Lithological displacement of an evaporite mineral stratum
    1.
    发明申请
    Lithological displacement of an evaporite mineral stratum 审中-公开
    蒸发岩矿物层的岩性位移

    公开(公告)号:US20160356140A1

    公开(公告)日:2016-12-08

    申请号:US14062878

    申请日:2013-10-24

    Applicant: SOLVAY SA

    CPC classification number: E21B43/28 C01D3/06 C01D5/14 C01D7/10 C01D7/12 C01D7/14

    Abstract: A lithological displacement of an underground evaporite mineral stratum from an underlying non-evaporite stratum comprising the application of a lifting hydraulic pressure of a fluid at a weak interface between the strata, resulting in lifting the overburden above the interface, separating the evaporite stratum from the underlying non-evaporite stratum and thus forming a mineral free-surface. The lifting hydraulic pressure is greater than the overburden pressure. The formed mineral free-surface is accessible for dissolution by a solvent. The fluid used for lifting may comprise a solvent suitable to dissolve the mineral. The evaporite mineral stratum preferably comprises trona, nahcolite, wegscheiderite, or combinations thereof.

    Abstract translation: 地下蒸发岩矿物地层与下层非蒸发岩层的岩性位移,包括在地层之间的弱界面施加液体的提升液压,导致提升界面上方的覆盖层,将蒸发岩层与 潜在的非蒸发层,从而形成矿物自由表面。 提升液压压力大于上覆压力。 形成的矿物自由表面可通过溶剂溶解。 用于提升的流体可以包括适于溶解矿物的溶剂。 蒸发岩矿物层优选地包括天然碱,蓝宝石,wegscheiderite或其组合。

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