value of long-term monitoring efforts, which in this case were able to provide detailed information needed to manage the groundwater resources in areas potentially affected by further earthquakes. |
Author | Kim, Yongje Moon, Sang-Ho Kim, Yongcheol Jeong, Dan Bi Lee, Jae Min Ha, Kyoochul Lee, Soo-Hyoung |
Author_xml | – sequence: 1 givenname: Soo-Hyoung surname: Lee fullname: Lee, Soo-Hyoung organization: Korea Institute of Geoscience and Mineral Resources – sequence: 2 givenname: Jae Min surname: Lee fullname: Lee, Jae Min organization: Korea Institute of Geoscience and Mineral Resources – sequence: 3 givenname: Sang-Ho surname: Moon fullname: Moon, Sang-Ho organization: Korea Institute of Geoscience and Mineral Resources – sequence: 4 givenname: Kyoochul surname: Ha fullname: Ha, Kyoochul organization: Korea Institute of Geoscience and Mineral Resources – sequence: 5 givenname: Yongcheol surname: Kim fullname: Kim, Yongcheol organization: Korea Institute of Geoscience and Mineral Resources – sequence: 6 givenname: Dan Bi surname: Jeong fullname: Jeong, Dan Bi organization: Korea Institute of Geoscience and Mineral Resources – sequence: 7 givenname: Yongje orcidid: 0000-0002-8463-5374 surname: Kim fullname: Kim, Yongje email: yjkim@kigam.re.kr organization: Korea Institute of Geoscience and Mineral Resources |
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CitedBy_id | crossref_primary_10_1088_1755_1315_1091_1_012032 crossref_primary_10_1108_OHI_08_2023_0191 crossref_primary_10_1007_s00477_024_02734_y crossref_primary_10_2113_2022_7115985 crossref_primary_10_1016_j_gsd_2024_101195 crossref_primary_10_3390_w13172448 |
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DocumentTitle_FL | Changements d’origine sismique intervenus dans les niveaux et les températures des eaux souterraines à la suite du séisme ML5.8 (ML5.1) de Gyeongju en Corée du Sud |
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SubjectTerms | Aquatic Pollution Aquifer systems Aquifers Earth and Environmental Science Earth Sciences Earthquake damage Earthquakes Fluid pressure Fractures Geology Geophysics/Geodesy Groundwater Groundwater chemistry Groundwater levels Groundwater resources Hydrogeology Hydrology/Water Resources Information management Joints (timber) Microcracks Monitoring P-waves Seismic response Seismic waves Temperature changes Waste Water Technology Water level fluctuations Water levels Water Management Water Pollution Control Water Quality/Water Pollution Water temperature |
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Title | Seismically induced changes in groundwater levels and temperatures following the ML5.8 (ML5.1) Gyeongju earthquake in South Korea |
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