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Design of Deep Foundations in Marine Gas Hydrate-Bearing Sediments

机译:船用天然气水合物沉积物深层基础设计

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Design of deep foundations within oceanic gas hydrate-bearingsediments (HBS) can be problematic and calls for special attention toincorporate the effect of gas hydrate melting. As naturally occurringgas hydrates in the seabed sediments begin dissociation process due totemperature or pressure changes, the pore pressure increases associatedwith volume expansion of the gas released during gas hydratedissociation will likely result in fractures filled with pressurized fluidproducts open accompanied by softening of soil in gas and waterintrusion zone together with seafloor and subsurface sediment motions.In this paper, a numerical approach is described to investigate theeffects of gas hydrate dissociation induced by constant heating from ahot wellbore on sediment engineering properties and the radial extent ofhydrate dissociation influence zone. The effects of the followingprocess during gas hydrate melting on soil parameters are discussed: (1)thermal stresses; (2) gas exsolution during heating; (3)seepage- induced swelling effects and (4) fracturing. Estimation ofhydrate dissociation influence zone employs numerical assessment offracture formation taking into account of pore seepage of fluid and gasfrom fractures, which is premised on either (1) development of apattern of laterally expanding horizontal fractures evenly spacedvertically throughout the hydrate-bearing zone and centered on thewellbore, or (2) development of vertical fractures which will intersectthe seafloor to allow released gasses to vent into water column. If thefractures form vertically from the origin of hydrate dissociation, theeffects of hydrate melting on sediment parameters for determining deepfoundation capacities will be essentially confined within thedissociation front; on the other hand, in the event of horizontal soilfracture formation, the radial extent of dissociation influence zone onsoil properties will extend beyond the dissociation front especially forrelatively high gas hydrate concentration.Discussion of deep foundation design (tension-leg platform (TLP)piles) in hydrate environment considering effects of hydratedissociation due to elevated temperature is also presented herein. Thepotential sediment strength loss and soil loads exerted on the pileresulting from sediment motions induced by fracture growth should beincorporated in the design process.
机译:海洋天然气水合物承载沉积物(HBS)中的深层基础设计可能会出现问题,需要引起特别注意,以纳入天然气水合物熔融作用。随着温度或压力变化,海底沉积物中天然存在的天然气水合物开始分解,随着水合物分解过程中释放出的气体的体积膨胀,孔隙压力增加,这可能导致裂缝充满高压流体产品,伴有土壤软化和水侵入。本文介绍了一种数值方法,研究热井筒不断加热引起的天然气水合物分解对沉积物工程性质和径向分解程度的影响。讨论了天然气水合物熔融过程中以下过程对土壤参数的影响:(1)热应力; (2)加热过程中的气体逸出; (3)由渗流引起的溶胀作用和(4)压裂。水合物离解影响区的估计是利用考虑到裂缝中的流体和气体的孔隙渗漏的裂缝形成的数值评估,其前提是(1)形成横向扩展水平裂缝的格局,该横向裂缝在整个水合物含油区中均匀地垂直分布,并以井眼为中心或(2)垂直裂缝的发展,该裂缝将与海底相交,使释放的气体排入水柱。如果裂缝是从水合物离解的起点垂直形成的,则水合物熔融对沉积参数的影响(用于确定深基能力)将基本上限制在离解前沿。另一方面,在水平土壤裂缝形成的情况下,解离影响区对土壤性质的径向范围将超出解离前沿,尤其是相对较高的天然气水合物浓度。深层基础设计(张力腿平台(TLP)桩)的讨论在水合物环境中,还考虑了由于高温引起的水合物离解的影响。在设计过程中应考虑到潜在的沉积物强度损失和由于裂缝生长引起的沉积物运动而施加到桩上的土壤负荷。

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