QUALITY INVESTIGATION OF GRAVITY DATA FROM AIRBORNE GRAVIMETRY MEASUREMENT USING DOWNWARD CONTINUATION PROCESS IN KALIMANTAN REGION

Indonesia needs a high-quality geoid as a vertical measurement reference. Geoid is built on the geoid undulation value of the reference ellipsoid. The calculation of the undulation value uses the basic principle of the Stokes formulation which requires gravity data on the geoid surface. The gravi...

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Main Author: Ilfiyaningrum, Alfita
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/43960
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:43960
spelling id-itb.:439602019-10-01T08:54:55ZQUALITY INVESTIGATION OF GRAVITY DATA FROM AIRBORNE GRAVIMETRY MEASUREMENT USING DOWNWARD CONTINUATION PROCESS IN KALIMANTAN REGION Ilfiyaningrum, Alfita Indonesia Theses airborne gravimetry, gravity, cross-over analysis, downward continuation, fast-fourier transform INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/43960 Indonesia needs a high-quality geoid as a vertical measurement reference. Geoid is built on the geoid undulation value of the reference ellipsoid. The calculation of the undulation value uses the basic principle of the Stokes formulation which requires gravity data on the geoid surface. The gravity data must be of good quality, which has high accuracy and resolution. Airborne gravimetry can produce data that has high-density. However, acquisitions made in the air, not sticking to objects became a problem in this study. So we need a method to reduce data to the reference surface called downward continuation. In this research, gravity data quality control is carried out before and after the downward process using the fast-fourier transform method. This method performs downward continuation in the frequency domain of data, from the average flight height to the reference surface, the ellipsoid WGS1984. From the quality test results before DWC, the cross-over sample values were found in the range of 0-15 mgal. Two DWC methods are used, namely the RCR and non-RCR steps. RCR is a method that involves the process of removing global and terrain contributions before DWC and adding them back after DWC. Between RCR and Non-RCR methods produce the same results both spectral content and spatial patterns. So that for the processing of gravity disturbance data in the Kalimantan region the effect of the RCR method is not dominant in the DWC results. After comparing with another results, BIG and EGM2008, They have different results. All three results differ greatly with the EGM2008 value. In testing data quality before and after DWC, all results show that DWC increased power data in the frequency domain. There is shows that the DWC process produces data with stronger signals text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description Indonesia needs a high-quality geoid as a vertical measurement reference. Geoid is built on the geoid undulation value of the reference ellipsoid. The calculation of the undulation value uses the basic principle of the Stokes formulation which requires gravity data on the geoid surface. The gravity data must be of good quality, which has high accuracy and resolution. Airborne gravimetry can produce data that has high-density. However, acquisitions made in the air, not sticking to objects became a problem in this study. So we need a method to reduce data to the reference surface called downward continuation. In this research, gravity data quality control is carried out before and after the downward process using the fast-fourier transform method. This method performs downward continuation in the frequency domain of data, from the average flight height to the reference surface, the ellipsoid WGS1984. From the quality test results before DWC, the cross-over sample values were found in the range of 0-15 mgal. Two DWC methods are used, namely the RCR and non-RCR steps. RCR is a method that involves the process of removing global and terrain contributions before DWC and adding them back after DWC. Between RCR and Non-RCR methods produce the same results both spectral content and spatial patterns. So that for the processing of gravity disturbance data in the Kalimantan region the effect of the RCR method is not dominant in the DWC results. After comparing with another results, BIG and EGM2008, They have different results. All three results differ greatly with the EGM2008 value. In testing data quality before and after DWC, all results show that DWC increased power data in the frequency domain. There is shows that the DWC process produces data with stronger signals
format Theses
author Ilfiyaningrum, Alfita
spellingShingle Ilfiyaningrum, Alfita
QUALITY INVESTIGATION OF GRAVITY DATA FROM AIRBORNE GRAVIMETRY MEASUREMENT USING DOWNWARD CONTINUATION PROCESS IN KALIMANTAN REGION
author_facet Ilfiyaningrum, Alfita
author_sort Ilfiyaningrum, Alfita
title QUALITY INVESTIGATION OF GRAVITY DATA FROM AIRBORNE GRAVIMETRY MEASUREMENT USING DOWNWARD CONTINUATION PROCESS IN KALIMANTAN REGION
title_short QUALITY INVESTIGATION OF GRAVITY DATA FROM AIRBORNE GRAVIMETRY MEASUREMENT USING DOWNWARD CONTINUATION PROCESS IN KALIMANTAN REGION
title_full QUALITY INVESTIGATION OF GRAVITY DATA FROM AIRBORNE GRAVIMETRY MEASUREMENT USING DOWNWARD CONTINUATION PROCESS IN KALIMANTAN REGION
title_fullStr QUALITY INVESTIGATION OF GRAVITY DATA FROM AIRBORNE GRAVIMETRY MEASUREMENT USING DOWNWARD CONTINUATION PROCESS IN KALIMANTAN REGION
title_full_unstemmed QUALITY INVESTIGATION OF GRAVITY DATA FROM AIRBORNE GRAVIMETRY MEASUREMENT USING DOWNWARD CONTINUATION PROCESS IN KALIMANTAN REGION
title_sort quality investigation of gravity data from airborne gravimetry measurement using downward continuation process in kalimantan region
url https://digilib.itb.ac.id/gdl/view/43960
_version_ 1821999026973704192