دانلود رایگان مقاله انگلیسی مشخصات مورفولوژی هیدرات گاز از داده های لرزه ای در دریای شمال چین - الزویر 2018

عنوان فارسی
مشخصات مورفولوژی هیدرات گاز از داده های لرزه ای در دریای شمال چین
عنوان انگلیسی
Characterization of gas hydrate morphology from seismic data in the northern South China Sea
صفحات مقاله فارسی
0
صفحات مقاله انگلیسی
10
سال انتشار
2018
نشریه
الزویر - Elsevier
فرمت مقاله انگلیسی
PDF
کد محصول
E8149
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ژئوفیزیک
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لرزه نگاری
مجله
مرزهای علوم زمین - Geoscience Frontiers
دانشگاه
School of Geophysics and Information Technology - China University of Geosciences (Beijing) - China
کلمات کلیدی
مورفولوژی هیدرات گاز، دریای شمال چین، مکانیزم از دست دادن Mesoscopic، ضریب بازتاب در مقایسه با فرکانس
۰.۰ (بدون امتیاز)
امتیاز دهید
چکیده

abstract


The second gas hydrate expedition drilled 13 sites in northern South China Sea and recovered a large amount of gas hydrate. The logging data and core analysis indicate that the gas hydrate occurs as solid nodules, disseminated within pore spaces of sediments and fracture fillings in veins. In this study, we examine two sites (sites 08 and 16), where gas hydrates occur both near the BSR and near the surface. We use the mesoscopic-loss mechanism to study the reflection coefficient versus frequency at BSR in seismic frequency band. When the seismic wave passes through the pore-filling gas hydrate sediments, the high frequency energy is much reduced and the low frequency energy of reflected waves at BSR is strong. When the seismic wave passes through the fracture-filling gas hydrate sediments, the high frequency wave is easily propagated and its reflected energy at BSR is strong. This difference of these at BSR between two types of gas hydrate contained sediments can be utilized to distinguish the gas hydrate morphology. The seismic data in northern South China Sea is analyzed and the results correspond well with the forward modeling approach.

نتیجه گیری

7. Conclusion


Gas hydrate-bearing sediments include two main morphologies. They are pore-filling gas hydrates and fracture-filling gas hydrates. We use the mesoscopic-loss mechanism to do the forward modeling to study the reflection coefficient versus frequency at BSR of the gas hydrate layer. When gas exists beneath the fracturefilling gas hydrate sediment, the energy of the low frequency reflected wave is strong and the energy of the high frequency reflected wave is weak at BSR. As for the fracture-filling gas hydrate, the energy of high frequency reflected wave is stronger at BSR. This difference can be used to identify the gas hydrate morphology. We use this method to predict the gas hydrate types in northern South China Sea and get the same results with the site drilling.


بدون دیدگاه