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Synergy through CO_2 Storage by Mineral Trapping in Combination with Geothermal Heat Production

机译:矿物捕集与地热供热相结合,通过CO_2封存产生协同作用

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Storage of carbon dioxide (CO_2) by precipitation of carbon-bearing minerals in geological formations is, on the long run, more stable and therefore much safer than direct storage or solution trapping. Furthermore, options for CO_2 sequestration which offer additional economic benefits besides the positive effect for the atmosphere are attractive. Both arguments motivate us to study the novel approach of storing dissolved CO_2 as calcite in geothermally used aquifers. Geothermal energy in Germany is mainly provided from deep sandstone aquifers by a so called "doublet" installation consisting of one well for hot water production and one well for cooled water re-injection. After re-injection of CO_2 enriched, cold brine into the reservoir, anhydrite abundant as matrix mineral dissolves. As a consequence, the water becomes enriched in calcium ions. Numerical simulations demonstrate that alkaline buffering capacity provided by plagioclase in the reservoir rock or through surface water treatment with fly ashes subsequently result in the reaction of dissolved Ca and CO_2 to form and precipitate calcium carbonate. We show that anhydrite dissolution with concurrent pore space increase is important to balance pore space reduction by precipitation of calcite and secondary silicates. Laboratory experiments prove the feasibility of literally transforming anhydrite into calcite and provide necessary kinetic input data for the modelling. Suitable geothermal reservoirs exist with anhydrite as matrix mineral and plagioclase supplying alkalinity. Their CO_2 storage capacities depend on their volume and porosity as well as on the chemical and mineralogical composition of the formation brine and reservoir rock, respectively. Mass balance calculations yield that the storage capacity can be estimated from the abundance of anhydrite in the reservoir. Based on an operation time of 30 years this theoretical, quite significant storage capacity amounts to 0.5 million tons to 25 million tons of CO_2 around geothermal heating plants.
机译:从长远来看,通过含碳矿物在地质构造中的沉淀来存储二氧化碳(CO_2)更稳定,因此比直接存储或溶液捕集更安全。此外,除了对大气层具有积极作用外,CO 2固存的选择还具有其他经济利益,这是有吸引力的。两种论点都促使我们研究将溶解的CO_2作为方解石储存在地热含水层中的新方法。德国的地热能主要由深层砂岩含水层通过所谓的“双重”装置提供,该装置包括一口用于生产热水的井和一口用于再注入冷却水的井。将富集CO_2的冷盐水重新注入储层后,由于基质矿物溶解而形成的硬石膏丰富。结果,水变得富含钙离子。数值模拟表明,斜长石在储层岩石中或通过用飞灰进行地表水处理提供的碱性缓冲能力随后导致溶解的Ca和CO_2反应形成并沉淀出碳酸钙。我们表明,硬石膏的溶解与同时孔隙空间的增加对于平衡方解石和次要硅酸盐的沉淀所减少的孔隙空间很重要。实验室实验证明了将硬石膏转化为方解石的可行性,并为建模提供了必要的动力学输入数据。合适的地热储层以硬石膏为基质矿物,斜长石可提供碱性。它们的CO_2储存能力分别取决于其体积和孔隙率,以及地层盐水和储层岩石的化学和矿物组成。通过质量平衡计算得出,可以根据储层中大量的硬石膏来估算存储容量。基于30年的理论运行时间,在地热供热厂周围相当大的存储容量为50万吨至2500万吨CO_2。

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