[1]SHI Wei,LI Yongsheng,OUYANG Zhaoguo,et al.Hydrochemical Characteristics in the North Segment of the Yilan-Yitong Fault[J].Journal of Seismological Research,2022,45(02):257-263.[doi:10.20015/j.cnki.ISSN1000-0666.2022.0024
]
Copy
Journal of Seismological Research[ISSN 1000-0666/CN 53-1062/P] Volume:
45
Number of periods:
2022 02
Page number:
257-263
Column:
Public date:
2022-05-20
- Title:
-
Hydrochemical Characteristics in the North Segment of the Yilan-Yitong Fault
- Author(s):
-
SHI Wei; LI Yongsheng; OUYANG Zhaoguo; HU Baohui; GAO Feng
-
(Heilongjiang Earthquake Agency,Harbin 150090,Heilongjiang,China)
-
- Keywords:
-
the Yilan-Yitong Fault; hydrochemical characteristics; isotope; underground water
- CLC:
-
P315.724
- DOI:
-
10.20015/j.cnki.ISSN1000-0666.2022.0024
- Abstract:
-
In this paper we analyze the hydrochemical composition and the composition of the isotopes of hydrogen and oxygen of 19 water samples collected at 4 observation stations for underground fluid and their neighbouring ponits in the north segement of the Yilan-Yitong Fault in Northeast China,and study the types and genesis of the groundwater in the fault zone.The results indicate that:① The water temperature at these sampling points ranges from 8.5 ℃ to 23.4 ℃.The total dissolved solids(TDS)of the water samples,all of which are low salinity water,ranges from 32 to 568 mg /L.②The water samples can be classified into 10 chemical types,and the water-rock reaction does not reach complete equilibrium.The sample at Tonghe station belongs to “partial equilibrium water” and feautures deep source.③The δD-value ranges from -100.24‰ to -65.46‰,and δ18O from -13.47‰ to -8.53‰,indicating that the recharge source of the samples is mainly atmospheric precipitation.