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A Novel Mining Approach for Seafloor Massive Sulfide Deposits

机译:一种用于海底硫化物沉积物的新型采矿方法

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Sulfidic polymetallic ore deposits, known as seafloor massive sulfides (SMS) occur on the seabed as precipitation products from hot hydrothermal solutions as a result of mixing with cold seawater and are usually found at depths between 1,500 and 4,100 m. These deposits are formed basically in tectonically active spreading zones of oceans (mid-ocean ridges and back-arc spreading systems) and are the result of the global heat transfer from the mantle above the oceanic crust into the water column. In these SMS deposits, metals such as copper (Cu), zinc (Zn) and lead (Pb) as well as trace elements of silver (Ag), gold (Au) and rare antimony (Sb), cadmium (Cd), gallium (Ga), germanium (Ge), and indium (In) are present. This paper describes a novel technology for mining SMS deposits based on the vertical cutting approach developed by a joint research between BAUER Maschinen GmbH and Technip. A hyperbaric mathematical cutting model has been used to calculate the forces needed to excavate SMS deposits in water depth up to 2,000m. The model shows that in hyperbaric conditions, what influences the cutting energy is the water column rather than the geomechanical properties of the rock. Based on the mathematical model a preliminary cutting tool design is shown.
机译:由于与冷海水混合,硫胺多金属矿床沉积物,被称为海底硫化物(SMS),作为热水热水溶液的沉淀产品,通常在1,500至4,100米的深度处发现。这些沉积物基本上形成在海洋(中海脊和后弧扩展系统)的根部主动扩散区域,并且是从海底地壳上方到水柱上方的地幔的全球热传递的结果。在这些SMS沉积物中,如铜(Cu),锌(Zn)和铅(Pb)以及银(Ag),金(Au)和稀有锑(Sb),镉(Cd),镓的痕量元素(GA),锗(GE)和铟(IN)存在。本文介绍了一种基于由Bauer Maschinen GmbH和Technip之间的联合研究开发的垂直切割方法进行挖掘SMS沉积的新技术。已经使用高压数学切割模型来计算挖掘水深度高达2,000米的SMS沉积所需的力。该模型表明,在高压条件下,影响切削能量是水柱而不是岩石的地质力学特性。基于数学模型,示出了初步切削刀具设计。

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