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Method for predicting the amount and composition of fluids produced by mineral reactions operating in a sedimentary basin

机译:预测在沉积盆地中进行的矿物反应产生的流体量和组成的方法

摘要

- A method for predicting the amount and composition of the fluids produced by inorganic reactions operating in a sedimentary basin, and trapped with the hydrocarbons in the reservoirs.; - acquisition of geological basin characteristics and constructing a representation of the basin by a mesh. Then, one calculates, for at least a set of cells of the mesh, and using a model basin and geological data, changing the following parameters: a drilling depth (z), a temperature (T) , pore pressure (P), volume (V) and a porosity (Φ) at successive ages (t i) representative of the geological history of the basin. Is determined in each cell of the set of cells, a mineralogical or chemical composition of rock from the geological basin. Finally, it determines the amount and the fluid composition of mineral origin within the set of cells, by means of a geochemical model and an equation of state, from said parameters, of said composition, and a thermodynamic database.
机译:-一种方法,用于预测在沉积盆地中发生的无机反应所产生的流体的数量和组成,这些流体被碳氢化合物捕获在储层中。 -获取地质盆地特征并通过网格构建盆地的表示。然后,至少要对一组网格单元进行计算,并使用模型盆地和地质数据,更改以下参数:钻孔深度(z),温度(T),孔隙压力(P),体积(V)和连续年龄(t i)的孔隙度(Φ)代表该盆地的地质历史。确定在一组单元的每个单元中,是地质盆地中岩石的矿物学或化学组成。最后,它通过所述成分的地球化学模型和状态方程,所述成分的参数和热力学数据库,确定一组单元中矿物来源的数量和流体成分。

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