2023, 42(2) 343-350 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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Keywords
 airborne gravity gradient measurement
reference gradient field
surface continuation
gradient transformation
Authors
TENG Minqiang 1
HE Haoyuan 2
LI Tonglin 2
KANG Xinze 2
PubMed
Article by TM1
Article by He H2
Article by Li T2
Article by Kang X2

 Study on establishing methods of reference field for airborne gravity gradient test

 TENG Minqiang 1 , HE Haoyuan 2 , LI Tonglin 2 , KANG Xinze 2

 1. Heilongjiang Institute of Geophysical and Geochemical Exploration, Bureau of Geology and Mineral Resource of Heilongjiang Province, Harbin 150036, China; 

2.College of Geo?exploration Science and Technology, Jilin University, Changchun 130026, China

Abstract

 The measurement of airborne gravity gradient is affected by factors such as airflow in the flight area and aircraft acceleration, so it is necessary to select a height with weak anomaly for compensation flight. In order to evaluate the measurement effect of gradiometer and determine the compensation flight altitude, it is necessary to es? tablish the standard gradient fields of the corresponding altitudes as references. For this reason, the method of es? tablishing reference field by surface continuation and gradient transformation using ground gravity data is studied first, and the model verification is carried out. Then, using this method, the reference fields of an airborne gravity gradient test area in Jilin??Heilongjiang at the flight altitudes of precision test and compensation are established, and the feasibility of selecting the compensation flight altitude is determined. In addition, the gravity gradient field es? tablished by continuation and transformation is compared with the forward modeling field of undulating terrain. The results show that the reference fields established by the two methods can both be used to evaluate the measurement accuracy of the gradiometer and select the compensation flight altitude.

Keywords  airborne gravity gradient measurement   reference gradient field   surface continuation   gradient transformation  
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