Mapping seabed sediments for Sharm Obhur using multibeam echosounder backscatter data

Mohammed El-Diasty

نتاج البحث: المساهمة في مجلةمقالمراجعة النظراء

2 اقتباسات (Scopus)


The observed hydrographic surveying data from multibeam echosounder system (MBES) contains sounding and backscatter intensity data that can be utilized in many coastal and marine applications such as marine geological and environmental investigations. In this paper, the seabed sediments mapping for Sharm Obhur (Obhur Creek) was derived using backscatter intensity data. The backscatter data were radiometrically and geometrically corrected to produce a seabed backscatter mosaic for Sharm Obhur study area. Then, the angular response analysis was implemented to derive the seabed sediment’s grain size, classification (gravel, sand and mud) and associated confidence level values that identify the quality of the classification method implemented in this paper. It was shown that the mouth in the south of the Sharm Obhur mainly contains sand sediments, however, the north side of the Sharm Obhur contains mud sediments and gravel sediments can be seen in very small areas. Moreover, it was found that the successful rate of classification is 90% based on the estimated confidence values. To validate the derived seabed sedimentation map, a comparison was made between the grab sampling results reported in the literature and the seabed sediments types derived in this paper. The comparison showed that the derived seabed sediments results using angular response model agree with the grab sampling results. The advantage of mapping the seabed sedimentation using multibeam backscatter data over the grab sampling method is that it can provide the seabed sediment mapping for the entire area using the MBES due to its 100% coverage of the seabed.
اللغة الأصليةEnglish
الصفحات (من إلى)163-171
عدد الصفحات9
دوريةModeling Earth Systems and Environment
مستوى الصوت6
رقم الإصدار1
المعرِّفات الرقمية للأشياء
حالة النشرPublished - 2020

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