Analysis of Vertical Deformation in Shaanxi Area, China

YANG Hongshan; NIE Jianliang

doi:10.13203/j.whugis20200149

Volume 42 Issue 11

Nov. 2022

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Geomatics and Information Science of Wuhan University > 2022 > 47(11): 1854-1859. > DOI: 10.13203/j.whugis20200149

YANG Hongshan, NIE Jianliang. Analysis of Vertical Deformation in Shaanxi Area, China[J]. Geomatics and Information Science of Wuhan University, 2022, 47(11): 1854-1859. DOI: 10.13203/j.whugis20200149

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Analysis of Vertical Deformation in Shaanxi Area, China

YANG Hongshan^1,,
NIE Jianliang^1, ,

1.
Shaanxi Bureau of Surveying, Mapping and Geoinformation, Xi'an 710054, China

Funds:

The National Natural Science Foundation of China 41774004

The National Natural Science Foundation of China 41574003

The National Natural Science Foundation of China 41904040

the Technological Innovation of Shaanxi Bureau of Surveying, Mapping and Geoinformation 2020-4

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Author Bio:
YANG Hongshan, master, senior engineer, specializes in mapping geographic information management and services. E-mail: johnshx@sina.com
Corresponding author:
NIE Jianliang, PhD, senior engineer. E-mail: niejianliang@163.com
Received Date: April 07, 2020
Available Online: November 15, 2022
Published Date: November 04, 2022

Graphical Abstract

Abstract

Abstract

Objectives The vertical movement is obtained and analyzed with the different geodetic data of more than 40 years in Shaanxi area, China.
Methods Firstly, the adjustment result of the national first order level network in three periods is collected, the trend of 40 years is applied to describe the vertical movement as a whole which can show the uplift and downward of the crust, the data of the second order level network on the basis of the first order level points is adjusted, and the information with the higher resolution is obtained. Secondly, the other vertical information is collected from the result which includes global navigation satellite system (GNSS) network, crustal movement observation network of China and interferometric synthetic aperture radar (InSAR) result of the geography condition monitoring in Shaanxi area. Finally, the fusion result is computed with move fitting method.
Results Experimental result shows that the vertical movement of GNSS is consistent with the vertical movement of level on the whole.The uplift rate on the whole is about 4 mm/a in the north of Shaanxi area the maximum downward rate is 6 mm/a in Guanzhong plain, the uplift rate is about 3 mm/a in the south of Shaanxi area, and there is severe subsidence in the north of Shaanxi area and local area of Xi'an.
Conclusions From 1970 to 2018, a downward trend of vertical movement was shown in Guanzhong plain, and the uplift trend of vertical movement was displayed in mountains and plateaus around Guanzhong plain.
- vertical deformation,
- level,
- GNSS,
- land subsidence

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