Japan Geoscience Union Meeting 2016

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-TT Technology & Techniques

[S-TT52] Airborne surveys and monitoring of the Earth

Mon. May 23, 2016 9:00 AM - 10:30 AM A07 (APA HOTEL&RESORT TOKYO BAY MAKUHARI)

Convener:*Shigekazu Kusumoto(Graduate School of Science and Engineering for Research, University of Toyama), Shigeo Okuma(Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST)), Takao Koyama(Earthquake Research Institute, University of Tokyo), Yuji Mitsuhata(AdvancedIndustrial Science and Technology), Chair:Shigekazu Kusumoto(Graduate School of Science and Engineering for Research, University of Toyama), Shigeo Okuma(Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST)), Takao Koyama(Earthquake Research Institute, University of Tokyo), Yuji Mitsuhata(AdvancedIndustrial Science and Technology)

9:45 AM - 10:00 AM

[STT52-04] Influence of ground clearance on airborne gravity gradiometry survey

*Sho Aibe1, Atsushi Shirota1, Akihiko Chiba1, Hiroshi Yamaguchi2, Masato Fukuda3 (1.Sumiko Resources Exploration & Development Co., Ltd., 2.Fugro Japan Co., Ltd., 3.Japan Oil, Gas and Metals National Corporation)

Keywords:Airbornne Gravity Gradiometry, Vertical gravity gradient, Flight height

In geophysical surveys, increase in the distance between the sensors and the survey targets generally causes deterioration of resolution. Higher altitude above the ground level leads to degraded resolution in airborne surveys. While low-level flight is desirable for high resolution measurements, the ground clearance in actual surveys can increase to avoid rugged terrains, tall trees and high-rise structures including power lines. While the influence of higher clearance can be estimated by upward-continuing the gravity data to the flight surface, only a few case studies based on actual surveys are found.

Japan Oil, Gas and Metals National Corporation has been conducting airborne gravity gradiometer (AGG) surveys at the nominal terrain clearance of 120 m in the geothermal potential evaluation projects by using heliborne geophysical methods. We collected AGG data by varying the ground altitude at 120 m, 250 m, 500 m and 750m for the purpose of directly evaluating the influence of flight height on the vertical gravity gradient component (GDD) and vertical gravity (gD).

In the survey results, we observed a significant loss in the resolution of GDD due to the increased flight height, compared with that of gD. We plan to compare the measured results at each altitude with the calculated values by upward continuation of GDD and gD at 120m.