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首页> 外文期刊>Canadian journal of earth sciences >Modelisation d'un systeme karstique complexe (bassin de S~t-Chaptes, Gard, France): un outil de synthese des donnees geologiques et hydrogeologiques
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Modelisation d'un systeme karstique complexe (bassin de S~t-Chaptes, Gard, France): un outil de synthese des donnees geologiques et hydrogeologiques

机译:复杂的岩溶系统建模(S〜t-Chaptes盆地,法国加尔德):合成地质和水文地质数据的工具

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Numerous software packages allow the efficient modeling of the hydrodynamic behaviour of aquifers in continuous media. To study pressure transfer in discontinuous media like karsts, the black-box models are restrictive and the models that consider discrete conduit networks are unsuitable for reservoir scale. We show that the utilization of a continuous media model can lead to useful results, even in the case of complex systems, but needs to be adapted to karst specificity. The problem is approached by studying a hydrogeological system located in the Mediterranean Languedoc region: the S~t-Chaptes basin. This system consists of three superposed aquifers included in four different stratigraphic series. The main aquifer is a karst formation in contact with two other karst formations that belong to different hydrogeologic systems. Considering geological data in addition to hydrological data and with the hypothesis of a relative homogenization of the karst's hydraulic behaviour on a large spatial scale for daily to monthly increments, the model that takes into account the relations with the other aquifers allows (i) a preliminary identification of the main heterogeneities inside the reservoir; (ii) the location of barriers and low-permeability zones that isolate some parts of the aquifer; (iii) the observation of a curious behaviour of the piezometric levels in the confined zones of the aquifer; and (iv) the characterization of the exchanges with the other low-volume but existing aquifers.
机译:大量软件包可对连续介质中含水层的水动力行为进行有效建模。为了研究岩溶等非连续介质中的压力传递,黑盒模型是限制性的,考虑离散导管网络的模型不适用于储层规模。我们表明,即使在复杂的系统中,使用连续介质模型也可以产生有用的结果,但是需要适应岩溶的特异性。通过研究位于地中海朗格多克地区(S〜t-Chaptes盆地)的水文地质系统来解决该问题。该系统由四个不同的地层系列中包括的三个叠加的含水层组成。主要含水层是与属于不同水文地质系统的另外两个岩溶层接触的岩溶层。考虑到除了水文数据之外的地质数据,并假设岩溶水力行为在较大的空间尺度上相对均质,每天至每月递增,考虑到与其他含水层的关系的模型允许(i)初步识别储层内部的主要非均质性; (ii)隔离含水层某些部分的屏障和低渗透区的位置; (iii)观察含水层密闭区中测压水位的奇怪行为; (iv)与其他少量但现有的含水层进行交换的特征。

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