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Constructing Regional Groundwater Models from Geophysical Data of Varying Type, Age, and Quality

机译:从不同类型,年龄和质量的地球物理数据构建区域地下水模型

摘要

Regional hydrological models are important tools in water resources management, but prediction uncertainties are often high due to non-uniqueness of the hydrostratigraphical model. This model is often based on borehole lithology only. However, a much better resolution can be obtained from large geophysical datasets covering the entire domain. Using boreholes to link between hydrostratigraphical classes and resistivity is efficient and emphasizes the need for an all-inclusive data interpretation procedure that can be integrated in groundwater model calibration.We present an automatic method for parameterization of a 3D model of the subsurface, integrating lithological information from boreholes with resistivity models. The objective is to create a direct input to regional groundwater models for sedimentary areas, where the sand/clay distribution governs the groundwater flow. The resistivity input is all-inclusive in the sense that we include data from a variety of instruments (DC and EM, ground-based and airborne), with a varying spatial density and varying ages and quality. The coupling between hydrological and geophysical parameters is managed using a translator function with spatially variable parameters, which is calibrated against observed lithological data. In other words, the translator function interprets the geophysical resistivities into a 3D clay fraction model and the 3D clay fraction model is then turned into a zonation for the hydrological model by a K-means clustering.We present the methodology by show-casing a study from Denmark were a regional groundwater model is constructed by including lithological information from 3100 boreholes over an 710 sqkm area. The geophysical models spans more than 30 years of data collection and includes approx. 225,000 DC models, and 35,000 EM models, airborne as well as groundbased. The final model was calibrated giving parameters that were comparable with existing models based on thorough and time-consuming manual model construction.
机译:区域水文模型是水资源管理中的重要工具,但由于水文地层模型的不唯一性,预测不确定性通常很高。该模型通常仅基于钻孔岩性。但是,可以从覆盖整个域的大型地球物理数据集获得更好的分辨率。利用井眼将水文地层类别与电阻率联系起来是有效的,并强调了对可整合到地下水模型校准中的全包数据解释程序的需求。我们提出了一种自动方法,用于对地下3D模型进行参数化,整合岩性信息使用电阻率模型从钻孔中提取。目的是为沉积区域的区域地下水模型创建直接输入,在该模型中,沙子/粘土的分布决定了地下水的流量。电阻率输入是包罗万象的,因为我们包括来自各种仪器(DC和EM,地面和机载)的数据,这些数据具有不同的空间密度以及不同的年龄和质量。水文参数与地球物理参数之间的耦合是使用具有空间可变参数的转换函数来管理的,该函数可根据观测到的岩性数据进行校准。换句话说,翻译器功能将地球物理电阻率解释为3D粘土组分模型,然后通过K-均值聚类将3D粘土组分模型转换为水文模型的分区。来自丹麦的一个区域地下水模型是通过包含710平方公里区域中3100个钻孔的岩性信息而构建的。地球物理模型跨越了30多年的数据收集,并包括大约30年。机载和陆载225,000 DC模型和35,000 EM模型。基于彻底且耗时的手动模型构建,对最终模型进行校准,以提供与现有模型相当的参数。

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