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Influence of the Hyperbaric Effect on Apparent Material Strength of Fully Saturated Porous Rock for Low Strain Rates

机译:低应变速率下高压作用对全饱和多孔岩表观材料强度的影响

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Excavation of rock materials such as Seafloor Massive Sulfide deposits at great depths is greatly influenced by ambient waterpressure, but little is known about the processes involved. Dry rock specimens are known to exhibit a large increase ofapparent material properties in high-pressure environments. However, in deep-sea mining processes rock material is fullysaturated and it is unknown how the hyperbaric effect changes apparent material strengths and involved physical processesunder these conditions.This paper discusses the influence of hyperbaric effect on fully saturated brittle rock specimens during deep-sea excavationusing a grab, and the resulting changes in apparent material properties. Computations are described which are used to predictthe outcome of this effect, and the validating experiments that were carried out.A new theorem is stated based on elastic deformation of the grain matrix, which causes a pressure difference in the matrixand reinforces the material. This is based on the low cutting speed of a grab, allowing the material to deform elastically andenabling water ingress into the deformed material, resulting in less cutting energy. Moreover the cutting mechanism of a grabhas a very low ratio of cutting energy over excavated rock volume. The theoretical model was developed in collaboration withDelft University of Technology and experiments were carried out with Seatools BV.Experiments were conducted to investigate the phenomenon and to validate the stated theorem for saturated rock material.An experimental setup was developed in collaboration with Seatools BV, to test rock material properties at differenthyperbaric conditions with a low rate of loading. The experiments were designed to carry out standard material tests of theAmerican Society for Testing and Materials to determine the compressive and tensile strength, by crushing the materialspecimens up to their breaking point in different hyperbaric conditions.The experiments were used to validate the theoretical computations that predicted differences in tensile strength betweensaturated and dried specimen, due to ingress of water during deformation causing not the full increase of the apparent materialstrength. The results were consistent and a correlation between the environment pressure and the added apparent materialstrength was found.
机译:诸如深海海底块状硫化物沉积物之类的岩石材料的开挖受环境水的影响很大 压力,但对所涉及的过程知之甚少。已知干岩石标本显示出很大的增加 在高压环境下具有明显的材料特性。但是,在深海采矿过程中,岩石材料是完全的 尚不清楚,高压作用如何改变表观材料强度和涉及的物理过程 在这些条件下。 本文讨论了高压作用对深海开挖过程中完全饱和的脆性岩石标本的影响 使用抓斗,从而导致表观材料特性发生变化。描述了用于预测的计算 效果的结果,以及进行的验证实验。 基于晶粒基体的弹性变形提出了一个新的定理,该定理导致基体中的压力差 并增强材料。这是基于抓斗的低切割速度,从而使材料发生弹性变形并 使水进入变形的材料,从而减少切割能量。而且抓斗的切割机理 相对于挖掘的岩石体积,其切割能量的比率非常低。理论模型是与 代尔夫特理工大学和实验是使用Seatools BV进行的。 进行实验以研究该现象并验证饱和岩石材料的所述定理。 与Seatools BV合作开发了一个实验装置,以测试不同岩石材料的性能 低负荷条件下的高压条件。设计这些实验是为了进行标准的材料测试。 美国材料试验学会通过压碎材料来确定抗压强度和抗拉强度 样品在不同的高压条件下达到其断裂点。 实验被用来验证理论计算,该理论计算预测了抗拉强度之间的差异。 饱和和干燥的样品,由于变形过程中的水分进入而导致表观材料未完全增加 力量。结果是一致的,并且环境压力与添加的表观材料之间具有相关性 发现力量。

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